Scattering of Polarized Radiation by Atoms in Magnetic and Electric Fields
电磁场微波词汇汉英对照表
电磁场微波词汇汉英对照表二画二端口网络two port network二重傅立叶级数double Fourier series入射场incident field入射波incident wave三画小波wavelet四画无功功率reactive power无限(界)区域unbound region无源网络passive network互易性reciprocity互阻抗mutual impedance互耦合mutual coupling互连interconnect天线antennas天线方向性图pattern of antenna匹配负载matched load孔aperture孔(缝)隙天线aperture antennas内阻抗internal impedance介电常数permittivity介质dielectric介质波导dielectric guide介质损耗dielectric loss介质损耗角dielectric loss angle介电常数dielectric constant反射reflection反射系数reflection coefficient分离变量法separation of variables五画主模dominant mode正交性orthogonality正弦的sinusoidal右手定则right hand rule平行板波导parallel plate waveguide平面波plane wave功率密度density of power功率流(通量)密度density of power flux 布魯斯特角Brewster angle本征值eigen value本征函数eigen function边值问题boundary value problem四端口网络four terminal network矢量位vector potential电压voltage电压源voltage source电导率conductivity电流元current element电流密度electric current density电荷守恒定律law of conservation of charge 电荷密度electric charge density电容器capacitor电路尺寸circuit dimension电路元件circuit element电场强度electric field intensity电偶极子electric dipole电磁兼容electromagnetic compatibility矢量vector矢径radius vector失真distortions平移translation击穿功率breakdown power节点node六画安培电流定律Ampere’s circuital law传播常数propagation constant亥姆霍兹方程Helmholtz equation动态场dynamic field共轭问题conjugate problem共面波导coplanar waveguide (CPW)有限区域finite region有源网络active network有耗介质lossy dielectric导纳率admittivity同轴线coaxial line全反射total reflection全透射total transmission各向同性物质isotropic matter各向异性nonisotropy行波traveling wave光纤optic fiber色散dispersion网格mesh全向天线omnidirectional antennas阵列arrays七画串扰cross-talk回波echo良导体good conductor均匀平面波uniform plane wave均匀传输线uniform transmission line近场near-field麦克斯韦方程Maxwell equation克希荷夫电流定律Kirchhoff’s current law 环行器circulator贝塞尔函数Bessel function时谐time harmonic时延time delay位移电流electric displacement current芯片chip芯片组chipset远场far-field八画变分法variational method定向耦合器directional coupler取向orientation法拉第感应定律Faraday’s law of induction 实部real part空间分量spatial components波导waveguide波导波长guide wave length波导相速度guide phase velocity波阻抗wave impedance波函数wave function波数wave number泊松方程Poisson’s equation拉普拉斯方程Laplace’s equation坡印亭矢量Poynting vector奇异性singularity 阻抗矩阵impedance matrix表面电阻surface resistance表面阻抗surface impedance表面波surface wave直角坐标rectangular coordinate极化电流polarization current极点pole非均匀媒质inhomogeneous media非可逆器件nonreciprocal devices固有(本征)阻抗intrinsic impedance单位矢量unit vector单位法线unit normal单位切线unit tangent单极天线monopole antenna单模single mode环行器circulator驻波standing wave驻波比standing wave ratio直流偏置DC bias九画标量位scalar potential品质因子quality factor差分法difference method矩量法method of moment洛伦兹互易定理Lorentz reciprocity theorem 屏蔽shield带状线stripline标量格林定理scalar Green’s theorem面积分surface integral相对磁导率relative permeability相位常数phase constant相移器phase shifter相速度phase velocity红外频谱infra-red frequency spectrum矩形波导rectangular waveguide柱面坐标cylindrical coordinates脉冲函数impulse function复介电常数complex permittivity复功率密度complex power density复磁导率complex permeability复矢量波动方程complex vector wave equation贴片patch信号完整性signal integrity信道channel寄生效应parasite effect指向天线directional antennas喇叭天线horn antennas十画准静态quasi-static旁路电流shunt current高阶模high order mode高斯定律Gauss law格林函数Green’s function连续性方程equation of continuity耗散电流dissipative current耗散功率dissipative power偶极子dipole脊形波导ridge waveguide径向波导radial waveguide径向波radial wave径向模radial mode能量守恒conservation of energy能量储存energy storage能量密度power density衰减常数attenuation constant特性阻抗characteristic impedance特征值characteristic value特解particular solution勒让德多项式Legendre polynomial积分方程integral equation涂层coating谐振resonance谐振长度resonance length十一画混合模hybrid mode部分填充波导partially filled waveguide 递推公式recurrence formula探针馈电probe feed接头junction基本单位fundamental unit理想介质perfect dielectric理想导体perfect conductor唯一性uniqueness虚部imaginary part透射波transmission wave透射系数transmission coefficient 球形腔spherical cavity球面波spherical wave球面坐标spherical coordinate终端termination终端电压terminal voltage射频radio frequency探针probe十二画涡旋vortices散度方程divergence equation散射scattering散杂电容stray capacitance散射矩阵scattering matrix斯托克斯定理Stoke’s theorem斯涅尔折射定律Snell’s law of refraction阴影区shadow region超越方程transcendental equation超增益天线supergain antenna喇叭horn幅角argument最速下降法method of steepest descent趋肤效应skin effect趋肤深度skin depth微扰法perturbational method等相面equi-phase surface等幅面equi-amplitude surface等效原理equivalence principle短路板shorting plate短截线stub傅立叶级数Fourier series傅立叶变换Fourier transformation第一类贝塞耳函数Bessel function of the first kind第二类汉克尔函数Hankel function of the second kind解析函数analytic function激励excitation集中参数元件lumped-element场方程field equation场源field source场量field quantity遥感remote sensing振荡器oscillators滤波器filter十三画隔离器isolator雷达反射截面radar cross section (RCS)损耗角loss angle感应电流induced current感应场induction field圆波导circular waveguide圆极化circularly polarized圆柱腔circular cavity铁磁性ferromagnetic铁氧体陶瓷ferrite ceramics传导电流conducting current传导损耗conduction loss传播常数propagation constant传播模式propagation mode传输线模式transmission line mode传输矩阵transmission matrix零点Zero静态场static field算子operator输入阻抗input impedance椭圆极化elliptically polarized微带microstrip微波microwave微波单片集成电路microwave monolithic integrated circuit MMIC毫米波单片集成电路millimeter wave monolithic integrated circuit M3IC十四画漏电电流leakage current渐进表示式asymptotic expression模式mode模式展开mode expansion模式函数mode模式图mode pattern截止波长cut off wavelength截止频率cut off frequency鞍点saddle频谱spectrum线性极化linearly polarized线积分line integral磁矢量位magnetic vector potential磁通magnetic flux 磁场强度magnetic intensity磁矩magnetic moment磁损耗角magnetic loss angle磁滞损耗magnetic hysteresis磁导率permeability十五画辐射radiate增益gain横电场transverse electric field横电磁波transverse electromagnetic wave 劈wedge十六画雕落场evanescent field雕落模式evanescent mode霍尔效应Hall effect辐射电阻radiation resistance辐射电导radiation conductance辐射功率radiation power辐射方向性图radiation pattern谱域方法spectral method十七画以上瞬时量insaneous quantity镜像image峰值peak value函数delta function注:本词汇表参考了《正弦电磁场》(哈林顿著孟侃译)。
放射性同位素伽玛源准直照射辐射场模拟研究
·核科学与工程·放射性同位素伽玛源准直照射辐射场模拟研究*黄宇晨1,2, 钱易坤1,2, 冯 鹏2, 刘易鑫1, 张 颂1,2,何 鹏2, 魏 彪2, 毛本将1, 朱亚地1(1. 中国工程物理研究院 核物理与化学研究所,四川 绵阳 621900; 2. 重庆大学 光电技术及系统教育部重点实验室,重庆 400044)摘 要: 针对各向同性伽玛源参考辐射场尺寸关键技术问题,GB/T 12162系列标准虽然进行了相关规定,但是该规定并未对准直照射状态下照射室尺寸提出具体要求。
为减小用于辐射检测或监测类仪器仪表检定与量值校准时伽玛参考辐射场内散射影响,本文采用蒙特卡罗方法,研究了同位素放射源准直照射时,照射室尺寸变化对检验点处的剂量率值与能量分布的影响情况,获得了准直照射时伽玛辐射场照射室尺寸的边界条件,建立并完善了伽玛参考辐射场边界研究方法及相关标准细节,为准直照射状态下照射室尺寸设计提供了一种新方法或途径。
关键词: 核仪器仪表校准; 参考辐射; 准直照射; 蒙特卡罗; 边界条件 中图分类号: TL72 文献标志码: A doi : 10.11884/HPLPB202133.200294Simulation of radiation field from isotopic gamma source collimationHuang Yuchen 1,2, Qian Yikun 1,2, Feng Peng 2, Liu Yixin 1, Zhang Song 1,2,He Peng 2, Wei Biao 2, Mao Benjiang 1, Zhu Yadi 1(1. Institute of Nuclear Physics and Chemistry , CAEP , Mianyang 621900, China ;2. Key Laboratory of Optoelectronic Technology & Systems , Ministry of Education , Chongqing University , Chongqing 400044, China )Abstract : Aiming at the key technical issues of the reference radiation field size of isotropic sources, GB/T 12162 series of GB standards stipulates the size of the reference radiation field when using an isotropic source.However, there is no specific regulation for the size of the irradiation under collimation. To reduce the influence of scattering in the gamma reference radiation field when used for radiation detection or monitoring instrument verification and value calibration, Monte Carlo simulation was carried out to explore the effect of the size change of the irradiation chamber on the energy distribution and dose rate value during the radiation source collimation. The boundary conditions of the collimated gamma radiation irradiation chamber were obtained, and the details of the gamma reference radiation field boundary research method and related standards are established and improved. The study provides a new method or approach for the size design of the irradiation chamber under the collimated irradiation state.Key words : nuclear instrument calibration ; reference radiation ; collimated irradiation ; Monte Carlo ;boundary conditions众所周知,核电站与核设施场所中,伽玛射线辐射剂量(率)仪表不仅是辐射防护工作必需的重要工具,更是监测和保障核应用场所与射线应用装置安全的必要条件。
大气和环境对遥感的影响
2. 米氏散射:当微粒的直径与辐射波长差不多 时的大气散射。
➢ 云、雾的粒子大小与红外线的波长接近, 所以云雾对对红外线的米氏散射不可忽视。
3. 无选择性散射:当微粒的直径比辐射波长大 得多时所发生的散射。符合无选择性散射条 件的波段中,任何波段的散射强度相同。
➢ 水滴、雾、尘埃、烟等气溶胶常常产生非 选择性散射。
Non-Selective scatter of EM radiation by a cloud
三种散射作用
1. 瑞利散射:当微粒的直径比辐射波长小得多时, 此时的散射称为瑞利散射。
➢ 散射率与波长的四次方成反比,因此,瑞利散 射的强度随着波长变短而迅速增大。紫外线是 红光散射的30倍,0.4微米的蓝光是4微米红外 线散射的1万倍。
四、大气窗口
1、大气窗口:通过大气而较少被反射、吸收或 散射的投射率较高的电磁辐射波段。
• 大气窗口是选择遥感工作波段的重要依据。 • 常见的大气窗口:
Atmospheric Windows
▪ Some sensors, especially those on meteorological satellites, seek to directly measure absorption phenomena such as those associated with CO2 and other gaseous molecules.
▪ Note that the atmosphere is nearly opaque to EM radiation in the mid and far IR
▪ In the microwave region, by contrast, most of the EM radiation moves through unimpeded - so that radar at commonly used wavelengths will nearly all reach the Earth surface unimpeded - although specific wavelengths are scattered by raindrops.
Flourence polarization(荧光偏振)
Polarization
Light is a harmonic electromagnetic wave. When considering its interaction with matter we can in most cases neglect the magnetic part. The plain in which the electric vector E oscillates defines the polarization of light.
Polarization in a fluorescence experiment
Z
excitation
X
I
I detection Y
The polarization state of fluorescence is described by: Polarization
Ill I P Ill I Ill I Ill I r IT Ill 2I
B
B
E
n E c
I E2
Natural light contains randomly all possible orientations of electric vector
Unpolarized (random) light
Polarizer
an optical component that selects from passing light only the component polarized in a given direction
hnexc hnexc
hnem
hnem > hnexc
The kinematic Sunyaev Zeldovich effect and transverse cluster velocities
Printed 1 February 2008
A (MN L TEX style file v1.4)
The kinematic Sunyaev Zeldovich effect and transverse cluster veloc812310v1 16 Dec 1998
Accepted 199- Received 199- in original form 199-
ABSTRACT
The polarization of the CMBR scattered by galaxy clusters in the kinematic Sunyaev Zeldovich effect depends on the transverse velocity of the cluster. This polarizing effect is proportional to the transverse velocity squared, and so weaker that the change in intensity due to the radial motion in the kinematic effect. The value given by Sunyaev and Zeldovich, and which is frequently cited, underestimates the polarizing effect by a factor of ten. We show furthermore that the polarization has a strong frequency dependence. This means that the polarization should be detectable with the new generation of CMBR probes, at least for some clusters. Thus this effect offers, almost uniquely, a method of obtaining the vectorial velocity of clusters. Key words: Cosmology: theory – cosmic microwave – polarization
晶体光学_英文参考教材
http://www.brocku.ca/earthsciences/people/gfinn/optical/CH. 1 Properties of Light∙Introduction∙Electromagnetic Radiation∙Wave Front, Wave Normal∙Phase and Interference∙Reflection and Refraction∙Polarization of LightCh. 2 Refractometry∙Relief∙Becke Lineo Definedo Lens Effecto Internal Reflectiono Becke Line MovementCh. 3 Isotropic Materials∙Optics∙Indicatrix∙Isotropic vs. AnisotropicCh. 4 Anisotropic Minerals∙Introduction∙Packing∙Interference Phenomenao Retardationo Interference at the Upper Polaro Monochromatic Lighto Polychromatic LightCh. 5 Optical Properties∙Extinction∙Accessory Plates∙Vibration Directions in Minerals∙Sign of Elongation∙Relief and PleochroismCh. 6 Uniaxial Minerals∙Uniaxial Optics∙Uniaxial Optic Sign∙Paths Followed by Light∙Uniaxial Indicatrix∙Birefringence and Interference Colours∙Extinction in Uniaxial Minerals∙Pleochroism in Uniaxial Minerals∙Interference figureso How to obtain an Interference Figureo Optic Axis Figure▪Interference Figure▪Formation of the Isochromes▪Formation of the Isogyres▪Optic Sign Determinationo Off-Centred Optic Axis Figureo Uniaxial Flash Figure∙Summary of Uniaxial Interference FiguresCh. 7 Biaxial Minerals∙Biaxial Optics∙Biaxial Indicatrix∙Optic Sign∙Crystallographic Orientation and the Indicatrix∙Biaxial Inteference Figureso Acute Bisectrix Figure (Bxa)▪Formation of the Isochromes▪Vibration Directions and Formation of the Isogyres▪Rotation of the Isogyreo Centred Optic Axis Figureo Obtuse Bisectrix Figure (Bxo)o Optic Normal or Biaxial Flash Figureo Off Centred Figures∙Optic sign determinationo Acute Bisectrix Figureo Obtuse Bisectrix Figureo Optic Axis Figureo Optic Normal∙Identifying Grains Which Will Produce Usable Interference Figures ∙Other Properties of Biaxial MineralsCh. 8 Other MineralsKnown Minerals - How to Describe Them?<<Optical Mineralogy>>Properties of Light1. INTRODUCTIONLight- a form of energy, detectable with the eye, which can be transmitted from one place to another at finite velocity.Visible light is a small portion of a continuous spectrum of radiation ranging from cosmic rays to radio waves.Fig. Light spectrumWhite or visible light, that which the eye detects, is only a fraction of the complete spectrum - produced by shining white light through a glass prism.Two complimentary theories have been proposed to explain how light behaves and the form by which it travels.1.Particle theory - release of a small amount of energy as a photon when an atom is excited.2.Wave theory - radiant energy travels as a wave from one point to another.Waves have electrical and magnetic properties => electromagnetic variations.Wave theory effectively describes the phenomena of polarization, reflection, refraction and interference, which form the basis for optical mineralogy.Fig. Components of a light ray2. ELECTROMAGNETIC RADIATIONThe electromagnetic radiation theory of light implies that light consists of electric and magnetic components which vibrate at right angles to the direction of propagation.In optical mineralogy only the electric component, referred to as the electric vector, is considered and is referred to as the vibration direction of the light ray.The vibration direction of the electric vector is perpendicular to the direction in which the light is propagating.The behaviour of light within minerals results from the interaction of the electric vector of the light ray with the electric character of the mineral, which is a reflection of the atoms and the chemical bonds within that minerals.Light waves are described in terms of velocity, frequency and wavelength.The velocity (V) and the wavelength are related in the following equation,where:F = Frequency or number of wave crests per second which pass a reference points =>cycles/second of Hertz (Hz).For the purposes of optical mineralogy, F = constant, regardless of the material through which the light travels. If velocity changes, then the wavelength must change to maintain constant F.Light does not consist of a single wave => infinite number of waves which travel together.3. WAVE FRONT, WAVE NORMALWith an infinite number of waves travelling together from a light source, we now define:1.Wave front - parallel surface connecting similaror equivalent points on adjacent waves.2.Wave Normal - a line perpendicular to the wavefront, representing the direction the waveis moving.3.Light Ray is the direction of propagation of the light energy.Minerals can be subdivided, based on the interaction of the light ray travelling through the mineral and the nature of the chemical bonds holding the mineral together, into two classes:a)Isotropic MineralsIsotropic materials show the same velocity of light in all directions because the chemical bonds holding the minerals together are the same in all directions, so light travels at the same velocity in all directions.Examples of isotropic material are volcanic glass and isometric minerals (cubic) Fluorite, Garnet, HaliteIn isotropic materials the Wave Normal and Light Ray are parallel.b)Anisotropic MineralsAnisotropic minerals have a different velocity for light, depending on the direction the light is travelling through the mineral. The chemical bonds holding the mineral together will differ depending on the direction the light ray travels through the mineral.a)Anisotropic minerals belong to tetragonal, hexagonal, orthorhombic, monoclinicand triclinic systems.In anisotropic minerals the Wave Normal and Light Ray are not parallel.Light waves travelling along the same path in the same plane will interfere with each other.4. PHASE AND INTERFERENCEBefore going on to examine how light inteacts with minerals we must define one term:RETARDATION - (delta) represents the distance that one ray lags behind another. Retardation is measured in nanometres, 1nm = 10-7cm, or the number of wavelengths by which a wave lags behind another light wave.The relationship between rays travelling along the same path and the interference between the rays is illustrated in the following three figures.1.If retardation is a whole number (i.e., 0, 1, 2, 3, etc.) of wavelengths.The two waves, A and B, are IN PHASE, and they constructively interfere with each other. The resultant wave (R) is the sum of wave A and B.2.When retardation is = ½, 1½, 2½ . . . wavelengths.The two waves are OUT OF PHASE they destructively interfere, cancelling each other out, producing the resultant wave (R), which has no amplitude or wavelength.3.If the retardation is an intermediate value, the the two waves will:1.be partially in phase, with the interference being partially constructive2.be partially out of phase, partially destructive.In a vacuum light travels at 3x1010 cm/sec (3x1017 nm/sec).When light travels through any other medium it is slowed down, to maintain constant frequency the wavelength of light in the new medium must also changed.5. REFLECTION AND REFRACTIONAt the interface between the two materials, e.g. air and water, light may be reflected at the interface or refracted (bent) into the new medium.For Reflection the angle of incidence = angle of reflection.For Refraction the light is bent when passing from one material to another, at an angle other than perpendicular.A measure of how effective a material is in bending light is called the Index of Refraction (n), where:Index of Refraction in Vacuum = 1 and for all other materials n > 1.0.Most minerals have n values in the range 1.4 to 2.0.A high Refractive Index indicates a low velocity for light travelling through that particular medium.Snell's LawSnell's law can be used to calculate how much the light will bend on travelling into the new medium.If the interface between the two materials represents the boundary between air (n ~ 1) and water (n = 1.33) and if angle of incidence = 45°, using Snell's Law the angle of refraction = 32°.The equation holds whether light travels from air to water, or water to air.In general, the light is refracted towards the normal to the boundary on entering the material with a higher refractive index and is refracted away from the normal on entering the material with lower refractive index.In labs, you will be examining refraction and actually determine the refractive index of various materials.6. POLARIZATION OF LIGHTAll of this introductory material on light and its behaviour brings us to the most critical aspect of optical mineralogy - that of Polarization of Light.Light emanating from some source, sun, or a light bulb, vibrates in all directions at right angles to the direction of propagation and is unpolarized.In optical mineralogy we need to produce light which vibrates in a single direction and we need to know the vibration direction of the light ray. These two requirements can be easily met but polarizing the light coming from the light source, by means of a polarizing filter.Three types of polarization are possible.1.Plane Polarization2.Circular Polarization3.Elliptical PolarizationFig. Three types of Polarized lightIn the petrographic microscope plane polarized light is used. For plane polarized light the electric vector of the light ray is allowed to vibrate in a single plane, producing a simple sine wave with a vibration direction lying in the plane of polarization - this is termed plane light or plane polarized light.Plane ploarized light may be produced by reflection, selective absorption, double refraction and scattering.1.ReflectionUnpolarized light strikes a smooth surface, such as a pane of glass, tabletop, and thereflected light is polarized such that its vibration direction is parallel to the reflecting surface.The reflected light is completely polarized only when the angle between the reflected and the refracted ray = 90°.2.Selective AbsorptionThis method is used to produce plane polarized light in microscopes, using polarized filters.Some anisotropic materials have the ability to strongly absorb light vibrating in onedirection and transmitting light vibrating at right angles more easily. The ability toselectively transmit and absorb light is termed pleochroism, seen in minerals such astourmaline, biotite, hornblende, (most amphiboles), some pyroxenes.Upon entering an anisotropic material, unpolarized light is split into two plane polarizedrays whose vibratioin directions are perpendicular to each other, with each ray havingabout half the total light energy.If anisotropic material is thick enough and strongly pleochroic, one ray is completelyabsorbed, the other ray passes through the material to emerge and retain its polarization.3.Double RefractionThis method of producing plane polarized light was employed prior to selective absorption in microscopes. The most common method used was the Nicol Prism. See page 14 and Figure 1.14 in Nesse.4.ScatteringPolarization by scattering, not relevant to optical mineralogy, is responsible for the blue colour of the sky and the colours observed at sunset.Ch.2 Refractometry1. RELIEFThis section is covered in Chapter 3 of Nesse.Refractometry involves the determination of the refractive index of minerals, using the immersion method. This method relys on having immersion oils of known refractive index and comparing the unknown mineral to the oil.If the indices of refraction on the oil and mineral are the same light passes through the oil-mineral boundary un-refracted and the mineral grains do not appear to stand out.If n oil <> n mineral then the light travelling though the oil-mineral boundary is refracted and the mineral grain appears to stand out.Fig. Relief - the degree to which a mineral grain or grains appear to stand out from the mounting material, whether it is an immersion oil, Canada balsam or another mineral.When examining minerals you can have:1.Strong reliefo mineral stands out strongly from the mounting medium,o whether the medium is oil, in grain mounts, or other minerals in thin section,o for strong relief the indices of the mineral and surrounding medium differ by greater than 0.12 RI units.2.Moderate reliefo mineral does not strongly stand out, but is still visible,o indices differ by 0.04 to 0.12 RI units.3.Low reliefo mineral does not stand out from the mounting medium,o indices differ by or are within 0.04 RI units of each other.A mineral may exhibit positive or negative relief:∙+ve relief - index of refraction for the material is greater than the index of the oil.- e.g. garnet 1.76∙-ve relief n min < n oil- e.g. fluorite 1.433It is useful to know whether the index of the mineral is higher or lower that the oil. This will be covered in the second lab section - Becke Line and Refractive Index Determination.2. BECKE LINEIn order to determine whether the idex of refraction of a mineral is greater than or less than the mounting material the Becke Line Method is used.Fig. Becke line - a band or rim of light visible along the grain boundary in plane light when the grain mount is slightly out of focus.Becke line may lie inside or outside the mineral grain depending on how the microscope is focused.To observe the Becke line:e medium or high power,2.close aperture diagram,3.for high power flip auxiliary condenser into place.Increasing the focus by lowering the stage, i.e. increase the distance between the sample and the objective, the Becke line appears to move into the material with the higher index of refraction.The Becke lines observed are interpreted to be produced as a result of the lens effect and/or internal reflection effect.LENS EFFECTMost mineral grains are thinner at their edges than in the middle, i.e. they have a lens shape and as such they act as a lens.If n min > n oil the grain acts as a converging lens, concentrating light at the centre of the grain.If n min < n oil, grain is a diverging lens, light concentrated in oil.INTERNAL REFLECTIONThis hypothesis to explain why Becke Lines form requires that grain edges be vertical, which in a normal thin section most grain edges are believed to be more or less vertical.With the converging light hitting the vertical grain boundary, the light is either refracted or internally reflected, depending on angles of incidence and indices of refraction.Result of refraction and internal reflection concentrates light into a thin band in the material of higher refractive index.If n min > n oil the band of light is concentrated within the grain.If n min < n oil the band of light is concentrated within the oil.BECKE LINE MOVEMENTThe direction of movement of the Becke Line is determined by lowering the stage with the Becke Line always moving into the material with the higher refractive index. The Becke Line can be considered to form from a cone of light that extends upwards from the edge of the mineral grain.Becke line can be considered to represent a cone of light propagating up from the edges of the mineral.If n min < n oil, the cone converges above the mineral.If n min > n oil, the cone diverges above the mineral.By changing focus the movement of the Becke line can be observed.If focus is sharp, such that the grain boundaries are clear the Becke line will coincide with the grain boundary.Increasing the distance between the sample and objective, i.e. lower stage, light at the top of the sample is in focus, the Becke line appears:∙in the mineral if n min >n oil∙or in the oil if n min << n oilBecke line will always move towards the material of higher RI upon lowering the stage.A series of three photographs showing a grain of orthoclase:1. The grain in focus, with the Becke line lying at the grain boundary.2. The stage is raised up, such that the grain boundary is out of focus, but the Becke line isvisible inside the grain.3. The stage is lowered, the grain boundary is out of focus, and the Becke line is visibleoutside the grain.When the RI of the mineral and the RI of the mounting material are equal, the Becke line splits into two lines, a blue line and an orange line. In order to see the Becke line the microscope is slightly out of focus, the grain appears fuzzy, and the two Becke lines are visible. The blue line lies outside the grain and the orange line lies inside the grain. As the stage is raised or lowered the two lines will shift through the grain boundary to lie inside and outside the grain, respectively.Index of Refraction in Thin SectionIt is not possible to get an accurate determination of the refractive index of a mineral in thin section, but the RI can be bracket the index for an unknown mineral by comparison or the unknown mineral with a mineral whose RI is known.Comparisons can be made with:1.epoxy or balsam, material (glue) which holds the sample to the slide n = 1.5402.Quartzo n w = 1.544o n e = 1.553Becke lines form at mineral-epoxy, mineral-mineral boundaries and are interpreted just as with grain mounts, they always move into higher RI material when the stage is lowered.Ch.3 Isotropic Materials1. OPTICSThis section is covered in Chapter 4 of Nesse.In Isotropic Materials - the velocity of light is the same in all directions. The chemical bonds holding the material together are the same in all directions, so that light passing through the material sees the same electronic environment in all directions regardless of the direction the light takes through the material.Isotropic materials of interest include the following isometric minerals: Halite - NaClIf an isometric mineral is deformed or strained then the chemical bonds holding the mineral together will be effected, some will be stretched, others will be compressed. The result is that the mineral may appear to be anisotropic.2. ISOTROPIC INDICATRIXTo examine how light travels through a mineral, either isotropic or anisotropic, an indicatrix is used.INDICATRIX - a 3 dimensional geometric figure on which the index of refraction for the mineral and the vibration direction for light travelling through the mineral are related.Isotropic IndicatrixIndicatrix is constructed such that the indices of refraction are plotted on lines from the origin that are parallel to the vibration directions.It is possible to determine the index of a refraction for a light wave of random orientation travelling in any direction through the indicatrix.1. a wave normal, is constructed through the centre of the indicatrix2. a slice through the indicatrix perpendicular to the wave normal is taken.3.the wave normal for isotropic minerals is parallel to the direction of propagation of lightray.4.index of refraction of this light ray is the radius of this slice that is parallel to the vibrationdirection of the light.For isotropic minerals the indicatrix is not needed to tell that the index of refraction is the same in all directions.Indicatrix introduced to prepare for its application with anisotropic materials.3. ISOTROPIC vs. ANISOTROPICDistinguishing between the two mineral groups with the microscope can be accomplished quickly by crossing the polars, with the following being obvious:1.All isotropic minerals will appear dark, and stay dark on rotation of the stage.2.Anisotropic minerals will allow some light to pass, and thus will be generally light, unlessin specific orientations.Why are isotropic materials dark?1.Isotropic minerals do no affect the polarization direction of the light which has passedthrough lower polarizer;2.Light which passes through the mineral is absorbed by the upper polar.Why do anisotropic minerals not appear dark and stay dark as the stage is rotated?1.Anisotropic minerals do affect the polarization of light passing through them, so somecomponent of the light is able to pass through the upper polar.2.Anisotropic minerals will appear dark or extinct every 90° of rotation of the microscopestage.3.Any grains which are extinct will become light again, under crossed polars as the stage isrotated slightly.To see the difference between Isotropic vs. Anisotriopic minerals viewed with the petrographic microscope look atthe following images:1.Image 1- plane light view of a metamorphic rock containing three garnet grains, in amatrix of biotite, muscovite, quartz and a large stauroite grain at the top of the image.2.Image 2- Crossed polar view of the same image. Note that the three garnet grains are'extinct" or black, while the remainnder of the minerals allow some light to pass.Ch. 4 Anisotropic MineralsINTRODUCTIONAnisotropic minerals are covered in Chapter 5 of Nesse.Anisotropic minerals differ from isotropic minerals because:1.the velocity of light varies depending on direction through the mineral;2.they show double refraction.When light enters an anisotropic mineral it is split into two rays of different velocity which vibrate at right angles to each other.In anisotropic minerals there are one or two directions, through the mineral, along which light behaves as though the mineral were isotropic. This direction or these directions are referred to as the optic axis.Hexagonal and tetragonal minerals have one optic axis and are optically UNIAXIAL.Orthorhombic, monoclinic and triclinic minerals have two optic axes and are optically BIAXIAL.In Lab # 3, you will examine double refraction in anisotropic minerals, using calcite rhombs.Calcite Rhomb Displaying Double RefractionLight travelling through the calcite rhomb is split into two rays which vibrate at right angles to each other. The two rays and the corresponding images produced by the two rays are apparent in the above image. The two rays are:1.Ordinary Ray, labelled omega w, n w = 1.6582.Extraordinary Ray, labelled epsilon e, n e = 1.486.Vibration Directions of the Two RaysThe vibration directions for the ordinary and extraordinary rays, the two rays which exit the calcite rhomb, can be determined using a piece of polarized film. The polarized film has a single vibration direction and as such only allows light, which has the same vibration direction as the filter, to pass through the filter to be detected by your eye.1.Preferred Vibration Direction NSWith the polaroid filter in this orientation only one row of dots is visible within the area of the calcite rhomb covered by the filter. This row of dots corresponds to the light ray which has a vibration direction parallel to the filter's preferred or permitted vibration direction and as such it passes through the filter. The other light ray represented by the other row of dots, clearly visible on the left, in the calcite rhomb is completely absorbed by the filter.2.Preferred Vibration Direction EWWith the polaroid filter in this orientation again only one row of dots is visible, within the area of the calcite coverd by the filter. This is the other row of dots thatn that observed in the previous image. The light corresponding to this row has a vibration direction parallel to the filter's preferred vibration direction.It is possible to measure the index of refraction for the two rays using the immersion oils, and one index will be higher than the other.1.The ray with the lower index is called the fast rayo recall that n = V vac/V mediumIf n Fast Ray = 1.486, then V Fast Ray = 2.02X1010 m/sec2.The ray with the higher index is the slow rayo If n Slow Ray = 1.658, then V Slow Ray = 1.8 1x1010 m/secRemember the difference between:∙vibration direction - side to side oscillation of the electric vector of the plane light and∙propagation direction - the direction light is travelling.Electromagnetic theory can be used to explain why light velocity varies with the direction it travels through an anisotropic mineral.1.Strength of chemical bonds and atom density are different in different directions foranisotropic minerals.2. A light ray will "see" a different electronic arrangement depending on the direction ittakes through the mineral.3.The electron clouds around each atom vibrate with different resonant frequencies indifferent directions.Velocity of light travelling though an anisotropic mineral is dependant on the interaction between the vibration direction of the electric vector of the light and the resonant frequency of the electron clouds. Resulting in the variation in velocity with direction.Can also use electromagnetic theory to explain why light entering an anisotropic mineral is split into two rays (fast and slow rays) which vibrate at right angles to each other.PACKINGAs was discussed in the previous section we can use the electromagnetic theory for light to explain how a light ray is split into two rays (FAST and SLOW) which vibrate at right angles to each other.The above image shows a hypothetical anisotropic mineral in which the atoms of the mineral are:1.closely packed along the X axis2.moderately packed along Y axis3.widely packed along Z axisThe strength of the electric field produced by the electrons around each atom must therefore be a maximum, intermediate and minimum value along X, Y and Z axes respectively, as shown in the following image.With a random wavefront the strength of the electric field, generated by the mineral, must have a minimum in one direction and a maximum at right angles to that.Result is that the electronic field strengths within the plane of the wavefront define an ellipse whose axes are;1.at 90° to each other,2.represent maximum and minimum field strengths, and3.correspond to the vibration directions of the two resulting rays.The two rays encounter different electric configurations therefore their velocities and indices of refraction must be different.There will always be one or two planes through any anisotropic material which show uniform electron configurations, resulting in the electric field strengths plotting as a circle rather than an ellipse.Lines at right angles to this plane or planes are the optic axis (axes) representing the direction through the mineral along which light propagates without being split, i.e., the anisotropic mineral behaves as if it were an isotropic mineral.INTERFERENCE PHENOMENAThe colours for an anisotropic mineral observed in thin section, between crossed polars are called interference colours and are produced as a consequence of splitting the light into two rays on passing through the mineral.In the lectures we will examine interference phenomena first using monochromatic light and then apply the concepts to polychromatic or white light.RETARDATIONMonochromatic ray, of plane polarized light, upon entering an anisotropic mineral is split into two rays, the FAST and SLOW rays, which vibrate at right angles to each other.Development of RetardationDue to differences in velocity the slow ray lags behind the fast ray, and the distance represented by this lagging after both rays have exited the crystal is the retardation - D.The magnitude of the retardation is dependant on the thickness (d) of the mineral and the differences in the velocity of the slow (V s) and fast (V f) rays.The time it takes the slow ray to pass through the mineral is given by:during this same interval of time the fast ray has already passed through the mineral and has travelled an additional distance = retardation.。
具有纹理特征的二维高斯粗糙面单双站极化散射
具有纹理特征的二维高斯粗糙面单双站极化散射刘伟;郭立新;王安琪【摘要】A two-dimensional Gauss rough surface characterized by textures is presented and the properties of polarimetric scattering from the surface are studied. Trie rough surface characterized by textures can be obtained through the angle rotating in Fourier transform with the ratio of the two correlation lengths large enough. The scattered field is derived in the Cartesian coordinate system through the integration of scattering facets with the elliptic polarized incidence wave. The polarized radar cross section ( RCS) from the Gaussian rough surface characterized by textures is computed. Several numerical results exhibit the influence of incident angle, texture angle, correlation length and root mean square height on the polarimetric scattering from the texture rough surface.%提出了具有纹理特征的二维高斯粗糙面并研究了其极化散射特性.发现将高斯粗糙面在两个方向上的相关长度的比值取到足够大,能从粗糙面上直观地观察到纹理特征,并且可以利用傅里叶变换中的角度旋转得到任意的纹理走向.通过粗糙面的小面元积分,推导出椭圆极化入射时笛卡尔坐标系下的散射场,并得到了不同纹理特征高斯粗糙面的极化雷达散射截面.数值结果显示了入射角、纹理角、相关长度以及高度起伏均方根对于纹理粗糙面极化散射特性的影响.【期刊名称】《西安电子科技大学学报(自然科学版)》【年(卷),期】2011(038)006【总页数】8页(P75-81,102)【关键词】极化;粗糙面;雷达散射截面;纹理;相关长度【作者】刘伟;郭立新;王安琪【作者单位】西安电子科技大学理学院,陕西西安710071;西安电子科技大学理学院,陕西西安710071;西安电子科技大学理学院,陕西西安710071【正文语种】中文【中图分类】TN011随机粗糙面电磁散射研究因其广泛应用于地球遥感、表面探测等领域而倍受重视[1-2].在实际应用中,粗糙面电磁散射数据主要来自实际测量和理论模型推演.显然,前者需要耗费大量的人力、物力,并且对环境的要求很高.而后者可以通过理论计算,并与实测数据比较建立电磁散射的理论模型,方法简单并且不受环境的影响,具有很强的应用价值.目前,粗糙面散射的理论计算方法主要有两大类:解析近似方法和精确数值方法.其中解析近似方法主要是基尔霍夫近似、微扰法、双尺度法、小斜率近似等[3];数值方法包括矩量法、时域有限差分法、有限元法等[4].近年来,国内外学者在粗糙面散射的理论模型研究中取得了大量的研究成果.Elfouhaily等[5]在小斜率近似的基础上改进了积分核,提出了三阶简化局部曲率近似方法(RLCA3).Joel 等[6]比较了几何光学(GO)和物理光学(PO)在指数相关表面上的散射理论,并通过与精确解的比较证实了物理光学有效的条件.闫沛文等[7]针对具有大介电常数的介质粗糙面的电磁散射问题,提出了灵活的广义最小余量法(FGMRES)和基于物理意义的双网格法(PBTG)的混合算法.杨超等[8]在极坐标下采用小斜率近似方法导出了二维高斯介质粗糙面散射系数的计算公式.刘伟等[9]将海面离散化为散射面元,推导了二维分形海面的极化散射.Ma等[10]将锥形波引入到传统基尔霍夫近似(KA)中,研究了一维有耗介质粗糙面的双站散射,其计算结果与矩量法吻合.Hu等[11]比较了几种近似方法,并讨论了粗糙面上的高度起伏均方根和相关长度对近似方法的影响.纹理特征作为遥感图像中重要的信息,通过灰度的空间变化及其重复性来反映地物的视觉粗糙度,能充分反映影像特征,无论从理论上还是从应用上都是描述和识别图像的重要依据[12].实际海面上的沙丘、山脉、海浪等均表现出较明显的纹理特征.目前,针对纹理特征的研究多见于有关雷达图像等的文章中,而针对纹理粗糙面电磁散射研究尚不多见,Prakash等[13]仅研究了X波段镜向散射随着土壤纹理变化的情况.因此,建立具有纹理特征的粗糙面与电磁散射的联系就显得尤为重要.1.1 具有纹理特征的高斯粗糙面模拟笔者用有限脉冲响应滤波器理论和快速傅里叶变换相结合的方法[14]模拟了二维高斯随机粗糙面.其功率谱表示为其中,δ是二维高斯粗糙面的均方根高度;lx和ly是x和y方向上的相关长度;kx和ky是x和y方向上的空间波数.如果lx和ly之间比值大于4,那么所形成的二维高斯粗糙面就会表现出很明显的纹理走向(如图1).将纹理走向和x坐标方向的夹角定义为纹理角φ.对式(1)进行角度旋转得W(k0x,k0y),则快速傅里叶变换得到的二维高斯粗糙面也相应发生了角度旋转.其中,图1(a)给出了粗糙面尺寸为30m×30m,均方根高度δ= 0.6m,相关长度lx=10m,ly=2m,纹理角φ=30°的二维高斯粗糙面俯视图.在此参数保持不变的基础上,图1(b)改变ly,即ly=1m;图1(c)改变lx和ly,即lx=5m,ly=1m.可以看到图1(b)上的粗糙面较之图1(a)纹理的宽度变窄了,而图1(c)上的粗糙面较之图1(b)沿纹理方向上高度起伏更为明显.1.2 极化散射图2给出了二维粗糙面电磁散射的几何示意图,其中θ1为入射角,θ2为散射角,θ3为散射方位角.入射场、散射场的正交坐标系分别为它们与笛卡儿坐标系的关系如下:将入射电场表示为平行和垂直极化矢量之和:式中,ki为入射波数矢量;γ是分量相对于分量的相位延迟;E01和E02分别为两个分量的幅值.定义为粗糙面点r′=(x′,y′,z′)处向上的法线单位矢量:其中,αi和βi,j分别为粗糙面点r′在x,y方向上的斜率,简写为α,β.同时,此处定义一个局部正交坐标系,j它们与的关系为是点r′处的平行和垂直极化单位矢量,且可得不同坐标系之间平行和垂直极化单位矢量的关系:式中,D=β2+(αcosθ1-sinθ1)2.根据式(5)和式(7),局部正交坐标系下入射电场的垂直分量与水平分量分别为式中,A0是观测粗糙面范围;=-.F(α,β)主要与电磁波极化特性、入射角、粗糙面电磁介电常数和粗糙度有关,可以表示为由式(4)中散射场正交系和笛卡尔坐标系的关系,即可得到散射极化电磁波的平行和垂直极化矢量和.发射和接收的极化电磁波矢量Ei和Es之间的关系可以通过一个2×2的矩阵来表示,这个矩阵就称为极化散射矩阵,即这样,极化散射矩阵中各元素可由式(4)和式(22)求出:由此可以得到粗糙面极化雷达散射截面其中,m,n分别为散射波和入射波的极化状态.在满足互易原理并使用后向散射坐标系的条件下,有σhv= σvh[9].取入射电磁波频率f=1.3GHz,入射角θ1=30°,粗糙面介电常数εr=4.1+0.98i,粗糙面的长度L=30m,计算样本数为50.图3是不同极化状态下,纹理角为0°、45°及90°时的双站极化散射截面随散射角的变化图,其中高斯粗糙面相关长度lx=10m,ly=1m,高度起伏均方根δ=0.5m.通过图3中的散射截面比较,可以发现纹理角对极化散射的影响.由于菲涅耳散射系数的影响,在纹理角等于0°和45°时,与HH极化散射截面相比,VV极化散射截面在近后向散射区域(θ2<0°)随着散射角的增大而迅速下降;当纹理角等于90°时,同极化散射却在近后向散射区域有明显的增强,并且VV散射截面增强的幅度更大.这是由于在90°时纹理方向与入射面垂直,将有更多散射面元的相干散射对后向散射区域有较大的贡献.另外,比较交叉极化散射截面,发现在纹理角等于0°和90°时VH和HV散射截面之间的差异并不突出,而在纹理角等于45°时两种交叉极化的差异是显著的,尤其是在镜向方位,HV散射截面还出现了明显的峰值.这是因为当纹理角为45°时,粗糙面的小面元在局部坐标系下将入射波在其正交方向上分解达到最大;当纹理角为0°和90°时,交叉极化散射截面的变化趋势也有明显区别.当纹理角等于0°时,交叉极化散射截面在前向位置达到最大;当纹理角等于90°时,交叉极化则表现出与所对应的同极化一样的后向增强.相对于双站散射,单站散射具有更广泛的实际应用.由于在后向单站散射条件下,交叉极化是相等的,图4在图3参数的基础上仍取入射角30°,仅给出了HH、VV和HV 单站散射截面随纹理角从0°到180°变化的曲线.按照相关长度和高度起伏均方根的不同,将算例分为4组:第1组(case 1)中,lx=10m,ly=2m,δ=1m; 第2组(case 2)中,lx=10m,ly=1m,δ=1m;第3组(case 3)中,lx=5m,ly=1m,δ=1m;第4组(case 4)中, lx=10m,ly=1m,δ=0.5m.从图4可以明显看出,在不同的相关长度和高度起伏均方根下,纹理角对极化散射截面有较为显著的影响.在以上4种情况下,当纹理角等于90°时,同极化散射截面基本上达到峰值;随着纹理角偏离90°,同极化散射截面逐渐减小.这主要是因为纹理角越接近90°,粗糙面上的纹理走向对于后向散射的贡献越大.如图1所示相关长度对纹理特征的影响,对比图4(a)和图4(b),可见第1组同极化散射截面较第2组更大,这是因为纹理较宽的粗糙面上对后向散射贡献大的散射面元多而集中.但在纹理角接近0°和180°时,由于纹理走向平行于入射面,散射面元对后向散射的影响差异很小,所以此时两者的同极化散射截面是相近的.第3组比第2组相关长度lx更短,在纹理方向上高度起伏更为明显,对应于同极化散射截面的变化,可以看到第3组的数据在纹理角接近0°和180°时较第2组大了约3 dB,但在纹理角接近90°时与第2组差异较小.第4组的数据由于粗糙面高度起伏均方根较小,同极化散射截面仅在纹理角处于60°到120°范围内出现起伏,而在此之外的范围几乎保持不变.这说明小的高度起伏粗糙面在纹理走向和入射面接近正交方向时才会表现出较为明显的后向增强.由图4(c)可以观察到,这4组情况下交叉极化散射截面变化的趋势大体相同.在纹理角分别在60°到80°和100°到120°范围内的时候出现双峰值,而在纹理角等于0°和180°的时候散射截面达到最小,两者之间的差距大约是8 dB.在双峰值之间,局部最小值处在90°纹理角左右,且此处的局部最小值还是要比在0°和180°出现的全局最小值高近6 dB,这说明了粗糙面的纹理方向在后向散射中对去极化效应的影响.可以看到,第1组在纹理角处于60°到120°范围内时交叉散射截面最大,其他3组较为相似;而在剩余范围内相关长度的比值和第1组同(为5∶1)的第3组散射截面最大,第1组其次,第2组再次,高度起伏均方根最小的第4组最小.这充分说明除了高度起伏均方根之外,两个相关长度的大小乃至两者的比值都会影响后向交叉极化散射.由于图4中第4组(case 4)情况下同极化散射截面在很大范围内保持不变,特别给出图5说明此种情况下不同纹理角时单站极化散射截面随入射角改变的曲线.可以看到,在纹理角为0°和45°时,两种不同纹理角对应的同极化散射截面在不同入射角下差异很小,得到了与图4相同的结果;而纹理角为90°时,后向散射截面随着入射角的增加表现出很明显的后向增强.从图5(c)中看到,不同纹理角的后向交叉散射截面有着明显的不同:纹理角为45°的交叉极化散射截面始终大于纹理角为0°的,并且这两种情况下所得到的交叉散射截面都保持着随着入射角的增大而下降的趋势;但纹理角为90°时交叉散射截面对于入射角的增大并未出现明显的变化趋势.另外,因为任何电磁波在垂直入射纹理角为90°粗糙面时沿着纹理方向分解的线极化波和垂直入射纹理角为0°粗糙面时沿着纹理方向分解的线极化波刚好是正交的,而在单站散射条件下, HV极化和VH极化是相等的,所以,在入射角较小时纹理角为90°和0°的交叉极化截面几乎相等.纹理是二维粗糙面的重要特征,对于利用遥感信息研究地貌和海洋的粗糙面散射都具有很重要的意义.当二维高斯粗糙面在两个方向上的相关长度之间的比值足够大时,就会表现出明显的纹理特征,因此相关长度的比值就是影响纹理特征的重要参数.笔者采取粗糙面离散面元积分的方法计算不同相关长度、纹理角以及高度起伏均方根对二维高斯粗糙面单双站极化散射截面的影响,数值结果均符合相关物理解释.可以看到,极化散射截面对于纹理的敏感度取决于入射角、纹理角、相关长度以及高度起伏均方根,这对于利用极化散射截面提取粗糙面的纹理信息有着重要的理论参考价值.需要说明的是,具有纹理特征的粗糙面极化散射数值结果还有待于今后进一步的实验验证.【相关文献】[1]郭立新,陈建军,韦国晖,等.粗糙面电磁散射的小斜率近似方法研究[J].西安电子科技大学学报,2005,32(3):408-413. 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Yang Chao,Guo Lixin.Electromagnetic Scattering from Gaussian Dielectric Rough Surface Using Small Slope Approximation Method[J].Chinese Journal of Radio Science,2009,24(1):77-82.[9]刘伟,郭立新,王蕊,等.计算二维海面极化电磁散射的新方法[J].西安电子科学大学学报,2009,36(3):517-523. Liu Wei,Guo Lixin,Wang Rui,et al.New Study of Polarimetric Scattering of the Two-dimensional Sea Surface[J].Journal of Xidian University,2009,36(3):517-523.[10]Ma Jun,Guo Lixin,Cheng Xiangzhe.Unification of the Kirchhoff Approximation and the Method of Moment for Optical Wave Scattering from the Lossy Dielectric Gaussian Random Rough Surface[J].Chinese Optics Letters,2009,7(3):259-262. [11]Hu Shanzheng,Fu Liyun,Yao parison of Various Approximation Theories for Randomly Rough Surface Scattering [J].Wave Motion,2009,46(5):281-292.[12]曹广真,侯鹏,金亚秋,等.基于纹理特征的拉普拉斯金字塔形微波遥感图像融合[J].遥感技术与应用,2007,22 (5):628-632. 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水下偏振成像技术英文文章
水下偏振成像技术英文文章Underwater Polarized Imaging TechnologyPolarized imaging is a powerful technique that has gained significant attention in the field of underwater imaging and sensing. This technology leverages the unique properties of light to extract valuable information about the underwater environment, enabling a wide range of applications, from marine biology and oceanography to underwater navigation and object detection.At its core, polarized imaging relies on the fact that light interacts differently with various materials and surfaces, depending on its polarization state. When light travels through water, it can become partially polarized due to scattering and other optical phenomena. By analyzing the polarization characteristics of the reflected or transmitted light, researchers and engineers can gain insights into the properties of the underwater objects or environments.One of the primary advantages of polarized imaging in the underwater domain is its ability to enhance contrast and visibility. In turbid or murky waters, the scattering of light can significantly degrade the quality of traditional imaging systems, making it difficultto distinguish between objects and the background. Polarized imaging, however, can effectively reduce the effects of this scattering, allowing for clearer and more detailed images to be captured.This is achieved by exploiting the fact that the scattered light tendsto have a different polarization state than the light reflected from the objects of interest. By using specialized optical filters or polarizers, the imaging system can selectively capture the light with the desired polarization, effectively suppressing the scattered light and enhancing the contrast of the target objects.Another key application of polarized imaging in the underwater environment is the detection and identification of submerged objects. The unique polarization signatures of different materials and surfaces can be used as a fingerprint to distinguish between various objects, such as mines, shipwrecks, or marine life. This information can be valuable for a wide range of applications, from military and security operations to marine conservation and exploration.In addition to object detection, polarized imaging has also found applications in the field of underwater navigation and guidance. By analyzing the polarization patterns of the light reflected from the seafloor or other underwater features, autonomous underwater vehicles (AUVs) and remotely operated vehicles (ROVs) can navigate more effectively, even in low-visibility conditions.The development of polarized imaging technology for underwater applications has been an active area of research and innovation. Researchers have explored various techniques, such as the use of liquid crystal variable retarders, Stokes polarimeters, and Mueller matrix imaging, to capture and analyze the polarization state of the light in the underwater environment.One particularly promising area of research is the integration of polarized imaging with other sensing modalities, such as sonar or laser imaging. By combining these technologies, researchers can create more comprehensive and robust underwater imaging and sensing systems, capable of providing a more complete understanding of the underwater environment.Despite the significant progress made in this field, there are still several challenges that need to be addressed. For example, the development of compact, cost-effective, and reliable polarized imaging systems that can withstand the harsh underwater conditions is an ongoing area of research. Additionally, the interpretation and analysis of the complex polarization data collected by these systems require advanced signal processing and machine learning algorithms, which continue to be an active area of investigation.In conclusion, underwater polarized imaging technology is apowerful tool that has the potential to revolutionize the way we interact with and explore the underwater world. By leveraging the unique properties of light, researchers and engineers can develop innovative solutions for a wide range of applications, from marine biology and oceanography to underwater navigation and object detection. As the field continues to evolve, we can expect to see even more exciting advancements in this technology, paving the way for a deeper understanding and better stewardship of our aquatic environments.。
物理专业英语词汇(I)题库
物理专业英语词汇(I)ice 冰ice calorimeter 冰量热计ice model 冰模型iconoscope 光电摄象管icosahedron 二十面体ideal black body 理想黑体ideal constraints 理想拘束ideal crystal 理想晶体ideal fluid 完整铃ideal gas 理想气体ideal gas law 理想气体定律ideal lattice 理想晶格ideal liquid 理想液体ideal solid 理想固体ideal solution 理想溶液ideally imperfect crystal 理想非完满晶体ideally perfect crystal 理想完满晶体identity parameter 晶体参数ignition 点火ignition potential 点火电位ignitron 点火管illuminance 光照度illuminant 光源illuminating engineering 照盲程学illuminating lamp照闷illumination 光照度illumination curve 照度曲线illumination photometer 照度计illumination photometry 照度丈量illuminator 照冒置illuminometer 照度计image 象image analyzer 图象剖析器image charge 象电荷image contrast 象对照度image converter 变象管image converter tube 变象管image distortion 图象失真image force 象力image formation 成象image frequency 象频image hologram 象全息图image iconoscope 图象光电摄象管image intensifier 影象加强器影象放大器image intensifier tube 影象加强器影象放大器image orthicon 超正析象管image parameter 成象参数image pickup tube 摄象管image plane 象平面image point 象点image processing 图象办理image ratio 镜频波道的相对增益image restoration 象恢复image space 象空间image surface 象曲面imagelyzer 图象剖析器immersion 淹没immersion lens 淹没透镜immersion method 淹无法immersion microscope 油浸显微镜immersion objective 淹没物镜immersion refractometer 淹没折射计impact 冲击impact ionization 碰撞电离impact matrix 碰撞矩阵impact parameter 碰撞参数impact parameter method 碰撞参数法impact strength 冲豢度impact stress 冲沪力impact test 冲辉验impedance 阻抗impedance bridge 阻抗电桥impedance matching 阻抗般配imperfect crystal 非完满晶体imperfect gas 非理想气体impressed forces 外力imprisonment of resonance radiation 共振辐射陷获improper variable 准变星impulse 冲击冲量impulse approximation 冲稽似impulse function 脉冲函数impulse generator 脉冲发生器impulse of force 冲量impulsive current 脉冲电流impulsive force 冲力impulsive sound 冲基impulsive tone 撞霍impurity 杂质impurity atom 杂质原子impurity band 杂质能带impurity center 杂质中心impurity conduction 杂质导电impurity level 杂质能级impurity scattering 杂质散射impurity semiconductor 杂质半导体in clockwise direction 向顺时针的方向in counter colckwise direction 向反时针的方向in situ observation 就地察看incandescence 白炽incandescent lamp 白炽灯inch 英寸incidence 入射incidence angle 入射角incident beam 入射束incident light 入射光incident particle 入射粒子incident plane 入射面incident ray 入射光芒incident wave 入射波inclination factor 倾斜因子inclinometer 磁倾计incoherence 非相关性incoherent light 非相关光incoherent scatteering 非相关散射incommensurate structure 不相应构造incompressibility 不行压缩性incompressible flow 不行压缩流indefinite metric 不定胸怀independent atom model 独立原子模型independent particle 独立粒子independent particle model 独立粒子模型independent variable 自变数indeterminancy 不确立性indeterminancy principle 测禁止原理index 指数index of refraction 折射率indicating lamp 指示灯indicator 指示器指示剂indifferent equilibrium 中性均衡indirect exchange interaction 间接交换互相酌indirect illumination 间接照明indirect measurement间接丈量indirect transition 间接跃迁indirectly heated cathode 旁热式阴极indistinguishability of identical particles 全同粒子的不行分辨性indium 铟individual error 人为偏差individual excitation 独自激发induced current 感觉电流induced electromotive force 感觉电动势induced emission 感觉发射induced radioactivity 感觉放射性induced representation 引诱表示inductance 电感感觉系数inductance coil 感觉线圈induction 感觉; 概括induction accelerator 感觉加快器induction coefficient 感觉系数induction coil感觉线圈induction field 感觉磁场induction furnace 感觉电炉induction heating 感觉加热induction method 概括法induction motor 感觉电动机inductive 感觉的inductor coil 感觉线圈indus 印第安座inelastic collision 非弹性碰撞inelastic scattering 非弹性散射inert gas 惰性气体inertia 惯性inertial force 惯性力inertial frame of reference 惯性系inertial mass 惯性质量inertial resistance 惯性阻力inertial system 惯性系inertial wave 惯性波inferior conjunction 下合inferior mirage 下现幻景inferior planet 地行家星infinite medium 无穷介质infinite universe 无穷宇宙infinitesimal rotation 无量小转动infinitesimal transformation 无量小变换inflationary universe 狂涨宇宙inflector 偏转器influence machine感觉起电机information processing 信息办理information quantity 信息量information retrieval 信息恢复information theory 信息论infra acoustic 声下的infra acoustic frequency 亚声频infra sound 次声infranics 红外线电子学infrared 红外线的infrared active 红外激活的infrared astronomical satellite 红外天文卫星infrared astronomy 红外天文学infrared catastrophe 红外灾变infrared divergence 红外发散infrared lamp 红外灯infrared laser 红外激光器infrared magnitude 红外星等infrared microscope 红外线显微镜infrared photocell 红外线光电管infrared photography 红外拍照infrared radiation 红外辐射infrared rays 红外线infrared spectrophotometer 红外分光光度计infrared spectroscopy 红外光谱学infrared spectrum 红外光谱inhomogeneous broadening 非平均增宽inhomogeneous plasma 非平均等离子体inhomogeneous superconductor 非均质超导体inhomogeneous universe 非平均宇宙initial black hole 原始黑洞initial permeability 初始磁导率initial phase 初相initial state 初态initial stress 初应力initial velocity 初速度injection 注入injection laser 注入型激光器注入型二极管激光器injector accelerator 注入加快器injury 损害inlet pressure 入口压力inner bremsstrahlung 内韧致辐射inner corona 内冕inner electron 内层电子inner product 内积inner quantum number 内量子数inner shell 内壳层input 输入input output channel 输入输出通道input output unit 输出输入装置input program 输入程序input routine 输入程序insolation 日射inspection 检查instability 不稳固性instability energy 不稳固能instantaneous axis of rotation 刹时转动轴instantaneous neutron 瞬发中子instantaneous pole 刹时极instantaneous power 刹时功率instanton 瞬子instruction 指令instrument 仪器仪表instrument transformer 仪表变换器instrumental error 仪企差instrumental function 仪漂数insulating paper绝缘纸insulating transformer 绝缘变压器insulation 绝缘insulation resistance 绝缘电阻insulator 绝缘体integral calculus 积分学integral equation 积分方程integral invariant 积分不变式integral transform 积分变换integrated circuit 集成电路integrated optics 集成光学integrated reflection intensity 积分反射强度integrating sphere 乌布利希球integrating wattmeter 积累瓦特计integration circuit 积分电路integration type analog to digital conversion 积分型模拟数字变换intense slow positron beam 强慢速阳电子束intensifier 加厚剂intensity 强度intensity alternation 强度交变intensity factors of spectral lines 谱线强度因子intensity modulation 亮度灯intensity of magnetic field 磁场强度intensity of magnetization 磁化强度intensity of radioactivity 放射性强度intensity of sound 声强intensity region 强度范围intensive quantity 内包量intensive variable 示强变量interaction 互相酌interaction energy 互相酌能interaction force 互相酌力interaction potential 互相酌势interaction range 互相酌区interatomic 原子间的interatomic distance 原子间距离interatomic forces 原子间力intercalation 夹层interchange instability 变换不稳固性interchangeability 交换性intercombination 互相组合intercrystalline 晶粒间的interdiffusion 互扩散interface 界限面interfacial electric phenomenon 界面电现象interfacial potential 界面势interfacial tension 界面张力interfacial viscosity 界面粘性interference 干预interference color 扰乱色interference filter 扰乱滤光片interference fringe 干预条纹interference microscope 干预显微镜interference of equal inclination 等倾角干预interference of equal thickness 等厚度干预interference of light 光的干预interference of polarized light 偏振光的干预interference refractometer 干预折射计interference spectroscope 干预分光镜interferometer 干预仪interferometry 干预胸怀学intergalactic matter 星系际物质intergalactic space 星系际空间intermediate coupling 中间耦合intermediate energy 中间能量intermediate energy physics 中能物理学intermediate frequency 中频intermediate frequency transformer 中频变换器intermediate image 中间影象intermediate neutron 中速中子intermediate nucleus 复核intermediate orbit 中间轨道intermediate state 中间态intermediate vector boson 弱玻色子intermetallic compounds 金属间化合物intermittent discharge 间歇放电intermolecular 分子间的intermolecular force 分子间力intermolecular interaction 分子间互相酌internal adsorption 内吸附internal conversion 内变换internal conversion electron 内变换电子internal electron pair creation 内电子对产生internal energy 内能internal exposure 内照耀internal force 内力internal friction 内摩擦internal impedance 内阻抗internal ionization 内电离internal magnetic field 内磁场internal photoelectric effect 内光电效应internal pressure 内压internal quantum number 内量子数internal reflection 内反射internal resistance 内阻internal rotation 内旋转internal storage 内部储存器internal stress 内应力internal target 内靶internal viscosity 内粘滞international atomic time 国际原子时international geophysical year 国际地球物理年international latitude service 国际纬度服务international practical temperature scale 国际适用温标international prototype metre 国际米原器international standard atomsphere 国际标准大气international system of units 国际单位制international temperature scale 国际温标international thermonuclear experimental reactor 国际热核实验反响堆international unit 国际单位interpenetration 互相穿透interplanar crystal spacing 晶面间距interplanetary dust 行星际灰尘interplanetary magnetic field 行星际磁场interplanetary matter 行星际物质interplanetary space 行星际空间interpolation formula 内插公式interrupt 中止interrupter 断续器interspace 缝隙interstellar absorption 星际汲取interstellar absorption line 星际线interstellar cloud 星际云interstellar dust 星际灰尘interstellar gas 星际气体interstellar line 星际线interstellar magnetic field 星际磁场interstellar matter 星际物质interstellar molecule 星际分子interstellar reddening 星际红化interstellar space 星际空间interstice 缝隙interstitial alloy 填隙式合金interstitial atom 填隙原子interstitial diffusion 填隙式扩散interstitial ion 填隙离子interstitial solid solution 填隙式固溶体interval间隔interval rule 间隔规则intraatomic 原子内的intracrystalline 晶体内的intramolecular分子内的intramolecular bond 分子内键intramolecular forces 分子内力intramolecular rotation 分子内转动intrinsic conduction 本占电intrinsic energy 内能intrinsic magnetic moment 固有磁矩intrinsic magnetization 内倥化intrinsic parity 内兕称intrinsic permeability 固有磁导率intrinsic semiconductor 本针导体intrinsic viscosity 本粘性intrinsic wavelength 固有波长invar 殷钢invariable plane 不变平面invariance 不变性invariant 不变式invariant of strain 应变不变量invariant subgroup 不变子群inverse circuit 反演电路inverse compton effect 逆康普顿效应inverse fluorite structure 逆萤石构造inverse photoelectric effect 逆光电效应inverse photoelectron spectroscopy 逆光电光谱学inverse piezoelectric effect 逆压电效应inverse predissociation 逆前级离解inverse problem 逆问题inverse process 逆过程inverse proportion 反比率inverse raman effect 反转喇曼效应inverse raman spectroscopy反转喇曼光谱学inverse reaction 逆反响inverse scattering method 逆散射法inverse spinel 反尖晶石inverse spinel structure 反尖晶石型构造inverse square law 平方反比律inverse transformation 逆变换inverse voltage 逆电压inverse zeeman effect 反向塞曼效应inversion 反演inversion axis 反演轴inversion doublet 反转两重线inversion formula 反演公式inversion layer 反转层 ; 逆温层inversion spectrum 反转光谱inversion system 倒象系inversion temperature 变换温度invert 反演inverted magnetron gage 逆磁控管计inverted multiplet 反转多重态inverted term颠倒项inverter 逆变换装置inviscid flow 无粘性流invisible radiation 不行见的辐射invisible rays 不行见的射线iodine 碘ion 离子ion accelerator 离子加快器ion acceptor 离子接受体ion acoustic instability 离子声波不稳固性ion activity 离子活度ion avalanche 离子雪崩ion beam 离子束ion beam probe 离子束探针ion bombardment 离子轰击ion channelling 离子沟道效应ion cloud 离子云ion cluster 离子簇ion concentration 离子浓度ion condensation 离子凝集ion cyclotron frequency 离子盘旋频次ion cyclotron resonance heating 离子盘旋共振加热ion cyclotron resonance method 离子盘旋共振法ion density 离子密度ion diffusion 离子扩散ion electron recombination 离子电子再化合ion exchange 离子交换ion exchange resin 离子交换尸ion impact 离子碰撞ion implantation 离子注入ion implanted junction 离子注入结ion induced desorption 离子感觉退吸ion induced x ray analysis 离子感觉 x 射线剖析ion lattice 离子晶格ion loss 离子消耗ion microprobe analyzer 离子微探针剖析器ion microscope 离子显微镜ion molecule 离子型分子ion neutralization 离子中和ion neutralization spectroscopy 离子中和波谱学ion optics 离子光学ion orbit 离子轨道ion pair 离子对ion pair formation 离子对生成ion plasma frequency 离子等离子体频次ion pump 离子泵ion recombination 离子复合ion saturation current 离子饱和电流ion scattering spectroscopy 离子散射能谱学ion selective electrode 离子选择电极ion sheath 离子鞘ion source 离子源ion temperature 离子温度ion trap 离子圈套ion yield 离子产额ionic atmosphere 离子氛围ionic bond 异极键ionic charge 离子电荷ionic compound 离子化合物ionic conduction 离子导电ionic crystal 离子晶体ionic current 离子电流ionic laser 离子激光器ionic migration 离子迁徙ionic mobility 离子迁徙率ionic molecule 离子型分子ionic polymerization 离子聚合ionic radius 离子半径ionic recombination 离子复合ionic strength 离子强度ionic structure 离子构造ionium 锾ionization 电离ionization by collision 碰撞电离ionization chamber 电离室ionization current 电离电流ionization density 电离密度ionization fluctuation 电离涨落ionization limit 电离极限ionization loss 电离损失ionization potential 电离电势ionization power 致电离能力ionization rate 电离率ionization vacuumgage 电离真空计ionized atom 电离原子ionized layer 电离层ionizer 电离装置ionizing energy 电离能量ionizing power 致电离能力ionizing radiation 电离线ionoluminescence 离子发光ionometer离子计ionosphere电离层ionospheric disturbance电离层扰动ionospheric storm 电离层暴iras object iras 天体iridescence 虹色iridium 铱iris 可变光栏iris diaphragm锁定光栏iris type accelerator guide 隔阂型加快波导管iron 铁iron constantan thermocouple 铁康铜热电偶iron group elements 铁族元素iron loss 铁耗irradiation 辐照irradiation damage 辐照损害irradiation hardening 辐照硬化irradiation reactor 辐照用堆irreducible representation 不行约表示irregular galaxy 不规则星系irregular nebula 不规则星云irregular reflection 不规则反射irregular variable 不规则变星irreversibility 不行逆性irreversible process 不行逆过程irreversible reaction 不行逆反响irrotational field 非旋场isentrope 等熵线isentropic analysis 等熵剖析isentropic surface 等熵面ising model 伊辛模型isoanomalous line 等异样线isobar 等压线isobaric 等压的isobaric analog resonance同质异位素相像共振isobaric analog state 同质异位素相像态isobaric process 等压过程isobaric surface 等压面isocandle diagram 等烛光图isochor 等容线isochromatic 等色的isochromatic line 等色线isochromatic surface 等色面isochrone 等时线isochronism 等时性isochronous cyclotron 等时性盘旋加快器isoclinal 等倾线isoclinal line 等倾线isoclinic line 等倾线isodiaphere 同差素isodynamic line 等力线isoelectric point 等电点isogon 等偏线isolated point 孤点isolation 隔绝isolator 隔绝器绝缘体isolux curve 等照度线isomagnetism 等偏isomer 同质异能素isomer shift 同质异能位移isomeric state 同质异能态isomeric transition 同质异能跃迁isomerism 同质异能性isomerization energy 同质异能化能isometric process 等容过程isomorphism 同构isopycnic 等密度的isopycnic line 等密度线isospace 电荷空间isospin 同位旋isostasy 地壳均衡说isostere 等比容线isosteric molecule 电子等排分子isotherm 等温线isothermal 等温的isothermal atmosphere 等温大气isothermal change 等温变化isothermal equilibrium 等温均衡isothermal expansion 等温膨胀isothermal process 等温过程isotone 同中子素isotope 同位素isotope analysis 同位素剖析isotope effect 同位素效应isotope incoherence 同位素非相关性isotope separation 同位素分别isotope separator 同位素分别器isotope shift 同位素位移isotopic abundance 同位素丰度isotopic dating 同位素测年纪isotopic invariance 同位旋不变性isotopic spin同位旋isotopic tracer 示踪同位素isotropic scattering 蛤同性散射isotropic turbulence 蛤同性湍流isotropic universe 蛤同性宇宙isotropy 蛤同性iterative method 迭代法itinerant electron 巡回电子itinerant electron magnetism 遍历电子磁性。
胶体与界面化学英文5Static and Dynamic Light Scattering and Other Radiation Scattering
establish: the information on the diffusion coefficients of the particles, particle size, particles size distribution and etc.
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§ 5.3 Scattering by small particles: Theory of Rayleigh scattering
1. Scattering by single molecules and gases
light
transmitted light
absorption light scattering light
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(1) Rayleigh theory
A. The scattering centers are small in dimension compared to the wavelength of the radiation (about 1/20). B. The refractive index gradient (dn/dc) is not very large. C.The particles moves independently (exp. gas).
At sunset, we see mostly transmitted light. Since the blue has been most extensively removed from sunset light by scattering, the sky appears red at sunset.
核专业英语背诵材料2.0
Unit 1Helium---------------------氦uranium------------铀Gaseous state-----------气态的artificially------------人工的The perfect gas law------理想气体定律Boltzmann constant--- 玻尔兹曼常数neutrons --------------中子electrostatic -------静电的,静电学的Specific heat capacity--- 比热容Plank constant---------普朗克常量Fission----------------裂变fusion-----------------聚变Maxwellian distribution--麦克斯韦分布microscopic------------微观的Macroscopic-----------宏观的quantum number-------量子数Laser-----------------激光deuterium--------------氘Tritium----------------氚deuteron---------------氘核Trition----------------氚核atomic mass unit------原子质量单位Avogadro’s number----阿伏伽德罗常数binding energy----------结合能Substance-------------物质internal-----------------内部的Spontaneously --------自发地circular-----------------循环的Electronic ------------电子的neutral-----------------中性的Qualitative -----------定性的dissociation-------------分解分离Disrupt--------------使分裂A complete understanding of the microscopic structure of matter and the exact nature of the forces acting (作用力的准确性质) is yet to be realized. However, excellent models have been developed to predict behavior to an adequate degree of accuracy for most practical purposes. These models are descriptive or mathematical often based on analogy with large-scale process, on experimental data, or on advanced theory.一个完整的理解物质的微观结构和力的确切性质(作用力的准确性质)尚未实现。
哈佛大学Capasso教授小组研究用界面位相突变的超材料实现超常折射的论文
Conventional optical components rely on gradual phase shifts accumulated during light propagation to shape light beams. New degrees of freedom are attained by introducing abrupt phase changes over the scale of the wavelength. A two-dimensional array of optical resonators with spatially varying phase response and sub-wavelength separation can imprint such phase discontinuities on propagating light as it traverses the interface between two media. Anomalous reflection and refraction phenomena are observed in this regime in optically thin arrays of metallic antennas on silicon with a linear phase variation along the interface, in excellent agreement with generalized laws derived from Fermat’s principle. Phase discontinuities provide great flexibility in the design of light beams as illustrated by the generation of optical vortices using planar designer metallic interfaces. The shaping of the wavefront of light by optical components such as lenses and prisms, as well as diffractive elements like gratings and holograms, relies on gradual phase changes accumulated along the optical path. This approach is generalized in transformation optics (1, 2) which utilizesmetamaterials to bend light in unusual ways, achieving suchphenomena as negative refraction, subwavelength-focusing,and cloaking (3, 4) and even to explore unusual geometries ofspace-time in the early universe (5). A new degree of freedomof controlling wavefronts can be attained by introducingabrupt phase shifts over the scale of the wavelength along theoptical path, with the propagation of light governed byFermat’s principle. The latter states that the trajectory takenbetween two points A and B by a ray of light is that of leastoptical path, ()B A n r dr ∫r , where ()n r r is the local index of refraction, and readily gives the laws of reflection and refraction between two media. In its most general form,Fermat’s principle can be stated as the principle of stationaryphase (6–8); that is, the derivative of the phase()B A d r ϕ∫r accumulated along the actual light path will be zero with respect to infinitesimal variations of the path. We show that an abrupt phase delay ()s r Φr over the scale of the wavelength can be introduced in the optical path by suitably engineering the interface between two media; ()s r Φr depends on the coordinate s r r along the interface. Then the total phase shift ()B s A r k dr Φ+⋅∫r r r will be stationary for the actual path that light takes; k r is the wavevector of the propagating light. This provides a generalization of the laws of reflection and refraction, which is applicable to a wide range of subwavelength structured interfaces between two media throughout the optical spectrum. Generalized laws of reflection and refraction. The introduction of an abrupt phase delay, denoted as phase discontinuity, at the interface between two media allows us to revisit the laws of reflection and refraction by applying Fermat’s principle. Consider an incident plane wave at an angle θi . Assuming that the two rays are infinitesimally close to the actual light path (Fig. 1), then the phase difference between them is zero ()()()s in s in 0o i i o t t kn d x d kn d x θθ+Φ+Φ−+Φ=⎡⎤⎡⎤⎣⎦⎣⎦ (1) where θt is the angle of refraction, Φ and Φ+d Φ are, respectively, the phase discontinuities at the locations where the two paths cross the interface, dx is the distance between the crossing points, n i and n t are the refractive indices of thetwo media, and k o = 2π/λo , where λo is the vacuumwavelength. If the phase gradient along the interface isdesigned to be constant, the previous equation leads to thegeneralized Snell’s law of refraction Light Propagation with Phase Discontinuities: Generalized Laws of Reflection and RefractionNanfang Yu ,1 Patrice Genevet ,1,2 Mikhail A. Kats ,1 Francesco Aieta ,1,3 Jean-Philippe Tetienne ,1,4 Federico Capasso ,1 Zeno Gaburro 1,51School of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts 02138, USA. 2Institute for Quantum Studies and Department of Physics, Texas A&M University, College Station, Texas 77843, USA. 3Dipartimento di Fisica e Ingegneria dei Materiali e del Territorio, Università Politecnica delle Marche, via Brecce Bianche, 60131 Ancona, Italy. 4Laboratoire de Photonique Quantique et Moléculaire, Ecole Normale Supérieure de Cachan and CNRS, 94235 Cachan, France. 5Dipartimento di Fisica, Università degli Studi di Trento, via Sommarive 14, 38100 Trento, Italy.o n S e p t e m b e r 1, 2011w w w .s c i e n c e m a g .o r g D o w n l o a d e d f r o m()()sin sin 2o t t i i d n n dx λθθπΦ−= (2) Equation 2 implies that the refracted ray can have an arbitrary direction, provided that a suitable constant gradient of phase discontinuity along the interface (d Φ/dx ) is introduced. Note that because of the non-zero phase gradient in this modified Snell’s law, the two angles of incidence ±θi lead to different values for the angle of refraction. As a consequence there are two possible critical angles for total internal reflection, provided that n t < n i : arcsin 2to c i i n d n n dx λθπ⎛⎞Φ=±−⎜⎟⎝⎠ (3)Similarly, for the reflected light we have ()()sin sin 2o r i i d n dx λθθπΦ−= (4) where θr is the angle of reflection. Note the nonlinear relationbetween θr and θI , which is markedly different fromconventional specular reflection. Equation 4 predicts that there is always a critical incidence angle arcsin 12o c i d n dx λθπ⎛⎞Φ′=−⎜⎟⎝⎠ (5) above which the reflected beam becomes evanescent. In the above derivation we have assumed that Φ is a continuous function of the position along the interface; thus all the incident energy is transferred into the anomalous reflection and refraction. However because experimentally we use an array of optically thin resonators with sub-wavelength separation to achieve the phase change along the interface, this discreteness implies that there are also regularly reflected and refracted beams, which follow conventional laws of reflection and refraction (i.e., d Φ/dx =0 in Eqs. 2 and 4). The separation between the resonators controls the relative amount of energy in the anomalously reflected and refracted beams. We have also assumed that the amplitudes of the scattered radiation by each resonator are identical, so that the refracted and reflected beams are plane waves. In the next section we will show by simulations, which represent numerical solutions of Maxwell’s equations, how indeed one can achieve the equal-amplitude condition and the constant phase gradient along the interface by suitable design of the resonators. Note that there is a fundamental difference between the anomalous refraction phenomena caused by phase discontinuities and those found in bulk designer metamaterials, which are caused by either negative dielectric permittivity and negative magnetic permeability or anisotropic dielectric permittivity with different signs ofpermittivity tensor components along and transverse to thesurface (3, 4).Phase response of optical antennas. The phase shift between the emitted and the incident radiation of an optical resonator changes appreciably across a resonance. By spatially tailoring the geometry of the resonators in an array and hence their frequency response, one can design the phase shift along the interface and mold the wavefront of the reflected and refracted beams in nearly arbitrary ways. The choice of the resonators is potentially wide-ranging, fromelectromagnetic cavities (9, 10), to nanoparticles clusters (11,12) and plasmonic antennas (13, 14). We concentrated on thelatter, due to their widely tailorable optical properties (15–19)and the ease of fabricating planar antennas of nanoscalethickness. The resonant nature of a rod antenna made of aperfect electric conductor is shown in Fig. 2A (20).Phase shifts covering the 0 to 2π range are needed toprovide full control of the wavefront. To achieve the requiredphase coverage while maintaining large scatteringamplitudes, we utilized the double resonance properties of V-shaped antennas, which consist of two arms of equal length h connected at one end at an angle Δ (Fig. 2B). We define twounit vectors to describe the orientation of a V-antenna: ŝalong the symmetry axis of the antenna and â perpendicular to ŝ (Fig. 2B). V-antennas support “symmetric” and “antisymmetric” modes (middle and right panels of Fig. 2B),which are excited by electric-field components along ŝ and â axes, respectively. In the symmetric mode, the current distribution in each arm approximates that of an individual straight antenna of length h (Fig. 2B middle panel), and therefore the first-order antenna resonance occurs at h ≈ λeff /2, where λeff is the effective wavelength (14). In the antisymmetric mode, the current distribution in each arm approximates that of one half of a straight antenna of length 2h (Fig. 2B right panel), and the condition for the first-order resonance of this mode is 2h ≈ λeff /2.The polarization of the scattered radiation is the same as that of the incident light when the latter is polarized along ŝ or â. For an arbitrary incident polarization, both antenna modes are excited but with substantially different amplitude and phase due to their distinctive resonance conditions. As a result, the scattered light can have a polarization different from that of the incident light. These modal properties of the V-antennas allow one to design the amplitude, phase, and polarization state of the scattered light. We chose the incident polarization to be at 45 degrees with respect to ŝ and â, so that both the symmetric and antisymmetric modes can be excited and the scattered light has a significant component polarized orthogonal to that of the incident light. Experimentally this allows us to use a polarizer to decouple the scattered light from the excitation.o n S e p t e m b e r 1, 2011w w w .s c i e n c e m a g .o r g Do w n l o a d e d f r o mAs a result of the modal properties of the V-antennas and the degrees of freedom in choosing antenna geometry (h and Δ), the cross-polarized scattered light can have a large range of phases and amplitudes for a given wavelength λo; see Figs. 2D and E for analytical calculations of the amplitude and phase response of V-antennas assumed to be made of gold rods. In Fig. 2D the blue and red dashed curves correspond to the resonance peaks of the symmetric and antisymmetric mode, respectively. We chose four antennas detuned from the resonance peaks as indicated by circles in Figs. 2D and E, which provide an incremental phase of π/4 from left to right for the cross-polarized scattered light. By simply taking the mirror structure (Fig. 2C) of an existing V-antenna (Fig. 2B), one creates a new antenna whose cross-polarized emission has an additional π phase shift. This is evident by observing that the currents leading to cross-polarized radiation are π out of phase in Figs. 2B and C. A set of eight antennas were thus created from the initial four antennas as shown in Fig. 2F. Full-wave simulations confirm that the amplitudes of the cross-polarized radiation scattered by the eight antennas are nearly equal with phases in π/4 increments (Fig. 2G).Note that a large phase coverage (~300 degrees) can also be achieved using arrays of straight antennas (fig. S3). However, to obtain the same range of phase shift their scattering amplitudes will be significantly smaller than those of V-antennas (fig. S3). As a consequence of its double resonances, the V-antenna instead allows one to design an array with phase coverage of 2π and equal, yet high, scattering amplitudes for all of the array elements, leading to anomalously refracted and reflected beams of substantially higher intensities.Experiments on anomalous reflection and refraction. We demonstrated experimentally the generalized laws of reflection and refraction using plasmonic interfaces constructed by periodically arranging the eight constituent antennas as explained in the caption of Fig. 2F. The spacing between the antennas should be sub-wavelength to provide efficient scattering and to prevent the occurrence of grating diffraction. However it should not be too small; otherwise the strong near-field coupling between neighboring antennas would perturb the designed scattering amplitudes and phases.A representative sample with the densest packing of antennas, Γ= 11 µm, is shown in Fig. 3A, where Γ is the lateral period of the antenna array. In the schematic of the experimental setup (Fig. 3B), we assume that the cross-polarized scattered light from the antennas on the left-hand side is phase delayed compared to the ones on the right. By substituting into Eq. 2 -2π/Γ for dΦ/dx and the refractive indices of silicon and air (n Si and 1) for n i and n t, we obtain the angle of refraction for the cross-polarized lightθt,٣= arcsin[n Si sin(θi) – λo/Γ] (6) Figure 3C summarizes the experimental results of theordinary and the anomalous refraction for six samples with different Γ at normal incidence. The incident polarization isalong the y-axis in Fig. 3A. The sample with the smallest Γcorresponds to the largest phase gradient and the mostefficient light scattering into the cross polarized beams. We observed that the angles of anomalous refraction agree wellwith theoretical predictions of Eq. 6 (Fig. 3C). The same peak positions were observed for normal incidence withpolarization along the x-axis in Fig. 3A (Fig. 3D). To a good approximation, we expect that the V-antennas were operating independently at the packing density used in experiments (20). The purpose of using a large antenna array (~230 µm ×230 µm) is solely to accommodate the size of the plane-wave-like excitation (beam radius ~100 µm). The periodic antenna arrangement is used here for convenience, but is notnecessary to satisfy the generalized laws of reflection and refraction. It is only necessary that the phase gradient isconstant along the plasmonic interface and that the scattering amplitudes of the antennas are all equal. The phaseincrements between nearest neighbors do not need to be constant, if one relaxes the unnecessary constraint of equal spacing between nearest antennas.Figures 4A and B show the angles of refraction and reflection, respectively, as a function of θi for both thesilicon-air interface (black curves and symbols) and the plasmonic interface (red curves and symbols) (20). In therange of θi = 0-9 degrees, the plasmonic interface exhibits “negative” refraction and reflection for the cross-polarized scattered light (schematics are shown in the lower right insetsof Figs. 4A and B). Note that the critical angle for totalinternal reflection is modified to about -8 and +27 degrees(blue arrows in Fig. 4A) for the plasmonic interface in accordance with Eq. 3 compared to ±17 degrees for thesilicon-air interface; the anomalous reflection does not exist beyond θi = -57 degrees (blue arrow in Fig. 4B).At normal incidence, the ratio of intensity R between the anomalously and ordinarily refracted beams is ~ 0.32 for the sample with Γ = 15 µm (Fig. 3C). R rises for increasingantenna packing densities (Figs. 3C and D) and increasingangles of incidence (up to R≈ 0.97 at θi = 14 degrees (fig.S1B)). Because of the experimental configuration, we are notable to determine the ratio of intensity between the reflected beams (20), but we expect comparable values.Vortex beams created by plasmonic interfaces. To demonstrate the versatility of the concept of interfacial phase discontinuities, we fabricated a plasmonic interface that isable to create a vortex beam (21, 22) upon illumination by normally incident linearly polarized light. A vortex beam hasa helicoidal (or “corkscrew-shaped”) equal-phase wavefront. Specifically, the beam has an azimuthal phase dependenceexp(i lφ) with respect to the beam axis and carries an orbitalonSeptember1,211www.sciencemag.orgDownloadedfromangular momentum of L l=h per photon (23), where the topological charge l is an integer, indicating the number of twists of the wavefront within one wavelength; h is the reduced Planck constant. These peculiar states of light are commonly generated using a spiral phase plate (24) or a computer generated hologram (25) and can be used to rotate particles (26) or to encode information in optical communication systems (27).The plasmonic interface was created by arranging the eight constituent antennas as shown in Figs. 5A and B. The interface introduces a spiral-like phase delay with respect to the planar wavefront of the incident light, thereby creating a vortex beam with l = 1. The vortex beam has an annular intensity distribution in the cross-section, as viewed in a mid-infrared camera (Fig. 5C); the dark region at the center corresponds to a phase singularity (22). The spiral wavefront of the vortex beam can be revealed by interfering the beam with a co-propagating Gaussian beam (25), producing a spiral interference pattern (Fig. 5E). The latter rotates when the path length of the Gaussian beam was changed continuously relative to that of the vortex beam (movie S1). Alternatively, the topological charge l = 1 can be identified by a dislocated interference fringe when the vortex and Gaussian beams interfere with a small angle (25) (Fig. 5G). The annular intensity distribution and the interference patterns were well reproduced in simulations (Figs. D, F, and H) by using the calculated amplitude and phase responses of the V-antennas (Figs. 2D and E).Concluding remarks. Our plasmonic interfaces, consisting of an array of V-antennas, impart abrupt phase shifts in the optical path, thus providing great flexibility in molding of the optical wavefront. This breaks the constraint of standard optical components, which rely on gradual phase accumulation along the optical path to change the wavefront of propagating light. We have derived and experimentally confirmed generalized reflection and refraction laws and studied a series of intriguing anomalous reflection and refraction phenomena that descend from the latter: arbitrary reflection and refraction angles that depend on the phase gradient along the interface, two different critical angles for total internal reflection that depend on the relative direction of the incident light with respect to the phase gradient, critical angle for the reflected light to be evanescent. We have also utilized a plasmonic interface to generate optical vortices that have a helicoidal wavefront and carry orbital angular momentum, thus demonstrating the power of phase discontinuities as a design tool of complex beams. The design strategies presented in this article allow one to tailor in an almost arbitrary way the phase and amplitude of an optical wavefront, which should have major implications for transformation optics and integrated optics. We expect that a variety of novel planar optical components such as phased antenna arrays in the optical domain, planar lenses,polarization converters, perfect absorbers, and spatial phase modulators will emerge from this approach.Antenna arrays in the microwave and millimeter-waveregion have been widely used for the shaping of reflected and transmitted beams in the so-called “reflectarrays” and “transmitarrays” (28–31). There is a connection between thatbody of work and our results in that both use abrupt phase changes associated with antenna resonances. However the generalization of the laws of reflection and refraction wepresent is made possible by the deep-subwavelengththickness of our optical antennas and their subwavelength spacing. It is this metasurface nature of the plasmonicinterface that distinguishes it from reflectarrays and transmitarrays. The last two cannot be treated as an interfacein the effective medium approximation for which one canwrite down the generalized laws, because they typicallyconsist of a double layer structure comprising a planar arrayof antennas, with lateral separation larger than the free-space wavelength, and a ground plane (in the case of reflectarrays)or another array (in the case of transmitarrays), separated by distances ranging from a fraction of to approximately one wavelength. In this case the phase along the plane of the array cannot be treated as a continuous variable. This makes it impossible to derive for example the generalized Snell’s lawin terms of a phase gradient along the interface. This generalized law along with its counterpart for reflectionapplies to the whole optical spectrum for suitable designer interfaces and it can be a guide for the design of new photonic devices.References and Notes1. J. B. Pendry, D. Schurig, D. R. Smith, “Controllingelectromagnetic fields,” Science 312, 1780 (2006).2. U. Leonhardt, “Optical conformal mapping,” Science 312,1777 (2006).3. W. Cai, V. Shalaev, Optical Metamaterials: Fundamentalsand Applications (Springer, 2009)4. N. Engheta, R. W. Ziolkowski, Metamaterials: Physics andEngineering Explorations (Wiley-IEEE Press, 2006).5. I. I Smolyaninov, E. E. Narimanov, Metric signaturetransitions in optical metamaterials. Phys. Rev. Lett.105,067402 (2010).6. S. D. Brorson, H. A. Haus, “Diffraction gratings andgeometrical optics,” J. Opt. Soc. Am. B 5, 247 (1988).7. R. P. Feynman, A. R. Hibbs, Quantum Mechanics andPath Integrals (McGraw-Hill, New York, 1965).8. E. Hecht, Optics (3rd ed.) (Addison Wesley PublishingCompany, 1997).9. H. T. Miyazaki, Y. Kurokawa, “Controlled plasmonnresonance in closed metal/insulator/metal nanocavities,”Appl. Phys. Lett. 89, 211126 (2006).onSeptember1,211www.sciencemag.orgDownloadedfrom10. D. Fattal, J. Li, Z. Peng, M. Fiorentino, R. G. Beausoleil,“Flat dielectric grating reflectors with focusing abilities,”Nature Photon. 4, 466 (2010).11. J. A. Fan et al., “Self-assembled plasmonic nanoparticleclusters,” Science 328, 1135 (2010).12. B. Luk’yanchuk et al., “The Fano resonance in plasmonicnanostructures and metamaterials,” Nature Mater. 9, 707 (2010).13. R. D. Grober, R. J. Schoelkopf, D. E. Prober, “Opticalantenna: Towards a unity efficiency near-field opticalprobe,” Appl. Phys. Lett. 70, 1354 (1997).14. L. Novotny, N. van Hulst, “Antennas for light,” NaturePhoton. 5, 83 (2011).15. Q. Xu et al., “Fabrication of large-area patternednanostructures for optical applications by nanoskiving,”Nano Lett. 7, 2800 (2007).16. M. Sukharev, J. Sung, K. G. Spears, T. Seideman,“Optical properties of metal nanoparticles with no center of inversion symmetry: Observation of volume plasmons,”Phys. Rev. B 76, 184302 (2007).17. P. Biagioni, J. S. Huang, L. Duò, M. Finazzi, B. Hecht,“Cross resonant optical antenna,” Phys. Rev. Lett. 102,256801 (2009).18. S. Liu et al., “Double-grating-structured light microscopyusing plasmonic nanoparticle arrays,” Opt. Lett. 34, 1255 (2009).19. J. Ginn, D. Shelton, P. Krenz, B. Lail, G. Boreman,“Polarized infrared emission using frequency selectivesurfaces,” Opt. Express 18, 4557 (2010).20. Materials and methods are available as supportingmaterial on Science Online.21. J. F. Nye, M. V. Berry, “Dislocations in wave trains,”Proc. R. Soc. Lond. A. 336, 165 (1974).22. M. Padgett, J. Courtial, L. Allen, “Ligh’'s orbital angularmomentum,” Phys. Today 57, 35 (2004).23. L. Allen, M. W. Beijersbergen, R. J. C. Spreeuw, J. P.Woerdman, “Orbital angular momentum of light and the transformation of Laguerre-Gaussian laser modes,” Phys.Rev. A, 45, 8185 (1992).24. M. W. Beijersbergen, R. P. C. Coerwinkel, M. Kristensen,J. P. Woerdman, “Helical-wavefront laser beams produced with a spiral phaseplate,” Opt. Commun. 112, 321 (1994).25. N. R. Heckenberg, R. McDuff, C. P. Smith, A. G. White,“Generation of optical phase singularities by computer-generated holograms,” Opt. Lett. 17, 221 (1992).26. H. He, M. E. J. Friese, N. R. Heckenberg, H. Rubinsztein-Dunlop, “Direct observation of transfer of angularmomentum to absorptive particles from a laser beam witha phase singularity,” Phys. Rev. Lett. 75, 826 (1995).27. G. Gibson et al, “Free-space information transfer usinglight beams carrying orbital angular momentum,” Opt.Express 12, 5448 (2004). 28. D. M. Pozar, S. D. Targonski, H. D. Syrigos, “Design ofmillimeter wave microstrip reflectarrays,” IEEE Trans.Antennas Propag. 45, 287 (1997).29. J. A. Encinar, “Design of two-layer printed reflectarraysusing patches of variable size,” IEEE Trans. AntennasPropag. 49, 1403 (2001).30. C. G. M. Ryan et al., “A wideband transmitarray usingdual-resonant double square rings,” IEEE Trans. AntennasPropag. 58, 1486 (2010).31. P. Padilla, A. Muñoz-Acevedo, M. Sierra-Castañer, M.Sierra-Pérez, “Electronically reconfigurable transmitarrayat Ku band for microwave applications,” IEEE Trans.Antennas Propag. 58, 2571 (2010).32. H. R. Philipp, “The infrared optical properties of SiO2 andSiO2 layers on silicon,” J. Appl. Phys. 50, 1053 (1979).33. R. W. P. King, The Theory of Linear Antennas (HarvardUniversity Press, 1956).34. J. D. Jackson, Classical Electrodynamics (3rd edition)(John Wiley & Sons, Inc. 1999) pp. 665.35. E. D. Palik, Handbook of Optical Constants of Solids(Academic Press, 1998).36. I. Puscasu, D. Spencer, G. D. Boreman, “Refractive-indexand element-spacing effects on the spectral behavior ofinfrared frequency-selective surfaces,” Appl. Opt. 39,1570 (2000).37. G. W. Hanson, “On the applicability of the surfaceimpedance integral equation for optical and near infraredcopper dipole antennas,” IEEE Trans. Antennas Propag.54, 3677 (2006).38. C. R. Brewitt-Taylor, D. J. Gunton, H. D. Rees, “Planarantennas on a dielectric surface,” Electron. Lett. 17, 729(1981).39. D. B. Rutledge, M. S. Muha, “Imaging antenna arrays,”IEEE Trans. Antennas Propag. 30, 535 (1982). Acknowledgements: The authors acknowledge helpful discussion with J. Lin, R. Blanchard, and A. Belyanin. Theauthors acknowledge support from the National ScienceFoundation, Harvard Nanoscale Science and EngineeringCenter (NSEC) under contract NSF/PHY 06-46094, andthe Center for Nanoscale Systems (CNS) at HarvardUniversity. Z. G. acknowledges funding from theEuropean Communities Seventh Framework Programme(FP7/2007-2013) under grant agreement PIOF-GA-2009-235860. M.A.K. is supported by the National ScienceFoundation through a Graduate Research Fellowship.Harvard CNS is a member of the NationalNanotechnology Infrastructure Network (NNIN). TheLumerical FDTD simulations in this work were run on theOdyssey cluster supported by the Harvard Faculty of Artsand Sciences (FAS) Sciences Division ResearchComputing Group.onSeptember1,211www.sciencemag.orgDownloadedfrom。
Atomic and molecular vibrations correspond to excited :原子和分子的振动对应激43页
• Quasi-elastic scattering – the wavelength (frequency) of the scattered light shifts (e.g., in moving matter due to Doppler effects)
• Multiple scattering: prevails in optically thick, strongly scattering and non-absorbing media
• Photons may be scattered hundreds of times before emerging
x 2r
• r is the radius of a spherical particle, λ is wavelength
• (3) The particelative to the surrounding medium: the complex refractive index
More types of scattering
• Single scattering: photons scattered only once • Prevails in optically thin media (τ << 1), since photons have a high
probability of exiting the medium (e.g., a thin cloud) before being scattered again • Also favored in strongly absorbing media (ω << 1)
Atomic and molecular vibrations correspond to excited :原子和分子的振动对应激
nБайду номын сангаас (n = nr+ i ni)
0 0 0 0 0 0 -0.79 -0.006
(λ = 550 nm) (λ = 550 nm) (λ = 550 nm)
The most significant absorbing component of atmospheric particles is elemental carbon (soot); reflected in the large value of the imaginary part of the refractive index.
Horizontally polarized Unpolarized
Rayleigh and Mie scattering
• Scattering determines the brightness and color of the sky
Variation in sky brightness
• The horizon sky is usually brighter than the zenith sky • This is a result of single scattering (zenith) vs. multiple scattering (horizon)
Rayleigh scattering
Atmospheric composition: N2 (78%), O2 (21%), Ar (1%) Size of N2 molecule: 0.31 nm Size of O2 molecule: 0.29 nm Size of Ar molecule: 0.3 nm Visible wavelengths ~400-700 nm
Exploring the World of Polarized Light
58CHINA TODAYsoCieTy/liFe / new VisTasON July 21, 2017, the famous aca-demic journal Physical Review Letters published a paper by a research team led by ProfessorMa Hui from Tsinghua University, indi-cating the great achievements made in polarized light scattering.Polarized light may sound new to many people. Actually, it has already been put into use. For example, the liq-uid crystal display (LCD) of electronic watches, 3D movies, and glare-reducing polarized sunglasses, to name just a few.In addition, polarization techniques are potentially powerful tools for the early diagnosis of cancer, identification of marine algae and plankton, and clas-sification and tracing of gas particles in air pollutants.An Eye-opening DiscoveryWhen we put on a pair of 3D glasses when watching movies, the stereoscopic images will instantly pop up. By far, this may be the most widely known applica-tion of polarized light.According to Professor Ma Hui, polar-ization is a major feature of light. People live in a world full of polarized light but are unaware of it. The study of polar-ized light enables people to understandBy special correspondentHUANG YUANJUNExploring the World of Polarized LightThe polarization imaging technique has been applied to liquid crystal display and 3D glasses, and has shown many potential applications in medical diagnosis, marine life identification, and air pollution tracing.the world from a new perspective. “Just as telescopes and microscopes assist people in exploring the universe and the microscopic world, this technique helps people obtain information using optical methods. For instance, a camera with a polarization sensor can help detect cancer cells, which is a huge technologi-cal breakthrough for early cancer detec-tion,” he said.Fundamental research is the source of innovation. The breakthroughs made by Ma Hui and his team in polarized light can be attributed to a new theo-retical algorithm and relevant calcula-tion model they developed. “The calcu-lation speed and capacity of our newalgorithm are very remarkable,” Ma Hui said. Almost all the subsequent break-throughs by his team are based on this algorithm.Application in Three Major FieldsFirstly, the polarization technique can be applied to optical detection and imaging in biomedicine. “In biomedical diagnosis and treatment, optical imag-ing within living organism is very dif-ficult due to light scattering and opaque biological tissues. Knowing this, the most direct way to improve imaging is to avoid light scattering.” According to Ma Hui, a polarization technique can reduce the negative effect of scatter-ing. This technique, once applied, will improve the imaging resolution of epi-dermal tissue and help doctors detect cancerous tissues; on the other hand, it can help people acquire more informa-tion about the sample microstructure, detect abnormalities of biological tis-sues, and make pathological diagnosis possible. Moreover, as a non-destructive detection method for organisms, it is safe, timely, and effective.At present, Ma Hui and his team have achieved satisfactory imaging in lesion location by using this polariza-tion technique. In addition, comparedwith traditional time-consuming dyedProfessor Ma Hui in his office.Copyright©博看网 . All Rights Reserved.pathological section, real-time diagnosis can be displayed online direct from the operating table. By measuring the can-cerous tissues together with the hospi-tal, the team members have obtained a crucial scientific basis to prove that full polarization imaging is indeed likely to be used for the quantitative representa-tion of cancerous tissues. In 2015, with the support of the national major scien-tific instrument development program, they researched and developed the full polarization imaging microscope, push-ing for industrialized application. Secondly, this polarization technique can be applied to marine detection. As the attenuation and scattering of light are much stronger in seawater than in the atmosphere, visibility in water is much worse, making marine detection quite inconvenient. In re-cent years, with the support of major scientific research programs in China, a new oceanographic instrument was developed. Thanks to the polarization technique, the visibility and imaging of marine detection was improved and typical algae differentiated.The new oceanographic instrument can be used for algae or sea particles detection, red tide warning alerts, and ecological environmental monitoring. For instance, scientists have various conjectures about global warming. “Al-gae have a great effect on environmen-tal changes, scientists can figure out the cause of global warming by monitoring various types of algae and measuring algae concentration in different waters,”said Ma Hui.Thirdly, polarization technology can be applied to air pollution control. Over the past couple of years, by coop-erating with enterprises and top insti-tutions of environmental monitoring, Ma Hui and his team are committed to developing an instrument to count, classify, and source analyze Particulate Matter (PM) in the air.According to Ma Hui, people used toevaluate air quality by measuring thePM such as PM2.5 and PM10. However,his team aims to tell people what thesePMs are, where they come from, andhow they change with time. “By adopt-ing physical methods, besides traditionalmeteorological observation and chemi-cal analysis, we can build a database onphysical science,” commented Ma Hui.“By having a speed advantage over theoptical method, a rapid evaluation sys-tem for air pollution can also be built.”Until now, few people have carriedout polarization research and there arefew applications. The research find-ings by Ma Hui and his team still needtime to be used in industries, but theconcrete progress has so far convincedpeople that their polarization techniquehas broad application prospects for avariety of areas.InterdisciplinaryAcademic TeamThe Graduate School at Shenzhen,Tsinghua University has two distinctivefeatures. One is industrial cooperation,and the other is the cross-disciplinarycomposition.“The two features are interconnectedwith each other,” Ma Hui said. The com-mercialization of research findings isa process that includes stages such asfundamental research, applied research,technological development, engineeringand industrialization. Each stage hasdifferent operation rules, bottlenecksthat impede synergy innovation, andfactor allocation barriers. An interdisci-plinary team can help link this “innova-tion chain” and promote the applicationof research findings.Ma Hui and his team have always at-tached great importance to the applica-tion of their research findings. The teammembers are teachers and studentsmajoring in physics, electronics, medi-cine, chemistry, and materials. Theycan share their ideas and strengths andhope to apply their findings to the fieldsof biomedicine, marine detection, andair pollution, and others. CProfessor Ma and his R&D team in Guangdong Province.Copyright©博看网 . All Rights Reserved.59March 2018。
灯具行业的必备中英词汇
电工术语照明1.电磁辐射——electromagnetic radiation2.光学辐射——optical radiation3.可见辐射——visible radiation4.红外辐射——infrared radiation5.紫外辐射——ultraviolet radiation6.单色辐射——monochromatic radiation7.光谱——spectrum8.光谱线——spectral line9.偏振辐射——polarized radiation10.相干辐射——coherent radiation11.干涉——interference12.衍射——diffraction13.波长——wavelength14.波数——wave number15.光谱的——spectral16.光谱密集度——spectral concentration17.光谱分布——spectral concentration18.相对光谱分布——relative spectral distribution19.电源——point source20.球面度——steradian21.辐射量光度量和光子量及其单位——radiation luminous and photon quantities and theirunits22.光刺激——light stimulus23.光谱光视效率——spectral luminous efficiency24.CIE标准光度观测者——CIE standard photometric observer25.辐通量——radiant flux26.辐射功率——radiant power27.光通量——luminous flux28.光子通量——photon flux29.辐射通量——radiant energy30.光量——quantity of light31.光子数——number of photon ;photon number32.辐射强度——radiant intensity33.发光强度——luminous intensity34.光子强度——photonintensity35.几何因子——geometric extent36.辐射亮度——radiance37.光亮度——luminance38.光子辐亮度——photon radiance39.辐射强度——irradiance40.照度——illuminance41.光子辐照度——photon irradiance42.球面辐照度;辐射流率——spherical irradiance ;radiant fluence rate43.柱面辐照度——cylindrical irradiance44.曝辐射量——radiant exposure45.曝光量——luminous exposure;46.曝光子量——photon exposure47.球面曝辐射量——radiant spherical exposure;radiant fluence48.柱面曝辐射量——radiant cylindrical exposure49.辐射出射度——radiant exitance50.光出射度——luminous exitance51.光子出射度——photon exitance52.坎德拉——candela53.流明——lumen54.勒克斯——Lux55.坎德拉每平方米——candela per square metre56.辐射效率——radiant efficiency57.光源的光视效能——luminous efficacy of a source58.辐射的光视效能——luminous efficacy of radiation59.光视效率——luminous efficiency60.等效(光)亮度——equivalent luminous61.点耀度——point brilliance62.视星等(天体的)——apparent magnitude63.视网膜——retina64.锥状细胞——cones65.柱状细胞——rods66.黄斑——yellow spot;macula lutea67.中央凹——fovea;fovea centralis68.小凹——foveola69.色适应——chromatic adaptation70.明视觉——photopic vision71.暗视觉——scotopic vision72.中间视觉——mesopic vision73.夜盲——hemeralopia;night-blindness74.色觉缺陷——defective colour vision75.普尔金耶现象——Purkinje phenomenon76.方向效应——directional effect77.物体色——object-colour78.表面色——surface colour79.小孔色——aperture colour80.发光色——luminous colour81.非发光色——non-luminous colour82.相关色——related colour83.非相关色——unrelated colour84.非彩色——achromatic colour85.彩色——chromatic colour86.视亮度——brightness87.明亮的——bright88.暗淡的——dim89.明度——lightness90.光亮的——light91.黑暗的——dark92.色调——hue93.单一色调——unitary hue;unique hue94.二元色调——binary hue95.阿布尼现象——Abney phenomenon96.色浓度——chromaticness;colourfulness97.色饱和度——saturation98.彩度——chroma99.视觉分辨力——visual acuity;visual resolution100.调式——accommodation101.对比——contrast102.对比灵敏度——contrast sensitivity103.闪烁——flicker104.融合频率——fusion frequency105.塔尔波特定律——Talbot’law106.眩光——glare107.直接眩光——direct glare108.反射眩光——glare by reflections109.光幕眩光——veiling glare110.不舒适眩光——discomfort glare111.失能眩光——disability glare112.等效光幕亮度——equivalent veiling luminous113.显色性——colour rendering114.参照照明体——reference illuminant115.显色指数——colour rendering index116.CIE1974特殊显色指数——CIE 1974 special colour rendering index 117.CIE1974平均显色指数——CIE1974 general colour rendering index 118.照明体色位移——illuminant colorimetric shift119.适应色位移——adaptive colour shift120.总的色位移——resultant colour shift121.色刺激——colour stimulus122.色刺激函数——colour stimulus function123.相对色刺激函数——relative colour stimulus function124.同色异谱色刺激——metameric stimulus125.同色异谱——metamers126.非彩色刺激——achromatic stimulus127.彩色刺激——chromatic stimulus128.单色刺激——monochromatic stimulus129.光谱刺激——spectral stimulus130.互补色刺激——complementary colour stimulus131.照明体——illuminant132.日光照明体——daylight illuminant133.CIE 标准照明体——CIE standard illuminant134.CIE 标准光源——CIE standard source135.等能光源——equi-energy spectrum;equal energy spectrum136.三色系统——trichromatic systems137.色刺激相加混合——additive mixture of colour stimulus138.色匹配——colour matching139.三色系统——trichromatic system140.参照物刺激——reference colour timulus141.三刺激值——tristimulus value142.色匹配函数——colour-matching functions143.色方程——colour equation144.色空间——colour space145.色立体——colour solid146.色集——colour atlas147.CIE 1931标准色度系(XYZ)——CIE 1931 standard colorimetric system148.CIE 1964 补充标准色度系统——CIE 1964 supplementary standard colorimetric system 149.CIE 色匹配函数——CIE colour-matching function150.CIE 1931标准色度观测者——CIE 1931 standard colorimetric observer151.CIE 1964 补充标准色度观测者——CIE 1964 supplementary standard colorimetric observer152.色品——chromaticity153.色品坐标——chromaticty coordinates154.色品图——chromaticity diagram,155.光谱色的色品坐标——spectral chromaticity coordinates156.光谱轨迹——spectrum locus157.紫色刺激——purple stimulus158.紫色边界——purple boundary159.最佳色刺激——optimal colour stimuli160.普朗克轨迹——Planckian locus161.日光轨迹——daylight locus162.零亮度面——alychne163.主波长——dominant wavelength164.补色波长——complementary wavelength165.纯色——purity166.色度纯度——colorimetric purity167.兴奋纯度——excitation purity168.颜色温度,色度——colour temperature169.相关色温——correlated colour temperature170.均匀颜色空间——uniform colour spaces171.均匀色品标度图——uniform-chromaticity-scale diagram;UCS diagram 172.发射——emission173.热发射——thermal radiation174.黑体——blackbody175.普朗克定律——Planckian’s law176.方向发射率——directional emissivity177.选择性辐射体——selective radiator178.非选择性辐射体——non-selective radiator179.灰体——grey body180.(单色)辐射亮度温度——(monochromatic)radiance temperature 181.分布温度——distribution temperature182.白炽——incandescence183.能级——energy level184.激发——excitation185.发光——luminescence186.光致发光——photoluminescence187.荧光——fluorescence188.余辉——afterglow189.反斯托克斯发光——anti-Stokes luminescence190.磷光——phosphorescence191.场致发光——electroluminescence192.阴极发光——cathodoluminescence193.辐射发光——radioluminescence194.化学发光——chemiluminescence195.生物发光——bioluminescence196.摩擦发光——triboluminescence197.热致发光——thermally activated luminescence ; thermoluminescence 198.发光二极体——lighting emitting diode199.发射——reflection200.透射——transmission201.漫射——diffusion202.散射——scattering203.规则反射——regular reflection204.镜反射——direct transmission205.规则透射——regular transmission206.直透射——direct transmission207.漫反射——diffuse reflection208.漫透射——diffuse transmission209.混合发射——mixed transmission210.各向同性漫反射——isotropic diffuse reflection211.漫射体——diffuser212.完全漫发射体——perfect reflecting diffuser213.完全漫透射体——perfect transmitting diffuser214.透明煤质——transparent medium215.半透明煤质——translucent medium216.不透明煤质——opaque medium217.光度计——photometer218.照度计——illuminance meter219.光度计——luminance meter220.色度计——colorimeter221.闪烁光度计——flicker photometer222.上升时间——rise time223.下降时间——fall time224.光效应——photoeffect225.感光度——actinism226.自发光光源——primary light source227.次极光源——secondary light source228.灯——lamp229.白炽灯——incandescent lamps230.碳丝灯——carbon filament lamp231.金属丝灯——metal filament lamp232.钨丝灯——tungsten filament lamp233.真空白炽灯——vacuum incandescent lamp234.充气白炽灯——gas-filled incandescent lamp235.放电(在气体中)——electric discharge(in a gas)236.辉光放电——glow discharge237.阴极电压降——cathode fall238.正常阴极电压降——normal cathode fall239.异常阴极电压降——abnormal cathode fall240.放电灯——discharge lamp241.负辉光灯——negative-glow lamp242.高强度放电灯——high intensity discharge lamp243.高压汞(蒸汽)灯——high pressure mercury244.自镇流汞灯——blended lamp;self-ballasted245.低压汞(蒸汽)灯——low pressure mercury246.高压钠(蒸汽)灯——pressure sodium (vapour)lamp 247.低压钠(蒸汽)灯——low pressure sodium(vapour)lamp 248.金属卤化物灯——metal halide lamp249.荧光灯——fluorescent lamp250.冷阴极灯——cold cathode lamp251.热阴极灯——hot cathode lamp252.冷启动灯——cold-start lamp253.瞬时启动灯——instant lamp254.预热灯——preheat lamp255.热启动灯——hot-star lamp256.开关启动荧光灯——swith-start fluorescent lamp257.无启动器荧光灯——258.弧光灯——arc lamp259.短弧灯——short-arc lamp;compact-source arc discharge lamp 260.长弧灯——long-arc lamp261.特种灯或专用灯——lamps of special types or special purposes 262.聚光灯——prefocus lamp263.反射灯——reflector lamp264.压制玻璃灯——pressed glass lamp265.密闭光束灯——sealed beam lamp266.投光灯——projector lamp267.投影灯——projection lamp268.摄影灯——photoflood lamp269.闪光灯——photoflash lamp270.闪光管——flash lamp271.电子闪光灯——electronic-flash lamp272.昼光灯——daylight lamp273.黑光灯——black light lamp274.钨带灯——tungsten ribbon lamp275.红外线灯——infrared lamp276.紫外线灯——ultraviolet lamp277.杀菌灯——bactericidal lamp278.光谱灯——spectroscopic lamp279.基准灯——reference lamp280.次级标准灯——secondary standard lamp281.工作标准灯——working standard lamp282.额定功率——rated power283.寿命——life284.寿命试验——life test285.X%灯失效时的寿命——life to X% failures286.平均寿命——average life287.发光元件——luminous element288.灯丝——filament289.直丝灯丝——straight filament290.单螺旋灯丝——single-coil filament291.双螺旋灯丝——coiled-coil filament292.玻壳——bulb293.透明玻壳——clear bulb294.磨砂玻壳——frosted bulb295.乳白玻壳——opal bulb296.涂层玻壳——coated bulb297.反射玻壳——reflectorized bulb298.漆膜玻壳——enamelled bulb299.彩色玻壳——coloured bulb300.硬料玻壳——hard glass bulb301.灯头——cap;basse(USA)302.螺旋式灯头——screw cap;screw base(USA)303.卡口式灯头——bayonet cap;bayonet base (USA)304.圆筒式灯头——Shell cap;Shell base305.插脚式灯头——pin cap;pin base306.预聚焦式灯头——prefocus cap;prefocus base307.卡口销钉——bayonet pin308.接触片——contact plate;eyelet309.插脚——pin;post310.灯座——lampholder311.连接器——connector312.主电极——main electrode313.启动电极——staring electrode314.放电管——arc tube315.发射唔知——emissive material316.启动带——staring strip;staring stripe317.启动装置——staring device318.启动器——starter319.触发器——ignitor320.镇流器——ballast321.半导体镇流器——semiconductor ballast322.基准镇流器——reference ballast323.调光器——dimmer324.自然光——daylighting325.照明——lighting326.照明技术——lighting technology327.照明工程——illuminating engineering328.照明环境——lighting environment329.视觉功能——visual performance330.等效对比度——equivalent contrast331.照明类型——types of lighting332.普通照明——general lighting333.局部照明——local lighting334.定位照明——localized lighting335.昼光补充照明——permanent supplementary artificial lighting 336.应急照明——emergency lighting337.太平门照明——escape lighting338.安全照明——safety lighting339.备用照明——stand-by lighting340.直接照明——direct lighting341.半直接照明——semi-direct lighting342.普通漫射照明——general diffused lighting343.半间接照明——semi-indirect lighting344.间接照明——indirect lighting345.定向照明——directional lighting346.漫射照明——diffused lighting347.泛光照明——floodlighting348.聚光照明——spotlighting349.照明矢量——illuminance vector350.发光强度——distribution of luminous intensity351.对称光强度分布——symmetrical luminous intensity distribution352.旋转对称光强度分布——rotationally symmetrical luminous intensity distribution 353.平均球面光强度——mean spherical luminous intensity354.等光强曲线——iso-intensity curve;iso-intensity line(USA)355.等光强图——iso-intensity diagram356.半峰发散角——half-peak divergence;one-half-peak spread(USA)357.累计光通量——cumulative flux358.球面带光通量——zonal flux359.总光通量——total flux360.向下光通量——downward flux361.向上光通量——upward flux362.累积向下光通量比——cumulative downward flux proportion363.光通量三联体——flux triplet364.光学光输出效率——optical light output ratio365.灯具效率——light output ratio366.向下光通量——downward flux367.向上光通量——upward flux368.灯具效率——light output radio369.向下灯具效率——downward light output radio370.向下光通量损耗——downward flux fraction371.光通量规则——flux code372.放大率——magnification radio373.直接光通量——direct flux374.间接光通量——indirect flux375.正比——direct ratio376.照明灯光通量密度——installed lamp flux density377.照明装置光通量密度——installation flux density378.基准面——reference surface379.工作面——work plane;working plane380.照明利用率——utilization factor381.照明利用系数——coefficient of utilization382.对比照明利用率——reduced utilization factor383.固有照明利用率——utilance384.等亮度曲线——isoluminance curve385.等照度曲线——iso-illuminance curve386.照明均匀度——uniformity radio of illuminance387.间距——spacing388.对称灯具——symmetrical luminaire389.非对称灯具——asymmetrical luminaire390.广角灯具——wide angle luminaire391.普通灯具——ordinary luminaire392.防护灯具——protected luminaire393.隔爆型防爆灯具——flameproof luminaire394.可调式灯具——adjustable luminaire395.可移式灯具——portable luminaire396.悬挂式灯具——pendant luminaire;suspended luminaire 397.升降式悬挂灯具——rise and fall pendant398.嵌入式灯具——recessed luminaire399.槽形灯具——troffer400.格栅灯具——coffer401.下射灯具——downlight402.壁灯灯具——bulkhead light403.窗帘式灯具——valance lighting404.穹顶灯具——cove lighting405.落地灯具——standard lamp;floor lamp406.台灯——table lamp407.手提灯——hand-lamp408.手电筒——torch409.灯串——lighting chain410.投光灯具——projector411.探照灯——searchlight412.聚光灯——spotlight413.泛光灯——floodlight414.遮光——cut-off415.遮光角——cut-off angle416.屏蔽角——shielding angle417.折射角——refractor418.反射角——reflector419.漫射器——diffuser420.碗形罩——bowl421.球形罩——globe422.灯罩——shade423.漫射格网——louvre ;louve(USA)424.遮光罩——spiu shield425.防护玻璃——protective glass426.灯具防护罩——luminaire guard427.摄影室泛光照明——studio floodlight428.反射型聚光灯——reflector spotlight429.透镜聚光灯——lens spotlight430.轮廓聚光灯——profile spotlight431.效果投光灯——effects spotlight432.柔光照明——softlight433.矿井照明用灯具——luminaires for mine lighting434.矿井用灯具——mine luminaire435.头灯——cap lamp436.头灯前照灯——headpiece437.矿井安全灯——mine safety lamp438.便携式矿井用灯具——portable mine luminaire 439.矿井营救灯具——mine rescue luminaire440.气压灯——air-turbo lamp;compressed air luminaire 441.地道灯具——haulageway luminaire442.采掘面灯具——face luminaire443.感应式灯具——induction luminaire444.许可灯具——permissible luminaire445.本质安全灯具——intrinsically safe luminaire 446.矿车尾灯——paddy lamp;trip lamp447.视觉信号——visual signal448.光信号——light signal449.标志——sign450.矩阵标志——matrix sign451.信号灯——signal light452.(导航)标志——navigation mark453.浮标——beacon454.固定灯光——fixed light455.间歇灯光——rhythmic light456.闪烁灯光——flashing light457.等相灯光——isophase light458.隐显灯光——occulting light459.交变灯光——alternating460.摆动灯光——reciprocating lights461.日光幻象——sun phantom462.微光——loom463.有效强度——effective intensity464.能见度——visibility465.大气透射率——atmospheric transmissivity466.气象光学范围——meteorological optical range 467.视觉范围——visual range468.地理范围——geographical range469.点视觉——point vision470.发光范围——luminous range471.标称范围——nominal range472.灯塔——lighthouse473.扇形灯光——sector light474.定向灯光——directiona light475.方向标——leading marks476.导航标灯——leading lights477.灯船——light vessel478.浮标——buoy479.照明浮标——lighted buoy480.浮体船——float481.横向标志——lateral mark482.横向灯光——lateral light483.主标志——cardinal mark484.主灯光——cardinal light485.导航灯——navigation light486.侧灯——sidelight487.船尾灯——stern light488.导航地灯——aeronautical ground light 489.障碍灯——obstacle light490.识别标志灯——identification beacon 491.机场标志灯——aerodrome beacon492.条形灯光——barrette493.跑道灯——runway lights494.横向光带——cross bar495.侧面光带——wing bar496.防撞灯——anti-collision light497.着陆灯——landing light498.滑行灯——taxing light499.交通信号——traffic sign500.交通灯——traffic light501.标志杆——marker post502.界标——delineator503.道路标志——road marking504.地面路标——road stud505.前灯——headlight506.远光灯——main-beam headlight507.近光灯——dipped-beam headlight508.前雾灯——front fog light509.前示宽灯——front position light510.后示宽灯——rear position light511.停车灯——parking light512.后雾灯——rear fog light513.倒车灯——reversing light514.刹车灯——brake light515.方向指示灯——direction indicator516.示警灯——hazard warningsignal517.号码牌灯——number-plate light518.后注册牌灯——rear registration-plate light 519.牌照灯——licenceplate light520.标志灯——markerlight。
the tyndall effect介绍英文
the tyndall effect介绍英文English:The Tyndall effect, also known as Tyndall scattering, is the effect of light scattering in colloidal dispersion or in clear fluids with very small particles. When a beam of light passes through a colloid or a very fine suspension, the light is scattered by the particles, making the beam visible. This effect is named after John Tyndall, who first demonstrated it in 1869. The Tyndall effect is the reason why the sky appears blue, as the shorter wavelength blue light is scattered more than the longer wavelength red light by the gas molecules in the Earth's atmosphere, making the blue light more visible to the human eye. This effect is also commonly seen in everyday life, such as in the way light passes through a glass of water, making the beam visible. The Tyndall effect has important applications in various fields, including environmental monitoring, pharmaceuticals, and the food industry, where it can be used to determine the size and concentration of particles in a solution.中文翻译:泰德尔效应,也称为泰德尔散射,是指光在胶体分散体或具有微小颗粒的清澈液体中散射的效应。
光学和光子学 光学薄膜 第1部分:术语-最新国标
光学和光子学光学薄膜第1部分:术语1 范围本文件界定了光学薄膜相关术语。
术语分为3类:基本术语和定义、按功能定义薄膜、常见的薄膜缺陷定义。
本文件适用于光学元器件及基底的表面镀膜,给出了光学薄膜技术指标的标准表述形式,定义了通用特性和必要的测试和测量方法,但不拟用于规定镀制方法。
本文件不适用于眼科光学(眼镜)的表面镀膜。
2 规范性引用文件下列文件中的内容通过文中的规范性引用而构成本文件必不可少的条款。
其中,注日期的引用文件,仅该日期对应的版本适用于本文件;不注日期的引用文件,其最新版本(包括所有的修改单)适用于本文件。
ISO 11145,光学和光子学—激光器和与激光有关的设备—词汇和符号(Optics and photonics – Lasers and laser-related equipment – V ocabulary and symbols )ISO 80000-7,量和单位—第7部分:光和辐射(Quantities and units – Part 7: Light and radiation )3 术语和定义ISO 11145和ISO 80000-7中界定的以及下列术语和定义适用于本文件。
3.1 基本术语和定义3.1.1 通用术语3.1.1.1元件和基底的表面镀膜 surface coating of components and substrates使用一种或多种材料,在元件表面镀膜,用以改变元件原表面的光学、物理或化学性质。
注:基底被视为是几何完美和光学均质的。
在实际操作中,将基底和表面的薄膜作为一个整体进行检验测量。
3.1.1.2入射介质 incident medium光射入薄膜前经过的介质。
3.1.1.3出射介质emergent medium光射出薄膜后进入的介质。
注:基底除了作为薄膜的机械支撑基底,也是薄膜的出射介质和(或)入射介质。
3.1.1.4通光孔径clear aperture符合要求的表面区域。
瑞利散射的原理英文
瑞利散射的原理英文The Raleigh scattering phenomenon is a fundamental aspect of light scattering that occurs when electromagnetic radiation interacts with microscopic particles or structures in a medium. It was first described by Lord Rayleigh, also known as John William Strutt, in the late 19th century.To understand the principles of Raleigh scattering, it is important to understand the nature of light. Light is an electromagnetic wave that consists of oscillating electric and magnetic fields. When light interacts with matter, it can be either absorbed, transmitted, or scattered. Scattering refers to the redirection of light in different directions due to interactions with particles or structures.Another factor that influences the intensity of Raleigh scattering is the concentration or density of the scattering particles. Higher concentrations of particles result in stronger scattering effects. This is why fog or clouds appear white, as the water droplets or ice crystals in these atmospheric phenomena are of sufficient size and concentration to scatter light of all wavelengths equally, resulting in a white appearance.The principles of Raleigh scattering have important applications in various fields. In atmospheric science, Raleigh scattering is responsible for the blue color of the sky, thereddening of the sun during sunrise and sunset, and the whiteness of clouds and fog. It is also relevant in astronomy, where the scattering of starlight by interstellar dust canaffect the observed colors of celestial objects.In conclusion, Raleigh scattering is a fundamental phenomenon that occurs when light interacts with particles or structures much smaller than its wavelength. It involves the induction of charged or polarized oscillations in the scattering particles, which then emit secondary waves that interfere with the incident wave to produce the scattered light. The intensity and characteristics of the Raleigh scattered light depend on factors such as the size of the scattering particles, the wavelength of the incident light, the concentration ofscattering particles, and the polarization state of the incident light. Understanding the principles of Raleigh scattering is essential for explaining various optical phenomena in the atmosphere and beyond.。
基于聚苯乙烯微球阵列模板法制备有序纳米结构及表面增强拉曼应用
基于聚苯乙烯微球阵列模板法制备有序纳米结构及表面增强拉曼应用吕志成;李琴【摘要】以规则排列聚苯乙烯微球阵列为模板,在平面衬底上获得了六角形排列的开口球腔结构,在微观曲面衬底上制备了3种不同纳米球腔结构.偏振紫外可见吸收光谱表明,开口纳米球腔阵列光学性质以π/3为周期.两种基底对4-巯基苯甲酸(4-MBA)表面增强拉曼散射(SERS)增强能力的差异证明球腔型纳米结构的拉曼增强能力来源于开口部分.利用球腔型SERS基底实现了对农药甲基对硫磷的检测,此类基底具有用于农药残留分析的潜力.%In this paper,hexagonally ordered arranged spherical nanocavity structure with opened mouth on plane substrate and three different spherical nanocavity structures on micro-convex substrate were prepared using ordered array of polystyrene microsphere as a template.Polarized ultraviolet-visible absorption spectra of spherical nanocavity array showed a optical property regular change with π/3 as a period.The difference in surface enhanced Raman scattering(SERS) intensity of 4-mercaptobenzoic acid(4-MBA) on these two type of substrates clearly indicated that enhance of Raman signal came from opened mouth region.The spherical nanocavity SERS substrates were used to detect pesticide methyl parathion and revealed a potential for analyzing pesticide residues.【期刊名称】《化学与生物工程》【年(卷),期】2017(034)001【总页数】5页(P44-47,61)【关键词】聚苯乙烯微球阵列;纳米球腔;表面增强拉曼散射;农药残留【作者】吕志成;李琴【作者单位】华中农业大学理学院,湖北武汉430070;华中农业大学理学院,湖北武汉430070【正文语种】中文【中图分类】O657.37表面增强拉曼散射(surface enhanced Raman scattering,SERS)以其灵敏度高、结构鉴定能力强等特点在化学分析[1]、环境污染物检测[2]、生物分子结构鉴定[3]等领域发挥了重要作用。
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a r X i v :a s t r o -p h /0509775v 1 26 S e p 2005Astronomy &Astrophysics manuscript no.referee-format February 5,2008(DOI:will be inserted by hand later)Research NoteScattering of Polarized Radiation by Atoms inMagnetic and Electric FieldsYee Yee Oo 1,K.N.Nagendra 2,Sharath Ananthamurthy 1,and G.Ramachandran 21Department of Physics,Bangalore University,Bangalore-560056,India 2Indian Institute of Astrophysics,Bangalore-560034,IndiaReceived dd mm yy /Accepted dd mm yyAbstract.The polarization of radiation by scattering on an atom embedded in combined external quadrupole electric and uniform magnetic fields is studied the-oretically.Analytic formulae are derived for the scattering phase matrix.Limiting cases of scattering under Zeeman effect,and Hanle effect in weak magnetic fields are discussed.Key words.atomic processes –polarization –scattering –magnetic fields –line:profiles1.IntroductionScattering of polarized radiation by an atom is a topic of considerable interest to as-trophysics,especially with the advent of imaging polarimeter systems like ZIMPOL I &II (Gandorfer 2003)which reach accuracies of the order of 10−5for measuring the Stokes parameters characterising the observed radiation.The concept of scattering phase ma-trix connecting the Stokes vector S ′of incident radiation to the Stokes vector S of scat-tered radiation was introduced quite early in the context of Rayleigh ndi Degl’Innocenti (1983a;1983b;1984;1985),Landi Degl’Innocenti,Bommier and Sahal-Br´e chot (1990;1991a;1991b)and Bommier (1997a;1997b)developed a comprehensive theoretical framework to describe the generation and transfer of polarized radiation in spectral lines,formed in the presence of an external magnetic field.In the context of radiation transfer work,Stenflo and Stenholm (1976)and Rees (1978),used complete frequency redistribution (CRD)in the resonance scattering,and Dumont et al.(1977),2Oo et al.:ScatteringRees and Saliba(1982),Nagendra(1986;1988),Faurobert(1987),Ivanov et al.(1997) and later works employed partial frequency redistribution(PRD)line scattering mech-anisms in the absence of magneticfield.The Hanle effect is a depolarizing phenomenon which arises due to‘partially overlapping’magnetic substates in the presence of weak magneticfields,where the splitting produced is of the same order as or less than the natural widths.Favati et al.(1987)proposed the name‘second Hanle effect’for a similar effect in‘electrostaticfields’.Casini and Landi Degl’Innocenti(1993)have discussed the problem in the presence of electric and magneticfields for the particular case of hydrogen lines.The relative contributions of static external electricfields,motional electricfields and magneticfields in the case of hydrogen Balmer lines,have been studied by Brillant et al.(1998).A historical perspective and extensive references to earlier literature on polarized line scattering can be found in Stenflo(1994),Trujillo Bueno et al.(2002)and Landi Degl’Innocenti and Landolfi(2004).The purpose of this paper is to derive the scattering phase matrix for the case of combined magnetic and electric quadrupolefields with arbitrary strengths.The particular case of transitions between J=0and J=1 states is considered following Oo et al.(2004;2005).2.Theoretical FormalismThe Hamiltonian for an atom,when it is exposed to an external magneticfield B together with an arbitrary external CoulombfieldΦ,is of the form(Oo et al.2004)H=H0+g J·B+∞l=0lm=−l(−1)m V lm Q l−m,(1)where g denotes the gyromagnetic ratio,J the total angular momentum operator for the atom with components J x,J y,J z while V lm denote the2l-pole components ofΦand the components Q l−m characterise the electric charge distribution inside the atom.It is well-known that the magneticfield B splits an eigenstate of H0with energy E and total angular momentum quantum number J into(2J+1)equally spaced levels|J M with energies E M=E+gBM,where B=|B|and M denotes the magnetic quantum number with respect to an axis of quantization chosen along B.If the atomic states are eigenstates of parity,the l=1term makes no contribution.In an external electric quadrupolefield with l=2,V2m may equivalently be expressed in terms of the cartesian components Vα,βwithα,β=x,y,z of a traceless symmetric second rank tensor,which defines its own Principal Axes Frame(PAF),wherein Vα,β=Vα,αδα,β,so that2m=−2(−1)m V2m Q2−m=A 3J2z−J·J+η{J2x−J2y} ,(2) where A=Q V zz/{4J(J−1)},if Q denotes the electric quadrupole moment of the atom andη=(V xx−V yy)/V zz denotes the asymmetry parameter of thefield.In such a case, the(2J+1)substates|ψk k are neitherOo et al.:Scattering3 YZQFig.1.The scattering geometry:(X Q,Y Q,Z Q)refers to the Principal Axes Frame (PAF)characterising the electric quadrupolefield.The radiation is incident along(θ′,φ′) and scattered along(θ,φ)with respect to the astrophysical reference frame denoted by (X,Y,Z).The magneticfield B is oriented along( θB, φB)with reference to PAF and(θB,φB)with reference to the astrophysical reference frame(the azimuthal angles φB andφB are not marked in thefigure).equally spaced nor are they identifiable as|J M states.We may,however,representthem as|ψk =JM=−Ja k M(B,A,η)|J M ,(3)in terms of|J M states defined with respect to PAF,where the expansion coefficients a k M as well as the energies E k are not only functions of B,A,ηbut also of the angles ( θB, φB)of B with respect to PAF(see Fig.1).For a detailed discussion for J=1,34Oo et al.:Scatteringparityπi to afinal state|ψf with energy E f,total angular momentum J f and parityπf when polarized radiation with frequencyν′is incident on the atom in the astrophysical frame in a direction(θ′,φ′)and gets scattered into a direction(θ,φ)with frequrncyν. The left and right circular states of polarization as defined by Rose(1957)are denoted by µ=±1.The second order transition matrix element for scattering of polarized radiation may then be written,with respect to the polarization states asTµµ′= n E fn(µ)Φn A ni(µ′),(6) where the summation is with respect to the intermediate states|ψn of the atom with energy E n,total angular momentum J n and parityπn.Following(Oo et al.2004),the matrix elements for emission from|J u m u to|J l m l are of the formE m l m u(µ)=LJ LLM L=−LC(J l,L,J u;m l,M L,m u)D L MLµ(φ,θ,0)∗,(7)where J L is proportional to the reduced matrix element.The complex conjugate of Eq.(7) defines the matrix elements A mu m l(µ)for absorption of radiation with polarizationµincident along(θ,φ)leading to|J u m u from|J l m l .Using the notationsω=2πν;ω′= 2πν′;ωn=E n−E f andω′n=E n−E i,the profile functionΦn=(ωn−ω−iΓn)−1= (ω′n−ω′−iΓn)−1where the width associated with|ψn is denoted byΓn and energy conservation requires E i+ω′=E f+ω.Angular momentum and parity are conserved individually during the absorption and the emission.3.Scattering Phase MatrixIf S′denotes the Stokes vector,which characterizes the state of polarization of the incident radiation,the Stokes vector S characterizing the scattered radiation isS=R S′,(8) where R is a(4×4)matrix whose elements are of the formR pp′=nn′ΦnΦ∗n′P nn′pp′,(9)where the phase matrix elements are given by P nn′pp′=1Oo et al.:Scattering5 of the(2J f+1)×(2J f+1)matrix contained within the square bracket.The C i,C f,C n and C n′are defined in terms of their elementsC i m i m′i=c i m i c i∗m′i;C f m f m′f=c f m f c f∗m′f,C n m n m′n=c n m n c n∗m′n;C n′m n′m′n′=c n′m n′c n′∗m′n′.(11) Each of these matrices C i,C f,C n,C n′are clearly hermitian and satisfy the condition C2=C.Note that the P nn′pp′depend not only on n and n′but also on the direction( θB, φB)and the strength B of the magneticfield B and on(A,η;αQ,βQ,γQ)characterising the electric quadrupolefield(because of Eq.(4)for the c k m with k=i,f,n,n′),apart from the angles(θ′,φ′)of the incident and(θ,φ)of the scattered radiation.Explicitly,therefore, P nn′pp′≡P nn′pp′(θ,φ;θ′φ′;B;A,η;αQ,βQ,γQ)for any given J i,J f.In the case of resonance scattering,when only a single intermediate state|ψn with E n=E i+ω′=E f+ωcontributes to Eq.(6),one can replace the summation over n,n′by n=n′corresponding to a single excited level,whereas the double summation over n,n′has to be retained in Hanle scattering.4.Particular CaseWe consider the simple case of scattering with electric dipole transitions between a total angular momentum zero lower level and a total angular momentum one upper level,i.e., J l=J i=J f=0and J u=J n=1.Clearly,C i=C f=1.We may then use Eq.(7)to simplify the product E†(µ′′)E(µ)and use the complex conjugate of Eq.(7)to simplify the product A(µ′)A†(µ′′′)in Eq.(10),so thatP nn′pp′=1√√2δξ,0δλ,1.(14) In the absence of the electricfield,n=M,n′=M′and the c M m=D1mM(φB,θB,0), leading to the well-known Hanle scattering phase matrix given by Eqs.(9)to(16)of Landi and Landi(1988)ifΦMΦ∗M′can be assumed to be independent of M,M′in the6Oo et al.:Scatteringlimiting case of weakfields.If the Doppler convolution is effected following exactly the procedure outlined by Stenflo(1998),the Hanle-Zeeman scattering matrix represented by Eqs.(49)and(50)of Stenflo(1998)is recovered forθB=φB=0.In the case of strongfields i.e,if g B is large compared to the line widths(Zeeman effect),one may set M=M′and recover Eq.(52)of Stenflo(1998)forθB=φB=0and the results obtained much earlier by Obridko(1965a).5.Numerical Results and DiscussionIf we consider the simplest geometry of the combined magnetic and quadrupole electric fields with B along the Z-axis of the PAF with the PAF itself coinciding with the astro-physical frame i.e.,αQ=βQ=γQ= θB= φB=θB=φB=0,the upper level withJ u=1is split into three levels n=1,2,3(Oo et al.2004)with energiesE1=−2r g B;E2,3=(r∓s)g B,(15)where r=A/gB the ratio of the electric quadrupole and magneticfield strengths,s= (r2η2+1)1/2and the corresponding eigen states|ψ1 ,|ψ2 and|ψ3 characterized by c10=1,c1±1=c2,30=0c3±1=±c2∓1=(s+rη±1)/2(s2+rηs)1/2,(16)using Eqs.(4)and(5),with the electric quadrupolefield strength A>0.To understand the combined effect of magnetic and electric quadrupolefields,we present in Figs.(2d-2f)the general behavior of the scattered Stokes line profiles S for a given unpolarized incident radiation,S′=(1000)T,for particular choices of the,φ=π).We compare these with the pure Zeeman directions(θ′=π4scattering case(see Figs.2a-2c).In the Stokes Q profile,the positive maximum at the line center and the negative maximum symmetrically placed atσ±1components,which are typical of the well known Zeeman effect.The maximum of the V profile atσ±1 components have opposite sign,which is also a well known characterisitc of Zeeman effect.We assume here that the magneticfield and the quadrupole electricfield are equally strong(i.e.,r=A/B=1).We also assume B to be four times the natural line width and set n=n′=1,2,3.The solid and dashed curves in Figs.(2d-2f)are computed for the values ofη=0and1respectively.In the combinedfields case,the line component arising due to the|ψ1 =|1,0 state(which represents the central component in the corresponding pure Zeeman case)is positioned in the red wing(see Figs.2d-2f). The unequal strengths of the scattered line profiles arising from|ψ2 and|ψ3 states are clearly seen in all the scattered Stokes line profiles(I,Q,V).This is due to the weighted superposition of the magnetic substates|1,−1 and|1,1 .In the scattered Stokes V line profile,|ψ1 state does not contribute,as in the case of pure Zeeman scattering.Therefore the shape of the scattered Stokes V profile is similar to the Zeeman case,except for theOo et al.:Scattering7Frequency xIFrequency xFrequency xQxFrequency xFrequency VFrequency xFig.2.Stokes line profiles in arbitrary units comparing the Zeeman scattering in a pure magnetic field (panels a −c ),and scattering under the combined magnetic and electric quadrupole fields (panels d −f )with r =1.The solid lines correspond to asymmetry parameter η=0,and the dashed lines to η=1.In all panels,x is the frequency displacement from the line center in natural width units.shifting of the position and the change in the relative strength of components when η>0.If ηvanishes,the strengths of both components are same.Acknowledgements.The authors are indebted to Prof.J.O.Stenflo for kindly examining the manuscript,and for useful remarks,and comments.They also wish to thank an anonymous referee of this paper for pertinent remarks and suggestions that proved very useful while revising the manuscript.One of the authors (YYO)wishes to express her gratitude to the Chairman,Department of Physics,Bangalore University and the Director,Indian Institute of Astrophysics (IIA),for providing research facilities.She gratefully acknowledges the award of a scholarship by Indian Council for Cultural Relations (ICCR),Ministry of External Affairs (MEA),Government of India.Another author (GR)is grateful to Professor B.V.Sreekantan,Professor R.Cowsik and Professor J.H.Sastri for much encouragement and facilities provided for research at IIA.ReferencesBommier,V.1997a,A&A,328,7068Oo et al.:ScatteringBommier,V.1997b,A&A,328,726Brillant,S.,Mathys,G.,&Stehle,C.1998,A&A,339,286Casini,R.,&Landi Degl’Innocenti,E.1993,A&A,276,289Dumont,S.,Pecker,J.C.,Omont,A.,&Rees,D.E.1977,A&A,54,675Favati,B.,Landi Degl’Innocenti,E.,Landolfi,M.1987,A&A,179,329Faurobert,M.1987,A&A,178,269Gandorfer,A.M.2003,Astron.Nachr./AN,324,318Ivanov,V.V.,Grachev,S.I.,&Loskutov,V.M.1997,A&A,318,315Landi Degl’Innocenti,E.1983a,Solar Phys,85,3Landi Degl’Innocenti,E.1983b,Solar Phys,85,33Landi Degl’Innocenti,E.1984,Solar Phys,91,1Landi Degl’Innocenti,E.1985,Solar Phys,102,1Landi Degl’Innocenti,M.,&Landi Degl’Innocenti,E.1988,A&A,192,374Landi Degl’Innocenti,E.,Bommier,V.,&Sahal-Br´e shot,S.1990,A&A,235,459Landi Degl’Innocenti,E.,Bommier,V.,&Sahal-Br´e chot,S.1991a,A&A,244,391Landi Degl’Innocenti,E.,Bommier,V.,&Sahal-Br´e chot,S.1991b,A&A,244,401Landi Degl’Innocenti, E.,&Landolfi,M.2004,Polarization in Spectral Lines,Kluwer, NetherlandsMcMaster,W.H.1961,Rev.Mod.Phys.,33,8Nagendra,K.N.1986,Ph.D.Thesis,Bangalore University,IndiaNagendra,K.N.1988,ApJ,335,269Obridko,V.N.1965a,Soviet Physics-Astronomy,9,77Rees,D.E.Publ.Astron.Soc.Japan,1978,30,455Rees,D.E.&Saliba,G.J.1982,A&A,115,1Rose,M.E.,1957,Elementary Theory of Angular Momentum,John Willy,New YorkStenflo,J.O.,&Stenholm,L.1976,A&A,46,69Stenflo,J.O.1994,Solar Magnetic Fields-Polarized Radiation Diagnostics,Kluwer,Dordrecht Stenflo,J.O.1998,A&A,338,301Trujillo Bueno,J.,Moreno Insertis, F.,S´a nchez, F.(Eds.)2002,Astrophysical Spectropolarimetry,Cambridge Univ.Press,CambridgeYee Yee Oo,Nagendra,K.N.,Sharath Ananthamurthy,Vijayshankar,R.,&Ramachandran, G.2004,J.Quant.Spec.Radiat.Transf.,84,35Yee Yee Oo,Nagendra,K.N.,Sharath Ananthamurthy,Swarnamala Sirsi,Vijayshankar,R., &Ramachandran,G.2005,J.Quant.Spec.Radiat.Transf.,90,343。