Local Flattening of the Fermi Surface and Quantum Oscillations in the Magnetoacoustic Respo
高级英语视听(辅修) 椭球面
高级英语视听(辅修)椭球面Ellipsoid refers to a three-dimensional geometric figure that resembles a slightly flattened sphere. It is formed by the rotation of an ellipse around one of its axes. Ellipsoids are commonly used in various scientific and engineering fields to approximate the shape of Earth, as well as other celestial bodies.In the context of geodesy and Earth sciences, the Earth is often modeled as an ellipsoid to simplify calculations and measurements. This is because the Earth's shape is not a perfect sphere, but rather an oblate spheroid, meaning it is slightly flattened at the poles and bulging at the equator.There are several different reference ellipsoids used to model the Earth, with varying levels of accuracy. The most widely used ellipsoid is the World Geodetic System (WGS84), which serves as the basis for global positioning systems (GPS) and mapping systems.In addition to Earth, other planets and moons in our solar system can also be approximated as ellipsoids. For example, Mars and Saturn's largest moon, Titan, have been modeled as ellipsoids to study their surface characteristics and gravitational fields.In summary, an ellipsoid is a mathematical representation of a slightly flattened sphere. It is commonly used to approximate the shape of Earth and other celestial bodies in scientific and engineering calculations.。
地质中英译文(DOC)
The South China Sea is a classic example of the marginal basins that typify the margin of Southeast Asia, and one with a relatively complicated tectonic history that has been linked both to the development of the active margins of the Western Pacific and to the tectonics of continental Asia following the India–Asia collision starting around 50 Ma.南海边缘盆地是一个典型的例子,代表的东南亚边缘,它有一个相对复杂的构造史,与西太平洋活动大陆边的发展以及从5000万年前开始的印度-亚洲大陆碰撞所形成的地质构造都密切相关。
The tectonics of continental break-up and seafloor spreading have been studied in this area for a significant period of time, yet our understanding of why the basin formed in the first places still remains controversial.大陆解体的构造和海底传播研究在这一区域已有相当一段时间,但是我们对于该盆地最初的形成的理解仍然是有争议的。
Two competing schools have suggested two opposing visions for what caused the basin to open.两个相互对立的学派对于该盆地的形成提出了两种对立的观点。
薄膜物理国外课题组
薄膜物理国外课题组
以下是一些国外专注于薄膜物理的课题组:
Flatiron Institute:位于美国纽约的Flatiron Institute是隶属于美国国家点火装置(NIF)的量子材料科学部门。
The research group for Graphene and 2D Materials at the University of Manchester:该课题组致力于研究单层和多层石墨烯以及二维材料的电子结构和物理性质,并探索其在电子学、化学传感器和能量存储方面的
The Nanotechnology and Nanomaterials Physics Group at the University of Almer[ì]{}a:该课题组专注于研究纳米技术和纳米物理学领域的不同方面,包括薄膜、纳米结构、低维材料和量子器件等^[4
The Surface and Interface Analysis Group at the Max Planck Institute for Solid State Research:该课题组研究领域包括材料科学、固体物理学、表面和界面分析以及薄膜技术等。
以上仅是一些国外专注于薄膜物理的课题组例子,还有很多其他课题组也在这一领域进行研究和探索。
土力学词汇英汉对照
Aabsorbed water吸着水accumulation sedimentation method累积沉淀法active earth pressure主动土压力E aactivity index活性指数Aadamic earth,red soil红粘土additional stress(pressure)of subsoil地基附加应力(压力)zadverse geologic phenomena不良地质现象aeolian soils风积土aeolotropic soil各向异性土air dried soils风干土allowable subsoil bearing capacity地基容许承载力[ 0]allowable settlement容许沉降alluvial soil冲积土angle between failure plane and major principal plane 破坏面与大主平面的夹角angle of internal,external (wall) friction内摩擦角ϕ、外(墙背)摩擦角angular gravel,angular pebble角砾anisotropic soil各向异性土aquifer含水层aquifuge,impermeabler layer不透水层area of foundation base基础底面面积Aartesian water head承压水头artificial fills人工填土artificial foundation人工地基Atterberg Limits阿太堡界限attitude产状average consolidation pressure平均固结压力σaverage heaving ratio of frozen soil layer冻土层的平均冻胀率average pressure ,additional pressure offoundation base基底平均压力、平均附加压力p、p0Bbase tilt factor of foundation基础倾斜系数b c、b q、bγbase tilt factors基底倾斜系数b c、b q、bγbearing capacity 承载力bearing capacity factors承载力系数N c,、N q,、Nγ[California]Bearing Ratio[CBR] 承载比bearing stratum持力层bedrock,original rock 基岩beginning hydraulic gradient起始水力梯度(坡降)i oBiot consolidation theory 比奥固结理论Bishop’s slice method比肖普条分法bound water 结合水(束缚水)boulder漂石Boussinesq theory 布辛奈斯克理论bridge桥梁bridge pier桥墩broken stone,crushed stone碎石bulk modulus体积模量buried depth of foundation基础埋置深度d buoyant density 浮密度ρ'buoyant gravity density(unit weight)浮重度(容重) ’CCalifornia Bearing Ratio(CBR) 加州承载比capillary rise毛细水上升高度capillary water毛细(管)水categorization of geotechnical projects岩土工程分级cementation胶结作用central load 中心荷载(轴心荷载)characteristic value of subsoil bearing capacity 地基承载力特征值f akchemical grouting 化学灌浆circular footing 圆形基础clay粘土clay content粘粒含量clay minerals粘土矿物clayey silt粘质粉土clayey soils ,clayly soils粘性土coarse aggregate粗骨料coarse-grained soils粗粒土coarse sand粗砂cobble卵石Code for design of building foundation建筑地基基础设计规范coefficient of active earth pressure主动土压力系数K acoefficient of passive earth pressure被动土压力系数K Pcoefficient ofcollapsibility湿陷系数 scoefficient of compressibility压缩系数acoefficient of curvature曲率系数C ccoefficient of earth pressure at rest静止土压力系数Kcoefficient of lateral pressure侧压力系数K0coefficient of permeability渗透系数kcoefficient of secondary consolidation次固结系数coefficient of uniformity 不均匀系数coefficient of vertical consolidation竖向固结(压密)系数c v.coefficient of vertical ,horizontal permeability 竖向、水平向渗透系数k hcoefficient of vertical ,horizontal,tangential additional stress beneath a uniform strip load均布条形荷载下竖向、水平向、切向附加应力系数 sz、 sx、 sxzcoefficient of vertical additional ,average additional stress beneatha uniform round load at centre point均布圆形荷载中点下竖向、平均附加应力系数 r、rαcoefficient of vertical additional ,average additional stress beneath a triangular distributed rectangle load at corner point三角形分布矩形荷载角点下竖向、附加、平均附加应力系数t1、 t2、1tα、2tαcoefficient of vertical additional ,average additional stress of beneath a uniform rectangle load at corner point均布矩形荷载角点下竖向、附加、平均附加应力系数 c、cαcoefficient of vertical additional stress beneatha concentration load集中应力系数αcoefficient of viscosity 粘滞系数coefficient of volume compression体积压缩系数m Vcoefficient of weathering 风化系数cohesionless soils无粘性土cohesive soils粘性土collapsibility湿陷性compactibility压实性compaction by rolling 碾压法compactiontest 击实试验compaction factor压实系数 ccompactness 密实度composite ground 复合地基compressibility 压缩性compression index压缩指数C ccompression(constrained modulus)压缩(侧限)模量E scompression zone受力层,压缩层compression-curves压缩曲线(e-p和e-log p曲线)compressive strength 抗压强度concentrated load集中力P[static]cone penetration test[CPT]静力触探试验confined water head承压水头confining pressure[周]围压[力]consistency稠度consistency limit稠度界限consolidated quick (direct) shear test固结快剪(直剪)试验consolidated quick shear cohesion、angle of internal friction固结快剪粘聚力、内摩擦角c cq、ϕcqconsolidated undrained triaxial compression test [CU-test]固结不排水三轴压缩试验consolidated-undrained cohesion、angle of internal friction固结不排水粘聚力、内摩擦角c cu、ϕcuconsolidation apparatus固结仪、压缩仪、渗压仪consolidation curve 固结(d-t和d-log t曲线) consolidation settlement固结沉降s cconsolidation test (contain compression test ) 固结(压密)试验(含有压缩试验)constrained diameter of soil partical限制粒径d60constrained modulus侧限模量E scontact stress( pressure)接触应力(压力)contaminatedsoil 污染土corner-point method 角点法Coulomb’s theory of earth pressure库伦土压力理论creep蠕变critical edge、critical, ultimate load of subsoil bearing capacity 地基承载力的临塑荷载p cr、临界荷载p1/3 p1/4、极限荷载p u critical height of slope (土坡)临界高度critical hydraulic gradient临界水力梯度i crcritical void raio 临界孔隙比crushed stone,broken stone碎石culvert涵洞cushion垫层cyclic triaxial test周期三轴试验Ddamping ratio阻尼比Darcy’s law 达西定律Debris flow泥石流deep foundation 深基础deep mixing method 深层搅拌法degree of compaction 压实度 cdegree of consolidation固结度Udegree of saturation饱和度S rdensification by sand pile 挤密砂桩density密度depth factor of foundation基础深度系数d c、d q、dγdifferential settlement沉降差dike,levee 堤dilatancy 剪胀性diluvial fan洪积扇diluvial soils洪积土direct shear test直[接]剪[切]试验dispersive clay分散性粘土disturbed samples扰动土样double layer双电层drainage cohesion, angle of internal friction排水[剪]粘聚力、内摩擦角c d、ϕddrained shear strength排水抗剪强度τd[consolidated]drained triaxial[compression]test [CD-test][固结]排水三轴[压缩]试验drift-sand流砂[现象]dry density干密度 ddry gravity density (unit weight)干重度(容重) ddynamic elastic modulus动弹性模量E d dynamic load动荷载dynamic penetration test 动力触探试验dynamic triaxial test动三轴试验dynamic shear modulus动剪切模量G d dynamic strain,stress动应变 d、动应力 dEEarth dam土坝Earth material 土料earth pressure at rest静止土压力E0 earthquake engineering 地震工程学earth-rock dam 土石坝earthwork土石方工程eccentric load偏心荷载eccentricity of foundation base loading (result of forces) 基础底面荷载合力偏心距e effective angle of internal friction有效内摩擦角 ’effective cohesion 有效粘聚力c’effective grain size有效粒径d10effective stress有效应力 ’effective stress path[ESP] 有效应力路径elastic modulus,Young’s modulus弹性模量E electro-osmosis 电渗embankments路堤engineering geologic columnar profile工程地质柱状图engineering geologic exploration工程地质勘察engineering geologic drilling工程地质钻探engineering geologic evaluation 工程地质评价engineering geologic map工程地质图engineering geologicmapping 工程地质测绘engineering geologicprofile工程地质剖面图engineering geology工程地质学environmental geotechnics 环境岩土工程学equipotential lines 等势线excavation开挖excess hydrostatic pressure超静水压力excess pore water pressure(stress)超孔隙水压力(应力)expansibility and contractility胀缩性expansion ,swelling index回弹指数C eexpansive soil膨胀土experience factor of settlement calculation沉降计算经验系数Ffactor of safety安全系数failure strength破坏强度failure surface 破坏面fault断层field identification 土的现场鉴别field observation 现场观测fill填土film water,film moisture 薄膜水filter反滤层final settlement最终沉降量sfinal settlement by settlement observation calculating沉降观测推算的最终沉降量s∞fine sand细砂fine-grained soils, fines细粒土fissured soils裂隙粘土fissured water裂隙水flocculent structure絮凝结构flow line 流线flow net流网fold 褶皱flowing sand流砂[现象]fluvial soils冲积土footing,foundation基础foundation settlement地基(基础)沉降fraction粒组free swelling ratio自由膨胀率 effree water自由水free water elevation ,surface地下水位freezingmethod 冻结法friction coefficient offoundation base 基底摩擦系数μfriction-resistance ratio摩阻比frost boiling翻浆frozen heaving properties冻胀性frozen soils冻土GGap-graded soil不连续级配土General-shear failure 整体剪切破坏generalized procedure of slices[GPS]普通条分法[vertical]geostatic(self weight)stress (pressure)[竖向]自重应力(压力)σc、σczgeosynthetics 土工合成材料geotechnical engineering岩土工程geotechnical investigation岩土工程勘察geotextiles 土工织物glacial soils冰积土grading curve级配曲线grain size粒径grain size accumulation curve粒径累计(积)曲线granularity粒度gravel圆砾gravelly sand砾砂gravelly soils砾类土gravitational acceleration重力加速度ggravitational water重力水gravity density重[力密]度γgravity retaining wall重力式挡土墙ground tilt factor地面倾斜系数g c、g q、gγground treatment地基处理ground water地下水、潜水ground water level [GWL],groundwater elevation ,surface,[ground] water table[GWT]地下水位groundwater dynamics 地下水动力学grouting 灌浆Hhalf-space(semi-infinite body)半空间(半无限体)Hansen’s formula of ultimate bearing capacity汉森极限承载力公式hardness degree of rock 岩石坚硬程度head [of water]水头Hheavy dynamic penetration test[HDPT] 重型动力触探试验height of retaining wall挡土墙高度H heigth of tensile area拉力区高度h0 high liquid limit clay ,mo[CH],[MH]高液限粘土、粉土highway公路honeycomb structure蜂窝结构hydraulic gradient水力梯度I hydraulic head水头Hhydrometer method比重计法hydrostatic pressure静水压力Iillite伊利石immediate settlement瞬时沉降s d impermeable lager,impervious stratum 不透水层inclined load倾斜荷载influence coefficients of settlement沉降影响系数 、 o、 c、 m、 r initial collapse pressure 湿陷起始压力initial tangent modulus初始切线模量E i inorganic mineral substance无机矿物质in-situ test原位测试in-situ bearing test现场承载力试验intermediam liquid limit clay [CI]中液限粘土internal friction angle 内摩擦角internal scour潜蚀isotropic soil各向同性土J Janbu’s method of slices 杨布条分法jet grouting method 高压喷射注浆法joint 节理K kaolinite 高岭石karst land feature 喀斯特地貌K0-consolidation K0固结Llaminar flow层流landslide滑坡land subsidence 地面下沉lateral geostatic stress侧向自重应力σcx,σcylaterite 红土layer-wise summation method分层总和法length of foundation base基础底面长度llimit equilibrium condition极限平衡条件limit of plasticity塑限w Plinear shrinkage ratio 线缩率line load线荷载liquefaction液化liquefaction resistance抗液化强度liquid limit[LL]液限w Lliquidity index[LI]液性指数I Lloading test载荷试验local shear failure 局部剪切破坏loess黄土logarithmic spiral对数螺旋线low liquid limit clay,mo[CL],[ML]低液限粘土、粉土MMagmatic rock (igneous rock)岩浆岩(火成岩)major, intermediate, minor principle stress 大、中、小主应力σ1、σ2、σ3marine soils海积土mass circle sliding method整体圆弧滑动法maximum ,minimum void ratio最大、最小孔隙比emax、eminmaximum 、minimum pressure of foundation base基底最大、最小压力p max、p minmaximum, minimum dry density最大、最小干密度ρdmax、 dminmaximum dry density 最大干密度maximum expanded depth of plasticity region塑性区最大发展深度z maxmedian grain diameter中值粒径d30medium sand中砂meniscus弯液面metamorphic rock 变质岩method of slice 条分法mingle soils混合土miscellaneous fill杂填土mo,silts,silty soils粉土(粉性土、粉质土) modulus of deformation, elasticity变形模量E0弹性模量Emodulus of recompression再压缩模量modulus of resilience回弹模量Mohr-Coulomb law摩尔库仑定律moisture-density test 击实试验moisture ,water content含水量(率)w montmorillonite蒙脱石muck, muck soils淤泥、淤泥质土mulching soils覆盖土mud pumping 翻浆冒泥Nnatural angle of repose自然(天然)休止角nomal stress法向应力 x、 y、 znon-cohesive soils无粘性土non-uniform settlement 不均匀沉降normallyconsolidation归一化normally consolidated soils[N.C.soils]正常固结土Ooptimum moisture content 最优含水率organic soil 有机质土Oedometer modulus 侧向压缩模量Eoed、Es oedometer 固结仪、压缩仪、渗透仪one-dimensional consolidation单向固结(压密)optimum moisture,(water)content最优含水量(率)w oporganic soil有机质土,有机土organic substance,organic matter有机质original rock 基岩over coarse-grained soils巨粒土overburden soils覆盖土overconsolidated soils[O.C,soils]超固结(过压密)土overconsolidation ratio [OCR]超固结(过压密)比Pparameters of shear strength 抗剪强度参数partical size粒径partical size analysis颗粒分析试验passive earth pressure被动土压力E ppath of percolation渗[透途]径Hpeat泥炭pebble圆砾penetration resistace贯入阻力percent of soil particles土粒百分含量p i perched water上层滞水perennially frozen soil多年冻土permeable layer ,pervious stratum 透水层permeability渗透性permeability test渗透试验phreatic line浸润线phreatic water潜水、地下水physical properties of rock岩石的物理性质piezocone test[CPTU]孔压静力触探试验piezometric head测压管水头piezometer head测压管水头hpiping管涌plane strain test平面应变试验plastic failure塑性破坏plastic flow塑流plastic limit[PL]塑限w Pplastic strain 塑性应变plastic zone塑性区plasticity chart塑性图plasticity index[PI]塑性指数I pplate loading test平板载荷试验point loading点荷载试验Poisson’s ratio泊松比μpoorly-graded soils不良级配土pore air pressure孔隙气压力pore water pressure(stress)孔隙水压力(应力)upore pressure(stress) parameters孔隙压力(应力)系数A、Bpore pressure ratio孔隙压力比porewater孔隙水porosity孔隙率npreconsolidation pressure先(前)期固结压力p cpreloading method预压法pressure bulb压力泡pressuremeter test[PMT]旁(横)压试验primary consolidation主固结primary mineral原生矿物principal stress主应力 1、 2、 3principle of effective strress有效应力原理proctor [compaction]test普罗克特[击实]试验proportional limit load 比例界限荷载p prpumping test抽水试验punching-shear failure冲[切]剪[切]破坏Qquality of soil, soil particles (solids),water土、土粒、水的质量m、m s、m wQuaternary deposit第四纪沉积层quicksand流砂[现象]quick shear cohesion, angle of internal friction快剪粘聚力、内摩擦角c q、ϕqquick[shear] test快剪试验RRadius of influence影响半径Rankine’s theory of earth pressure朗肯土压力理论rate of settlement沉降速率ratio of length to width长宽比mrebound modulus回弹摸量recompression curve再压缩曲线rectangular footing矩形基础red clay ,adamic earth红粘土regional soils 特殊[性]土,区域性土relative density [RD]相对密(实)度D rresidual deformation残余变形residual soils 残积土residual strength 残余强度rubble ,rubble-stone 块石running sand流砂[现象]rupture surface破坏面Ssaline soil盐积土sand drain排水砂井sand particle content砂粒含量sand boiling砂沸(涌)现象、喷水冒砂sandy silt砂质粉土sandy soils, sands砂土(砂类土、砂性土、砂质土)saturated density饱和密度ρsatsaturated gravity density饱和重度γsatscale effect尺度效应screw plate loading test[SPLT]螺旋板载荷试验seasonally frozen soil季节冻土secondary compression (consolidation)index次压缩(固结)指数Cαsecondary compression (consolidation)settlement ,creep settlement次压缩(固结)沉降s ssecondary mineral次生矿物secondary red clay次生红粘土seepage[flow] 渗流(漏)seepage deformation 渗透变形seepage failure 渗透破坏seepage discharge渗流量Qseepage force渗流力(动水力)G Dseepage line浸润线(渗流线)seepage velocity渗流速度vseepage path渗径[verticale ]self weight (geostatic)stress (pressure)[竖向]自重应力(压力)σcz、σcsemi—infinite elastic半无限弹性体sensitivity灵敏度Stsettlement calculation depth沉降计算深度znshallow foundation 浅基础shape factor of foundation基础形状系数s c、s q、sγshear failure剪切破坏shear modulus剪切模量Gshear resistance 剪阻力或抗剪力shear strain剪应变shear strength抗剪强度 fshear strength envelope抗剪强度包线shear stress剪应力sheet pile wall板桩墙shrinkage limit[SL]缩限w ssieve analysis test筛分试验silty clay粉质粘土silty sand粉砂silty soils,silts,mo粉土(粉性土、粉质土)single-grained structure单粒结构size fraction粒组slip surface滑动面slope stability土坡稳定性slope wash,slope materials坡积土slow shear cohesion,angle of internal friction慢剪粘聚力、内摩擦角c s、ϕsslow(direct)shear test慢剪试验soft clay软粘土soft foundation 软弱地基soil土soil classification土的分类soil cohesion,angle of internal friction土的粘聚力c、内摩擦角soil dynamics土动力学soil fabric土的组构soil flow流土soil mechanics土力学soil nailing土钉soil sampler取土器soil skeleton土骨架soil structure and texture土的结构和构造soil supporting layer,substrate地基持力层、下卧层soil,foundation and superstructure interaction 地基、基础与上部结构相互作用soils and Foundations 地基及基础soils improvement 地基处理special soils特殊(性)土specific gravity of soil particles土粒比重G sspecific penetration resistance比贯入阻力p sspecific surface比表面(积)split test劈裂试验(巴西试验)SPT blow count标[准]贯[入试验锤]击数N square footing方形基础stabilityof foundation soil 地基稳定性stability against sliding抗滑稳定性stability number稳定数N sstability number method稳定数法standard penetration test [SPT]标准贯入试验static penetration test[CPT]静力触探试验static failure strength静力破坏强度 fstip foundation 条形基础Stokes’ law司笃克斯定律Stones,stoney soils碎石[类]土stress、strain 应力 、应变stress history,path,level应力历史、路径、水平stress concentration应力集中strength envelope 强度包线strength of active earth pressure主动土压力强度σastrength of passive earth pressure主动土压力强度σpstrength of earth pressure at rest静止土压力强度σ0strip load条形荷载subgrade路基、地基subgrade reaction地基反力superimposed pressure of foundation base基底平均附加压力psuperimposed stress (pressure)of subsoil地基附加应力(压力) zsurcharge[load]超载surface tension表面张力surface water地表水surface wave velocity method表面波法Swedish circle method瑞典圆弧法swelling force膨胀力swelling,expansion index 回弹(膨胀)指数C e swelling ratio膨胀率syncline向斜T[ground]table 地下水Terzaghi’s theory of one dimensional consolidation 太沙基一维固结理论Terzaghi’s ultimate bearing capacity太沙基极限承载力thaw collapse融陷thick wall sampler厚壁取土器thinwall sampler薄壁取土器thixotropy触变性three phase diagram三相图tilt factors of load荷载倾斜系数i c、i q、iγtime factor时间因数total stress总应力σtotal stress path [TSP]总应力路径transducer传感器triaxial compression test三轴压缩试验true triaxial test 真三轴试验two-dimensional consolidation二维固结(压密)two-dimensional flow二维流turbulent flow紊流Uultimate bearing capacity 极限承载力unconfined compression strength of remolded soil 重塑土的无侧限抗压强度q u'unconfined compressive strength无侧限抗压强度q uunder consolidated soil欠固结土underground diaphragm wall地下连续墙underlying stratum 下卧层undisturbed soil sample不扰动土样(原状土样) uniformly distributed load均布荷载undrained shear strength cohesion ,angle of internal f riction不排水抗剪强度τu、粘聚力c u、内摩擦角 [unconsolidation]undrained triaxial compression test[UU-test][不固结]不排水三轴压缩试验unit weight 容重[un]uniformity coefficient不均匀系数C u unsaturated soil非饱和土VVan der Waals’ [bonding]forces范德华(键)力[field]Vane shear test [FVT] [现场]十字板剪切试验vertical average degree of consolidation竖向平均固结度zUvertical force of foundation top基础顶面竖向力Fvertical time factor竖向时间因数T vVesic’s formula of ultimate bearing capacity魏锡克极限承载力公式vibration frequency振次n[dynamic]viscosity[动力]粘[滞]度ηvoid ratio孔隙比evolumetric strain体应变volume of soil,soil particles (solids), water , air土、土粒、土中水、土中气的体积V、V s、V w、V avolume of void孔隙体积V vvolume shrinkage ratio体缩率WWater,moisture content含水量(率)wwater content ratio含水比uwater table地下水位weak ground软弱地基weathering风化weighted average gravity density(unit weight)加权平均重度(容重) 0well-graded soil良好级配土wet density湿密度width of foundation base基础底面宽度bYyeilding flow塑流yellow clay ,loess黄土yield 屈服yield criteria 屈服准则Young’s modulus,elastic m odulus弹性模量E。
Tectonic Uplift and Mountain Formation
Tectonic Uplift and Mountain Formation Tectonic uplift and mountain formation are geological processes that have shaped the Earth's surface for millions of years. These processes are driven by the movement of the Earth's tectonic plates, which can result in the formation of towering mountain ranges and breathtaking landscapes. In this response, we will explore the complexities of tectonic uplift and mountain formation from various perspectives, including the geological, environmental, and human impact of these processes.From a geological perspective, tectonic uplift is the process by which the Earth's crust is pushed upwards due to the movement of tectonic plates. This can occur through a variety of mechanisms, including the collision of tectonic plates, the subduction of one plate beneath another, or the upwelling of magma from the Earth's mantle. As the crust is pushed upwards, it can result in the formation of mountain ranges, as well as other landforms such as plateaus and hills. This process is incredibly slow, occurring over millions of years, but its effects are profound and long-lasting.Mountain formation, on the other hand, is the result of tectonic uplift combined with other geological processes such as erosion and weathering. As mountains are uplifted, they are also subject to the forces of erosion, which can wear away at the rock and soil, shaping the landscape into its characteristic rugged and steep terrain. This interplay between uplift and erosion is what gives mountains their distinctive appearance and contributes to the diversity of landscapes found around the world.From an environmental perspective, tectonic uplift and mountain formation have a significant impact on the Earth's ecosystems and biodiversity. The creation of mountain ranges can result in the formation of diverse habitats, including alpine meadows, forests, and high-altitude deserts. These habitats support a wide variety of plant and animal species, many of which are unique to mountain environments. Additionally, the presence of mountains can influence local weather patterns, leading to the creation of microclimates and affecting the distribution of precipitation. As a result, mountains play a crucial role in regulating the Earth's climate and supporting a healthy and diverse biosphere.However, the environmental impact of tectonic uplift and mountain formation is not solely positive. The creation of mountains can also lead to the displacement of existing ecosystems and species, as well as the disruption of natural migration patterns. Additionally, the erosion of mountains can result in the deposition of sediment into nearby rivers and streams, leading to changes in water quality and the potential for flooding. These environmental challenges must be carefully managed in order to preserve the unique habitats and biodiversity found in mountainous regions.From a human perspective, tectonic uplift and mountain formation have had a profound impact on the development of human societies and cultures. Throughout history, mountains have served as both barriers and conduits for human migration and trade, shaping the movement of people and the exchange of ideas and resources. In many cultures, mountains are revered as sacred places, and their unique landscapes have inspired countless works of art, literature, and spirituality. Additionally, the natural resources found in mountainous regions, such as minerals, timber, and water, have been vital to the development of human societies and economies.However, the presence of mountains also presents challenges for human communities. The rugged terrain and harsh climate of mountainous regions can make agriculture and infrastructure development difficult, leading to a reliance on imported goods and services. Additionally, the potential for natural hazards such as landslides, avalanches, and earthquakes poses a constant threat to human settlements in mountainous areas. As a result, the unique opportunities and challenges presented by mountains have shaped the cultural and economic development of human societies around the world.In conclusion, tectonic uplift and mountain formation are complex geological processes that have far-reaching implications for the Earth's surface, ecosystems, and human societies. From the slow and powerful forces of tectonic uplift to the dynamic interplay of erosion and weathering, these processes have shaped the landscapes we see today and will continue to do so in the future. By understanding and appreciating the complexities of tectonic uplift and mountain formation, we can better steward the natural resources and uniqueenvironments found in mountainous regions, ensuring their preservation for future generations.。
北极冻土层英文阅读理解
北极冻土层英文阅读理解The Arctic tundra, a vast expanse of frozen soil, holds secrets that have been frozen in time for centuries. With layers of permafrost extending deep beneath the surface,it's a natural freezer for ancient remains and organisms.Exploring the tundra feels like stepping into a world untouched by modern civilization. The cold air bites at your nose, and the quiet is so absolute, you can almost hear the earth breathe. Beneath the snow and ice, there's a story that's slowly being revealed to us.The frozen soil acts as a time capsule, preserving things that have been lost to the rest of the world. From ancient mammals to mysterious microbes, the tundra is a treasure trove for scientists. But as the climate warms, these fragile ecosystems are under threat.Walking across the tundra, you can see evidence of how the environment is changing. Pools of meltwater form whereonce there was solid ice. Plants are beginning to grow in areas that were once barren. It's a reminder of thefragility of our planet and the need to protect these unique habitats.And yet, there's beauty in this desolate landscape. The stark contrast between the white snow and the blue sky is breathtaking. The silence is deafening, yet it's a silence that feels cleansing and pure. In the Arctic tundra, nature is at its most raw and unforgiving, yet it's also its most captivating.。
科技核心论文写作时态的使用要妥当
例6
We will examine if parallel universes exit.
练习:下列各句应使用过去时还是现在时(如果答案不只一个,请解释原因)。
1.In our study, tree size __________(increase) with reduction of pesticides.
15.Coupled climate-carbon cycle models__________(suggest) that Amazon forests__________(be) vulnerable to droughts, but satellite observations__________(show) a green-up in intact evergreen forests of the Amazon in response to a short, intense drought in 2005.
参考答案
1. increased
2. feed
3. found … indicates
4. diverged
5. have
6. showed… reproduce
定心锥面的英文
定心锥面的英文Defining the Conical FrustumThe conical frustum, a captivating geometric shape, has long been a subject of fascination for mathematicians, engineers, and designers alike. This three-dimensional figure, formed by slicing a cone parallel to its base, possesses a unique blend of elegance and functionality that has made it a staple in various industries and applications.At its core, the conical frustum is defined as the portion of a cone that remains after the top section has been removed. This truncated cone retains the essential characteristics of its parent shape, including a circular base and a tapered upper surface. However, the removal of the top section gives rise to a distinct geometry, one that is both visually striking and inherently practical.One of the defining features of the conical frustum is its ability to maintain a stable and balanced form. Unlike a complete cone, which can be prone to tipping or rolling, the frustum's flat base provides a sturdy foundation that allows it to stand upright and resist external forces. This property has made the conical frustum a popular choice for a wide range of applications, from architectural design toindustrial equipment.In the realm of architecture, the conical frustum has been employed as a structural element in various building styles, from the ancient pyramids of Egypt to the modern skyscrapers of today. Its tapered shape not only adds visual interest to a structure but also contributes to its overall stability and load-bearing capabilities. Additionally, the frustum's versatility has led to its use in the design of domes, spires, and other distinctive architectural features, often serving as a striking focal point within a building or landscape.Beyond the realm of architecture, the conical frustum has found applications in numerous industries, including engineering, manufacturing, and even household products. In engineering, the frustum's shape is often used in the design of components such as gears, bearings, and various types of machinery. The tapered form allows for efficient transmission of forces and the creation of secure, interlocking connections between parts.In the manufacturing sector, the conical frustum has become a crucial element in the production of a wide array of goods. From the precise molding of plastic parts to the efficient shaping of metal components, the frustum's geometric properties have been leveraged to streamline manufacturing processes and ensure the consistent quality of the final products.Even in the realm of everyday household items, the conical frustum can be found. From the classic ice cream cone to the sleek design of certain kitchen appliances, this versatile shape has been embraced for its aesthetic appeal and functional advantages. The frustum's ability to concentrate and direct forces, as well as its inherent stability, have made it a popular choice for a diverse range of consumer goods.The fascination with the conical frustum extends beyond its practical applications, however. This geometric form has also captured the imagination of artists, designers, and mathematicians, who have explored its intriguing properties and incorporated it into their creative works.In the realm of art, the conical frustum has been used as a motif in various mediums, from sculptures and installations to two-dimensional works. Artists have often drawn inspiration from the frustum's elegant lines and the interplay of light and shadow that it creates, using it as a means of exploring themes of balance, proportion, and the relationship between form and function.In the field of mathematics, the conical frustum has been the subject of extensive study and analysis. Mathematicians have delved into the intricate calculations and formulas that govern the frustum'sdimensions, volume, and surface area, seeking to unlock the deeper insights that lie within this deceptively simple shape.Through this exploration, a deeper understanding of the conical frustum has emerged, revealing its rich mathematical properties and the underlying principles that govern its behavior. From the calculation of its surface area to the derivation of its volume, the frustum has proven to be a fascinating subject of study, offering insights into the fundamental laws of geometry and the nature of three-dimensional space.In conclusion, the conical frustum is a remarkable geometric shape that has captivated the minds of individuals across various disciplines. Its unique blend of form, function, and mathematical elegance has made it a ubiquitous presence in the realms of architecture, engineering, manufacturing, and even art and design. As we continue to explore and harness the potential of this versatile shape, the conical frustum promises to remain a source of fascination and inspiration for generations to come.。
地质工程专业英语
1地形地貌geographic and geomorphic工程地质条件engineering geological conditions地形地貌条件geographic and geomorphic conditions 地形land form地貌geomorphology, relief微地貌microrelief地貌单元landform unit, geomorphic unit坡度grade地形图relief map河谷river valley河道river course河床river bed(channel)冲沟gully, gulley, erosion gully,stream(brook)河漫滩floodplain(valley flat)阶地terrace冲积平原alluvial plain三角洲delta古河道fossil river course, fossil stream channel冲积扇alluvial fan洪积扇diluvial fan坡积裙talus apron分水岭divide盆地basin岩溶地貌karst land feature, karst landform溶洞solution cave, karst cave落水洞sinkhole土洞Karstic earth cave2地层岩性地层geostrome (stratum, strata)岩性lithologic character, rock property岩体rock mass岩层bed stratum岩层layer, rock stratum母岩matrix, parent rock相变facies change硬质岩strong rock, film软质岩weak rock硬质的competent软质的incompetent基岩bedrock岩组petrofabric覆盖层overburden交错层理cross bedding层面bedding plane片理schistosity层理bedding板理(叶理)foliation波痕ripple-mark泥痕mud crack雨痕raindrop imprints造岩矿物rock-forming minerals 粘土矿物clay mineral高岭土kaolinite蒙脱石montmorillonite伊利石illite云母mica白云母muscovite黑云母biotite石英quartz长石feldspar正长石orthoclase斜长石plagioclase辉石pyroxene, picrite角闪石hornblende方解石calcite构造structure结构texture组构fabric(tissue)矿物组成mineral composition结晶质crystalline非晶质amorphous产状attitude火成岩igneous岩浆岩magmatic rock火山岩(熔岩)lava火山volcano侵入岩intrusive(invade) rock 喷出岩effusive rock深成岩plutonic rock浅成岩pypabysal rock酸性岩acid rock中性岩inter-mediate rock基性岩basic rock超基性岩ultrabasic rock岩基rock base (batholith)岩脉(墙)dike岩株rock stock岩流rock flow岩盖rock laccolith (laccolite) 岩盆rock lopolith岩墙rock dike岩床rock sill岩脉vein dyke花岗岩granite斑岩porphyry玢岩porphyrite流纹岩rhyolite正长岩syenite粗面岩trachyte闪长岩diorite安山岩andesite辉长岩gabbro玄武岩basalt细晶岩aplite伟晶岩pegmatite煌斑岩lamprophyre辉绿岩diabase橄榄岩dunite黑曜岩obsidian浮岩pumice火山角砾岩vulcanic breccia火山集块岩volcanic agglomerate凝灰岩tuff沉积岩sedimentary rock碎屑岩clastic rock粘土岩clay rock粉砂质粘土岩silty claystone化学岩chemical rock生物岩biolith砾岩conglomerate角砾岩breccia砂岩sandstone石英砂岩quartz sandstone粉砂岩siltstone钙质粉砂岩calcareous siltstone泥岩mudstone页岩shale盐岩saline石灰岩limestone白云岩dolomite泥灰岩marl泥钙岩argillo-calcareous泥砂岩argillo-arenaceous砂质arenaceous泥质argillaceous硅质的siliceous有机质organic matter粗粒coarse grain中粒medium-grained沉积物sediment (deposit)漂石、顽石boulder卵石cobble砾石gravel砂sand粉土silt粘土clay粘粒clay grain砂质粘土sandy clay粘质砂土clayey sand壤土、亚粘土loam砂壤土、亚砂土轻亚粘土sandy loam浮土、表土regolith (topsoil)黄土loess红土laterite泥灰peat软泥ooze淤泥mire, oozed mud, sludge, warp clay 冲积物(层)alluvion冲积的alluvial 洪积物(层)proluvium, diluvium, diluvion洪积的 diluvial坡积物(层) deluvium残积物(层) eluvium残积的eluvial风积物(层) eolian deposits湖积物(层) lake deposits海积物(层) marine deposits冰川沉积物(层)glacier (drift)deposits崩积物(层)colluvial deposits, colluvium残积粘土residual clay变质岩metamorphic rock板岩slate千枚岩phyllite片岩schist片麻岩gneiss石英岩quartzite大理岩marble糜棱岩mylonite混合岩migmatite碎裂岩cataclasite3地质构造地质构造geologic structure结构构造structural texture大地构造geotectonic构造运动tectogenesis造山运动orogeny升降运动vertical movement水平运动horizontal movement完整性perfection(integrity)起伏度waviness尺寸效应size effect围压效应confining pressure effect产状要素elements of attitude产状attitude, orientation走向strike倾向dip倾角dip angle, angle of dip褶皱fold褶曲fold单斜monocline向斜syncline背斜anticline穹隆dome挤压squeeze上盘upper section下盘bottom wall, footwall, lower wall 断距separation相交intersect断层fault正断层normal fault逆断层reversed fault平移断层parallel fault层理bedding, stratification微层理light stratification地堑graben地垒horst, fault ridge断层泥gouge, pug, selvage, fault gouge 擦痕stria, striation断裂fracture破碎带fracture zone节理joint节理组joint set裂隙fissure, crack微裂隙fine fissure, microscopic fissure劈理cleavage原生裂隙original joint次生裂隙epigenetic joint张裂隙tension joint剪裂隙shear joint卸荷裂隙relief crack裂隙率fracture porosity结构类型structural pattern岩体结构rock mass structure岩块block mass结构体structural element块度blockness结构面structural plane软弱结构面weak plane临空面free face碎裂结构cataclastic texture板状结构platy structure薄板状lamellose块状的lumpy, massive层状的laminated巨厚层giant thick-laminated薄层状的finely laminated软弱夹层weak intercalated layer夹层inter bedding,intercalated bed, interlayer, intermediate layer 夹泥层clayey intercalation夹泥inter-clay连通性connectivity切层insequent影响带affecting zone完整性integrity n.Integrate v. & a.degree of integrality破碎crumble胶结cement泥化argillization尖灭taper-out错动diastrophism错动层面faulted bedding plane断续的intermittent破碎crumble共轭节理conjugated joint散状loose 透镜状的lens-shaped a.岩石碎片crag岩屑cuttings, debris薄膜membrane, film层理stratification高角度high dip angle缓倾角low dip angle反倾anti-dip互层interbed v.Interbedding n.起伏的unplanar波状起伏的undulate, undulating粒径particle size构造层tectonosphere挤压compression均一的homogeneous剪切错动面shear faulted, bedding zone切割dissection切割的dissected致密close, compact构造岩tectonite糜棱岩mylonite断层角砾岩fault breccia方解石脉calcite vein碎块岩clastic rock角砾breccia岩粉rock powder岩屑debris, debry固结consolidation定向排列oriented spread构造应力tectonic stress残余应力residual stress4水文地质条件hydrogeological conditions 水文循环hydrologic cycle大气圈atmosphere水圈hydrosphere岩石圈geosphere地表径流surface runoff地下径流subsurface runoff流域valley, drainage basin流域面积drainage area, river basin area 汇水面积catchment area地下水ground water, subsurface water 地表水surface water大气水atmospheric water气态水aqueous (vapour) water液态水liquid water固态水solid water上层滞水perched water潜水phreatic water承压水confined water吸着水hygroscopic (adsorptive) water 介质medium空隙void孔隙水压力pore water pressure渗透压力osmotic pressure, seepage force扬压力uplift pressure静水压力hydrostatic pressure外静水压力external hydrostatic pressure动水压力hydrodynamic pressure渗透力seepage pressure外水压力external water pressure内水压力internal water pressure水力联系hydraulic interrelation水力折减系数hydraulic reduction coefficient水头损失water head loss渗透途径filtration path, seepage path渗透系数penetration coefficient潜水位water table level水位water level, stage level水头water head含水层aquifer弱含水层(弱透水层)aquitard滞水层aquiclude透水层permeable layer, pervious layer不透水层(隔水层)aquifuge, impervious layer,impermeable layer, aquiclude潜水含水层phreatic aquifer承压含水层confined aquifer, artesian aquifer承压面bearing surface潜水面phreatic surface, water table浸润线phreatic curve不透水边界impervious boundary地下分水岭groundwater ridge粘滞性viscosity富水性abundance透水性(渗透性)permeability淋滤(溶滤作用)lixiviation, leaching反滤层inverted gravel filter水锈incrustation渗滴seep饱和saturation, saturated潜水位变化带zone of variable phreatic level气象因素meteorological factor饱水带zone of saturation包气带aeration zone, zone of aeration包气带水aeration zone water上层滞水perched water孔隙水pore water裂隙水fissure water岩溶水karstic water结合水bound water, combined water吸着水hydroscopic water薄膜水pellicular water毛细水capillary water重力水gravitational water凝结水condensation water地下水埋藏条件condition of groundwater occurrence 地下水埋藏深度depth of groundwater occurrence 压水试验packer permeability test抽水试验pumping test5物理力学性质物理力学physical mechanics n.Physico-mechanical a.屈服准则yield criteria米赛斯屈服准则Von Mises yield criteria朗肯土压力理论Ranking’s earth pressure theory 剑桥模型Cambridge model, Cam-model邓肯-张模型Duncan-chang model本构方程constitutive equation局部剪切破坏 local shear failure整体剪切破坏 general shear failure岩体完整性指数intactness index of rock mass安全系数factor of safety埋深embedment depth试件coupons挠度deflection里氏震级Richter scale设计烈度design intensity基本烈度basic intensity场地烈度site intensity地震烈度seismic intensity, intensity scale卓越周期predominant period持力层sustained yield超载surcharge围岩压力surrounding rock stress附加压力superimposed stress应力松弛stress relaxation应力路迳stress path卸荷unload渗透率specific permeability饱和度degree of saturation含水量moisture content平均粒径mean diameter颗粒grain, granule, particle颗粒级配distribution of grain-size,grain composition, size distribution级配graduation,grain-size distribution, gradation, grading 粒度coarseness grain size, granularity, lump不均匀系数coefficient of non-uniformity,variation coefficient, variation factor颗粒分级gradation, size grading孔隙水pore water孔隙比void ratio (ration)空隙率air voids孔隙率porosity裂隙率crackity溶隙率karstity密度density重度unit weight, bulk weight浮重度buoyant unit weight折减系数reduction factor压力消散dissipation of pressure抗力系数coefficient of resistance软化系数softening coefficient含水量water content稠度consistency塑限plastic limit液限liquid limit塑性指数plasticity index液性指数liquidity index流变rheological蠕变creep塑性plastic脆性brittleness(fragility)粘性stickness刚性rigidity弹性的elastic粘弹性viso-elasticity弹塑性elasto-plasticity压缩性compressibility均质性homogeneity非均质性nonhomogeneity (heterogeneity) 各向同性isotropy各向异性anisotropy总应力total stress有效应力effective stress超孔隙水压力excess pore pressure孔隙水压力pore water pressure抗压强度compressive strength抗拉强度tensile strength抗剪强度shear strength不排水抗剪强度undrained shear strenght峰值抗剪强度 peak share strength长期抗剪强度 long-term shear strength残余抗剪强度 residual shear strength负摩擦力negative skin friction, dragdown 摩擦角angle of friction内摩擦角angle of internal friction外摩擦角angle of external friction内聚力cohesion粘聚力cohesion假凝聚力pseudo-cohesion粘着力adhesion摩尔圆Mohr’s circle包络线envelope休止角angle of repose,angle of friction(repose, rest), repose angle峰值peak模量modulus弹性模量modulus of elasticity,Young’s modulus, elastic modulus压缩模量modulus of compressibility 变形模量modulus of deformation卸荷模量unloading modulus切线模量tangent modulus剪切模量shear modulus割线模量secant modulus旁压模量pressurmeter modulus泊松比poisson’s ration固结consolidation固结系数coefficient of consolidation固结度degree of consolidation超固结比over consolidation ration应变strain压缩比compressibility ratio压缩系数coefficient of compressibility压缩指数compression index初始曲线virgin curve正常固结土normally consolidated soil欠固结土under-consolidated soil超固结土over-consolidated soil被动土压力passive earth pressure主动土压力active earth pressure静止土压力earth pressure at rest覆盖压力overburden pressure初始应力initial stress地应力场ground(geostatic) stress field有效应力effective stress动应力dynamic stress动荷载dynamic load偏心荷载eccentric loads循环荷载inclined loads地应力ground stress, geostatic stress初始应力initial stress应力场stress field纵波longitudinal wave液化势liquefaction potential液化指数liquefaction index交角angular岩石抗力系数 coefficient of rock resistance容许承载力allowable bearing capacity临塑压力critical pressure接触压力contact pressure6工程地质问题工程地质问题engineering geological problem 定性评价qualitative estimate定量评价quantitative estimate极限平衡法limit equilibrium method不良地质现象unfavorable geological condition 风化weathering变形deformation位移displacement不均匀位移differential movement相对位移relative displacement沉陷settlement山崩avalanche, toppling崩塌toppling, toppling collapse滑坡、地滑creep, slide切层滑坡insequent landslide深层滑坡deep slide浅层滑坡shallow slide顺层滑坡consequent landslide滑动面sliding surface, sliding plane, slip surface滑动带sliding zone滑床slide bed滑坡体slide(sliding) mass古滑坡fossil landslide推移式滑坡slumping slide牵引式滑坡retrogressive slide管涌piping, internal erosion渗漏leakage流砂quicksand渗流seepage液化liquefaction7工程勘察engineering investigation工程地质勘察 engineering geology investigation岩土工程勘察 geotechnical investigation工程地质条件 engineering geological condition工程地质评价 engineering geological evaluation勘测survey岩芯采取率core recovery, core extraction岩芯获得率RQD(岩石质量指标)rock quality designation程序(步骤) procedure勘察阶段investigational stage选点踏勘reconnaissance初步设计primary design初步规划preliminary scheme初步勘探preliminary prospecting初步踏勘ground reconnaissance可行性研究阶段feasibility stage初步设计阶段 preliminary stage施工阶段construction sage踏勘reconnaissance, inspection地质测绘geological survey工程地质测绘 engineering geological mapping钻探borehole operation, boring物探geophysical exploration洞探exploratory adits钎探rod sounding坑探exploring mining槽探trenching天然建材调查natural materials surveying (examination)岩土工程勘察报告geotechnical investigation report 鉴定identification, appraisal鉴定书expertise report鉴定人identifier, surveyor 校核verification总监chief inspector比例proportion地形图geographic map地貌图geomorphological map地质图geological map工程地质图engineering geological map实测地质剖面图field-acquired geological profile(section) 构造地质图geological structure map第四纪地质图quarternary geological map地质详图detail map of geology地质柱状图geologic columnar section, geologic log钻孔柱状图logs of bore hole纵剖面图longitudinal section横剖面图cross section展示图reveal detail map节理玫瑰图rose of joints基岩等高线bed rock contour层底等高线contour of stratum bottom岩层界线strata boundary岩面高程elevation of bed rock surface坐标coordinate分层bed separation地质点geological observation point勘探点exploratory point (spot)勘探线exploratory line勘探孔exploration hole平洞adit竖井riser, shaft, vertical shaft探槽exploratory trench探井exploratory pit钻孔borehole, drill hole机钻孔ordinary drill hole套钻孔sleeve drill hole管钻孔pipe drill hole岩芯core岩芯钻探core drilling回转钻探(进)rotary drilling冲击钻探churn drilling, percussion drilling钢砂钻探shot drilling铁砂钻进iron shot drilling跟管钻进follow-down drilling振动钻进vibro-boring, vibro-drilling泥浆钻探mud flush drilling金刚石钻进diamond drilling单动式single acting双层double layer空气钻探air flush drilling钻机drilling rig钻头drill bit, drilling bit螺旋钻头auger勺钻spoon bit冲击钻头percussion bit, chopping bit桶式钻头bucket auger钻杆drill rod套管casing岩芯管core barrel冲洗掖flush fluid正循环冲洗direct circulation反循环冲洗reverse circulation泥浆mud, slurry泥皮mud cake护壁dado止水seal, water seal扫孔cleaning bottom of hole钻进drilling平硐adit竖井shaft钻探drilling boring8工程地质试验击实试验compaction test压缩试验compression test固结试验consolidation test单轴试验uniaxial compression test现场剪切试验in-situ shear test单剪试验simple shear test直剪试验direct shear test慢剪试验slow test单剪试验simple shear test快剪试验quick test三轴剪切试验triaxial shear test三轴压缩试验triaxial compression test动三轴试验dynamic triaxial test不固结不排水剪试验unconsolidated undrained test(quick test)固结不排水剪试验consolidated undrained test(consolidated quick test)固结排水试验consolidated drained test(slow test) 原位测试in-situ test现场监测on-site(in-site) monitoring现场检测on-site (in-site) inspection观测孔observation borehole静力触探试验cone penetration test,static penetration test, static cone test 标贯试验standard penetration test十字板剪切试验vane shear test, vane test检层法up-hole method, borehole method旁压试验pressuremeter test动力触探试验dynamic penetration test, dynamic sounding点荷载试验point load test岩石试验rock test应力解除法stress relief method应力恢复法stress recovery method 套孔法over-coring method9岩土体加固掌子面breast, driving face,heading face, tunnel face顶拱vault底拱invert洞室开挖excavation超挖overbreak风钻pneumatic drill开挖断面excavated section塌落slump细骨料混凝土 concrete made with fine aggregate细骨料fine aggregate, fine adjustment料场stock ground土料earth material矿渣cinder, mineral water residue, scoria, slag性能function, performance, property, nature凝结coagulate, congeal, congealment, coagulation 合格qualified, on test, up to standard初凝initial set初凝时间initial setting time终凝final set配合比mix proportion塌落度slump水化热heat of hydration,hydration heat, setting heat水灰比water-cement ratio粉煤灰fly ash梅花状quincuncial pattern喷射shotcrete浇注pouring钢筋网coiremesh加固reinforce锚杆anchored bar, rock bolt锚索anchored cable锚紧端anchor station锚桩anchored peg采石场rock quarry开挖excavation清基cleanup foundation明挖open-cut爆破explosion光面爆破smooth blasting预裂法presplitting10 水工概论坝址toe of dam坝踵heel坝段monolith坝顶crest坝肩shoulders左坝肩left dam abutment副坝saddle dam三坝址the third dam site标高height mark上游水位headwater正常库水位normal reservoir level地下洞室underground opening (tunnel)压力隧洞pressure tunnel无压隧洞gravity tunnel交通洞access tunnel灌浆洞grouting tunnel明流洞free-flow tunnel孔板洞orifice tunnel排砂洞sediment tunnel尾水洞tailrace tunnel排水洞drainage tunnel导流洞diversion tunnel隧道tunnel围岩surrounding rock, ambient rock围岩应力secondary stress static应力集中stress concentrate覆盖层over burden冒顶cave in, roof fall底鼓bottom heave回弹rebound岩爆rock burst冻结法freezing method超载over break衬砌lining围堰cofferdam堤dike近坝岸坡abutments施工(收缩)缝construction joint心墙core截水墙cutoff wall防渗墙diaphragm wall排水井drainage wells排水幕drainage curtain减压井relief wells反滤层filter zone灌浆材料grout水力劈裂hydraulic fracturing帷幔线curtain line上游围堰upstream cofferdam混凝土防渗墙 concrete cutoff wall截流interim completion导水墙channel training wall正常溢洪道渠首工程service spillway headwork 消力塘lined plunge pool隔墙divider walls混凝土护坦concrete apron副厂房auxiliary power house闸门室gate chamber中闸室mid gate chamber开关站switch yard电梯井elevator shaft尾水渠tail race非常溢洪道emergency spillway 11桥梁及基础工程江阴大桥Jiangyin Bridge悬索桥suspension bridge锚碇anchorage重力式嵌岩锚gravity socketed anchorage北锚碇前(后)锚面front(back) surface of northern anchorage 塔墩tower墩pier散索鞍splay saddle猫道footbridge主缆main cable索股cable strand主鞍main saddle, tower saddle主跨main span边跨side span引桥approach钢箱梁steel box main girder埋深embedment depth北塔墩基础north tower base基础foundation, footing浅基础shallow foundation深基础deep foundation联合基础combined footing筏形基础raft(mat) foundation钢模steel form桩pile基桩foundation pile群桩pile groups桩基础pile foundation桩承台pile cap高桩承台high-rise pile cap低桩承台buried pile cap摩擦桩friction pile端承桩end bearing pile嵌岩桩socketed pile板桩sheet pile旋喷桩jet-grouted pile灌注桩cast-in-place pile沉管灌注桩driven cast-in-place pile支护桩soldier piles, tangent piles刚性桩rigid pile柔性桩flexible pile侧向受荷桩laterally loaded pile轴向受荷桩axially loaded pile预制桩precast concrete pile振动打桩vibratory pile driving振动钻进vibratory drilling沉箱caisson沉井(沉箱) (open) caisson地下连续墙diaphragm wall, slurry wall支撑bracing超载surcharge接触应力contact pressure井点降水well-point dewatering桩极限承载力ultimate bearing capacity of pile承载力bearing capacity阻力resistance桩端阻力end resistance表面摩擦力skin friction粘着系数adhesion factor负摩擦力negative skin friction安全系数factor of safety压缩层compressed layer附加应力additional stress, superimposed stress 持力层bearing layer, sustaining layer地基土foundation soil, subsoil临塑压力critical pressure剪切破坏shear failure地基失效foundation failure冲剪破坏punching failure渐进破坏progressive failure容许荷载allowable load极限承载力ultimate bearing capacity沉降settlement沉降差differential settlement尾部倾斜angular distortion倾斜tilting坑底隆起bottom heave静止土压力earth pressure at rest稳定数stability number路堤embankment地基处理ground treatment soil improvement 垫层cushion加固stabilization注浆injection灌浆guniting帷幕curtain挡土墙retaining wall锚固anchoring喷浆guniting锚杆earth anchor盲沟French drain振冲法vibro jet12监测仪器观测孔observation bore/hole仪器观测instrumentation读数装置readout device传感器transducer探头probe压力盒pressure cell振弦式应变计vibrating wire strain gauge伸长计、变位计extension meter板式沉降仪foundation base/pate测斜仪inclinometer测压计,渗压计piezometer垂线plumb垂直度plumbness 13安全监控可靠性检查reliability checking监控模型monitoring and prediction model 监测monitoring资料datum, data可靠性reliability稳定性stability安全safety评估evaluation, appraise评定assessment, assess, rate评价准则criterion灾害hazard, calamity确定性方法论Deterministic methodology应急行动计划EAP(emergency action plan)事故accident紧急状态emergency紧急检查emergency inspection灾情等级hazard classification灾害评价hazard evaluation风险评估risk assessment静力(Static Analysis)动力(Dynamic Analysis)蠕变(Creep Material Model)渗流(Fluid-mechanical Interaction)热力学(Thermal Option)headward erosion溯源侵蚀scouring of levee or bank淘刷strongly weathered siliceous rock mass with quasi-lamellarweakly weathered siliceous rock mass withquasi-lamellarof continually aftershocks of 7 or 8-degree intensityEvidently 明显的Correspondingly adv. ?相应地; 相关地; 相同地the hanging wall of triggering seismic fault oblique~bedding bank slope。
物理专业英语词汇F汇总
物理专业英语词汇(F) f band f 带f center f 心f center laser f 心激光器f center maser f心微波激射器f layer f 层f value振子强度f/d ratio f/d 比face centered crystal 面心晶体face centered cubic lattice 面心立方晶格face centered cubic structure 面心立方结构face centered lattice 面心点阵factor因子factor group 剩余群facula光斑faddeev equation法捷耶夫方程faddeev popov ghost法捷耶夫波波夫鬼态fading衰退;褪色fahrenheit scale 华氏温标fahrenheit temperature scale 华氏温标fahrenheit thermometer 华氏温度计fall降低fall of potential 电压降fall time下降时间falling sphere viscometer 落球粘度计fallout放射性沉降物false image 鬼象family 族family of asteroids 小行星族family of comets 彗星族fano factor 法诺因子far field pattern 远场图样far infrared远红外区far infrared laser远红外激光器far infrared radiation 远红外卜辐射far infrared rays 远红外卜线far point 远点far ultraviolet 远紫外区far ultraviolet laser 远紫外激光器far ultraviolet radiation 紫外线辐射far ultraviolet rays 远紫夕卜线farad 法faraday法拉第faraday cage法拉第笼faraday cell 法拉第盒faraday constant 法拉第常数faraday cup法拉第笼faraday dark space 法拉第暗区faraday effect 磁致旋光faraday rotation 磁致旋光faraday tube法拉第管faraday,s law法拉第定律farvitron线振质谱仪fast迅速的fast breeder reactor 快增殖堆fast fission快中子裂变fast fission effect快中子裂变效应fast fourier transform快速傅里叶变换fast neutron 快中子fast neutron reactor 快中子堆fast nova快新星fast reactor 快中子堆fatigue 疲劳fatigue limit疲劳极限fatigue strength 疲劳强度fcc structure面心立方结构feedback 反馈feedback amplifier 反馈放大器feedback circuit 反馈电路feedback control 反馈控制feedback factor 反馈系数feedback ratio 反馈比feeder馈电线femto 飞femtometer 费密femtosecond 飞秒femtosecond region 飞秒区域fermat,s principle 费马原理fermi费密fermi acceleration 费密加速fermi age费密年龄fermi dirac statistics 费密统计法fermi distribution 费密分布fermi energy 费密能fermi gas费密气体fermi glass费密玻璃fermi hole费密空穴fermi interaction 费密相互酌fermi level费密能级fermi liquid费密液体fermi particle 费密子fermi pasta ulam problem费密巴斯德乌拉姆问题fermi resonance 费密共振fermi selection rule 费密选择定则fermi statistics费密统计法fermi surface 费密面fermi temperature 费密温度fermi transition 费密跃迁fermi's golden rule费密黄金定律fermiology费密面学fermion费密子fermionic dark matter 费密子暗物质fermium 镄ferrielectricity 亚电性ferrimagnetic resonance 亚铁磁共振ferrimagnetism铁氧体磁性ferrite铁氧体ferrite magnetostrictive vibrator 铁氧体磁致伸缩振子ferro resonance 铁磁共振ferroelastic phase transition 铁弹性相变ferroelasticity 铁弹性ferroelectric 铁电的ferroelectric domain 铁电畴ferroelectric mode 铁电模ferroelectric phase transition 铁电相变ferroelectric semiconductor 铁电半导体ferroelectric substance 铁电性材料ferroelectricity 铁电性ferrofluid 铁磁铃ferromagnet 铁磁体ferromagnetic 铁磁的ferromagnetic dielectrics 铁磁电介质ferromagnetic fluid 铁磁铃ferromagnetic material 铁磁性材料ferromagnetic resonance 铁磁共振ferromagnetic substance 铁磁性材料ferromagnetic superconductor 铁磁超导体ferromagnetic thin film 铁磁薄膜ferromagnetism 铁磁性feynman diagram 费因曼图feynman path integral费因曼的路径积分feynman spectrum 费因曼谱ffag synchrotron固定场交变梯度回旋加速器fiber纤维fiber bundle 纤维丛fiber electrometer 悬丝静电计fiber laser纤维激光器fiber optics纤维光学fiber structure 纤维结构fibonacci semiconductor superlattice 菲博纳奇半导体超晶格fibril小纤维fibril structure 纤维结构fick,s law斐克定律fictitious spin quantum number 假想自旋量子数fictitious year 假年field场;体field adsorption 场吸附field current 励磁电流field density 场密度field desorption 场致退吸field distortion 场畸变field distribution 场的分布field effect transistor 场效应晶体管field electron emission 场致电子发射field emission 场致发射field emission microscope场致发射显微镜;自动电子显微镜field emitted electron 场致发射电子field equation 场方程field intensity 场强field ion microscope场致离子显微镜field lens 场镜field magnet 场磁铁field of forces 力场field of gravity 重力场field of view 视场field of vision 视场field operator 场算符field particle 场粒子field quantum 场量子field stop 场栏field strength 场强field structure 场结构field theory 场论fifth force第五种力fifth fundamental force 第五种基本力figure图形figure of merit 优值figure of noise 噪声指数file文件filled band 满带filled level满带能级filled shell 满壳层film软片film badge胶片剂量计film boiling膜态沸腾film dosimeter胶片剂量计film type condensation 膜状凝结filter滤器滤光器滤波器filtration 过滤final product最终产物final state interaction 终态相互酌final vacuum极限真空finder取景器finding telescope 寻星镜fine particle 微粒子fine structure 精细结构fine structure constant 精细结构常数fine structure splitting 精细结构劈裂finesse 锐度finite difference method 差分法finite element method 有限元法finite group 有限群finite universe 有限宇宙fireball 火球fireball model 火球模型first harmonics 基波first integral 初积分first law of thermodynamics 热力学第一定律first order phase transition 一级相转变first point of aries 春分点first quarter 上弦first resonance 一次共振first sound第一次声波fish finder鱼群探测器fissible可裂变的fissile可裂变的fissile nucleus可分裂的核fissility可分变性fission 分裂fission chain reaction 裂变链式反应fission chamber 裂变室fission counter 裂变计数器fission energy 裂变能量fission event裂变事件fission fragment 裂变碎片fission neutron 裂变中子fission yield裂变产额fissionable可裂变的fissionable nucleus 可裂变核 fissioning isomer 裂变同质异能素 fit适合five minute oscillations 五分钟振动 fixation 定影fixed capacitor固定电容器fixed point 定点fixed resistor固定电阻器fixed star 恒星fixing定影fixing solution 定影液fizeau fringe 菲佐条纹fizeau interferometer 菲佐干涉仪flame火焰flame photometer 火焰光度计flame photometry火焰光度法flame spectrum 火焰光谱flare太阳耀斑flare star 耀星flash闪光flash of light 闪光flash photolysis 闪烁光解flash spectrum 闪光光谱flat surface 平面flatness problem平坦性问题flattening 扁率flavor 味flexibility 挠性flexible polymer挠性聚合体flexural rigidity 弯曲刚度flexural strength 抗挠强度flexure 挠曲flexure vibration 弯曲振动flicker 闪烁flicker effect 闪烁效应flicker noise闪变噪声flicker photometer 闪烁光度计flight path飞越距离flight time飞越时间flint glass火石玻璃flip flop触发器flip flop circuit双稳态触发电路floating body 浮体floating point representation 浮点表示floating zone melting method 浮区熔炼法flocculation 凝聚flood and ebb 潮汐flooding 溢流floppy disk 软磁盘flow 流flow birefringence 怜双折射flow counter柳式计数管flow dichroism 怜二色性flow equation 怜方程flow parameter 怜参数flow pattern 镣flow proportional counter 怜正比计数器flow rate 量flow visualization 辽视化flowmeter 量计fluctuating force 涨落力fluctuation 起伏fluctuation dissipation theorem 涨落耗散定理fluctuon起伏量子fluent变数fluid 铃fluid dynamics 铃动力学fluid elasticity 水弹性fluid model 铃模型fluidal 铃的fluidic 铃的fluidity 怜性fluorescence 荧光fluorescence center 荧光中心fluorescence dosimeter 荧光剂量计fluorescence spectrophotometer 荧光分光光度计fluorescence spectrum 荧光光谱fluorescence yield 荧光产额fluorescent 萤光的fluorescent indicator tube 荧光指示管fluorescent lamp 荧光灯fluorescent material 萤光材料fluorescent radiation 特狰射fluorescent scattering 荧光散射fluorescent screen 荧光屏fluorescent x rays 荧光 x 射线fluorimeter 荧光计fluorine 氟fluorite structure 萤石型结构fluorography荧光照相法fluorometer 荧光计fluorometric analysis 荧光分析fluoroscope 荧光镜fluoroscopy荧光检查法fluorspar structure 萤石型结构flux通量flux creep磁通量蠕变flux density通量密度flux flow磁通量流flux jump磁通量跃变flux method 熔剂法flux motion 磁通量运动flux of energy 能通量flux of light 光通量flux of radiation 辐射通量flux pinning 通量锁住flux pump 通量泵flux quantization 磁通量量子化flux quantum磁通量子fluxmeter磁通计fluxoid磁通量子fluxon磁通量子fly苍蝇座flying spot electron microscope 扫描电子显微镜fm receiver档接受器focal distance 焦星巨focal length 焦星巨focal line 焦线focal plane 焦面focal point 焦点focal power 光焦度focal surface 焦曲面fock representation 福克表示fock space福克空间focometer焦距计focon聚焦锥focus焦点focused ion beam聚焦离子束focusing 倒focusing camera 倒照相机focusing coil聚焦线圈focusing cone 聚焦锥focusing lens 聚焦透镜focusing quadrupole magnet 聚焦四极磁铁focuson聚焦子foil 箔fokker planck equation 福克普朗克方程follow up control 随动控制foot pound second system 英尺磅秒单位制forbidden禁戒的forbidden band 禁带forbidden decay 禁戒衰变forbidden line 禁线forbidden lines in astrophysics 天体物理学中的禁线forbidden reflection 禁戒反射forbidden transition 禁戒跃迁forbiddenness 禁戒force 力force function 力函数force of attraction 弓|力force of gravity 重力force of inertia 惯性力force of repulsion 斥力force of rolling friction 滚动摩擦力force of sliding friction 滑动摩擦力force polygon力的多边形force triangle力的三角形forced circulation 强制循环forced convection 强制对流forced emission 强迫发射forced oscillations 受迫振荡forced vibration 受迫振荡forced vortex 强迫涡流fore vacuum 前级真空forecast 预报forecast of solar activity 太阳活动预告foreign atom 杂质原子forepump预备真空泵fork mounting 叉式装置form drag 型阻form factor形状因子formant共振峰formation of order 秩序形成formula 公式formulation 公式化fornax天炉座fortran程序语言forward scattering 前方散射foucault currents 涡电流foucault knife edge test 傅科刀口检验foucault's pendulum 傅科摆fountain effect 喷水效应four current 四维电流four dimensional space 四维空间four dimensional structure of the universe 宇宙四维结构four dimensionality 四维性four factor formula 四因子公式four force四维力four momentum 四维动量four potential 四维势four terminal network 四端网络four vector 四维矢four velocity四维速度four wave mixing 四波混合fourier component 谐波分量fourier integral傅里叶积分fourier number 傅里叶数fourier series傅里叶级数fourier spectroscopy 傅里叶光谱学fourier transform hologram傅里叶变换全息图fourier transform spectrometer 傅里叶光谱仪fourier transformation 傅里叶变换fourth sound第四次声波fractal 分形fractal dimension 分形维数fractional charge 分数电荷fractional crystallization 分级结晶fractional quantum hall effect 分数量子霍尔效应fracton分形子fracture 破裂fracture mechanics 断裂力学fragility 脆性frame antenna环形天线frame of reference 参考系francium 钫franck condon principle 富兰克康登原理franck hertz,s experiment 富兰克赫兹实验 frank read source弗朗克里德源franklin富兰克林fraunhofer diffraction 夫琅和费衍射fraunhofer hologram夫琅和费全息图fraunhofer line夫琅和费谱线fre量子free自由的free charge自由电荷free convection自由对流自然对流free electron自由电子free electron laser自由电子激光器free energy 自由能free energy of activation 激活的自由能free field自由场free free transition 自由自由跃迁free group自由群free gyroscope自由陀螺仪free motion自由运动free neutron自由中子free oscillation 自由振动free path自由程free pendulum 自由摆free rotation自由旋转free space自由空间free state自由态free surface 自由面free system 自由系free vibration 自由振动free volume自由体积free volume theory自由体积理论freedom 自由freezing 凝固freezing mixture 冷冻剂freezing point 凝固点frenkel defect夫伦克尔缺陷frenkel exciton 夫伦克尔激子frequency 频率frequency analysis 频率分析frequency band 频带frequency characteristic 频率特性frequency converter 变频器frequency converter tube 变频管frequency counter 频率计数器frequency divider 分频器frequency domain 频域frequency factor 频率因子frequency meter 频率计frequency modulation 档frequency multiplier倍频器频率倍增器frequency range 频率范围frequency response 频率响应frequency response method 频率特性法frequency shift 移频frequency spectrum 频谱frequency stability 频率稳定度frequency stabilized laser 稳频激光器frequency transfer function 频率传递函数fresnel diffraction 菲涅耳衍射fresnel half period zones 菲涅耳半周期带fresnel hologram菲涅耳全息图fresnel lens菲涅耳透镜fresnel prism 菲涅耳棱镜fresnel rhomb菲涅耳斜方系fresnel zone 菲涅耳带fresnel,s biprism菲涅耳双棱镜fresnel's dragging coefficient 菲涅耳曳引系数fresnel,s zone plate 菲涅耳波带片friction 摩擦friction coefficient 摩擦系数friction cone 摩擦锥friction layer 摩擦层friction loss摩擦损失friction of fluid lubrication 液体润滑摩擦frictional drag 摩擦阻力frictional electricity 摩擦电frictional force 摩擦力frictional oscillation 摩擦振动frictional resistance 摩擦阻力 friedel sum rule弗里德尔的求和定则 friedmann equation 弗里德曼方程friedmann universe弗里德曼宇宙frigorimeter 深冷温度计fringes with white light 白光干涉条纹froude number 弗劳德数frozen in magnetic field 冻结磁场frustrated total internal reflection 衰减全内反射frustration 抑止ft value ft 值fuel assembly燃料组件fuel cell燃料电池fuel cycle燃料循环fuel regeneration 燃料再生fuel reprocessing 燃料再生fuel rod燃料元件棒fugacity挥发性fulcrum 支点full load 满载full moon 望月full wave rectification 全波整流full width at half maximum 半宽度fullerene球壳状碳分子function 函数functional 泛函functional analysis 泛函分析functional ceramics 机能陶瓷functional derivative 泛函微分fundamental absorption 基本吸收fundamental catalog 基本星表fundamental constants 基本常数fundamental doublet 基本双重线fundamental frequency 基频率fundamental interaction 基本相互酌fundamental law 基本定律fundamental magnitude 基本量fundamental mode 关Bfundamental particle 基础粒子fundamental research 基础研究fundamental series 伯格曼系fundamental star 基本星fundamental theorem 基本定理fundamental tone 基音fundamental unit 基本单位furnace 炉furry,s theorem 弗里定理fuse熔断器保险丝fused quartz 熔融石英fusible alloy易熔合金fusing point 熔点fusion熔化fusion fission hybrid reactor核聚变裂变混合反应堆fusion point 熔点fusion reaction 聚变反应fusion reactor 热核堆fusion temperature 聚变温度。
地球地表形态知识点
地球地表形态知识点英文回答:Geomorphic features refer to the various landforms and surface features found on the Earth's surface. These features are the result of various geological processes such as erosion, weathering, tectonic activity, and deposition. They can be classified into several categories based on their formation processes and characteristics.One common type of geomorphic feature is mountains. Mountains are elevated landforms that are typically characterized by steep slopes and high elevations. They are usually formed through tectonic activity, such as the collision of tectonic plates or volcanic activity. The Himalayas in Asia and the Rocky Mountains in North America are examples of mountain ranges.Another type of geomorphic feature is valleys. Valleys are low-lying areas between mountains or hills, often witha river or stream running through them. They are formed through erosion caused by the flow of water or the movement of glaciers. The Grand Canyon in the United States is a famous example of a valley formed by the Colorado River.Plains are another important geomorphic feature. Plains are flat or gently sloping areas that are usually formed by the deposition of sediment over time. They can be found in various sizes, from small coastal plains to vast grasslands. The Great Plains in the United States and the Pampas in South America are examples of plains.Rivers and lakes are also significant geomorphic features. Rivers are natural watercourses that flow from higher elevations to lower elevations, carving out valleys and creating diverse landscapes. Lakes, on the other hand, are bodies of water that are often formed by the filling of depressions or by the damming of rivers. The Nile River in Africa and the Great Lakes in North America are examples of prominent river and lake systems.Coastlines are another important type of geomorphicfeature. They are the meeting point of land and sea, constantly shaped by the action of waves, tides, and currents. Coastal features include beaches, cliffs, and estuaries. The Great Barrier Reef in Australia and the California coastline in the United States are examples of diverse and dynamic coastlines.In conclusion, geomorphic features are the result of various geological processes and can be classified into categories such as mountains, valleys, plains, rivers and lakes, and coastlines. These features play a crucial role in shaping the Earth's surface and creating diverse landscapes.中文回答:地表形态是指地球表面上各种地貌和地表特征。
斜面的科学知识
斜面的科学知识Slanted surfaces are common in our daily lives, whether in the form of ramps, hills, or even roofs. These inclined planes play a crucial role in various aspects of science, from physics to engineering, each with its own unique characteristics. For instance, in physics, the study of inclined planes is essential for understanding concepts such as gravity, friction, and mechanical advantage.倾斜表面在我们的日常生活中很常见,无论是在坡道、山坡,甚至是屋顶的形式。
这些倾斜面在各种科学领域中起着至关重要的作用,从物理学到工程学,每个领域都具有独特的特点。
例如,在物理学中,倾斜面的研究对于理解重力、摩擦和机械优势等概念至关重要。
One of the fundamental principles that govern inclined planes is the concept of gravitational force. When an object is placed on a slanted surface, the force of gravity acts perpendicular to the surface, pulling the object downward. The component of gravity parallel to the surface determines the object's tendency to slide down the incline. This relationship between gravity and the angle of incline is crucialfor calculating the acceleration and velocity of objects on inclined planes.支配倾斜面的基本原则之一是重力的概念。
地表沉降研究方法英语作文
地表沉降研究方法英语作文Title: Research Methods for Land Subsidence。
Land subsidence, the gradual sinking of the Earth's surface, is a complex phenomenon with multifaceted causes and impacts. Understanding and mitigating land subsidence require comprehensive research methodologies. In this essay, we delve into various research methods employed to study land subsidence.1. Geodetic Surveys: Geodetic surveys involve precise measurements of the Earth's surface using techniques suchas GPS (Global Positioning System), GNSS (Global Navigation Satellite System), and leveling. These surveys provide valuable data on ground deformation over time, aiding inthe identification and monitoring of subsidence-prone areas.2. Interferometric Synthetic Aperture Radar (InSAR): InSAR is a remote sensing technique that utilizessatellite-based radar to detect ground movements withmillimeter-scale accuracy. By analyzing interferograms generated from multiple radar images, researchers can map land subsidence over large areas and monitor its spatial and temporal evolution.3. Groundwater Monitoring: Land subsidence oftenresults from excessive groundwater extraction, causing aquifer compaction and subsequent surface sinking. Groundwater monitoring involves measuring water levels in wells and aquifers to assess groundwater depletion rates and its correlation with subsidence.4. Geotechnical Investigations: Geotechnical investigations focus on understanding the subsurface soil properties and geological conditions that contribute to land subsidence. Techniques such as borehole drilling, soil sampling, and geophysical surveys help characterize the subsurface and identify potential triggers of subsidence, such as clay layer compression or underground mining activities.5. Numerical Modeling: Numerical modeling plays acrucial role in simulating and predicting land subsidence phenomena. Finite element method (FEM) and finitedifference method (FDM) are commonly used numerical techniques to simulate groundwater flow, soil deformation, and surface subsidence processes. These models integrate geospatial data, hydrogeological parameters, and mechanical properties to simulate the complex interactions driving land subsidence.6. Remote Sensing and Geographic Information Systems (GIS): Remote sensing data, including optical imagery, thermal infrared, and LiDAR (Light Detection and Ranging), provide valuable information for land subsidence analysis. GIS platforms facilitate spatial data management, visualization, and spatial analysis, enabling researchers to integrate multi-source data for comprehensive subsidence assessment.7. Satellite Altimetry: Satellite altimetry measures variations in sea surface height, which indirectly reflect changes in land elevation due to subsidence. By analyzing long-term satellite altimetry data, researchers canestimate regional land subsidence rates in coastal areas and low-lying regions affected by sea-level rise and groundwater extraction.8. Collaborative Monitoring Networks: Collaborative monitoring networks involve partnerships between government agencies, research institutions, and local communities to establish comprehensive subsidence monitoring programs. These networks leverage resources, expertise, and data-sharing mechanisms to enhance subsidence research, raise public awareness, and support informed decision-making for sustainable land use planning.In conclusion, the study of land subsidence requires a multidisciplinary approach encompassing geodesy, remote sensing, hydrogeology, geotechnical engineering, and numerical modeling. By employing an array of research methods, scientists can gain insights into the causes, mechanisms, and impacts of land subsidence, ultimately contributing to effective mitigation strategies and sustainable land management practices.。
水位变化和降雨条件下的边坡稳定性分析---硕士论文
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大连理工大学硕士学位论文
Slope Stability Analysis of Unsaturated Seepage by
Abstract
Slope stability problem is a hot spot in the field of geotechnical engineering research, the natural slope and artificial slope exist extensively. In the highway subgrade and bank dike engineering, it becomes a difficult problem to determine safety coefficientexpressly whenconsidering the water level change and the complex factors such as rainfall. This paper uses the finite element limit equilibrium method proposed by professor Shao in analysis of the seepage slope stability considering fluid-solid interaction. As a kind of deterministic stability analysis methods based on limit equilibrium conditions, it gets the stress field through the numerical method (finite element and discrete element or boundary element, etc.) firstly, and then according to the definitions of safety factor, we can search the most dangerous slip surface using the mathematical programming method. The physical meaning of safety factor definition is clear in the method, it combines the advantages of the limit equilibrium method and finite element method (FEM), as long as the stress field is obtained, it can be convenient and quick to find out the safety coefficient, the method is very suitable for engineering calculation and its advantages are more obvious in the stability analysis under complicated conditions.
汉英地质学名词
汉英地质学名词(1993)面角守恒定律||law of constancy of angle面金属量||areal productivity面状构造||planar structure庙坡组||Miaopo Formation妙高阶||Miaogaoan Stage妙高期||Miaogaoan Age妙高组||Miaogao Formation敏感系数||sensitivity ratio敏感粘土||sensitive clay明矾石||alunite明化镇组||Minghuazhen Formation明水组||Mingshui Formation模||mold模拟实验||simulation experiment模式年龄||model age磨拉石||molasse磨蚀[作用]||abrasion莫尔包络线||Mohr failure envelope莫尔图||Mohr diagram莫尔应力圆||Mohr stress circle莫来石||mullite莫氏硬度||Moh's hardness莫斯科阶||Moscovian Stage莫斯科期||Moscovian Age墨西拿阶||Messinian Stage墨西拿期||Messinian Age木栓质体||suberinite穆斯堡尔谱||Moessbauer spectrum穆斯堡尔效应||Moessbauer effect钠长石-绿帘石-角岩相||albite-epidote-hornfels facies钠长石||albite钠交代型铀矿||sodic-metasomatism type uranium deposit钠闪石||riebeckite钠铁闪石||arfvedsonite; 又称“亚铁钠闪石”。
钠硝石||soda niter, nitronatrite, nitratine; 又称“智利硝石”。
钠硝石矿床||soda niter deposit, nitratine deposit; 又称“智利硝石矿床”。
地球地质演化分层
地球地质演化分层英文回答:The geological evolution of the Earth can be divided into multiple layers, from the outer to the inner:1. The surface layer: This is the most visible layer of the Earth's surface, including land and oceans. It is directly influenced by the atmosphere, water, biology, and human activities, serving as the foundation for the Earth's ecosystem and human civilization.2. The lithosphere: Located below the surface layer, it includes the crust and the top part of the upper mantle. The crust is the hard outer shell composed of various rocks, while the upper mantle is the asthenosphere beneath the crust. Together, they constitute the lithosphere of the Earth. The lithosphere is the birthplace of tectonic movements, earthquakes, volcanic activities, and other surface phenomena.3. The asthenosphere: Located beneath the lithosphere, it is part of the upper mantle. The asthenosphere consists of high-temperature, low-viscosity rocks that can flow and deform, serving as the main channel for heat transfer within the Earth.4. The lower mantle: Lying below the asthenosphere, it is the thickest layer inside the Earth. It is primarily composed of solid rocks, but the temperature and pressure are extremely high, resulting in rocks with high viscosity and plasticity.5. The outer core: Situated beneath the lower mantle, it consists of metals such as iron and nickel. The presence of the outer core gives the Earth its powerful magnetic field, and its flow generates changes in the Earth's magnetic field.6. The inner core: Located at the very center of the Earth, it is composed of solid iron and nickel. The temperature inside the inner core is extremely high, reachingapproximately 5,700 degrees Celsius, but due to the immense pressure, it remains solid.中文回答:地球的地质演化可以分为多个层次,从外到内依次是:1. 地表层:这是地球表面最直观的一层,包括陆地和海洋。
托福TPO真题高频词汇分享版
establishme nt
n.建立,
确立
appare nt
adj.明显
的,表面上
的
replace
vt.代替,
取代
scarcity
n.缺乏;不
足;稀少
profitable
a.有利可
图的
cou ncil
deliver
vt.投递
交;发表
n.委员会,
理事会
previously
adv.先前,
在此之前
含,列入
reveal
vt.揭露,泄
露
impact
n./v.影响,
作用
lava
n.熔岩
exte nsive
a.广大的,广
阔的
cha nnel
n.频道;[常
pl.]渠道
crater
n.火山口
disti nctive
a.有区别 的;有特色 的
eno rmous
a.巨大的
molte n
v.(使)融
化;(使)消
tran siti on
n.过渡,
转变
desolate
a.荒芜的
ashore
ad.在岸
in hospitable
adj.待客不
上,上岸
亲切的,冷淡
的
predator
n.食肉动 物
diversify
v.(使)不同
obstacle
n.障碍
(物),妨碍
buoyancy
n.浮力,弹 性,心情愉快
terrestrial
散
equator
n.赤道
shield
vt.保护,
地貌学英文词典
地貌学英文词典Geomorphology DictionaryThe study of the Earth's surface and its landforms is known as geomorphology. This field of science encompasses the examination of the physical features and processes that shape the planet's landscape. From towering mountains to meandering rivers, the diverse array of landforms found on Earth are the result of a complex interplay between various geological, climatic, and biological factors. To effectively communicate and understand this intricate field, the development of a comprehensive geomorphology dictionary is essential.The geomorphology dictionary serves as a valuable tool for researchers, students, and enthusiasts alike, providing a standardized vocabulary to describe the myriad of landforms and associated processes. This dictionary not only aids in the accurate identification and classification of different landforms but also facilitates the exchange of knowledge and ideas within the scientific community.One of the fundamental components of the geomorphology dictionary is the classification and definition of various landforms.This includes features such as mountains, valleys, plateaus, plains, and coastal landforms, each with their own unique characteristics and formation processes. For instance, a mountain is defined as a large, natural elevation of the earth's surface rising abruptly from the surrounding level. Mountains can be formed through a variety of processes, including tectonic plate movements, volcanic activity, and erosion.Similarly, a valley is a low area of land between hills or mountains, typically with a river or stream flowing through it. Valleys can be formed through the erosive action of water, glaciers, or tectonic forces. The geomorphology dictionary also includes terms to describe the different types of valleys, such as U-shaped valleys, V-shaped valleys, and rift valleys, each with its own distinctive features and formation mechanisms.In addition to the classification of landforms, the geomorphology dictionary also encompasses the various processes that shape the Earth's surface. This includes weathering, erosion, deposition, and tectonic activity, among others. Weathering, for example, is the physical and chemical breakdown of rocks and minerals due to exposure to the elements, such as wind, water, and temperature changes. Erosion, on the other hand, is the process by which these weathered materials are transported and removed from their original location, often by the action of water, wind, or ice.The geomorphology dictionary also includes terms related to the specific features and characteristics of different landscapes, such as the formation of glaciers, the dynamics of rivers and streams, and the evolution of coastal environments. For instance, the term "moraine" refers to the accumulation of rock debris carried and deposited by a glacier, while "meander" describes the sinuous, looping pattern of a river as it flows across a relatively flat landscape.Moreover, the geomorphology dictionary extends beyond the physical features of the Earth's surface, delving into the interactions between the biosphere, hydrosphere, and atmosphere, and how these interconnected systems influence the development and transformation of landforms. For example, the term "pedogenesis" refers to the formation of soil, a critical component in the support of terrestrial ecosystems and the shaping of landscapes.The comprehensive nature of the geomorphology dictionary also includes the specialized terminology used in the study of geological time and the processes that have shaped the Earth over vast stretches of history. This includes terms such as "Pleistocene," "Holocene," and "Quaternary," which refer to specific geological epochs and the associated changes in climate, sea levels, and the distribution of landforms.In conclusion, the geomorphology dictionary is an indispensable tool for the study and understanding of the Earth's surface and its dynamic processes. By providing a standardized vocabulary and clear definitions, this dictionary facilitates effective communication and collaboration among geomorphologists, geologists, and other Earth scientists. As our knowledge of the Earth's landforms and their formation continues to evolve, the geomorphology dictionary will remain a crucial resource for advancing our understanding of the complex and ever-changing face of our planet.。
地质学专业术语翻译
凹坑pool,chute 白垩chalk白云化灰岩dolomitized limestone白云母muscovite白云石dolomite白云岩dolostone, dolomitite斑点构造mottled structure斑礁patch reef斑晶porphyrotope斑脱岩bentonite搬运作用transportation板状晶体laths半深海helmipelagic半自形晶subhedral棒形蛀木虫迹teredolites clavatus包卷层理convolute lamination包卷构造comvolute structure堡礁(障壁礁) barrier reef抱球虫软泥globigerina ooze比拟试验模式scaled experimental model碧玉jasper边滩point bar辫状河braided channel标志层key bed标准偏差standard deviation表面结构surface texture表皮鲕superficial Oolits表栖动物epifauna表生成岩作用epidiagenesis表生作用epigenesis表土regolith滨湖亚相lake-shore滨面shoreface滨线shoreline冰雹痕hail impression冰川glacier冰-海沉积物glacier-marine sediment 1/21冰川相glacial facies冰碛物till冰碛岩tillite冰水沉积outwash波长wave length波高wave height波痕ripple波状层理wavy bedding剥离线理parting lineation不等粒inequigranular不整合unconformity槽痕flute槽模flute casts侧向沉积作用lateral sedimentation侧向加积lateral accretion测井沉积学well-logging sedimentology 测井相electrofacies层bed层间流interflow层孔虫stromatoporoid层理stratification,bedding,lamination 层流laminar flow层内溶解作用intrastratal solution层系set层系组coset层序地层学sequence stratigraphy次长石净砂岩subarkose次生孔隙secondary porosity次岩屑净砂岩sublitharenite长石feldspar长石砂岩feldspar sandstone长石净砂岩arkose长石净砂岩类arkosic arenite长石杂砂岩feldspathic greywacke长石杂砂岩类arkosic greywacke潮道tidal channel潮间带intertidal潮控三角洲tidal-dominated delta2/21潮坪tidal flat潮上带supratidal潮汐层理tidal- bedding潮汐流ebb current潮汐三角洲tidal delta潮下带subtidal zone沉积分异作用sedimentary differentiation沉积构造sedimentary structure沉积后作用postdeposition沉积环境depositional environment沉积模式sedimentary model沉积盆地sedimentary basin沉积铁矿sedimentary iron ores沉积物sediment沉积物重力流sediment gravity flow沉积相sedimentary(depositional)facies 沉积学sedimentology沉积岩sedimentary rocks沉积岩石学sedimentary petrology沉积作用sedimentation,deposition成分成熟度compositional matuarity成岩作用diagenesis赤铁矿hematite冲积平原alluvial plain冲积扇alluvial fan冲裂avulsion冲流swash冲流回流带zone of swash and backwash冲刷痕scour mark冲洗交错层理swash bedding 冲溢扇washover fan储层reservoir储油窗oil–windows床沙bed床沙形体bed form床沙载荷bed load吹程fetch垂向沉积作用vertical accretion 3/21丛藻迹chondrites粗砾cobble粗枝藻门dasyclads大潮spring tide大陆架continental shelf大陆隆continental rise大陆坡continental slope大洋盆地basin带穴迹taenidium带状迹teanidium袋状钻孔迹rogerella单杯迹monocraterion单成份砾岩oligomictic conglomerate 岛(弧)-海(沟)体系arc-trench system 岛弧island arc等深流contour current等深积岩contourite等趾迹isopodichnus等足迹isopodichnus低镁方解石low-magnesian calcite低弯度河道low-sinuosity channel低位体系域low-stand systems tract 堤岸bank底痕sole mark底积层bottomset底模solecast底栖生物benthos底载河道bedload channel地层strata地层倾斜录井dipmeter log地层水formation water地球化学geochemistry地球物理geophysics地震地层学seismic stratigraphy地震勘探seismic exploration递变层graded layer递变悬浮作用graded suspension 4/21典型浊积岩clastic turbidite电测井electric log叠层石stromatolite叠瓦状排列imbricate arrangement 顶积层topsets动态模式dynamic model动藻迹zoophycus豆粒pisolite段member对称波痕symmetrical ripple鲕粒oolite二叶石迹cruziana反递变层理reverse grading反沙丘层理antidune bedding反向递变的inversely graded泛滥盆地flood basin泛滥平原flood plain方沸石Analcime方解石calcite放射虫Radiolarians放射性测井radioactivity log非补偿(饥饿)沉积starved basin 非显晶质的aphanitic沸石zeolite分流河道distributary channel分流河口砂坝distributary-mouth bar 分流间湾interdistributary分选系数So分选作用sorting粉砂silt粉砂岩siltite,siltstone粉砂页岩silt shale球粒pellet风暴大潮storm surge风成eolian风成波痕eolian ripple,wind ripple风成交错层理aeolian cross bedding 风成岩eolianite5/21风化作用weathering风生流wind-drift current风蚀deflation峰度curtosis缝合线stylolite弗劳德数Froude number浮游生物plankton腐泥sapropel负载(荷)构造load structure复成分砾岩polymictic conglomerate 复理石flysch钙结层caliche干酪根kerogen干盐湖playa高岭石kaolinite高弯度河道high-sinuosity channel 高位体系域high-stand systems tract根珊瑚迹rhizocoralliun耕作迹agrichnia沟模groove casts沟蠕形迹taphrhelminthopsis古拉迹paleohelcura古生态学paleoecology古生物paleontological古水流标志paleocurrent indicator古土壤paleosols古网迹palaeodictyon古斜坡paleoslope骨架岩framestone固着底栖生物sessile benthos光合作用photosynthesis硅镁层sima硅土,二氧化硅silica硅质silic-硅质碎屑siliciclastic国际沉积学家学会IAS(International Association of Sedimentologists) 文档来自于网络搜索海(湖)泛面flooding surface6/21海(湖)滩beach海岸带coastal zone海底扇submarine fan海底峡谷submarine canyon海沟trench海进体系域transgressive systems tract 海浪sea wave海绿石glauconite海平面变化sea-level changes海平面升降eustasy海侵transgression海侵层序transgressive sequence海生迹thalassinoides海滩marine beach海滩脊ridge of a beach海相三角洲marine delta海洋ocean旱谷arroyo, wadi河床(道)channel河床滞留lag河底滞留沉积channel floor lag河控三角洲fluvial delta河口湾estuary河流相fluvial河漫overbank核形石oncilite褐铁矿limonite黑色页岩black shale黑云母biotite红藻植物门rhodophyta后滨backshore后成作用katagenesis,anadiagenesis 弧间盆地interarc basin弧内盆地intra-arc basin弧前盆地forearc basin湖lake湖泊环境lacustrine environment湖泊相lacustrine7/21湖面波动seiche湖沼学limnology滑[动]痕slide mark滑塌构造slump structure滑塌岩slumps还原硫酸盐细菌desulfouibrio,desulfomaculmi 还原作用reduction环境沉积学environmental sedimentology环线迹spirorhaphe黄铁矿pyrite黄土loess灰泥micrite灰泥岩mudstone灰质白云岩calcareous dolostone回流backflow,backwash混杂沉积岩diamicton混杂堆积物mélange混载荷流mixed-load channel火山弹bomb火山灰ash火山灰流ash flow火山角砾岩volcanic breccia火山块block火山泥石流lahar火山碎屑pyroclastic debris,tephra火山碎屑流pyroclastic flow火山碎屑岩pyroclastic rock火焰构造flame structure鸡笼状的chickenwire集合粒aggregate集块岩agglomerate加积accretion加积作用aggradation假亮晶pseudospar尖峰度的jeptokurtic剪切shearing交错层cross beds交错层理cross bedding; cross stratification 8/21交错纹crossed-lamellar交错纹层cross laminae胶结物cement胶结作用cementation胶磷矿collophane礁reef礁核reef core礁后相backreef facies礁麓堆积reeftalus礁前相forereef facies礁相reef facies角度不整合angular unconformity 角砾岩breccias节藻迹phycodes结晶碳酸盐岩crystalline carbonate 界面bounding surfaces金藻门chrysophyta津(波)浪tsunami近滨nearshore进潮口tidal inlet进积作用progradation进食构造feeding structures进食迹fodinichnia晶面crystal face晶体crystal井形穴shafts净砂岩arenite静态模式static model居住构造dwelling structure居住迹domichnia居住潜穴dwelling burrows巨画迹megagrapton巨砾boulder决口扇crevasse,crevasse splay均匀悬浮uniform suspension颗粒grain,particle颗粒流grain flow颗粒岩grainstone9/21颗粒支撑的particle -supported,grain-supported 可劈性fissility可容空间accommodation space克拉通craton孔隙(度)pore,porosity块状层理massive bedding块状砂岩massive sandstone浪成波痕wave-generated ripple浪成沙纹层理wave- ripple bedding浪基面wave base浪控三角洲wave-dominated delta雷诺数Reynolds number-Re类沙蚕迹nereites累积频率曲线cumulative-frequency curve 离岸(裂)流rip current犁沟迹aulichnites丽线迹cosmorhaphe砾gravel砾漠reg砾屑灰岩calcirudite砾屑岩rudite砾岩conglomerate粒度grain size粒度概率图probability plot粒度中值Md粒间孔隙度intergranular porosity粒屑灰岩grainstone粒序层理graded bedding亮晶sparite亮晶方解石sparry calcite亮晶灰岩sparite亮煤clarain裂隙fracture临滨shoreface磷灰岩phosphorite磷酸盐岩phosphate rock菱铁矿siderite流动体制flow regimes10/21流痕rill impression流态flow regime流体化作用fluidization硫酸盐sulphate漏斗形funnel shape陆表海epicontinental sea陆架边缘体系域shelf margin systems tract 陆相terrestrial陆缘海marginal sea陆源碎屑岩terrigenous clastic rocks陆表海epeiric sea绿泥岩chlorite绿藻门chlorophyta,卵石质砂岩pebbly sandstone螺管迹gyrolithes洛伦茨迹corenzinia脉状层理flaser bedding漫流sheet flow漫游迹planoliies煤coal煤化作用coalification锰质岩manganess rock觅食迹pascichnia觅食拖迹grazing trails密度底流density underflow密度流density current密度跃层pycnocline磨拉石molasses母岩source rock, parent rock母岩区provenance,source area 内成岩endogenetic内栖动物infauna内碎屑intraclast钠长石albite钠长石化albitization能量带energy belt泥mud泥板岩argillite11/21泥晶micrite泥晶套micrite envelope泥粒灰岩(泥质颗粒岩)packstone 泥裂mud crack泥流mud flow泥石流debris flow泥质岩mudrock泥页岩argillutite泥支撑的mud supported泥质的argil拟蠕形迹helminthopsis逆行沙波regressive sand wave逆行沙丘antidune年代地层单位chronostratigraphic unit鸟眼构造birds-eyes structure鸟足状三角洲bird-foot delta凝灰岩tuff凝聚颗粒aggregate grains凝块灰岩thrombolite牛顿流体Newtonian fluid牛轭湖ox-bow lake爬迹repichnia爬升沙纹层理climbing ripple bedding 爬行crawling拍岸浪surf盘旋虫科spirillinidae螃蟹迹psilonichnus跑动running泡沫痕foam impression盆内岩intrabasinal rock盆外岩石extrabasinal rock片流sheetwash偏度Sk1,skewness漂砾erratic平均粒径Mz平均值mean平行层理parallel bedding平直河straight channel12/21破浪breaker破浪带breaker zone葡萄石grapestones气候带climate belts牵引[作用] traction牵引流tractive current牵引毯状沉积traction carpet前滨foreshore前积层foresets前三角洲沉积prodelta deposit浅海区neritic province浅滩shoal墙形迹teichichus丘状交错层理hummocky cross bedding 球度sphericity球粒pellet,pellet peloids球状粒peloid曲带迹curuolithus曲流meander曲流裁直neck cutoff曲流河meandering river取心钻井core drilling全球海平面变化eustatic change of sea level 缺氧事件anoxic event群group群体生物colony(organisms)热云nuee ardente热云岩ignimbrite溶解载荷solutional load熔结凝灰岩ignimbrite蠕形迹helminthoida软流圈asthenosphere软泥ooze弱光带disphotic zone萨布哈(盐沼)sabkha三角洲delta三角洲平原delta plain三角洲前缘delta front13/21三联点triple junction扫毛虫sabellarians沙坝bar沙波sand wave沙流sand flow沙漠desert沙漠相desert facies沙丘dune沙蜀迹arenicolites沙体Sand body沙纹ripples沙嘴spit砂sand砂火山sand volcanoes砂流sand flow砂屑detritus砂屑灰岩calcarenite砂岩sandstone砂枕构造pillow structure 筛状沉积sieve deposition山鹿冲积平原bajada山麓piedmont珊瑚coral扇砾岩fanglomerate扇三角洲fan delta扇状三角洲fan-like delta 舌菌迹glossiofunhites蛇形迹ophiomorpha深海pelagic, deep sea深海带abyssal zone深海沟deep-sea trench/2114深海平原abyssal深海扇deep-sea fan深泓线thalweg深水bathymetric深水盆地bathymetric basin 渗透率permeability生长构造growth structure 生物层biostrome生物带biozone生物地层学biostratigraphy生物灰岩biolithite生物礁reef生物颗粒bioclast生物亮晶灰岩biosparite生物内碎屑bioclastic生物泥晶灰岩biomicrite生物丘bioherm生物扰动作用bioturbation生物遗迹化石trace fossil石膏gypsum石化作用lithification石灰岩limestone石漠hamada石英quarts石英砂岩quartz sandstone,silicarenita 石英净砂岩quartzarenite石英杂砂岩quartzwack石针迹skolithos石枝藻litho-thammium始成岩作用eodiagenesis示顶底标志geopetal criterion事实模式actual model数学模式mathematical model刷模brush casts双杯迹diplocraterion双形迹dimorphichus双趾迹diplichifes水道channel15/21水流current,aqueous flow水流痕current mark水流上涌upwelling水流线理current lineation水平层理horizontal bedding水体分层stratification of the water column 水下泥石流subaqueous debis flow水下岩崩subaqueous rockfall水悬浮作用aqueous suspension斯科阳迹scoyenia似海生迹thalassinoides似海星迹asteriacites似蠕形迹helminthopsis似藻迹phycodes碎屑颗粒detrital particle燧石flint,chert他生沉积物allochthonous sediments它形晶anhedral塌积角砾岩collapse braccia塔斯曼迹tasmanadia台地platform苔藓虫fenestrate bryozoans滩bank滩脊beach ridge碳酸盐carbonate碳酸盐岩carbonate rock, carbonatite碳酸盐岩补偿深度carbonate compensation depth 碳酸盐岩隆(建隆)carbonate buildup逃逸构造escape structure逃逸迹fugichnia体系域systems tract天然堤levee,natural levee填集作用packing跳模bounce casts跳跃作用saltation铁岩ironstone铁质岩ferruginous rock停息迹cubchnia16/21同沉积滑塌构造syndepositinal slump structure 同生白云岩syngenetic dolostone同生作用syngenesis透光带photic zone透镜状层理lenticular bedding湍流turbulent flow团块lumps退覆层序offlap sequence洼状交错层理swaley cross bedding外成岩exogenetic rock外来岩块exotic block外生沉积物exogentic sediments弯曲锚形迹ancorichnus coronus晚成岩作用telodiagenesis网状(交织)河流anastomosing stream,anastomosed river 微亮晶microspar微斜长石microcline胃形钻孔迹gastrochaenolites温跃层thermoclime纹层laminae,lamination纹层状的laminated纹理lamination纹泥,季节泥varve雯石(霰石)aragonite紊流turbulent flow无光带aphotic zone无粘结性颗粒cohesionless particle物源区provenance矽藻diatom细砾granule线管迹tigllites相facies相变facies change相标志facies mark相对海平面relative sea-level相序facies sequence(succession)向上变粗coarsening-upward向上变浅shoaling-upward,shallowing--upward 17/21小潮neap tide小间断diastem斜坡地形clinoform泄水构造water-escape structure泻湖lagoon新生变形作用neomorphism新月形沙丘barchan dune信风trade winds星瓣迹asterosoma休息迹resting traces悬浮(移)负载suspended load选择交代作用selective replacement压扁层理flaser bedding压刻痕toll mark压溶作用pressure solution压实作用compaction盐水楔saltwater wedge岩石地层单位lithostratigraphic unit岩石地层学lithostratigraphy岩石圈lithosphere岩石学petrology岩相lithofacies岩相古地理lithofacies paleogeography岩屑rock fragment,lithic岩屑砂岩lithic sandstone,rock fragment sandstone 岩屑净砂岩litharenite岩屑杂砂岩lithic greywacke岩屑质长石净砂岩lithic arkose岩性lithological沿岸流longshore current沿岸沙坝longshore bar盐度salinity盐湖salt lakes盐碱滩salina氧化作用oxidation页岩shale液化liguefaction液化沉积物流fluidized sediment flow18/21液化作用liquefaction伊利石illite遗迹化石ichnofossil,trace fossil遗迹相ichofacies异化颗粒allochem粘结灰岩bindstones硬砂岩greywacke硬石膏anhydrite涌浪swells尤尔斯特龙图解Hiulstrom diagram油气储层地质建模reservoir geological Modeling 油页岩oil shale游泳生物nekton organisms原生孔隙primary porosity有效孔隙度effective porosity羽状交错层理herringbone cross bedding雨痕rain impression原始古网迹protopalaeodictyon圆度roudness越岸沉积overbank deposit运动迹moving traces韵律层理rhythmic bedding杂基matrix杂基支撑matrix supported杂砂岩graywacke,wacke载荷load再作用面(复活面)reactivation surface 藻管迹phycosiphon藻类algae藻团块algae lumps藻团粒algal poliods藻席Algal mats造礁珊瑚hermatypic coral粘度viscosity粘结岩boundstone粘土级clay size粘土矿物clay mineral粘土岩claystone19/21涨潮流flood current帐篷构造tepees障壁barrier障壁岛barrier island障壁沙咀barrier spit障积岩bufflestone沼泽相swamp振荡波痕oscillation ripples 蒸发岩evaporites正常鲕normal Oolits正递变的normally graded正化颗粒orthochems正态分布normal distribution 直观模式visual model指状沙坝bar-finger sand指状钻孔迹trypanites中成岩作用mesodiagenesis 中峰度的mesokertic中砾pebble中值median钟形bell shape众数mode重晶石barite重流层heavy-fluid layer皱饰迹rusophycus蛀木虫迹teredolites铸模mold铸模孔隙moldic porosity铸型cast锥模prod casts坠积物colluvium准层序parasequence准层序组parasequence set浊积石灰岩allodapic limestone浊积岩turbidite浊流turbidity current自生沉积物autochthonous sediments 自生的authigentic20/21自形晶euhedral自悬浮autosuspension组formation组构fabric钻孔迹trypanites21/21。
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2 of the lens. In view of axial symmetry of the lens, the curvatures of both principal cross-sections turn zero at these points, so the vertices are the points of flattening of the FS. The lens could be a part of a multiply connected FS. For example, electron lenses are included in the FSs of cadmium and zinc, and there are grounds to believe that they are flattened. As usual, we assume the magnetic field to be directed along the z axis, so, the flattening points at the vertices of the lens belong to an effective cross section. We consider a longitudinal ultrasound wave travelling along the y axis with frequency ω and wave vector q = (0, q, 0). An expression for the wave vector of a sound wave can be written down as follows: q = ω/s + ∆q. (3) Another term ∆q2 originates from the quantization of the orbital motion of electrons in strong magnetic fields, and describes quantum oscillations in the velocity shift. Assuming that the cyclotron quantum h ¯ Ω is small compared to the chemical potential of electrons ζ (γ −1 = (¯ hΩ/ζ )1/2 << 1), we obtain: 1 N2 ∆q2 =− n(−q )n(q )∆ q 2 ρm s2 g (7)
2 p2 y + l − 1) 2 2 ∂vx × (vy + vx + vz ) ∂px m1
2 p2 y + pz p2 1
l− 1
(2)
.
For l > 1, the Gaussian curvature K (px , py , pz ) turns zero at the points (±p2 , 0, 0) coinciding with the vertices
PACS numbers: 62.20.Dc
Oscillations in observables arising due to quantization of conduction electrons motion in strong magnetic fields are well known. They were repeatedly observed in experiments and used as a tool in studies of electron characteristics of metals [1]. At present, these effects are extensively used to study geometrical characteristics of Fermi surfaces in various high-temperature superconductors. Quantum oscillations are specified with contributions from effective cross sections of the Fermi surface (FS) by planes perpendicular to the quantizing magnetic field B. These are cross sections with minimum and maximum cross sectional areas Aex . Accordingly, fine geometrical structure of the FS at the effective cross sections and in their vicinities may influence the oscillations. It was already shown that oscillations magnitude could be significantly enhanced when the FS includes nearly cylindrical segments of zero curvature, and some effective cross sections run along these segments [2, 3]. A simple explanation of this effect is that the contributions from nearly cylindrical segments of the FS to the electron density of states (DOS) could be sensibly greater than those from the rest of the surface. Therefore the number of effective electrons associated with a nearly cylindrical cross section is increased which amplifies the oscillations. It is likely that FSs of some metals include locally flattened segments. Even slight distortion of a Fermi sphere due to the effect of crystalline fields results in the FS flattening at some points [4]. There is an experimental evidence that points of flattening exist on the FSs of cadmium, zinc and potassium [5, 6, 7]. When the FS is flattened at some points, this also may bring along an enhancement in the number of effective electrons and amplify the oscillations. To the best of our knowledge, the effect of local flattening of the FS on quantum oscillations was never studied before. We analyze this effect in the present work. As shown below, quantum oscillations could be noticeably strengthened due to the effect of locally flattened segments of the FS, and this could help to locate such segments (if any) in the experiments. The latter brings extra informations concerning fine geometrical features of the FSs. These informations are especially
Local Flattening of the Fermi Surface and Quantum Oscillations in the Magnetoacoustic Response of a Metal
arXiv:cond-mat/0505301v2 [cond-mat.mtrl-sci] 7 Nov 2005
interesting for flattened pieces on the FSs (even small in area) could strongly contribute to the nesting function affecting the strength of the electron-phonon coupling and, consequently, the superconducting temperature in relevant metals. To make the presented results more specific we apply our analysis to study the effects of the FS local geometry on the quantum oscillations in the velocity of ultrasound waves travelling in a metal. When an ultrasound wave propagates in a metal the crystalline lattice is periodically deformed. It gives rise to electric fields which influence the electrons. Besides, the periodical deformations of the lattice cause changes in the electronic spectrum. Here, we omit these deformation corrections to simplify further calculations. To proceed we adopt the following energy-momentum relation: p2 E (p) = 1 2 m1