孔隙流体的英文

• interstitial fluid
• pore fluid

• "孔隙"英文翻译    small opening; hole; pore; a ...
• "流体"英文翻译    fluid; fluor
• "孔隙流体波" 英文翻译 :    fluid wave in soil
• "孔隙流体压力" 英文翻译 :    pore-fluid pressure
• "异常孔隙流体压力" 英文翻译 :    abnormal pore fluid pressure
• "土的动力性质孔隙流体波" 英文翻译 :    fluid wave in soil
• "孔隙流速" 英文翻译 :    pore velocity
• "间隙流体" 英文翻译 :    interstitial fluid
• "间隙流体压力" 英文翻译 :    interstitial fluid pressure
• "隙隙流体压力" 英文翻译 :    pore fluid pressure
• "隙流" 英文翻译 :    clearance flow
• "含流体的孔隙空间" 英文翻译 :    fluid-filled pore space
• "自由流体孔隙度" 英文翻译 :    free fluid porosity
• "缝隙流" 英文翻译 :    slit flow
• "裂隙流" 英文翻译 :    fissure flow
• "流体可驱移的孔隙容积" 英文翻译 :    movable pore volume
• "岩石孔隙中的各种流体" 英文翻译 :    geofluid
• "孔隙" 英文翻译 :    small opening; hole; [冶金学] pore; aperture gap; pore space; ventage; void
• "阀隙流速" 英文翻译 :    mean gas velocity in valve opening area
• "环隙流速" 英文翻译 :    annular velocity
• "间隙流量" 英文翻译 :    clearance flow
• "隙流束源" 英文翻译 :    effusive beam sourse
• "地层孔隙中流体的密度，单位为" 英文翻译 :    g /cm
• "流体" 英文翻译 :    [物理学] fluid; fluor◇流体力学 fluid mechanics; hydromechanics; 流体生物学 hydrobiology; 流体运动学 hydrokinematics
• "孔隙比；孔隙率" 英文翻译 :    void ratio

• Fluid wave in soil
  孔隙流体波
• The method was proposed to compute the rock modulus when one kind of pore fluid changed to another , and to identify the pore fluids by the use of poroelastic modulus
  提出孔隙流体变化时岩石有效模量的计算，及利用孔隙弹性模量辨别储层中不同流体类型的计算方法。
• The three models are : ( a ) hydrate is part of the pore fluid , ( b ) hydrate becomes part of the solid frame , and ( c ) hydrate cements grain contacts together
  这三个模型分别是： ( a )水合物为孔隙流体的一部分； ( b )水合物是岩石骨架的一部分； ( c )水合物和岩石颗粒胶结。
• The main conclusion made from the test is that the rock mechanics properties are always changed and mainly affected by stress state and saturation of pore fluid during developmentof oil and gas
  指出油气开发过程中岩石力学性质是不断变化的，且主要受岩石的应力状态和孔隙流体含量的影响。
• Under the condition of uniformity degradation the formation compression will have a whole fall on account of the reduce of overburden , the expanding of fluid hi the pore and rocks and the decrease of density
  在均匀剥蚀情况下，上覆岩层厚度减小，岩石和孔隙流体膨胀，密度减小，地层压力会整体降低。
• When waves propagate over the ocean surface , a sequence of wave pressure is induced on the mudline or seafloor , which causes the coupling interaction between the deformation of soil skeleton and seepage movements of porous fluid
  海洋表面传播的波浪在海水-海床的交界面处施加了循环波压力，在这种循环波压力作用下，海床内土骨架的变形与孔隙流体的渗流运动相互耦合。
• Based on biot ' s consolidation and simplified sea - bed to two dimensional sea - bed , numerical simulation about the response of sea bed to waves is developed . the assumption was wielding , such as linear wave loading , linear elastic skeleton of soil and darcy ' s law flow
  本文选用了基于biot固结理论，将海床进行二维简化的情况下海床对波浪响应的数学模型，在模型中采用下列假定：线性波浪作用，线弹性土骨架，孔隙流体的流动满足达西定律。
• Treating the soil as a two - phase mixture and considering the interactive influence of seepage and solid deformation , this paper analyzes the dynamic impedance of group piles in layered saturated porous media by indirect boundary element method and investigates the effects of pore fluid in saturated soils on dynamic impedance of piles
  摘要将饱水软土地基视为两相介质，考虑水的渗流和土骨架变形的耦合作用，用间接边界元法分析层状饱水软土地基中横向受荷群桩动力阻抗，探讨饱和土中孔隙流体对饱和土中横向受荷群桩动力阻抗的影响。
• Based on the analysis of thin sections by microscope , measurement of porosity and density , and geological setting , we tested the rock physical parameters of sandstone , siltstone , carbonate and other transitional sedimentary rocks by the mts system under formation conditions ( temperatures , pressures and pore fluid properties ) . the rocks we tested are from tertiary ( including zhujiang formation , zhuhai formation , enping formation , hanjiang formation ) of zhujiangkou basin in southern china sea . according to the analysis results , we studied the main ultrasonic wave velocity characters of rocks , which are compressive and shear wave velocity and poisson ' s ratio under different formation conditions
  在对珠江口盆地第三系储集岩进行显微镜薄片分析、孔隙度和密度分析，以及地质背景分析的基础上，利用岩石物理参数测试系统( mts )模拟地层条件(温度、压力和孔隙流体状况)测试了珠江口盆地第三系(包括珠江组、珠海组、恩平组、韩江组，以下有关讨论同)砂岩、粉砂岩、碳酸盐岩及其过渡性岩石物理性质，重点研究了不同地层条件下岩石的声学特征(岩石的纵横波速度和泊松比) 。
• The acidic liquid related to decomposition of organic mater during hydrocarbon enrichment in the late diagenesis , and m eteoric - waters during epidiagenesis , had resulted in dissolution of detrital feldspars and carbonate cements , which contributed a better retention of reservoir quality for the sandstones
  溶蚀作用是砂岩物性改善的主要原因，尤其是晚期成岩阶段，在富含有机酸和无机酸酸性孔隙流体的作用下形成一定量的次生溶蚀孔，使储层砂岩物性得到一定改善；在表生成岩阶段，由于大气降水的介入，储层物性再次得以改善。