Acceleration Waves in the von Karman Plate Theory
看书可以去海边吗英语作文
看书可以去海边吗英语作文标题,Can Reading be Enjoyed at the Seaside?In our fast-paced modern world, finding moments of tranquility and reflection is becoming increasingly rare. Many turn to the soothing embrace of nature, seeking solace in the calming rhythm of the ocean waves. However, amidst the allure of the seaside, can one truly indulge in the pleasure of reading? This question beckons exploration.The allure of the beach is undeniable. The soft, warm sand underfoot, the rhythmic crashing of waves against the shore, and the vast expanse of the horizon stretching endlessly before us. It's a scene that evokes a sense of peace and serenity, a perfect backdrop for relaxation and contemplation. But can this serene setting harmonize with the immersive world of literature?The notion of reading at the seaside may seem paradoxical at first glance. How can one focus on theintricacies of a novel when surrounded by the distractions of seagulls crying overhead and children playing in the sand? Yet, upon closer inspection, the beach offers a unique environment conducive to deep engagement with literature.Picture this: reclining on a comfortable beach chair, the gentle breeze carrying the scent of saltwater and sunscreen. With the sound of the waves as a soothing soundtrack, one can delve into the pages of a captivating book. The immersive experience of reading becomes enhanced by the sensory stimuli provided by the seaside ambiance. Every word read seems to echo the rhythm of the waves, creating a harmonious symphony of relaxation andintellectual stimulation.Moreover, the beach offers a respite from therelentless demands of daily life. In this tranquil setting, free from the distractions of technology and the pressures of work, one can fully immerse oneself in the world crafted by the author. The mind becomes unburdened, allowing for a deeper connection with the text and its underlying themes.As the sun sets on the horizon, casting hues of orange and pink across the sky, the beauty of nature serves to enrich the reading experience, imbuing it with a sense of wonder and awe.Furthermore, the beach provides ample opportunities for introspection and self-discovery. As one loses oneself in the pages of a book, the vastness of the ocean before them serves as a poignant reminder of the infinitude of human imagination. The act of reading becomes a journey of exploration, not only of the fictional worlds contained within the pages but also of the depths of one's own soul. In the quiet moments between chapters, as the sun dips below the horizon and the stars begin to twinkle overhead, one can reflect on the profound insights gleaned from the text and apply them to their own life journey.In conclusion, while it may initially seem incongruous, the combination of reading and the seaside is a match made in paradise. The beach offers a sanctuary for both body and mind, a place where one can escape the chaos of the world and find solace in the pages of a book. So, the next timeyou find yourself longing for a moment of respite, why not pack your favorite novel and head to the seaside? There, amidst the gentle lull of the waves and the warmth of the sun, you may just discover a newfound appreciation for the magic of reading.。
海底两万里 英文听力
海底两万里英文听力"Twenty Thousand Leagues Under the Sea" is a classic science fiction novel written by French author Jules Verne. The story follows the adventures of Captain Nemo and his submarine, the Nautilus, as they explore the depths of the ocean. The novel is considered one of the earliest works of science fiction and has inspired many adaptations and sequels.《海底两万里》是法国作家儒勒·凡尔纳创作的经典科幻小说。
故事讲述了船长尼摩和他的潜水艇“鹦鹉螺号”在海洋深处的探险。
这部小说被认为是科幻小说的早期作品之一,启发了许多改编和续集。
One of the most compelling aspects of "Twenty Thousand Leagues Under the Sea" is its vivid portrayal of the undersea world. Verne's detailed descriptions of the marine life and underwater landscapes captivate the reader's imagination and bring the ocean depths to life. The novel paints a rich and immersive picture of the wonders and mysteries hidden beneath the waves.《海底两万里》最吸引人的一点是它生动地描绘了海底世界。
海底两万里1到6章的妙词好句
海底两万里1到6章的妙词好句英文回答:Chapter 1:"The sea stretched out before me, its vastness both awe-inspiring and intimidating.""The waves crashed against the ship, their relentless force rocking us from side to side.""As the salty sea air filled my lungs, I couldn't help but feel a sense of adventure and anticipation."Chapter 2:"The underwater world came alive before my eyes, with vibrant coral reefs and colorful schools of fish.""The sunlight filtered through the water, creating amesmerizing dance of light and shadows.""The silence of the deep sea was broken only by the gentle swaying of seaweed and the occasional sound of a distant creature."Chapter 3:"The submarine descended into the depths, its metalhull creaking and groaning under the pressure.""The darkness engulfed us, and I relied on the dim glow of the control panel to navigate through the abyss.""The eerie stillness of the deep sea made me feel like a tiny speck in the vastness of the ocean."Chapter 4:"The encounter with the giant squid was a heart-stopping moment, as its massive tentacles reached out towards us.""The adrenaline coursed through my veins as I watched Captain Nemo skillfully maneuver the submarine to escape the creature's grasp.""The battle between man and beast was a testament to the indomitable spirit of the human will."Chapter 5:"The underwater volcano erupted, sending plumes of molten lava and billowing smoke into the water.""The heat was unbearable, and I could feel the sweat trickling down my forehead as we desperately tried to escape the fiery inferno.""The sight of the destruction and chaos reminded me of the power and unpredictability of nature."Chapter 6:"The underwater city of Atlantis was a marvel to behold, with its grand architecture and advanced technology.""The Atlanteans welcomed us with open arms, their hospitality and warmth making us feel like long-lost friends.""Exploring the ruins of Atlantis was like stepping back in time, unraveling the mysteries of a lost civilization."中文回答:第一章:"大海在我面前延伸开来,其广阔既令人敬畏又令人害怕。
P波入射下断层参数对地表地震动的影响
P波入射下断层参数对地表地震动的影响刘必灯;于淼;王伟;周正华;李小军【摘要】基于应用透射人工边界条件的显式有限元法计算断层破碎带宽度及力学参数变化、地震动入射角变化时二维断层场地模型P波入射下地表地震动场的分布.结果表明:(1)低速度破碎带的存在导致整个场地都有P波转换为SV波的分量,且在断层破碎带的区域出现断层陷波;(2)低速度破碎带的存在使输入场地恒定的能量向破碎带集聚放大,随着破碎带宽度增大或其介质波速降低集聚放大效应增大;(3)场地放大效应是频率相关的,宽度较宽或介质波速较低的断层破碎带对输入地震动中较低的频率成份放大显著;(4)竖向断层破碎带能阻隔斜入射地震P波,随着入射角增加隔震效应更显著.%In this study,a numerical solution for a 2-D fault site model under incident P waves using the explicit finite element method combined with transmission of artificial boundary condi-tion was derived.The distribution rules of peak ground acceleration (PGA)and the spectrum characteristics influenced by fault characteristics such as width and shear wave velocity of the fault and the incidence angle of the seismic waves were discussed.Numerical simulations shown that transform SV waves developed in the low velocity fault zone (LVFZ)when it struck by external incident P waves,and many trapped waves obviously developed in it.This result implied that the external incident seismic radiation congregated in the LVFZ,and the agglomeration effect increased with the increased width and decreased shear wave velocity of the LVFZ.Vertical LVFZs blocked the spread of oblique incident P waves,and the isolation effect decreased with the increased incidence angle of P waves.The seismicresponse of a variety of LVFZ models withdifferent width and shear wave velocity struck by external vertically incident P waves was deter-mined,and the results implied that the ground motion amplification characteristics in the near fault zone site are frequency dependent.The higher frequency components of ground seismic waves are obviously amplified by LVFZs with narrower widths and higher shear wave velocities, while the lower frequency components of ground seismic waves are obviously amplified by LVFZs with wider widths and lower shear wave velocities.In other words,the site amplification coeffi-cient is frequency dependent,such that the widening the width or decreasing the shear wave velocity of fault fracture zone,the predominant frequency of a larger site amplification coefficient is becoming lower.【期刊名称】《地震工程学报》【年(卷),期】2017(039)001【总页数】8页(P160-167)【关键词】非发震断层场地;断层破碎带;断层陷波;集聚效应;频率相关;隔震效应【作者】刘必灯;于淼;王伟;周正华;李小军【作者单位】防灾科技学院,河北三河 065201;防灾科技学院,河北三河 065201;防灾科技学院,河北三河 065201;南京工业大学,江苏南京 210000;中国地震局地球物理研究所,北京 100081【正文语种】中文【中图分类】P351.9断层对地震震害的显著影响可分为发震断层的震源影响及非发震断层的局部场地影响。
机械工程学专业词汇英语翻译(V)
vacancy 空位 vacant site 空位 vacuum 真空 vacuum apparatus 真空装置 vacuum chamber 真空室 vacuum diagram 真空图 vacuum diffusion 真空扩散 vacuum effect 真空效应 vacuum pump 真空泵 vacuum state 真空态 vacuum tank 真空罐 vacuum tight 真空密闭的 vacuum value of velocity 真空速度 vacuum valve 真空阀 vacuum vector 真空⽮量 validity 有效性 validity criteria 有效准则 valley floor ⾕底 value 值 valve lift 阀升程 valve lift curve 阀升距图 valve lift diagram 阀升距图 van der waals energy 范德⽡⽿能量 van der waals equation 范德⽡⽿斯⽅程 van der waals force 范德⽡⽿斯⼒ vane 叶⽚ vane grid 叶栅 vane type pump 叶轮泵 vane wheel 叶轮 vaned diffuser 叶⽚式扩散器 vaneless diffuser ⽆叶⽚式扩散器 vanishing 消失 vanishing point 消失点 vapor pressure 蒸汽压 vapor pressure equation 蒸汽压⽅程 vapor pump 蒸汽喷射泵 vaporization 汽化 vaporization heat 蒸发热 vapour 蒸汽 variability 变异性 variable 变数 variable acceleration 可变加速度 variable capacity 可变容量 variable geometry wing 可变翼 variable load 可变负荷 variable mass 变质量 variable mass body 变质量体 variable mass mechanics 变质量⼒学 variable motion 变速运动 variable of state 状态变数 variable pitch airscrew 变距螺旋桨 variable pitch propeller 变距螺旋桨 variable quantity 变量 variable rotation 可变旋转 variable sweep aerofoil 可变后掠翼 variable wind 变向风 variance ⽅差 variation 变化 variation method 变分法 variation of amplitude 幅度的变动 variational calculus 变分学 variational equation 变分⽅程 variational principle 变分原理 variational problem 变分问题 varied orbit 变化轨道 variometer 升降速度仪 vector analysis ⽮量分析 vector component ⽮量分量 vector coupling ⽮量耦合 vector diagram ⽮量图 vector equation ⽮量⽅程 vector field ⽮场 vector flux ⽮通量 vector function ⽮量函数 vector interaction ⽮量相互酌 vector of force ⼒⽮量 vector of oscillation 振荡⽮量 vector polygon ⽮量多边形 vector potential ⽮量势 vector product ⽮积 vector space ⽮量空间 vector sum ⽮量和 vector tube ⽮量管 vector wave equation ⽮量波⽅程 vector wave function ⽮量波函数 vectorial ⽮量的 velocimeter 速度计 velocity 速度 velocity circulation 速度环量 velocity coefficient 速度系数 velocity component 速度分量 velocity constant 速率常数 velocity correlation of turbulence 湍临度相关 velocity coupling 速度耦合 velocity curve 速度曲线 velocity diagram 速度图 velocity distribution 速度分布 velocity distribution function 速度分布函数 velocity ellipse 速度椭圆 velocity field 速度场 velocity gradient 速度梯度 velocity head 速度头 velocity head tachometer 液压转速计 velocity in free space ⾃由空间速度 velocity limit 极限速度 velocity load diagram 速度载荷图 velocity modulation 速度灯 velocity of blade 叶⽚速度 velocity of combustion 燃烧速度 velocity of flow 临 velocity of longitudinal wave 纵波速度 velocity of moving space 牵连速度 velocity of propagation 传播速度 velocity of propagation of flame ⽕焰传播速度 velocity of slip 滑临度 velocity of sound 声速 velocity of transformation 转变速度 velocity of transverse waves 横波速度 velocity of wave front 波前速度 velocity operator 速度算符 velocity parallelogram 速度平⾏四边形 velocity pickup 速度传感器 velocity plane 速度平⾯ velocity potential 速度势 velocity profile 速度剖⾯图 velocity rating 额定速度 velocity resonance 速度共振 velocity shock 速度冲击 velocity space 速度空间 velocity spectrum 速度谱 velocity time diagram 速度时间图 velocity triangle 速度三⾓形 ventilation loss 通风损耗 ventilator 风扇 ventilator pressure 通风机压⼒ venturi meter ⽂丘⾥量计 venturi tube ⽂丘⾥管 vernier 游标 vertex 顶点 vertex function 顶点函数 vertex tangent 顶点切线 vertical 垂直 vertical axis 垂直轴 vertical circle 等⾼圈 vertical component 垂直分量 vertical curve 竖直线 vertical deflection 竖直偏转 vertical displacement 垂直位移 vertical distribution 竖向分布 vertical fall 垂直落下 vertical flow 竖直怜 vertical force 垂直⼒ vertical hydrodynamic force 铃动⼒浮⼒ vertical line 铅垂线 vertical load 垂直荷载 vertical motion 竖向运动 vertical pendulum 竖直摆 vertical plane 垂直⾯ vertical plate 竖直板 vertical projection 垂直投影 vertical reaction 垂直反⼒ vertical section 竖直截⾯ vertical shock 竖震 vertical stream 竖直怜 vertical temperature grade 垂直温度梯度 vertical velocity 竖向速度 vertical velocity curve 竖向临曲线 vertical velocity distribution 竖直速度分布 vertical wind tunnel 竖直风洞 very low frequency 甚低频 vessel 船 vibrate 振动 vibrating compaction 振动压实 vibrating field 振荡场 vibrating load 振动负载 vibrating potential model 振动势模型 vibrating reed 振簧 vibrating rod 振荡棒 vibrating rotator 振动转⼦ vibrating screen 振动筛 vibrating string 振动弦 vibrating system 振动系统 vibrating table 振动台 vibration 振动 vibration absorber 消振器 vibration analysis 振动分析 vibration damper 振动阻尼器 vibration damping 减振 vibration frequency 振动频率 vibration galvanometer 振动式检疗 vibration generator 振动器 vibration instrument 振动仪表 vibration isolation 隔振 vibration isolator 隔振器 vibration level 振动级 vibration meter 振动计 vibration node 振动节点 vibration of bar 杆的振动 vibration of plate 板的振动 vibration of string 弦的振动 vibration pickup 振动传感器 vibration plane 振动平⾯ vibration proof 耐振的 vibration range 振荡范围 vibration resistance 抗振性 vibration resonance 振动共振 vibration rotation 振荡转动 vibration rotation band 振动转动谱带 vibration rotation spectrum 振动转动谱 vibration state 振动态 vibration stress 振动应⼒ vibration system 振动系统 vibration test 振动试验 vibration tester 振动试验仪 vibration testing machine 振动试验仪 vibrational angular momentum 振动⾓动量 vibrational constant 振动常数 vibrational coordinate 振动坐标 vibrational corrosion 振动腐蚀 vibrational energy 振动能 vibrational enthalpy 振动焓 vibrational entropy 振动熵 vibrational instability 振动不稳定性 vibrational line 振动线 vibrational mode 振动模式 vibrational period 振动周期 vibrational perturbation 振动扰动 vibrational relaxation 振动弛豫 vibrational scattering 振动散射 vibrational spectrum 振动谱 vibrational state 振动状态 vibrogram 振动记录图 vibrograph 测振计 vibrometer 振动计 vibroscope 振动仪 vickers hardness 维⽒硬度 virial equation of state 维⾥状态⽅程 virial expansion 维⾥展开 virial theorem 维⾥定理 virtual center 瞬时中⼼ virtual deformation 虚形变 virtual displacement 虚位移 virtual entropy 有效熵 virtual free energy 有效⾃由能 virtual free enthalphy 有效⾃由焓 virtual friction 表观摩擦 virtual inertia 表观惯性 virtual mass 虚质量 virtual particle 虚粒⼦ virtual transformation 虚转变 virtual velocity 假想速度 virtual work 虚功 virtual work method 虚功法 virtual work theorem 虚功定理 visco elasticity 粘弹性 viscoelastic 粘弹性的 viscoelastic body 粘弹性体 viscoelastic foundation 粘弹性基础 viscoelastic gas 粘弹性⽓体 viscoelastic material 粘弹性材料 viscoelastic model 粘弹性模型 viscoelastic solid 粘弹性固体 viscoelastic wave 粘弹性波 viscoelastic wave equation 粘弹性波动⽅程 viscometry 粘度测定法 viscoplastic 粘塑性的 viscoplastic constitutive equation 粘塑性本构⽅程 viscoplastic strain 粘塑性应变 viscoplasticity 粘塑性 viscosimeter 粘度计 viscosimetry 粘度测定法 viscosity 粘性 viscosity correction 粘性校正 viscosity force 粘性⼒ viscosity function 粘度函数 viscosity measurement 粘度测定 viscosity pump 粘性泵 viscosity tensor 粘性张量 viscous boundary layer 粘性边界层 viscous damping 粘性阻尼 viscous drag 粘滞阻⼒ viscous flow 粘性怜 viscous fluid 粘⼒ viscous friction 粘滞摩擦 viscous liquid 粘性液体 viscous motion 粘性怜 viscous resistance 粘滞阻⼒ viscous shearing stress 粘性切应⼒ viscous solid 粘滞固体 viscous strain 粘性应变 viscous stress 粘性应⼒ visibility 能见性 visualization of flow 怜显⽰ void 空隙 void coalescence 孔隙聚结 void coefficient 空隙系数 void fraction 空隙率 volplane 滑翔飞⾏ volume 体积 volume change by shear 切变体积变化 volume compressibility 体积压缩率 volume compression 体积压缩 volume concentration 体积浓度 volume contraction 体积收缩 volume density 体积密度 volume diffusion 体积扩散 volume diffusion coefficient 体积扩散系数 volume elasticity 体积弹性 volume element 体积元 volume energy 体积能 volume expansion coefficient 体积膨胀系数 volume fraction 体积率 volume parameter 体积参数 volume potential 体积势 volume ratio 体积⽐ volume resistance 体积阻⼒ volume resonance 体积共振 volume strain 体积应变 volume stress 体积应⼒ volume velocity 体积速度 volumetric diameter 体积径 volumetric efficiency 体积效率 volumetric energy 体积应变能 volumetric expansion 体积膨胀 volumetric flow rate 体积临 volumetric flowmeter 体积式量计 volumetric flux 体积通量 volumetric force 体积⼒ volumetric modulus of elasticity 体积弹性模量 volumetric strain 体积应变 von karman number 卡门数 vortex 涡旋 vortex center 涡旋中⼼ vortex chamber 涡旋室 vortex core 涡核 vortex field 涡场 vortex filament 涡丝 vortex flow 涡流 vortex flux 涡通量 vortex free motion ⽆涡运动 vortex frequency 涡旋频率 vortex invariant 涡旋不变量 vortex layer 旋涡层 vortex line 涡线 vortex line motion 涡线运动 vortex motion 涡了动 vortex nucleus 涡核 vortex path 涡道 vortex point 涡点 vortex pump 涡旋泵 vortex region 涡柳 vortex ring 涡环 vortex ring flow 涡环怜 vortex sheet 旋涡层 vortex source 涡源 vortex space 涡琳间 vortex street 涡街 vortex strength 涡量度 vortex surface 涡⾯ vortex tube 涡淋 vortex velocity 涡旋速度 vortex wake 涡粒 vorticity 涡量 vorticity density 涡量密度 vorticity tensor 涡度张量 vorticity transfer equation 涡度转移⽅程 vorticity transfer theory 涡度转移理论。
流体力学中英文术语
流体力学中英文术语Index 翻译(Fluid Mechanics)Absolute pressure,绝对压力(压强)Absolute temperature scales, 绝对温标Absolute viscosity, 绝对粘度Acceleration加速度centripetal, 向心的convective, 对流的Coriolis, 科氏的field of a fluid, 流场force and,作用力与……local, 局部的Uniform linear, 均一线性的Acceleration field加速度场Ackeret theory, 阿克莱特定理Active flow control, 主动流动控制Actuator disk, 促动盘Added mass, 附加质量Adiabatic flow绝热流with friction,考虑摩擦的isentropic,等熵的air, 气体with area changes, 伴有空间转换Bemoullii’s equation and, 伯努利方程Mach number relations,马赫数关系式,pressure and density relations, 压力-速度关系式sonic point,critical values, 音速点,临界值,stagnation enthalpy, 滞止焓Adiabatic processes, 绝热过程Adiabatic relations, 绝热关系Adverse pressure gradient, 逆压力梯度Aerodynamic forces, on road vehicles, 交通工具,空气动力Aerodynamics, 空气动力学Aeronautics, new trends in, 航空学,新趋势Air空气testing/modeling in, 对……实验/建模useful numbers for, 关于……的有用数字Airbus Industrie, 空中客车产业Aircraft航行器airfoils机翼new designs, 新型设计Airfoils, 翼型aspect ratio (AR), 展弦比cambered, 弧形的drag coefficient of , 阻力系数early, 早期的Kline-Fogleman, 克莱恩-佛莱曼lift coefficient, 升力系数NACA,(美国) 国家航空咨询委员会separation bubble, 分离泡stalls and, 失速stall speed, 失速速度starting vortex, 起动涡stopping vortex, 终止涡Airfoil theory, 翼型理论flat-plate vortex sheet theory, 平板面涡理论Kutta condition, 库塔条件Kutta-Joukowski theorem, 库塔-儒科夫斯基定理1thick cambered airfoils, 厚弧面翼型thin-airfoils, 薄翼型wings of finite span, 有限展宽的翼型A-380 jumbo jet, 大型喷气式客机Alternate states, 交替状态American multiblade farm HA WT, 美式农庄多叶水平轴风机Angle of attack, 攻角Angle valve, 角阀Angular momentum角动量differential equation of , 关于…的微分方程relation/theorem, 联系/理论Annular strips, 环形带Applied forces, linear momentum, 外加力,线性冲力Apron,of a dam, 大坝的护坦Arbitrarily moving/deformable control volume, 任意运动/可变形控制体Arbitrary fixed control volume, 任意固定控制体Arbitrary viscous motion, 随机粘性运动Archimedes, 阿基米德Area changes, isentropic flow. 域变换,等熵流Aspect ratio (AR), 展弦比Automobiles, aerodynamic forces on, 汽车,气动力A verage velocity, 平均速度Axial-flow pumps. 轴流泵Axisymmetric flow, stream function 轴对称流,流函数Axisymmetric Potential flow, 轴对称有势流hydrodynamic mass, 水力学质量Point doublet, 点偶极子point source or sink, 点源与点汇spherical Polar coordinates and, 球极坐标uniform stream in the x direction, x方向的均匀流uniform stream plus a point doublet, 均匀流附加点偶极子uniform stream plus a point source, 均匀流附加点源BBackward-curved impeller blades, 后向曲叶轮片,Backwater curves, 回水曲线Basic equations, non dimensional, 基本方程,无量纲的Bernoulli obstruction theory, 伯努利障碍理论Bernoulli's equation, 伯努利方程with adiabatic and isentropic steady flow, as绝热、等熵稳态流frictionless flow, 无摩擦流assumptions/restrictions for, 假想/约束HGLs and EGLs, 水力坡度线和能量梯度线steady flow energy and, 定常流动能量in rotating coordinates. 在旋转坐标下,Best efficiency point (BEP), pumps, 最佳效率点,Betz number, 贝兹数Bingham plastic idealization, 宾汉塑性理想化,Biological drag reduction, 生物学阻力衰减Blade angle effects, on pump head, 叶片安装角效率,泵头处Blasius equation, 布拉修斯方程Body drag, at high Mach numbers, 机体阻力,在高马赫数下Body forces, 体力Boeing Corp., 波音公司Boundaries, of systems, 边界,系统Boundary conditions. 边界条件,differential relations for fluid flow, 流体的微分关系nondimensionalizalion and, 无量纲化Boundary element method (BEM), 边界元方法2Boundary layer (BL) analysis, 边界层分析boundary layer flows, 边界层流动boundary layer separation on a half body, 边界层半体分离displacement thickness, 位移厚度drag force and, 阻力equations, 方程flat-plate. 平板,Karman's analysis, 卡门分析momentum integral estimates, 动量积分估计momentum integral relation. 动量积分关系momentum integral theory, 动量积分理论pressure gradient 压力梯度separation on a half body, 半模分离skin friction coefficient, 表面摩擦系数two-dimensional flow derivation, 二维流推导Boundary layers with Pressure gradient, 边界层压力梯度adverse gradient, 反梯度favorable gradient, 正梯度laminar integral theory, 层流积分理论,nozzle-diffuser example,喷口扩散算例Bourdon tube, 波登管Bow shock wave, 弓形激波Brake horsepower,制动马力Broad-crested weirs, 宽顶堰Buckingham Pi Theorem, 白金汉定理Bulb Protrusion, 球形突出物(船头)Bulk modulus. 体积模量Buoyancy, 浮力Buoyant particles, local velocity and, 悬浮颗粒,局部速度Buoyant rising light spheres, 浮力作用下自由上升的球体Butterfly valve, 蝶形阀CCambered airfoils, 弓型翼Cauchy-Riemann equations, 柯西-黎曼方程Cavitation/Cavitation number, 气穴/气蚀数Celsius temperature scales, 摄氏温标Center of buoyancy, 浮心Center of Pressure (CP),压力中心,压强中心Centrifugal pumps, 离心泵backward-curved impeller blades, 后曲叶轮片blade angle effects on pump head, 泵头处叶片安装角效率brake horsepower, 制动马力circulation losses, 环量损失closed blades, 闭叶片efficiency of, 效率的elementary pump theory. 基泵理论Euler turbomachine equations, 欧拉涡轮机方程eye of the casing, 泵体通风口friction losses, 摩擦损失hydraulic efficiency, 水力[液压]效率mechanical efficiency.机械效率open blades, 开放式叶片output parameters, 输出参数power, delivered, 功率,传递pump surge, 泵涌,scroll section of casing, 卷形截面,泵体,shock losses, 激波损失vaneless, 无叶片的3volumetric efficiency, 容积效率[系数]water horsepower, 水马力Centripetal acceleration, 向心加速度Channel control Point, 传送控制点Characteristic area. external flows, 特征区域,外流Chezy coefficient, 薛齐系数Chezy formula, 薛齐公式Chezy coefficient,薛齐系数flow in a Partly full circular pipe, 流体非充满的圆管流Manning roughness correlation. 曼宁粗糙度关系,normal depth estimates, 法向深度估计Choking, 壅塞;堵塞of compressors, 压缩机的due to friction, compressible duct and, 由于摩擦,可压缩管的isentropic flow with area changes, 变横截面积等熵流simple heating and, 单纯加热Circular cylinder, flow with circulation. 圆柱体,Circulation环量and flow past circular cylinder, 流体经过圆柱体losses, in centrifugal pumps, 损失,离心泵potential flow and, 有势流Circumferential pumps, 环型泵Classical venturi, 标准文氏管Closed blades, centrifugal pumps. 闭叶片,离心泵Closed-body shapes, 闭体外形,circular cylinder, with circulation, 圆柱体,环量Kelvin oval, 开尔文椭圆,Kutta-Joukowski lift theorem,库塔-儒科夫斯基升力定理,Potential flow analogs, 有势流模拟Rankine oval, 兰金椭圆rotating cylinders. lift and drag, 旋转柱体,升力与阻力Coanda effect, 柯恩达效应( 沿物体表面的高速气流在Cobra P-530 supersonic interceptor, 眼镜蛇超音速拦截机Coefficient matrix. 系数矩阵Coefficient of surface tension, 表面张力系数Coefficient of viscosity, 粘滞系数Commercial CFD codes, viscous flow, 商业的计算流体力学代码,粘流Commercial ducts, roughness values for, 商业管道Composite-flow, open channels, 合成流,开槽道Compressibility, non dimensional. 压缩性,无量纲Compressibility effects, 压缩效果Compressible duct flow with friction, 伴有摩擦的可压缩管流adiabatic, 绝热的, 隔热的choking and, 壅塞;堵塞isothermal flow in long pipelines, 管线中的等温流动,long pipelines, isothermal flow in, 管线,等温流动,mass flow for a given pressure drop, 给定压降下质量流动minor losses in, 最小损失subsonic inlet, choking due to friction, 亚音速进口,摩擦引发阻塞,supersonic inlet, choking due to friction, 超音速进口,摩擦引发阻塞,Compressible flow, 可压缩流flow with friction摩擦流choking and, 壅塞;堵塞converging-diverging nozzles, 拉瓦尔喷管converging nozzles, 收缩喷嘴Fanno flow, 法诺流动,gas flow correction factor, 气流校正参数hypersonic flow, 高超音速气流4incompressible flow, 不可压缩流isentropic.等熵的isentropic Process, 等熵过程,Mach number, 马赫数normal shock wave. 正激波the perfect gas, 理想气体Prandtl-Meyer waves. 普朗特-麦耶膨胀波shock waves. 激波specific-heat ratio, 比热比speed of sound and,声速subsonic, 亚音速的supersonic,超音速的transonic, 跨音速的two-dimensional supersonic, 二维超音速的Compressible gas flow correction factor, 可压缩气流校正因数Compressors, 压缩机Computational fluid dynamics (CFD), 计算流体力学pump simulations, 泵模拟viscous flow. 粘流Concentric annulus, viscous flows in, 同心环Cone flows, 锥体绕流Conformal mapping, 保角映射[变换] Conservation of energy, 能量守恒定律Conservation of mass. 质量守恒定律Consistent units, 相容单元Constants, 常量dimensional, 空间的pure, 纯粹的Constant velocity, fluid flow at, 常速度, 等速度Constructs, 结构Contact angle, 交会角Continuity, 连续性,equation of ,方程nondimensionalization and, 无量纲的Continuum, fluid as, 连续流体Contraction flow, 收缩流动Control Point, channel, 控制点,管道Control volume analysis,控制体分析angular momentum theorem. 角动量定理,arbitrarily moving/deformable CV,任意运动/可变形控制体arbitrarily fixed control volume, 任意固定控制体conservation of mass, 质量守恒定律control volume moving at constant velocity, 控制体以等速运动control volume of constant shape but variable velocity作变速运动的刚性控制体energy equation. 能量方程introductory definitions, 介绍性定义linear momentum equation. 线性动量方程,one-dimensional fixed control volume, 一维固定控制体,one-dimensional flux term approximations, 一维通量项近似Physical laws. 物理定律。
夏天的海边旅行 英语作文
A Summer Seaside EscapeThere is something undeniably alluring about a summer seaside trip,a time when the sun's rays are at their warmest,and the ocean's call is at its strongest.My journey to the coast was not just a vacation;it was an immersion into the heart of summer's embrace.The Anticipation of DepartureThe excitement began with the planning,the anticipation of sun-kissed days and starlit nights by the sea.The scent of sunscreen and the sound of waves in my mind,I packed my bags with a sense of adventure and a heart full of joy.The Arrival at the ShoreArriving at the shore,the first sight of the vast,shimmering ocean took my breath away.The azure expanse stretched out to the horizon, meeting the sky in a seamless blend of blues.The salty air filled my lungs, and the warmth of the sand beneath my feet was a welcome sensation. The Symphony of the SeaThe sound of the sea is a symphony of nature,with the crashing waves providing a rhythmic beat,the seagulls adding high notes,and the distant foghorns offering a deep,resonant call.This soundtrack of the sea is as timeless as it is soothing.Sunbathing and SurfingDays were spent sunbathing on the golden sands,the sun's rays a comforting caress on my skin.When the surf was up,I took to the waves, riding the surfboard as it danced with the ocean's rhythm.The thrill of surfing is a dance of balance,speed,and the raw power of the sea. Exploring the Coastal TreasuresThe coastline offered treasures to discover.I explored tide pools teeming with marine life,marveled at the intricate patterns of seashells, and hiked along cliffs that offered breathtaking views of the rugged coastline.Evening Strolls and SunsetsEvening strolls along the shoreline were a time of reflection and tranquility.The sun dipped into the ocean,painting the sky with hues of orange and pink,and the day's heat gently gave way to the cool evening breeze.The Night Sky Over the SeaAt night,the seaside took on a different charm.The inky sky was a canvas of stars,the Milky Way a river of light above the dark waters.The gentle lapping of the waves and the distant calls of nocturnal sea creatures created a lullaby that rocked me to sleep.The Taste of Seafood DelightsThe seaside offered a culinary adventure with fresh seafood delicacies. From succulent lobsters to flaky fish dishes,each meal was a celebration of the ocean's bounty,enjoyed with the backdrop of the setting sun. The Connection to the OceanThe seaside trip was a connection to the ocean's timeless beauty and its ever-changing moods.It was a reminder of the vastness of our planet and the simple pleasures that nature bestows upon us.The Memories MadeAs the trip came to an end,I carried with me more than just a tan;I carried memories of the sun,the sand,the sea,and the soul-soothing tranquility that only a summer seaside escape can offer.The Lasting ImpactThe summer seaside trip left an indelible mark on my heart.It was a reminder to seek the simple joys in life,to appreciate the beauty that surrounds us,and to cherish the moments that make life truly magical.。
ShockandDetonationWaves:激波和爆轰波
wave“In connection with the problem of the process of the chemical reaction in a detonation wave, the objections raised against theconceptions of Le Chatelier and Vieille of the 19to the ignition of the gas by the shock wave are refuted.”Zeldovich “On the theory of the propagation of detonation in gaseous 6/20/2007Detonation6Expansion waves catch up to wave and slow it down until CJ state is reached.Steady Reaction Zone2121122dYM u dx dP u M u dx du u M dx d uVU VV U U C2H4CO2H2O CO C2H4-3O2-9N2, 20kPa WarnatzOH H OConvection-reaction balanceC2H4-3O2-9N2, 20kPa Warnatz'V'HCharacteristic induction zone width 'Detonation10Propagating Pressure Wave GDT280mm diameter, 7.3m long•Velocity from time of arrival•Pressure from piezoelectric gauges•Structure from schieren, shadowgraph, PLIF imaging6/20/2007DetonationSchlieren OH emissionscale:4mm 2H2-O2-85%ArP o=20kPaC3H8-5O2-60%N2P o=20kPa0.0263 atm 2.7 km/s0.3 atm 2.2 km/s“Generalizations of available observations suggests that turbulenceDetonation H2+O2+7Ar mixtureSelf-propagating –near CJ velocityC2H4-O2 75% Ar H2-O2 40% ArC3H8-O2C2H2-O2“Notice that because of its innate complexity, there is virtually no hope that theoreticians will piece together an a priori theory for detonation structure; they •Cell width measurementsA sooted aluminum sheetData from R. Knystautas,McGill universityCH 4C 4H 10C 3H 8C 2H 6H 2C 2H 2Fuel Smoke PressureFoil OscillationsEQUIVALENCE RATIO0 1 2 3 41005020105210.50.2C 2H 46/20/2007Detonation21Quenching Q21= f(T,background)Absorption IQ= f (x)Boltzmann fcator N= f (T)Overlap integral* = f (T,p,background)2H2+O2+85%Ar, 20kPa2H2-O2-12Ar,P1=20kPa18x150mm test sectionimage height 60mmReference: J. Austin, F. PIntgen and J.E. Shepherd, ReactionZones in Highly Unstable Detonations, 30th Combustionimage height 150mmDetonation 256/20/2007Detonation 262H2+O2+17Ar,20kPa (Pintgen et al 2002)20 mm02468101214161820E a /R T Sf=12H2+O2+17Ar222C2H4-3O2-10.5N2C3H8-5O2-9N2C3H8-5O2-9N26/20/2007Detonation 29Numerical Tools for Shocks and Detonation (CJ) Computations •NASA CeC code•STANJAN (in CHEMKIN)•Cantera–Shock and detonation toolbox from Caltech•GASEQ–Computation not quite correct for detonations•CHEETAH (export controlled)–LLNL6/20/2007Detonation 30Numerical Tools for Reaction ZoneStructure •Chemkin-based programs–Reaction Design–ZND fortran program•Cantera-based programs–Caltech shock and detonation toolbox•NASA, …Detonation Phenomena•Initiation by Blast Waves•Diffraction through tubes openings and orifices•Limiting tube diameter•Deflagration-to-Detonation TransitionInitiation of Detonations•Direct initiation–Requires a strong blast wave –Fuel-oxygen mixtures•Exploding wire or•Electric discharge (spark) in air–Fuel-air mixtures•High explosives•Fuel-oxygen mixtures with DDT initiation•Deflagration-to-detonation transition–Weak ignition source (glowplug or spark plug)Detonation33What is the critical E needed to start a detonation?6/20/2007Detonation34Subcritical, E<EcSupercritical E>EcInside View Showing High-Explosive Detonating Cord Positioned on Bag AxisDetonation370.0 1.0 2.0 3.0 4.0EQUIVALENCE RATIOC 2H 4H 2C 2H 2C 3H 8CH 46/20/2007Detonation Diffraction CasesSuccessFailureSupercriticalCriticalIncreasing cell size and reaction timeTube Diameter = 1.83 m ; Bag Diameter = 3.66 mEQUIVALENCE RATIOc 0.4 0.6 0.8 1.0 1.2 1.4 1.6 1.85.02.01.00.50.20.1PROPANEETHYLENEHYDROGENACETYLENENo GoDetonationR STube Initiation ConfigurationHigh-Explosive Initiation Transmitted AirShock Wave Detonation WaveBag Trajectory (Contact Surface)6/20/2007Detonation45Deflagration to DetonationTransition in gases•Flames and detonation propagation regimes•Effect of confinement on flame propagation•Mechanisms of flame acceleration•Mechanisms involved in DDT•Pressure waves and structural response6/20/2007Detonation46Flames can become detonations!Example: DDT in tubesObstacles or roughness is verysignificantThe path of DDT6/20/2007Detonation 53Scaling of Detonation Onset 6/20/2007Detonation 54Effect of Expansion RatioReferences1. A discussion of high explosive detonation from a practicingengineer’s perspective is given by: P. W. Cooper. Explosives Engineering. VCH, 1996.2.More in-depth discussions are given in the compilation of: J. A.Zukas and W.P. Walters, editors. Explosive Effects andApplications. High Pressure Shock Compression of Condensed Matter. Springer, 1995.3.The classic reference on detonation is: Ya. B. Zel’dovich and A. S.Kompaneets. Theory of Detonation. Academic Press, NY, 1960. This is an English translation of original Russian. Out of print and in many ways out of date.4. A more up to date theoretical treatment is given by: W. Fickettand W. C. Davis. Detonation. University of California Press, Berkeley, CA, 1979 Now available as a Dover paperback.5.Gaseous detonations are discussed in most textbooks oncombustion.。
港航专业英语
23Scott L.DouglassRobert A.NathanJeffrey D.MalyszekProfessorDepartment of Civil Engineering University of South AlabamaMobile,AlabamaMoffat &Nichol EngineersTampa,FloridaMoffat &Nichol EngineersTampa,FloridaC OASTAL AND P ORTE NGINEERINGCoastal and port engineering encom-passes planning,design,and construc-tion of projects to satisfy society’s needs and concerns in the coastal environ-ment,such as harbor and marina development,shore protection,beach nourishment,and other constructed systems in the coastal wave and tide environment.Over time,the scope of this field of engineering has broadened from only navigation improvement and property protection to include recreational beaches and environmental considerations.It takes into account the environmental conditions unique to the coastal area,including wind,waves,tides,and sand movement.Thus,coastal engineering makes extensive use of the sciences of oceanogra-phy and coastal geomorphology as well as of geo-technical,environmental,structural,and hydraulic engineering principles.23.1Risk Level in Coastal ProjectsBecause of the nature of littoral drift,or longshore sand transport along the coasts,erosion caused by coastal engineering projects along adjacent shore-lines,sometimes several miles away,has been a recurring problem.Tools for prediction and evaluation of such shoreline dynamics are con-tinually improving but are still limited,in partbecause of nature’s unpredictability.Hence,post-construction monitoring of the response of nearby beaches is often a required component of coastal engineering projects.The design level of risk in many coastal engi-neering projects may be higher than in other civil engineering disciplines because the price of more effective design is often not warranted.The design environment is very challenging.It varies with time,since design conditions are often affected by storms that contain much more energy and induce very different loadings from those normally experienced.Also,because the physical processes are so complex,often too complex for theoretical description,the practice of coastal engineering is still much of an art.Con-sequently,practitioners should have a broad base of practical experience and should exercise sound judgment.The practice of coastal engineering has changed rapidly in the last several decades owing to in-creases in natural pressures,such as that created by sea-level rise,and societal pressures,such as those from growing populations along the coast with greater environmental awareness.The changes are recorded in the proceedings of specialty confer-ences,such as those of the American Society of Civil Engineering (ASCE),including Coastal Engineering Practice;Dredging,Ports,Coastal Sedi-ments,Coastal Zone,International Coastal Engin-eering Conference,and the Florida Shore andSource: Standard Handbook for Civil EngineersBeach Preservation Association’s Beach preser-vation Technology Conference series.Coastal Hydraulics and SedimentsWaves often apply the primary hydraulic forces of interest in coastal engineering.Tides and other water-level fluctuations control the location of wave attack on the shoreline.Waves and tides generate currents in the coastal zone.Breaking waves provide the forces that drive sand transport along the coast and can cause beach changes,including erosion due to coastal engineering projects.23.2Characteristics of WavesWater waves are caused by a disturbance of the water surface.The original disturbance may be caused by wind,boats or ships,earthquakes,or the gravitational attraction of the moon and sun.Most of the waves are initially formed by wind.Waves formed by moving ships or boats are wakes .Waves formed by earthquake disturbances are tsunamis .Waves formed by the gravitational attraction of the moon and sun are tides .After waves are formed,they can propagate across the surface of the sea for thousands of miles.The properties of propagating waves have been the subject of various wave theories for over a century.The most useful wave theory for engineers is the linear,or small-amplitude,theory.23.2.1Linear Wave TheoryEssentially,linear wave theory treats only a train of waves of the same length and period in a constant depth of water.As in optics,this is called a monochromatic wave train.Linear wave theory relates the length,period,and depth of waves as indicated by Eq.(23.1).L ¼gT 22p tan h 2p dL(23:1)where L ¼wavelength,ft,the horizontal distancebetween crestsd ¼vertical distance,ft,between mean orstill water level and the bottom g ¼acceleration due to gravity,32.2ft /s T ¼wave periods,the time required forpropagation of a wave crest over the wavelength (Fig.23.1)Wave height H ,the fourth value needed to com-pletely define a monochromatic wave train,is an independent value in linear wave theory,but not for higher-order wave theories (Art.23.2.2).Fig.23.1Wave in shallow water.Water particles follow an elliptical path.L indicates length of wave,crest to crest;H wave height,d depth from still-water level to the bottom.The wave period T is the time for a wave to move the distance L .23.2n Section Twenty-ThreeEquation (23.1),implicit in terms of L ,requires an iterative solution except for deep or shallow water.When the relative depth d /L is greater than 1⁄2,the wave is in deep water and Eq.(23.1)becomesL ¼gT 22(23:2)For shallow water,d =L ,1⁄25,eq.(23.1)reduces toL ¼T ffiffiffiffiffigd p (23:3)Individual water particles follow a closed orbit.They return to the same location with each passing wave.The orbits are circular in deep water and elliptical in shallow water.Linear wave theory equations for the water-particle trajectories,the fluctuating water-particle velocities and accelera-tions,and pressures under wave trains are given in R.G.Dean and R.A.Dalrymple,“Water Wave Mechanics for Scientists and Engineers,”Prentice-Hall,Englewood Cliffs,N.J.();R.M.Sorenson,“Basic Wave Mechanics:For Coastal and Ocean Engineers,”John Wiley &Sons,Inc.,New York ().)23.2.2Higher-Order Wave TheoriesThe linear wave theory provides adequate approxi-mations of the kinematics and dynamics of wave motion for many engineering applications.Some areas of concern to civil engineers where the linear theory is not adequate,however,are very large waves and shallow water.Higher-order wavetheories,such as Stokes’second order and cnoidal wave theories,address these important situations.Numerical wave theories,however,have the broadest range of eful tables from stream-function wave theory,a higher-order,num-erical theory,are given in R.G.Dean,“Evaluation and Development of Water Wave Theories For Engineering Applications,”Special Report No.1,U.S.Army Coastal Engineering Research Center,Ft.Belvoir,Va.Determination of the water surface elevations for large waves or waves in shallow water requires use of a higher-order wave theory.A typical waveform is shown in Fig.23.2.The crest of the wave is more peaked and the trough of the wave is flatter than for the sinusoidal water surface profile in linear wave theory.For a horizontal bottom,the height of the wave crest above the still-water level is a maximum of about 0.8d .(“Shore Protection Manual,”4th ed.,U.S.Army Coastal Engineering Research Center,Government Printing Office,Washington,D.C.();“Coastal Engineering Manual,”( /inet /usace-docs /eng-manuals /em-htm).)23.2.3Wave TransformationsAs waves move toward the coast into varying water depths,the wave period remains constant (until breaking).The wavelength and height,how-ever,change because of shoaling,refraction,diffraction,reflection,and wavebreaking.Fig.23.2Water surface for a large wave in shallow water.Coastal and Port Engineering n 23.3Shoaling n As a wave moves into shallower water the wavelength decreases,as indicated by Eq.(23.1),and the wave height increases.The increase in wave height is given by the shoaling coefficient K s.K s¼HH0o(23:4)where H¼wave height in a specific depth of water H0o¼deep-water unrefracted wave height K s varies as a function of relative depth d/L as shown in Table23.1.For an incident wave train of period T,Table23.1can be used to estimate the wave height and wavelength in any depth with Eq.(23.2)for L o.Refraction n This is a term,borrowed from optics,for the bending of waves as they slow down. As waves approach a beach at an angle,a portion of the wave is in shallower water and moving more slowly than the rest.Viewed from above,the wave crest appears to bend.Refraction changes the height of waves as well as the direction of propagation.Refraction can cause wave energy to be focused on headlands and defocused from embayments.There are two general types of refraction models.Wave-ray models trace the path of wave rays,lines perpendicular to the wave crests.The other type of computer refraction model computes solutions to differential equations for the wave-heightfield.The physics simulated varies slightly from model to model.Diffraction n Another term borrowed from optics,this is the spread of energy along a wave crest.An engineering example of wave diffraction is the spreading of energy around the tip of a breakwater into the lee of the breakwater.The wave crest wraps around the tip of a breakwater and appears to be propagating away from that point.Diffraction also occurs in open water where refraction occurs.It can reduce the focusing and bending due to refraction.Reflection n Waves are reflected from obstruc-tions in their path.Reflection of wave energy is greatest at vertical walls,90%to100%,and least for beaches and rubble structures.Undesirable wave-energy conditions in vertical-walled marinas can often be reduced by placing rubble at the water line.Breaking n This happens constantly along a beach,but the mechanics are not well modeled by theory.Thus,much of our knowledge of breaking is empirical.In shallow water,waves break when they reach a limiting depth for the individual wave. This depth-limited breaking is very useful in coastal structure design and surf-zone dynamics models.For an individual wave,the limiting depth is about equal to the water depth and lies in the range given by Eq.(23.5.).0:8,Hdmax,1:2(23:5)where(H/d)max¼maximum ratio of wave height to depth below mean water level for a breaking wave.The variation in(H/d)b(the subscript b means breaking)is due to beach slope and wave steepness H/L.Equation(23.5)is often useful in selecting the design wave height for coastal structures in shal-low water.Given an estimate of the design water depth at the structure location,the maximum wave height H max that can exist in that depth of water is about equal to the depth.Any larger waves would have already broken farther offshore and been reduced to H max.23.2.4Irregular WavesThe smooth water surfaces of monochromatic wave theories are not realistic representations ofTable23.1Shoaling Coefficient and Wavelength Changes as Waves Move into Shallower Waterd/L o d/L K s0.0050.028 1.700.0100.040 1.430.0200.058 1.230.0300.071 1.130.0400.083 1.060.0500.094 1.020.100.140.200.220.300.310.500.50 1.023.4n Section Twenty-Threethe real surf zone.Particularly under an active wind,the water surface will be much more irregular.Two different sets of tools have been developed by oceanographers to describe realistic sea surfaces.One is a statistical representation and one is a spectral representation.Statistics of Wave Height n The individual waves in a typical sea differ in height.The heights follow a theoretical Rayleigh distribution in deep water.In shallow water,the larger individual waves break sooner,and thus the upper tail of the distribution is lost.A commonly used,single wave-height para-meter is the significant wave height H1/3.This is the average of the highest one-third of the waves. Other wave heights used in design can be related to H1/3via the Rayleigh distribution as indicated in Table23.2.23.2.5Wave SpectraSpectral techniques are available that describe the amount of energy at the different frequencies or wave periods in an irregular sea.They provide more information about the irregular wave train and are used in some of the more advanced coastal-structure design methods.A wave-height parameter that is related to the total energy in asea is H mo .(H mois often called significant waveheight also.)Significant wave height H s is a term that has a long history of use in coastal engineering and oceanography.As indicated above and in Art.23.2.4,two fundamentally different definitions for significant wave height are used in coastal engineering.One is statistically based and the other is energy-or spectral-based.Since they are different,the notations,H1/3and H moare recom-mended to avoid confusion in use of H s:H1=3¼statistical significant wave heightH mo¼spectral significant wave heightIn deep water,H mois approximately equal to H1/3. In shallow water,and in particular in the surf zone, the two parameters diverge.(There is little that is truly significant about either parameter.Few of the waves in an actual wave train will have the significant height.It is basically a statistical artifact.)Transformations of actual wave seas such as shoaling,refraction,diffraction,and breaking are not completely understood and not well modeled. Although the monochromatic wave transforma-tions are well modeled,as described in the preceding,in actuality the individual waves and wave trains interact with each other and change the wavefield.(These wave-wave interactions are the subject of significant research efforts.)Thus, the more realistic conditions,that is,irregular seas, are the least understood.However,models that account for the transformation of wave spectra across arbitrary bottom contours are available.23.2.6Wave Generation by Wind Waves under the influence of the winds that generated them are called sea.Waves that have propagated beyond the initial winds that generated them are called swell.Fetch is the distance that a wind blows across the water.For enclosed bays,this is the distance across the water body in the direction of the wind. Duration is the time that a wind at a specific speed blows across the water.The waves at any spot may be fetch-limited or duration-limited.When a windTable23.2Wave Heights Used in DesignSymbol Description Multiple of H1/3 H1/3Average height of highest one-third of waves 1.0H av Average wave height0.6H10Average height of highest10%of waves 1.3H1%Wave height exceeded1%of the time 1.6H sin Height of simple sine waves with same energyas the actual irregular height wave train 0.8Coastal and Port Engineering n23.5starts to blow,wave heights are limited by the short time that the wind has blown;in other words,they are duration-limited.Seas not duration-limited are fully arisen .If the waves are limited by the fetch,they are fetch-limited.For enclosed bay and lake locations,simple parametric models can provide useful wave information.Table 23.3gives wave height and wave period estimates for deep water for different fetch distances and different wind speeds.The values are based on the assumption that the wind blows for a sufficient time to generate fully arisen conditions.In shallow water,the wave heights will be less.On the open ocean,waves are almost never fetch-limited.They are free to continue to move after the wind ceases or changes.Swell wave energy can propagate across entire oceans.The waves striking the beach at any moment in time may include swell from several different locations plus a local wind sea.Thus,for an open-ocean situation,numerical models that grid the entire ocean are required to keep track of wave-energy propagation and local generation.Wave-generation models can forecast waves for marine construction operations.They can also hindcast,that is,estimate waves based on measured or estimated winds at times in the past,for wave climatology studies,probabilistic design,or historic performance analysis.The U.S.Army Corps of Engineers “Wave Information Study(WIS)”has hindcast 40years of data,1956–1995,to generate probabilistic wave statistics for hun-dreds of locations along the coasts of the United States.The wave statistics are available in tabular form,and the actual time sequence of wave conditions is available in digital form.(J.B.Herbich,“Handbook of Coastal and Ocean Engineering,”Gulf Publishing Company,Houston,Tex ().)23.2.7Ship and Boat WakesShip wakes are sometimes the largest waves that occur at a location and thus become the design wave.Vessel wakes from large ships can be up to 6ft high and have wave periods less than 3s.Ship wakes can be estimated with methods presented in J.R.Weggel and R.M.Sorensen,“Ship Wave Prediction for Port and Channel Design,”Proceed-ings,Port Conference,1986,ASCE.Approaches for estimating the wakes due to recreational boats are presented in ASCE Manual 50,“Planning and Design Guidelines for Small-Craft Harbors,”and R.R.Bottin et al.,“Maryland Guide Book for Marina Owners and Operators on Alternatives Available for the Protection of Small Craft against Vessel Generated Waves,”U.S.Army Corps of Engineers Coastal Engineering Research Center,Washington,D.C.Table 23.3Spectral Significant Heights and Periods for Wind-Generated Deep-Water Waves*Wind speed,knotsFetch length,statute miles0.512105020H m o ,ft 0.60.8 1.1 2.2 4.1T p ,s 1.3 1.6 2.0 3.2 4.740H m o ,ft 1.3 1.8 2.5 5.411T p ,s 1.7 2.2 2.7 4.5760H m o ,ft 2.2 3.1 4.29.118T p ,s2.12.63.25.48*Based on method presented in S.L.Douglass et al.,“Wave Forecasting for Construction in Mobile Bay,”Proceedings,Coastal Engineering Practice,1992,pp.713–727,American Society of Civil Engineers.H m o ¼spectral significant wave height and T p ¼wave period.23.6n Section Twenty-Three23.3Design Coastal WaterLevelsThe design water level depends on the type of project.For design of some protective coastal structures,for example,a water level based on a recurrence interval such as a10-year or100-year return period often is selected.The Federal Emergency Management Agency(FEMA)“Flood Insurance Rate Maps(FIRM)”are based on such a concept.They provide afirst estimate of high-water levels along the U.S.coastlines.Since the design of some coastal structures can be extremely sensitive to the design water level,more in-depth analysis may be justified.For engineering projects con-cerned with normal water levels,for example, where dock elevations and beachfill elevations are determined by the water level,an estimate of the normal water level and the normal range around that mean is needed.All coastal engineer-ing projects should be designed to take into account the full range of potential water levels.The water level at any time in a specific location is influenced by the tides,mean sea-level elevation, storm surge,including wind influence,and other local influences,such as fresh-water inflow in estuaries.Tides n The tide is the periodic rise and fall of ocean waters produced by the attraction of the moon and sun.Generally,the average interval between successive high tides is12h25min,half the time between successive passages of the moon across a given meridian.The moon exerts a greater influence on the tides than the sun.Tides,however, are often affected by meteorological conditions, including propagation of storm tides from the sea into coastal waters.The highest tides,which occur at intervals of half a lunar month,are called spring tides.They occur at or near the time when the moon is new or full,i.e.,when the sun,moon,and earth fall in line, and the tide-generating forces of the moon and sun are additive.When the lines connecting the earth with the sun and the moon form a right angle,i.e., when the moon is in its quarters,then the actions of the moon and sun are subtractive,and the lowest tides of the month,the neap tides,occur.Tidal waves are retarded by frictional forces as the earth revolves daily around its axis,and the tide tends to follow the direction of the moon.Thus,the highest tide for each location is not coincident with conjunction and opposition but occurs at some constant time after new and full moon.This interval,known as the age of the tide,may amount to as much as21⁄2days.Large differences in tidal range occur at different locations along the ocean coast.They arise because of secondary tidal waves set up by the primary tidal wave or mass of water moving around the earth.These movements are also in-fluenced by the depth of shoaling water and con-figuration of the coast.The highest tides in the world occur in the Bay of Fundy,where a rise of 100ft has been recorded.Inland and landlocked seas,such as the Mediterranean and the Baltic, have less than1ft of tide,and the Great Lakes are not noticeably influenced.Tides that occur twice each lunar day are called semidiurnal tides.Since the lunar day,or time it takes the moon to make a complete revolution around the earth,is about50min longer than the solar day,the corresponding high tide on succes-sive days is about50min later.In some places,such as Pensacola,Florida,only one high tide a day occurs.These tides are called diurnal tides.If one of the two daily high tides is incomplete,i.e.,if it does not reach the height of the previous tide,as at San Francisco,then the tides are referred to as mixed diurnal tides.Table23.4gives the spring and mean tidal ranges for some major ports.There are other exceptional tidal phenomena. For instance,at Southampton,England,there are four daily high waters,occurring in pairs,separa-ted by a short interval.At Portsmouth,there are two sets of three tidal peaks per day.Tidal bores,a regular occurrence at certain locations are high-crested waves caused by the rush offlood tide up a river,as in the Amazon,or by the meeting of tides, as in the Bay of Fundy.The rise of the tide is referred to some estab-lished datum of the charts,which varies in different parts of the world.In the United States,it is mean lower low water(MLLW).Mean high water is the average of the high water over a19-year period,and mean low water is the average of the low water over a19-year period. Higher high water is the higher of the two high waters of any diurnal tidal day,and lower low water is the lower of the two low waters of any diurnal tidal day.Mean higher high water is the average height of the higher high water over a19-year period,and mean lower low water is the Coastal and Port Engineering n23.7average height of the lower low waters over a 19-year period (tidal epoch).Highest high water and lowest low water are the highest and lowest,respectively,of the spring tides of record.Mean range is the height of mean high water above mean low water.The mean of this height is generally referred to as mean sea level (MSL).Diurnal range is the difference in height between the mean higher high water and the mean lower low water.The National Ocean Service annually publishes tide tables that give the time and elevation of the high and low tides at thousands of locations around the world and that can be used to forecast water levels at all times.The tide tables forecast the repeating,astronomical portions of the tide for specific locations but do not directly account for the day-to-day effects of changes in local winds,pressures,and other factors.Along most coasts,the tide table forecasts are within 1ft of the actual water level 90%of the time.Relative sea-level rise is gradually changing all of the epoch-based datum at any coastal site.Although,the datum that is used for design and construction throughout an upland area is not particularly important,the relation between con-struction and actual water levels in the coastal zone can be extremely important.The level of the oceans of the world has been gradually increasing for thousands of years.The important change is the relative sea-level change,the combined effect of water level and land-mass elevation changes due to subsidence (typical of the U.S.Atlantic and Gulf coasts)or rebound or emergence (Pacific coast of the U.S.).Measured,long-term tide data for major U.S.ports show that the relative sea-level rise differs from location to location.For example,Table 23.4Mean and Spring Tidal Ranges for Some of the World’s Major Ports*Mean range,ftSpring range,ft Anchorage,Alaska 26.729.6†Antwerp,Belgium15.717.8Auckland,New Zealand 8.09.2Baltimore,Md 1.1 1.3Bilboa,Spain 9.011.8Bombay,India 8.711.8Boston,Mass.9.511.0Buenos Aires,Argentina2.2 2.4Burntcoat Head,Nova Scotia (Bay of Fundy)41.647.5Canal Zone,Atlantic side 0.7 1.1†Canal Zone,Pacific side 12.616.4Capetown,Union of South Africa 3.8 5.2Cherbourg,France 13.018.0Dakar,Africa 3.3 4.4Dover,England 14.518.6Galveston,Tex 1.0 1.4†Genoa,Italy 0.60.8Gibraltar,Spain2.33.1Hamburg,Germany 7.68.1Havana,Cuba1.0 1.2Hong Kong,China 3.1 5.3†Honolulu,Hawaii 1.2 1.9†Juneau,Alaska14.016.6†La Guaira,Venezuela 1.0†Lisbon,Portugal 8.410.8Liverpool,England 21.227.1Manila,Philippines 3.3†Marseilles,France 0.40.6Melbourne,Australia 1.7 1.9Murmansk,U.S.S.R.7.99.9New York,N.Y. 4.4 5.3Osaka,Japan 2.5 3.3Oslo,Norway 1.0 1.1Quebec,Canada 13.715.5Rangoon,Burma 13.417.0Reikjavik,Iceland 9.212.5Rio de Janeiro,Brazil 2.5 3.5Rotterdam,Netherlands 5.0 5.4San Diego,Calif. 4.2 5.8†San Francisco,Calif. 4.0 5.7†San Juan,Puerto Rico 1.1 1.3Seattle,Wash.7.611.3†Shanghai,China 6.78.9Singapore,Malaya5.67.4Table 23.4(Continued )Mean range,ftSpring range,ft Southampton,England 10.013.6Sydney,Australia 3.6 4.5Valparaiso,Chile 3.0 3.9Vladivostok,U.S.S.R.0.60.7Yokohama,Japan 3.5 4.7Zanzibar,Africa8.812.4*“Tide Tables,”National Ocean Service.†Diurnal range.23.8n Section Twenty-Threeat Galveston,Tex.,there has been about1ft of relative sea-level rise during the last50years.At Anchorage,Alaska,there has been about2ft of relative sea-level fall during the last50years.The impact of long-term sea-level rise has rarely been taken into account in design,except when it has already impacted the epoch-based tidal datum, such as MLLW.The National Geodetic Vertical Datum(NGVD)was established at the mean sea level(MSL)of1929.Since sea-level rise has con-tinued since then,the NGVD is now below the current day MSL along much of the U.S.Atlantic and Gulf coasts.At many locations,it is between the MSL and the MLLW.For accurate location of the NGVD relative to the MSL or MLLW,analysis with data from a local tide gage is required.For some harbor and coastal design,a staff gage is installed for recording water levels for a sustained period of time to confirm the relation between the local surveyor’s elevation datum,the assumed tidal datum,and the actual water surface elevation.Storm Surge n This can be defined broadly to include all the effects involved in a storm,inclu-ding wind stress across the continental shelf and within an estuary or body of water,barometric pressure,and wave-induced setup.The combined influence of these effects can change the water level by5to20ft depending on the intensity of the storm and coastal location.Engineers can use return-period analysis curves to estimate the likelihood of any particular elevation.The Federal Emergency Management Agency and the various Corps of Engineer Districts have developed such curves based on historic high-water-mark elevations and numerical models of the hydrodynamics of the continental shelf.23.4Coastal SedimentCharacteristicsMost beach sediments are sand.The day-to-day dynamics of the surf zone usually ensure that most fines,silts,and clays will be washed away to more quiescent locations offshore.Some beaches have layers of cobbles,rounded gravel,or shingles,flattened gravel.The size and composition of beach sands varies around the world and even along adjacent shore-lines.Essentially,the beach at any particular site consists of whatever loose material is available.Quartz is the most common mineral in beach sands. Other constituents in sands include feldspars and heavy minerals.Some beaches have significant por-tions of seashell fragments and some beaches are dominated by coral carbonate material.Beach sands are usually described in terms of grain-size distribution.The median diameter d50is a common measure of the central size of the distribution.The range of the distribution of sand sizes around this median is usually discussed in terms of sorting.The color of the sand depends primarily on the composition of the grains.The black sand beaches of Hawaii are derived from volcanic lava.The white sands of the panhandle of Florida are quartz that has developed a white color owing to mini-ature surface abrasions and bleaching.23.5Nearshore Currents andSand TransportAs wave energy enters the surf zone,some of the energy is transformed to nearshore currents and expended in sand movement.The nearshore cur-rentfield is dominated by the incident wave energy and the local windfield.The largest currents are the oscillatory currents associated with the waves. However,several forms of mean currents(long-shore currents,rip currents associated with nearshore circulation cells,and downwelling or upwelling associated with winds)can be important to sand transport.Longshore current is the mean current along the shore between the breaker line and the beach that is driven by an oblique angle of wave approach. The waves provide the power for the mean long-shore current and also provide the wave-by-wave agitation to suspend sand in the current.The resulting movement of sand is littoral drift or longshore sand transport.This process is referred to as a river of sand moving along the coast. Although the river-of-sand concept is an effective, simple explanation of much of the influence of engineering on adjacent beaches,the actual sand transport paths are more complex.This is par-ticularly so near inlets with large ebb-tidal shoals that influence the incident wave climate.Even on an open coast with straight and parallel offshore bottom contours,the longshore-sand-transport direction changes constantly in response to changes in the incident wave height,period,and Coastal and Port Engineering n23.9。
The Calm within the Storm of Emotion
**The Calm within the Storm of Emotion**In the tempestuous sea of human emotions, there exists a hidden refuge of calm, a serene oasis amid the swirling chaos and tumultuous waves.As the Stoic philosopher Epictetus once said, “It's not what happens to you, but how you react to it that matters.” This profound wisdom holds the key to uncovering the calm within the storm of emotion.The storm of emotion can often be overwhelming, like a fierce tempest that threatens to capsize our inner equilibrium. Picture a person who has just received devastating news – the loss of a job, a serious illness, or the end of a significant relationship. The initial shock and pain can feel like a violent storm, clouding judgment and filling the heart with turmoil.Yet, within this very storm lies the potential for finding calm. It might manifest as a moment of acceptance, a recognition that while the circumstances are beyond control, the response is within one's power. A person in such a situation might take a deep breath and decide to focus on the positive aspects of their life, or to view the setback as an opportunity for growth and change.Another example could be the stress and anxiety of a student facing an important examination. The pressure builds, creating a storm of nerves and self-doubt. But by practicing mindfulness and focusing on the present moment, the student can find a sense of calm, concentrating on the task at hand rather than succumbing to fear.In the midst of a collective emotional storm, such as a natural disaster or a global crisis, acts of kindness and solidarity can bring about an inner calm. Volunteers coming together to help those in need, strangers offering comfort and support –these gestures create a ripple of hope and compassion that calms the collective spirit.For instance, during a pandemic, while fear and uncertainty abound, healthcare workers selflessly dedicating themselves to saving lives serve as beacons of calm and inspiration. Their courage and commitment remind us of the strength of the human spirit and the possibility of finding tranquility even in the most trying times.However, attaining this inner calm is not an effortless feat. It requires discipline, self-awareness, and a conscious effort to shift perspective. But as the poet Rumi wisely stated, “The quieter you become, the more you can hear.” By quieting the noise of emotion and seeking the stillness within, we can access a wellspring of calm that sustains us through life's storms.In conclusion, the calm within the storm of emotion is not an elusive mirage but atangible reality that awaits our discovery. It is a source of strength, resilience, and wisdom that allows us to navigate the rough waters of life with grace and equanimity. Let us cultivate this inner calm, for it is the anchor that holds us steady when the winds of emotion howl.。
海底两万里第四章怒涛来袭读后感受
海底两万里第四章怒涛来袭读后感受英文回答:Chapter 4 of "Twenty Thousand Leagues Under the Sea" is an intense and thrilling chapter that showcases the power and danger of the sea. The chapter is titled "The Maelstrom," which refers to a powerful whirlpool that threatens the Nautilus and its crew.In this chapter, the Nautilus finds itself in the midst of a massive storm. The waves crash against the submarine, and the crew must do everything they can to keep the vessel afloat. The description of the storm and the sea is vivid and immersive, making the reader feel as if they are right there in the midst of the raging ocean.One of the most memorable moments in this chapter is when the Nautilus gets caught in the Maelstrom. Thewhirlpool threatens to swallow the submarine, and the crew must use all their skills and knowledge to escape its grasp.This scene is filled with tension and suspense, keeping the reader on the edge of their seat.Another aspect of this chapter that stands out is the portrayal of Captain Nemo. Despite the danger they face, Nemo remains calm and composed, showing his expertise and experience as a captain. His leadership and quick thinking are admirable, and it adds to the excitement of the chapter.Overall, the fourth chapter of "Twenty Thousand Leagues Under the Sea" is a thrilling and action-packed read. It showcases the power of the sea and the bravery of the Nautilus crew in the face of danger.中文回答:《海底两万里》第四章《怒涛来袭》是一章充满紧张和刺激的章节,展示了海洋的力量和危险。
Physics
KinematicsVocabularyKinematics--is the study of description of motionDisplacement--is the magnitude of the change in position and the direction. Scalar--a scalar quantity has only magnitude.Vector--a vector quantity has both magnitude and directionVelocity--displacement/time m/s ;vector, have directionSpeed--distance/time m/s ;scalarAcceleration--rate of change of velocityInstantaneous velocity--velocity at a particular instant.Acceleration of free fall--Force exerted by the earth on the objects (ignoring air friction)Stroboscope: Device (instrument) that captures images of objects every 1/50 of a second.Terminal velocity-- Constant (uniform) velocity when the forces are balanced. Direct proportion--the quantities vary directly. a∝bInverse proportion: vary inversely. a∝1/bExponential variation: a∝b2PLO-Designing an experimentAim:Materials required:Procedure: in point formDisplay of results:-table -graphResults:Errors in the experiment and ways to improve to get accurate results:PLO- Equation of motion-uniforming accelerated object.1)V f=V o+at2)a=(V f-V o)/t3)d=V o t+1/2×at24)d=(V f+V o)/2 ×t5)V f2=V o2+2adV f=final velocity m/s a=acceleration m/s2 t=time sV o= initial velocity m/s d=displacementPLO-Definition in motion and graphPLO-Projectiles-projectiles are objects which are fired into the air-their motion obeys kinematic equations completely if we ignore air resistance -objects launched with a horizontal velocity and dropped form the same height willalways strike the ground at the same time.-the time projectile spends in the air depends upon its initial velocity and vertical acceleration only.The horizontal: d x=V o t+1/2×at2The vertical: d y=-1/2×gt2DynamicsDifferent between kinematic and dynamics: kinematics describe how an object moves; dynamics describe why it moves.Force: push or pull exerted by an object on the other.Unit of force: Newton (N) 1Newton=1kgm/s2Types of forces:-frictional force (necessary evil)-gravitational fore (exist everywhere)-electric force-Magnetic force-air resistance-centrifugal force-centripetal force-normal force (F N): acts perpendicular to the surface on which the object is placed.PLO-Newton's law of motion:Newton's first law (law of inertia)When no external, unbalanced force acts on an objects, its velocity remain constant.If no net force acts on an object, it maintains its state of rest or its constant speed in a straight line.Newton's second law:When an external, unbalanced force acts on an object, the object accelerates. The accelerations is in the same direction as the net force acting on the object.The acceleration varies directly with the net force applied.The acceleration varies inversely with the mass of the object.F net=maNewton's third law:For every action there is an equal and opposite reaction.Action and reaction always occur in pairs.F1=-F2PLO-Newton's law of universal gravitationState the :a)the gravitational force is directly proportional to the product of their masses: Fg∝m1m2b)The gravitational force is inversely proportional to the square of the distance between the centre of the objects.Fg∝1/r2Fg∝m1m2/r2Fg=Gm1m2/r2G=universal gravitational constant=×10-11kg2→measured by Cavemdish using a torsion balance*mass of the earth=×1024kgRadius of the earth=×106mThe Frictional force:Acts in the opposite direction to the movement of the object. It's represented by F f.The frictional force depends on:I) the normal forceII) the nature of the surface →coefficient of friction→denoted by μ(mu)F f=μF NEnergyVocabularyElastic--able to stretch and return to its original size and shapeElastic potential energy--energy possessed by an elastic object.Extension--extended length-original lengthConservation--momentum doesn't changeMomentum--p=mvMechanical energy--The energy acquired by the objects upon which work is done is known as mechanical sum of andEnergy--the capacity to do workPotential energy--(stored energy) =mghKinetic energy--energy possessed by a moving object. =1/2(mv2)Work--W=F×dPower --is the rate at which work is done or energy transformed. (work done)/(time) & (energy changed)/(time)Efficiency=(work output)/(work input)×100%Work input: work supplied into the systemWork output: useful work doneConservation of energy: Law of conservation of energy--energy can either be created or destroyed but only transformed from a form to another.Hooke's law: The force applied is directly proportional to the extension.F=kxF=force applied, x=extension; k=force constant*breaking point: point to which the object exceeds its elastic limit.Momentum:-concept of momentum-Impulse and momentum-Collisions and explosions-Elastic and inelastic collisionF t=p=m△vConservation of momentum:-not changing conserved during collisions.-"head on"In linear Interaction:1)elastic--object collide and move away from each otherBefore collision:Total momentum=m1v1+m2v2After collision:Total momentum=m1v1'+m2v2'2)Inelastic--objects collide, stick together and travel at a common velocity. Before collision:Total momentum=m1v1+m2v2After collision:Total momentum=(m1+m2)V'Law of conservation of momentum:total momentum before collision=total momentum after collisionMechanical energyMechanical energy can be either kinetic energy or potential energy:Total mechanical energy= potential energy+kinetic energyLoss in PE=gain in KE →law of conservation of mechanical energyME=mgh+1/2( mv2)powerPower is the rate at which work is done or energy transformed.Power=(work done)/(time) & (energy changed)/(time) (J/s)Power=Force×velocity P=FVSI unit of power is Watt (W)P=I2 R P=V2/R P=IVWorkEfficiency=(work output)/(work input)×100%A.Energy is defined as the ability to do work.B.Work=force×displacementC.Work is measured in which is also called a joule (J)D.Although work is a product of two vector quantities, it is a scalar quantity.E.When the force is not in the same direction as the displacement, must use the component of the force that is in the direction of the displacement.PLO-waves: characteristicsVocabulary:Pulse-a single disturbance moving through a medium from one location to another location.Wave-a single pulse with a crest and a trough.Crest-upper part of the wave.Trough-lower portion of the waveWave motion-series of wavesRarefactions-air particles are far apartCompression-region where the air particle are closerMedium-the substance or material which carries the wave.(water air solids) Transverse wave-(light water) Direction of wave motion is vertical to the particle motionLongitudinal wave-(sound wave) direction of wave motion is in line with the displacement of the particles.Progressive wave-wave that continues.Frequency-The number of complete waves formed in a second. Measured in Hertz (Hz). Amplitude-The maximum displacement of the wave from the mean position. Wavelength-the distance travelled by a complete in metres lambda (λ)Simple harmonic motion-motion that make complete cycles over a period of time. Vibration-continuous movement of particles.Slinky-Transverse progressive wave-The direction of wave motion is perpendicular to the displacement of the particles.A wave transport only energy and not the particles-energy transport phenomenonSine wave-sinusoidal wave.Time period- time takes to make one complete wave, oscillation. F=1/T T=1/f=1/hertz=secondSpeed of sound-350m/sSpeed of light- 3×10^5 km/sMechanical wave- wave that require a medium to pass through.(ex: sound ,water) Universal wave equation-velocity(or speed)=frequency ×wavelength. V=f λPLO-properties of waves.1)ReflectionLight waves: reflection is bouncing of waves when they hit a reflecting surface wavesLaw of reflection:-The angle of incidence is equal to the angle of reflection ∠i =∠r- theincident ray, reflected ray and the normal lie on the same plane.Water waves: Reflect like light waves. Refract when they travel from deep to shallow region.Speed of the waves decreases wavelength decreases frequency remains unchanged.Sound waves:reflect when they hit objects.2)RefractionRefraction means bending waves reflect when they travel from one medium to the other.Light waves:- the speed of light increased when it goes into the less dense medium.(angle become bigger)- the speed of light depressed when it goes into the more dense medium.(angle become smaller)Absolute refractive index=(speed of light in vacuum)/(speed of light in medium) n=C/VRelative refractive index: If light travels from air to glass we talk about relative refractive index.Sin i/Sin r= refractive indexVocabulary:Mach number-the ratio of the speed of an object to the speed of sound.Sonic boom-the great sound happened when the airplane fly in a high speed across the compressed air in front.DecibelReverberationSonarRadar:PLO-properties of waves:Diffraction: waves become circular when they enter a narrow or wide opening.They tend to cancel out.Doppler effect: The frequency of a source increasses when it approaches the receiver.Polarisation: Changing the vibrational modes of electromagnetic radiation.PLO-Images-In optical instruments the images are formed when lenses (or) mirrors are used. - The image that is formed on a screen is called a real image. -The image that is not formed on a screen is called a virtual image.Characteristics of image:-real-inverted-smaller than the object-in Physics the characteristics of the image are stated in terms of its: Attitude (erect or inverted)Size (smaller or larger than the object)Nature (real or virtual)Magnification:Magnification (M) of any optical device is the ratio of the height of the image to the height of the object.Magnification=h i /h 0=d i /d 0PLO- Images formed by a plane and curved mirrors.Plane mirror:Characteristics of the image:-virtualLight vibrates at all plane Polarising filters are used to polarize light. Object Imageh ih 0 d 0 d i Optic centre-erect-same size as the objectCurved mirrors:1)concave 2)convex-Concave mirrors: curved inside (polished inside)C= The center of Sphere(Curvature point)- The distance between the vertex (V) and the principal focus (F) is called the focal length- The rays reflect and meet at F. The rays (converge) at F and therefore mirrors.The convex mirrors are mirrors, since the reflected rays diverge.-Spherical Aberration: Failure of the rays to converge at F, is called Spherical aberration, and is considered a defect in a mirror. This is not observed in a parabolic mirror.Ray diagrams:-A ray parallel to the principal axis will go though the principal focus.-A ray passing through the principal focus will reflect and go parallel to the principal axis.- A ray passing through the centre of curvature will be reflected on the same axis.*Images formed by concave mirrors:1) Object between F and C: Real inverted larger than the object.2) Object at F3) Object at C4) Object beyond C.5) Object between F and V.Mirror equation:1/f=1/d 0+1/d iSign convention:- If the image is formed below the principal axis, h=negative.i-The distance of virtual image is taken as negative.。
【英文读物】Under the Waves
【英文读物】Under the WavesPreface.This tale makes no claim to the character of an exhaustive illustration of all that belongs to the art of diving. It merely deals with the most important points, and some of the most interesting incidents connected therewith. In writing it I have sought carefully to exhibit the true and to ignore the false or improbable.I have to acknowledge myself indebted to the well-known submarine engineers Messrs Siebe and Gorman, and Messrs Heinke and Davis, of London, for much valuable information; and to Messrs Denayrouze, of Paris, for permitting me to go under water in one of their diving-dresses. Also—among many others—to Captain John Hewat, formerly Commander in the service of the Rajah of Sarawak, for much interesting material respecting the pirates of the Eastern Seas.R.M.B. Edinburgh, 1876.Chapter One.Introduces our Hero, one of his Advisers, and some of his Difficulties.“So, sir, it seems that you’ve set your heart on learning something of everything?”The man who said this was a tall and rugged professional diver. He to whom it was said was Edgar Berrington, our hero, a strapping youth of twenty-one.“Well—yes, I have set my heart upon something of that sort, Baldwin,”answered the youth. “You see, I hold that an engineer ought to be practically acquainted, more or less, with everything that bears, even remotely, on his profession; therefore I have come to you for some instruction in the noble art of diving.”“You’ve come to the right shop, Mister Edgar,”replied Baldwin, with a gratified look. “I taught you to swim when you wasn’t much bigger than a marlinespike, an’to make boats a’most before you could handle a clasp-knife without cuttin’your fingers, an’now that you’ve come to man’s estate nothin’ll please me more than to make a diver of you. But,”continued Baldwin, while a shade clouded his wrinkled and weatherbeaten visage, “I can’t let you go down in the dress without leave. I’m under authority, you know, and durstn’t overstep—”“Don’t let that trouble you,”interrupted his companion, drawing a letter from his pocket; “I had anticipated that difficulty, and wrote to your employers. Here is their answer, granting me permission to use their dresses.”“All right, sir,”said Baldwin, returning the letter without looking at it; “I’ll take your word for it, sir, as it’s not much in my line to make out the meanin’o’pot-hooks and hangers.—Now, then, when will you have your first lesson?”“The sooner the better.”“Just so,”said the diver, looking about him with a thoughtful air.The apartment in which the man and the youth conversed was a species of out-house or lumber-room which had been selected by Baldwin for the stowing away of his diving apparatus and stores while these were not in use at the new pier which was in process of erection in the neighbouring harbour. Its floor was littered with snaky coils of india-rubber tubing; enormous boots with leaden soles upwards of an inch thick; several diving helmets, two of which were of brightly polished metal, while the others were more or less battered, dulled, and dinted by hard service in the deep. The walls were adorned with large damp india-rubber dresses, which suggested the idea of baby-giants who had fallen into the water and been sent off to bed while their costumes were hung up to dry. In one corner lay several of the massive breast and back weights by which divers manage to sink themselves to the bottom of the sea; in another stood the chest containing the air-pump by means of which they are enabled to maintain themselves alive in that uncomfortable position; while in a third and very dark corner, an old worn-out helmet, catching a gleam from the solitary window by which the place was insufficiently lighted, seemed to glare enviously out of its goggle-eyes at its glittering successors. Altogether, what with the strange spectral objects and the dim light, there was something weird in the aspect of the place, that accorded well with the spirit of young Berrington, who, being a hero and twenty-one, was naturally romantic.But let us pause here to assert that he was also practical—eminently so. Practicality is compatible with romance as well as with rascality. If we be right in holding that romance is gushing enthusiasm, then are we entitled to hold that many methodical and practical men have been, are, and ever will be, romantic. Time sobers their enthusiasm a little, no doubt, but does by no means abate it, unless the object on which it is expended be unworthy.Recovering from his thoughtful air, and repeating “Just so,”the diver added, “Well, I suppose we’d better begin wi’them ’ere odds an’ends about us.”“Not so,”returned the youth quickly; “I have often seen the apparatus, and am quite familiar with it. Let us rather go to the pier at once. I’m anxious to go down.”“Ah! Mister Edgar—hasty as usual,”said Baldwin, shaking his head slowly. “It’s two years since I last saw you, and I had hoped to find that time had quieted you a bit, but—. Well, well—now, look here: you think you’ve seen all my apparatus, an’know all about it?”“Not exactly all,”returned the youth, with a smile; “but you know I’ve often been in this store of yours, and heard you enlarge on most if not all of the things in it.”“Yes—most, but not all, that’s where it lies, sir. You’ve often seen Siebe and Gorman’s dresses, but did you ever see this helmet made by Heinke and Davis?”“No, I don’t think I ever did.”“Or that noo helmet wi’the speakin’-toobe made by Denayrouze and Company, an’this dress made by the same?”“No, I’ve seen none of these things, and certainly this is the first time I have heard of a speaking-tube for divers.”“Well then, you see, Mister Edgar, you have something to larn here after all; among other things, that Denayrouze’s is not the first speakin’-toobe,”said Baldwin, who thereupon proceeded with the most impressive manner and earnest voice to explain minutely to his no less earnest pupil the various clever contrivances by which the several makers sought to render their apparatus perfect.With all this, however, we will not trouble the reader, but proceed at once to the port, where diving operations were being carried on in connection with repairs to the breakwater.On their way thither the diver and his young companion continued their conversation.“Which of the various dresses do you think the best?”asked Edgar.“I don’t know,”answered Baldwin.“Ah, then you are not bigotedly attached to that of your employer—like some of your fraternity with whom I have conversed?”“I am attached to Siebe and Gorman’s dress,”returned Baldwin, “but I am no bigot. I believe in every thing and every creature having good and bad points. The dress I wear and the apparatus I work seem to me as near perfection as may be, but I’ve lived too long in this world to suppose nobody can improve on ’em. I’ve heard men who go down in the dresses of other makers praise ’em just as much as I do mine, an’maybe with as good reason. I believe ’em all to be serviceable. When I’ve had more experience of ’em I’ll be able to say which I think the best.—I’ve got a noo hand on to-day,”continued Baldwin, “an’as he’s goin’down this afternoon for the first time, so you’ve come at a good time. He’s a smart young man, but I’m not very hopeful of him, for he’s an Irishman.”“Come, old fellow,”said Edgar, with a laugh, “mind what you say about Irishmen. I’ve got a dash of Irish blood in me through my mother, and won’t hear her countrymen spoken of with disrespect. Why should not an Irishman make a good diver?”“Because he’s too excitable, as a rule,”replied Baldwin. “You see, Mister Edgar, it takes a cool, quiet, collected sort of man to make a good diver, and Irishmen ain’t so cool as I should wish. Englishmen are better, but the best of all are Scotchmen. Give me a good, heavy, raw-boned lumpof a Scotchman, who’ll believe nothin’till he’s convinced, and accept nothin’till it’s proved, who’ll argue with a stone wall, if he’s got nobody else to dispute with, in that slow sedate humdrum way that drives everybody wild but himself, who’s got an amazin’conscience, but no nerves whatever to speak of—ah, that’s the man to go under water, an’crawl about by the hour among mud and wreckage without gittin’excited or makin’a fuss about it if he should get his life-line or air-toobe entangled among iron bolts, smashed-up timbers, twisted wire-ropes, or such like.”“Scotchmen should feel complimented by your opinion of them,”said Edgar.“So they should, for I mean it,”replied Baldwin, “but I hope the Irishman will turn up a trump this time.—May I take the liberty of askin’how you’re gittin’on wi’the engineering, Mister Edgar?”“Oh, famously. That is to say, I’ve just finished my engagement with the firm of Steel, Bolt, Hardy, and Company, and am now on the point of going to sea.”Baldwin looked at his companion in surprise. “Going to sea!”he repeated, “why, I thought you didn’t like the sea?”“You thought right, Baldwin, but men are sometimes under the necessity of submitting to what they don’t like. I have no love for the sea, except, indeed, as a beautiful object to be admired from the shore, but, you see, I want to finish my education by going a voyage as one of the subordinate engineers in an ocean-steamer, so as to get some practical acquaintance with marine engineering. Besides, I have taken a fancy to see something of foreign parts before settling down vigorously to my profession, and—”“Well?”said Baldwin, as the youth made rather a long pause.“Can you keep a secret, Baldwin, and give advice to a fellow who stands sorely in need of it?”The youth said this so earnestly that the huge diver, who was a sympathetic soul, declared with much fervour that he could do both.“You must know, then,”began Edgar with some hesitation, “the fact is—you’re such an old friend, Baldwin, and took such care of me when I was a boy up to that sad time when I lost my father, and you lost an employer—”“Ay, the best master I ever had,”interrupted the diver.“That—that I think I may trust you; in short, Baldwin, I’m over head and ears with a young girl, and—and—”“An’your love ain’t requited—eh?”said Baldwin interrogatively, while his weatherbeatenface elongated.“No, not exactly that,”rejoined Edgar, with a laugh. “Aileen loves me almost, I believe, as well as I love her, but her father is dead against us. He scorns me because I am not a man of wealth.”“What is he?”demanded Baldwin.“A rich China merchant.”“He’s more than that,”said Baldwin.“Indeed!”said Edgar, with a surprised look; “what more is he?”“He’s a goose!”returned the diver stoutly.“Don’t be too hard on him, Baldwin. Remember, I hope some day to call him father-in-law. But why do you hold so low an opinion of him?”“Why, because he forgets that riches may, and often do, take to themselves wings and fly away, whereas broad shoulders, and deep chest, and sound limbs, and a good brain, usually last the better part of a lifetime; and a brave heart will last for ever.”“I am afraid that I have yet to prove, to myself as well as to the old gentleman, that the brave heart is mine,”returned Edgar. “As to the physique—you may be so far right, but he evidently undervalues that.”“I said nothing about physic,”returned Baldwin, who still frowned as he thought of the China merchant, “and the less that you and I have to do wi’that the better. But what are you goin’to do, sir?”“That is just the point on which I want to have your advice. What ought I to do?”“Don’t run away with her, whatever you do,”said Baldwin emphatically.The youth laughed slightly as he explained that there was no chance whatever of his doing that, because Aileen would never consent to run away or to disobey her father.“Good—good,”said the diver, with still greater emphasis than before, “I like that. The gal that would sacrifice herself and her lover sooner than disobey her father—even though he is a goose —is made o’the right stuff. If it’s not takin’too great a liberty, Mister Edgar, may I ask what she’s like?”“What she’s like—eh?”murmured the other, dropping his head as if in reverie, and stroking the dark shadow on his chin which was beginning to do duty for a beard. “Why, she—she’s likenothing that I ever saw on earth before.”“No!”ejaculated Baldwin, elevating his eyebrows a little, as he said gravely, “what, not even like an angel?”“Well, yes; but even that does not sufficiently describe her. She’s fair,”—he waxed enthusiastic here,—“surpassingly fair, with wavy golden tresses and blue eyes, and a bright complexion and a winning voice, and a sylph-like figure and a thinnish but remarkably pretty face—”“Ah!”interrupted Baldwin, with a sigh, “I know: just like my missus.”“Why, my good fellow,”cried Edgar, unable to restrain a fit of laughter, “I do not wish to deny the good looks of Mrs Baldwin, but you know that she’s uncommonly ruddy and fat and heavy, as well as fair.”“Ay, an’forty, if you come to that,”said the diver. “She’s fourteen stun if she’s an ounce; but let me tell you, Mister Edgar, she wasn’t always heavy. There was a time when my Susan was as trim and taut and clipper-built as any Aileen that ever was born.”“I have no doubt of it whatever,”returned the youth, “but I was going to say, when you interrupted me, it is her eyes that are her strong point—her deep, liquid, melting blue eyes, that look at you so earnestly, and seem to pierce—”“Ay, just so,”interrupted the diver; “pierce into you like a gimblet, goin’slap agin the retina, turnin’short down the jugular, right into the heart, where they create an agreeable sort o’fermentation. Oh! Don’t I know?—my Susan all over!”Edgar’s amusement was tinged slightly with disgust at the diver’s persistent comparisons. However, mastering his feelings, he again demanded advice as to what he should do in the circumstances.“You han’t told me the circumstances yet,”said the diver quietly.“Well, here they are. Old Mr Hazlit—”“What! Hazlit? Miss Hazlit, is that her name?”cried Baldwin, with a look of pleased surprise.“Yes, do you know her?”“Know her? Of course I do. Why, she visits the poor in my district o’the old town—you know I’m a local preacher among the Wesleyans—an’she’s one o’the best an’sweetest—ha! Angel indeed! I’m glad she wasn’t made an angel of, for it would have bin the spoilin’of a splendid woman. Bless her!”The diver spoke with much enthusiasm, and the young man smiled as he said, “Of course I add Amen to your last words.—Well then,”he continued, “Aileen’s father has refused to allow me to pay my addresses to his daughter. He has even forbidden me to enter his house, or to hold any intercourse whatever with her. This unhappy state of things has induced me to hasten my departure from England. My intention is to go abroad, make a fortune, and then return to claim my bride, for the want of money is all that the old gentleman objects to. I cannot bear the thought of going away without saying good-bye, but that seems now unavoidable, for he has, as I have said, forbidden me the house.”Edgar looked anxiously at his companion’s face, but received no encouragement there, for Baldwin kept his eyes on the ground, and shook his head slowly.“If the old gentleman has forbid you his house, of course you mustn’t go into it. However, it seems to me that you might cruise about the house and watch till Sus—Aileen, I mean—comes out; but I don’t myself quite like the notion of that either, it don’t seem fair an’above-board like.”“You are right,”returned Edgar. “I cannot consent to hang about a man’s door, like a thief waiting to pounce on his treasure when it opens. Besides, he has forbidden Aileen to hold any intercourse with me, and I know her dear nature too well to subject it to a useless struggle between duty and inclination. She is certain to obey her father’s orders at any cost.”“Then, sir,”said Baldwin decidedly, “you’ll just have to go afloat without sayin’good-bye. There’s no help for it, but there’s this comfort, that, bein’what she is, she’ll like you all the better for it.—Now, here we are at the pier. Boat a-hoy-oy!”In reply to the diver’s hail a man in a punt waved his hand, and pulled for the landing-place.A few strokes of the oar soon placed them on the deck of a large clumsy vessel which lay anchored off the entrance to the harbour. This was the diver’s barge, which exhibited a ponderous crane with a pendulous hook and chain in the place where its fore-mast should have been. Several men were busied about the deck, one of whom sat clothed in the full dress of a diver, with the exception of the helmet, which was unscrewed and lay on the deck near his heavily-weighted feet. The dress was wet, and the man was enjoying a quiet pipe, from all which Edgar judged that he was resting after a dive. Near to the plank on which the diver was seated there stood the chest containing the air-pumps. It was open, the pumps were in working order, with two men standing by to work them. Coils of india-rubber tubing lay beside it. Elsewhere were strewn about stones for repairing the pier, and various building tools.“Has Machowl come on board yet?”asked Baldwin, as he stepped on the deck. “Ah, I see he has.—Well, Rooney lad, are you prepared to go down?”“Yis, sur, I am.”Rooney Machowl, who stepped forward as he spoke, was a fine specimen of a man, and would have done credit to any nationality. He was about the middle height, very broad and muscular, and apparently twenty-three years of age. His countenance was open, good-humoured, and good-looking, though by no means classic—the nose being turned-up, the eyes small and twinkling, and the mouth large.“Have you ever seen anything of this sort before?”asked Baldwin, with a motion of his hand towards the diving apparatus scattered on the deck.“No sur, nothin’.”“Was you bred to any trade?”“Yis, sur, I’m a ship-carpenter.”“An’why don’t you stick to that?”“Bekase, sur, it won’t stick to me. There’s nothin’doin’apparently in this poort. Annyhow I can’t git work, an’I’ve a wife an’chick at home, who’ve bin so long used to praties and bacon that their stummicks don’t take kindly to fresh air fried in nothin’. So ye see, sur, findin’it difficult to make a livin’above ground, I’m disposed to try to make it under water.”While Rooney Machowl was speaking Baldwin regarded him with a fixed and critical gaze. What his opinion of the recruit was did not, however, appear on his countenance or in his reply, for he merely said, “Humph! Well, we’ll see. You’ll begin your education in your noo profession by payin’partikler attention to all that is said an’done around you.”“Yis, sur,”returned Machowl, respectfully touching the peak of his cap and wrinkling his forehead very much, while he looked on at the further proceedings of the divers with that expression of deep earnest sincerity of attention which—whether assumed or genuine—is only possible to the countenance of an Irishman.During this colloquy the two men standing by the pump-case, and two other men who appeared to be supernumeraries, listened with much interest, but the diver seated on the plank, resting and calmly smoking his pipe, gazed with apparent indifference at the sea, from which he had recently emerged.This man was a very large fellow, with a dark surly countenance—not exactly bad in expression, but rather ill-tempered-looking. His diving-dress being necessarily very wide and baggy, made him seem larger than he really was—indeed, quite gigantic. The dress was made of very thick india-rubber cloth, and all—feet, legs, body, and arms—was of one piece, so perfectly secured at the seams as to be thoroughly impervious to air or water. To get into it was a matter of some difficulty, the entrance being effected at the neck. When this neck is properly attached to the helmet, the diver is thoroughly cut off from the external world, except through the air-tubecommunicating with his helmet and the pump afore mentioned.“Have ye got the hole finished, Maxwell?”said Baldwin, turning to the surly diver.“Yes,”he replied shortly.“Well, then, go down and fix the charge. Here it is,”said Baldwin, taking from a wooden case an object about eighteen inches long, which resembled a large office-ruler that had been coated thickly with pitch. It was an elongated shell filled to the muzzle with gunpowder. To one end of it was fastened the end of a coil of wire which was also coated with some protecting substance.As Baldwin spoke Maxwell slowly puffed the last “draw”from his lips and knocked the ashes out of his pipe on the plank, on which he still remained seated while the two supernumeraries busied themselves in completing his toilet for him; one screwing on his helmet, which appeared ridiculously large, the other loading his breast and back with two heavy leaden weights. When fully equipped, the diver carried on his person a weight fully equal to that of his own bulky person.“Now look here, Mister Edgar, an’pay partikler attention, Rooney Machowl. This here toobe, made of indyrubber, d’ee see? (‘Yis, sur,’from Rooney) I fix on, as you perceive, to the back of Maxwell’s helmet. It communicates with that there pump, and when these two men work the pump, air will be forced into the helmet and into the dress down to his very toes. We could bu’st him, if we were so disposed, if it wasn’t for an escape-valve, here close beside the air-toobe, at the back of the helmet, which keeps lettin’off the surplus air. Moreover, there is another valve, here in front of the breast-plate, which is under the control of the diver, so that he can let air escape by givin’it a half-turn when the men at the pumps are givin’him too much, or he can keep it in when they’re givin’him enough.”“An’what does he do,”asked Rooney, with an anxious expression, “whin they give him too little?”“He pulls on the air-pipe,—as I’ll explain to you in good time—the proper signal for ‘more air.’”“But what if he forgits, or misremimbers the signal?”asked the inquisitive recruit.“Why then,”replied Baldwin, “he suffocates, and we pull him up dead, an’give him decent burial. Keep yourself easy, my lad, an’you’ll know all about it in good time. I’ll soon give ’ee the chance to suffocate or bu’st yourself accordin’to taste.”“Come, cut it short and look alive,”said Maxwell gruffly, as he stood up to permit of a stout rope being fastened to his waist.“You shut up!”retorted Baldwin.Having exchanged these little civilities the two divers moved to the side of the barge—Maxwell with a slow ponderous tread.A short iron ladder dipped from the gunwale of the barge a few feet down into the sea. The diver stepped upon this, turning with his face inwards, descended knee-deep into the water, and then stopped. Baldwin handed him the blasting-charge. At the same moment one of the supernumeraries advanced with the front-glass or bull’s-eye in his hand, and the men at the pumps gave a turn or two to see that all was working well.“All right?”demanded the supernumerary.“Right,”responded Maxwell, in a voice which issued sepulchrally from the iron globe.There are three round windows fitted with thick plate-glass in the helmets to which we refer. The front one is made to screw off and on, and the fixing of this is always the last operation in completing a diver’s toilet.“Pump away,”said the man, holding the round glass in front of Maxwell’s nose, and looking over his shoulder to see that the order was obeyed. The glass was screwed on, and the man finished off by gravely patting Maxwell in an affectionate manner on the head.“Why does he pat him so?”asked Edgar, with a laugh at the apparent tenderness of the act.“It’s a tinder farewell, I suppose,”murmured Rooney, “in case he niver comes up again.”“It is to let him know that he may now descend in safety,”answered Baldwin. “The pump there is kep’goin’from a few moments before the front-glass is screwed on till the diver shows his head above water again—which he’ll do in quarter of an hour or so, for it don’t take long to lay a charge; but our ordinary spell under water, when work is steady, is about four hours—more or less—with perhaps a breath of ten minutes once or twice at the surface when they’re working deep.”“But why a breath at the surface?”asked Edgar. “Isn’t the air sent down fresh enough?”“Quite fresh enough, Mister Edgar, but the pressure when we go deep—say ten or fifteen fathoms—is severe on a man if long continued, so that he needs a little relief now and then. Some need more and some less relief, accordin’to their strength. Maxwell has only gone down fifteen feet, so that he wouldn’t need to come up at all durin’a spell of work. We’re goin’to blast a big rock that has bin’troublesome to us at low water. The hole was driven in it last week. We moored a raft over it and kep’men at work with a long iron jumper that reached from the rock to the surface of the sea. It was finished last night, and now he’s gone to fix the charge.”“But I don’t understand about the pressure, sur, at all at all,”said Machowl, with acomplicated look of puzzlement; “sure whin I putt my hand in wather I don’t feel no pressure whatsomediver.”“Of course not,”responded Baldwin, “because you don’t put it deep enough. You must know that our atmosphere presses on our bodies with a weight of about 20,000 pounds. Well, if you go thirty-two feet deep in the sea you get the pressure of exactly another atmosphere, which means that you’ve got to stand a pressure all over your body of 40,000 when you’ve got down as deep as thirty-two feet.”“But,”objected Rooney, “I don’t fed no pressure of the atmosphere on me body at all.”“That’s because you’re squeezed by the air inside of you, man, as well as by the atmosphere outside, which takes off the feelin’of it, an’, moreover, you’re used to it. If the weight of our atmosphere was took off your outside and not took off your inside—your lungs an’the like,—you’d come to feel it pretty strong, for you’d swell like a balloon an’bu’st a’most, if not altogether.”Baldwin paused a moment and regarded the puzzled countenance of his pupil with an air of pity.“Contrairywise,”he continued, “if the air was all took out of your inside an’allowed to remain on your outside, you’d go squash together like a collapsed indyrubber ball. Well then, if that be so with one atmosphere, what must it be with a pressure equal to two, which you have when you go down to thirty-two feet deep in the sea? An’if you go down to twenty-five fathoms, or 150 feet, which is often done, what must the pressure be there?”“Tightish, no doubt,”said Rooney.“True, lad,”continued Joe. “Of course, to counteract this we must force more air down to you the deeper you go, so that the pressure inside of you may be a little more than the pressure outside, in order to force the foul air out of the dress through the escape-valve; and what between the one an’the other your sensations are peculiar, you may be sure.—But come, young man, don’t be alarmed. We’ll not send you down very deep at first. If some divers go down as deep as twenty-five fathoms, surely you’ll not be frightened to try two and a half.”Whatever Rooney’s feelings might have been, the judicious allusion to the possibility of his being frightened was sufficient to call forth the emphatic assertion that he was ready to go down two thousand fathoms if they had ropes long enough and weights heavy enough to sink him!While the recruit is preparing for his subaqueous experiments, you and I, reader, will go see what Maxwell is about at the bottom of the sea.Chapter Two.Describes a first Visit to the Bottom of the Sea.When the diver received the encouraging pat on the head, as already related, he descended the。
Bytheendofthenin...
Ek of emitted electrons (J x 10-19)
Slope = h = 6.63 x 10-34 J.s
(0, -B)
Frequency of Incident Light, f,
(Hz x 1014)
2. When the kinetic energy of the emitted electrons vs frequency is measured for different metallic surfaces, the resulting graphs have identical values of the slope, h, but have different values of the intercept, B (This intercept is also referred to as W, standing for work function).
Ek of emitted electrons (J x 10-19)
Metal “III” Metal “II” Metal “I”
Slope = h
(0, -B)
Frequency of Incident Light, f,
(Hz x 1014)
3. When the Intensity of the light is varied, two observations result:
You can draw an analogy here to looking at the image on a TV screen. From some distance the image is continuous - if you look very closely however, you see the individual pixels which make up the image.
英文教材《Environmental Hydraulics for Open Channel Flows》List-of-Symbols_
∫
0
design upstream head (m) residual head (m) upstream total head (m) downstream total head (m) local total head (m) defined as:
Hϭ
2 P V ϩzϩ g 2g
h
specific enthalpy (i.e. enthalpy per unit mass) (J/kg): h ϭ e ϩ
List of symbols
A As B Bmax Bmin C Ca CChézy CD CL Cd Cdes Co Cp Cs (Cs)mean Csound Cv D DH
Cs
ቤተ መጻሕፍቲ ባይዱ
Ds Dt D1, D2 d dab db dc dcharac dconj do
flow cross-sectional area (m2) particle cross-sectional area (m2) open channel free-surface width (m) inlet lip width (m) of MEL culvert (1) minimum channel width (m) for onset of choking flow (2) barrel width (m) of a culvert (1) celerity (m/s): e.g. celerity of sound in a medium, celerity of a small disturbance at a free surface (2) dimensional discharge coefficient Cauchy number Chézy coefficient (m1/2/s) dimensionless discharge coefficient (SI units) lift coefficient (1) skin friction coefficient (also called drag coefficient) (2) drag coefficient design discharge coefficient (SI units) initial celerity (m/s) of a small disturbance ∂h specific heat at constant pressure (J/kg/K): C p ϭ ∂T P mean volumetric sediment concentration mean sediment suspension concentration sound celerity (m/s) specific heat at constant volume (J/kg/K) sediment concentration circular pipe diameter (m) hydraulic diameter (m), or equivalent pipe diameter, defined as: cross -sectional area 4A DH ϭ 4 ϭ wetted perimeter Pw 2 sediment diffusivity (m /s) diffusion coefficient (m2/s) characteristics of velocity distribution in turbulent boundary layer flow depth (m) measured perpendicular to the channel bed air bubble diameter (m) brink depth (m) critical flow depth (m) characteristic geometric length (m) conjugate flow depth (m) (1) uniform equilibrium flow depth (m): i.e. normal depth (2) initial flow depth (m)
描写海的英语作文
The sea is a vast expanse of water that covers more than70%of the Earths surface. It is a source of life,a playground for recreation,and a mystery that continues to captivate the human imagination.1.The Beauty of the Sea:The sea is a spectacle of natural beauty.Its surface shimmers under the sun,reflecting the skys hues from a deep azure to a bright cerulean.At sunrise and sunset,the sea transforms into a canvas of fiery oranges and purples,as the sun dips below the horizon.2.The Power of the Waves:The sea is a testament to the power of nature.Its waves can be gentle,lapping at the shore,or they can be fierce,crashing against the cliffs with a force that is both aweinspiring and humbling.The rhythmic sound of the waves is a soothing melody that resonates with the ebb and flow of life.3.The Richness of Marine Life:Beneath the surface,the sea is a bustling world teeming with life.Coral reefs provide a vibrant habitat for an array of colorful fish and invertebrates.Whales,dolphins,and seals are just a few of the larger marine mammals that call the ocean home.4.The Sea as a Source of Resources:The sea is a treasure trove of resources.It provides food in the form of fish and seafood,and it is a source of minerals and oil.The sea also offers a means of transportation and trade,with shipping lanes connecting continents and economies.5.The Role of the Sea in Climate:The sea plays a crucial role in regulating the Earths climate.It absorbs carbon dioxide,helping to mitigate the effects of climate change.The ocean currents also distribute heat around the globe,influencing weather patterns and supporting the water cycle.6.The Threats to the Sea:Despite its grandeur,the sea faces numerous threats.Pollution, overfishing,and climate change are causing irreversible damage to marine ecosystems.It is imperative that we take action to protect this vital resource for future generations.7.The Cultural Significance of the Sea:Throughout history,the sea has held a special place in the hearts and minds of people around the world.It has been a source of inspiration for artists,writers,and explorers.The sea has also been a symbol of freedom, adventure,and the unknown.8.The Call of the Sea:For many,the sea is a call to adventure.It beckons with the promise of discovery and the thrill of exploration.Whether its a leisurely stroll along thebeach,a day of surfing,or a deepsea dive,the sea offers endless opportunities for enjoyment and learning.9.The Sea as a Place of Reflection:The sea is also a place for reflection and contemplation.Its vastness and tranquility can provide a sense of perspective and peace. Many find solace in the seas ability to calm the mind and inspire the soul.10.The Seas Future:As we look to the future,the health and preservation of the sea are of paramount importance.Sustainable practices,conservation efforts,and a greater understanding of the seas importance to our planet are essential for ensuring that the sea continues to be a source of life and wonder for generations to come.。
关于沙滩的英语作文
The beach is a place of tranquility and beauty,where the sound of the waves and the sight of the endless horizon can bring peace to the mind.Here is an essay about the beach that captures its essence and allure.The sun was just beginning to rise,casting a warm golden glow over the vast expanse of the ocean.The beach,still quiet at this early hour,was a canvas of untouched sand, waiting to be filled with footprints and laughter.The gentle lapping of the waves against the shore was the only sound that broke the silence,a soothing melody that echoed the rhythm of the earth itself.As the morning progressed,the beach began to come alive.Families arrived,carrying colorful umbrellas and beach chairs,setting up their temporary homes for the day. Children ran towards the water,their laughter ringing out as they splashed and played in the shallows.The beach was a playground,a place where the young and the young at heart could let go of their worries and simply enjoy the moment.The sand,warm from the sun,was a perfect place to bask and relax.Lying on a towel, one could feel the gentle caress of the breeze as it blew in from the sea,carrying with it the salty scent of the ocean.The sun,now high in the sky,provided a warm embrace,its rays dancing on the surface of the water,creating a dazzling spectacle of light and color. In the distance,seagulls soared and dipped,their cries mingling with the sound of the waves.They were the guardians of the beach,their keen eyes watching over the shore and its visitors.The beach was a sanctuary for many species,a place where nature thrived and coexisted with human life.As the day drew to a close,the beach began to empty.Families packed up their belongings,leaving behind only the faintest traces of their presence.The sun began to set, its light turning the sky into a canvas of fiery reds and oranges.The beach,once bustling with activity,was now a tranquil haven,a place to reflect on the days experiences and the simple beauty of nature.The beach is more than just a place to swim and sunbathe it is a sanctuary for the soul.It is a place where one can find solace,inspiration,and a connection to the natural world. The next time you find yourself at the beach,take a moment to appreciate the beauty that surrounds you,and let the tranquility of the shore wash over you,bringing with it a sense of peace and contentment.。
高中英语作文创意性开头与引人入胜故事构建单选题40题
高中英语作文创意性开头与引人入胜故事构建单选题40题1. Which of the following opening sentences is the most creative in attracting the reader's attention?A. Life is like a box of chocolates, you never know what you're going to get.B. Once upon a time, in a faraway land...C. Albert Einstein once said, "Insanity is doing the same thing over and over again and expecting different results."D. The early bird catches the worm.答案:C。
解析:选项C 引用了爱因斯坦的名言,这种方式独特且能引发读者对不同结果的思考,与作文开头构建引人入胜的氛围和引发思考的创意点相契合。
选项 A 是电影台词,比较常见;选项B 是传统的童话故事开头;选项D 是常见的谚语。
2. The best way to start a story that makes the reader eager to know more is to _____.A. describe a beautiful sceneryB. present a surprising factC. mention a famous personD. use a vivid metaphor答案:B。
解析:选项B 提出一个令人惊讶的事实能迅速抓住读者的好奇心,让读者迫切想要知道更多关于这个事实的后续发展,与作文开头制造悬念、吸引读者继续阅读的创意点紧密相关。
选项 A描述美丽景色较平淡;选项 C 提到名人可能不够新颖;选项 D 使用生动比喻有一定创意但不如B 直接。
投入大海的怀抱英语作文
Embracing the vastness and mystery of the ocean has always been a dream for many, symbolizing freedom,exploration,and the unknown.Heres a composition that captures the essence of being in the arms of the sea.Title:Embracing the Oceans EmbraceAs the sun begins to rise,casting a golden glow over the tranquil waters,I stand at the edge of the shore,my heart filled with anticipation.The ocean,a boundless expanse of azure,calls to me,inviting me to immerse myself in its depths.Today,I will embrace the oceans embrace,allowing it to cradle me in its waves and currents.The Call of the WavesThe rhythmic sound of the waves crashing against the shore is a sirens song,beckoning me closer.Each wave,a testament to the oceans power and beauty,draws me in with its promise of adventure and discovery.I take off my shoes,feeling the cool,wet sand beneath my feet,a reminder of the oceans touch.The Dive into the DeepWith a deep breath,I wade into the water,the waves lapping at my ankles,then knees, and finally,I dive in.The coolness of the water is a shock at first,but it quickly becomes a refreshing caress.I swim further out,feeling the oceans current gently guiding me,as if it were a mother cradling her child.The Dance with the SeaAs I swim,I become one with the ocean.The water supports me,buoying me up as I move through it with ease.I am surrounded by the life that thrives beneath the surfacethe colorful fish darting about,the seaweed swaying in the current,and the occasional curious sea creature that comes to investigate the newcomer.The ocean is a symphony of life,and I am a part of its grand performance.The Reflection on the SurfaceFloating on my back,I gaze at the sky above,a canvas of blue with the occasional wisp of cloud.The suns rays dance on the waters surface,creating a sparkling effect that is both mesmerizing and humbling.The vastness of the ocean makes me realize how small Iam in the grand scheme of things,yet it also fills me with a sense of belonging.The Return to the ShoreAs the day progresses,I decide its time to return to the shore.With a final stroke,I head back,the oceans embrace releasing me gently.I wade out of the water,the sand once again beneath my feet,and I look back at the ocean with gratitude.It has given me a moment of peace,a connection to the natural world,and a reminder of the beauty that lies just beyond our everyday lives.The Lasting ImpactThe experience of being in the oceans embrace is one that stays with me long after Ive left the shore.Its a reminder to seek out the unknown,to embrace the vastness of the world,and to appreciate the simple yet profound moments that life has to offer.The ocean has a way of humbling us while also inspiring us to reach for the horizon.In conclusion,the ocean is more than just a body of water its a living,breathing entity that offers us a glimpse into the depths of our own existence.To be in the oceans embrace is to be reminded of our place in the world and the endless possibilities that await us when we dare to dive in.This composition is a tribute to the ocean and the profound experiences it offers to those who dare to immerse themselves in its depths.Whether youre a seasoned swimmer or someone whos never dipped a toe in the sea,the oceans embrace is a universal experience that speaks to the human spirits desire for exploration and connection.。
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suffer jump discontinuities at a certain curve.
4 Acceleration waves
2 Conservation laws
In the recent paper [2], all Lie point symmetries of system (1) are shown to be variational symmetries of the functional (2), and all corresponding (via Noether’s theorem) conservation laws admitted by the smooth solutions of the von K´arm´an equations are established. Each such conservation law is a linear combination of the basic linearly independent conservation laws
arXiv:math-ph/0006016v2 27 Jun 2000
1 Introduction
The von K´arm´an plate theory is governed by two coupled nonlinear fourth-order partial differential equations in three independent variables (Cartesian coordinates on the plate middle-plane x1, x2 and the time x3) and two dependent variables (the transversal displacement function w and Airy’s stress function Φ), namely
(Latin) indices range over 1, 2 (1, 2, 3), unless explicitly stated otherwise; the usual
summation convention over a repeated index is used and subscripts after a comma at a certain function f denote its partial derivatives, that is f,i = ∂f /∂xi, f,ij = ∂f /∂xi∂xj, etc.
bending tensor Kαβ being given in terms of w and Φ through the following expressions:
N αβ = εαµεβν Φ,µν , M αβ = −D (1 − ν)δαµδβν + νδαβδµν w,µν , Qα = M,αµµ + N αµw,µ, Eαβ = (1/Eh) (1 + ν)εαµεβν − vδαβδµν Φ,µν, Kαβ = w,αβ.
The theory under consideration allows an exact variational formulation, the von
K´arm´an equations being the Euler-Lagrange equations [1] associated with the action
Gαβ = (1/Eh) (1 + ν)δαµδβν − νδαβδµν Φ,µν − (1/2) εαµεβνw,µw,ν, F α = Gα,νν.
Table 1 Conservation laws
w - translations
X1
=
∂ ∂w
Φ - translations
X14
=
∂ ∂Φ
time - translations
energy P(α4) = −w,3Qα − Φ,3F α + w,3βM αβ + Φ,3βGαβ Ψ(4) = T + Π
wave momentum P(α2) = δα1L + w,1Qα + Φ,1F α − w,1βM αβ − Φ,1βGαβ Ψ(2) = −ρ w,1w,3 P(α3) = δα2L + w,2Qα + Φ,2F α − w,2βM αβ − Φ,2βGαβ Ψ(3) = −ρ w,2w,3
∂Ψ(j) ∂x3
+
∂P(µj) ∂xµ
=0
(j = 1, 2, . . . , 14) ,
whose densities Ψ(j) and fluxes P(µj) are presented (together with the generators of the respective symmetries) on the Table 1 below in terms of Qα, M αβ, Gαβ and F α,
The von K´arm´an equations (1) describe entirely the motion of a plate, the membrane stress tensor N αβ, moment tensor M αβ, shear-force vector Qα, strain tensor Eαβ and
is the strain energy per unit area of the plate middle-plane and T = (ρ/2) (w,3)2 ,
is the kinetic energy per unit area of the plate middle-plane.
1Published in: Integral Methods in Science and Engineering, Chapman & Hall / CRC Research Notes in Mathematics 418, Boca Raton, FL, pp. 131-136 (2000).
the bending rigidity, E is Young’s modulus, ν is Poisson’s ratio, h is the thickness of the plate, ρ is the mass per unit area of the plate middle-plane, δαβ is the Kronecker delta symbol and εαβ is the alternating symbol. Here and throughout the work: Greek
rotations
X6
=
x2
∂
∂ x1
−
x1
∂
∂ x2
moment of the wave momentum P(α6) = x2P(α2) − x1P(α3) + ενµw,µM αν + ενµΦ,µGαν Ψ(6) = x2Ψ(2) − x1Ψ(3)
rigid body rotations
X7
functional
I [w, T − Π
(2)
where
Π = (D/2) (∆w)2 − (1 − ν) εαµεβνw,αβw,µν − (1/2Eh) (∆Φ)2 − (1 + ν) εαµεβνΦ,αβΦ,µν + (1/2)εαµεβνΦ,αβw,µw,ν,
∂ ∂Φ
center-of-mass theorem P(α9) = −x3Qα, Ψ(9) = ρ (x3w,3 − w) P(α10) = x3P(α7), Ψ(10) = x1Ψ(9) P(α11) = x3P(α8), Ψ(11) = x2Ψ(9) P(α12) = x1F α − Gα1, Ψ(12) = 0 P(α13) = x2F α − Gα2, Ψ(13) = 0
D∆2w − εαµεβν w,αβΦ,µν + ρw,33 = 0, (1/Eh) ∆2Φ + (1/2) εαµεβν w,αβw,µν = 0,
(1)
where ∆ is the Laplace operator with respect to x1 and x2, D = Eh3/12(1 − ν2) is
=
x1
∂ ∂w
X8
=
x2
∂ ∂w
scaling
X5
=
xµ
∂
∂ xµ
+
2x3
∂
∂ x3
angular momentum P(α7) = M α1 − x1Qα + wεαν Φ,ν2, Ψ(7) = ρx1w,3 P(α8) = M α2 − x2Qα + wεναΦ,ν1, Ψ(8) = ρx2w,3
(3)
Ω
Σ
corresponds to each of the conservation laws listed in Table 1. It holds, just as the respective conservation law, for every smooth solution of the von K´arm´an equations.
The balance laws are applicable even if Ω is intersected by a discontinuity (singular) manifold (on which the corresponding densities Ψ(j) and fluxes P(αj) may suffer jump discontinuities) provided that the integrals exist. We are ready now to extend the “con-