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the fluid layer
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  “the fluid layer”译为未确定词的双语例句
     Correcting the ∑ Concept of the Fluid Layer Lag in the Bowl of Sedimentation Centrif-
     沉降离心机转鼓内液层滞后对∑理论的修正
短句来源
     In this paper, the roughly-cemented oil and gas-bearing sandstone is regarded as a viscous or viscoelastic fluid. A model of viscous (or vis-coelastic)fluid layer intercalated with elastic solids is set up. The reflection and transmission coefficients for simple harmonic plane SH wave on the fluid layer are determined.
     本文把胶结极差的含油气砂岩看成粘性或粘弹性流体,建立弹性固体中粘性(或粘弹性)流体夹层模型,求出了平面SH简谐波在流体层上的反射系数与透射系数,它们是与频率有关的函数.
短句来源
     the second occurs between the case and formation. When there is no or little cement in the well, the second Stoneley wave must exist, its velocity and attenuation depends on the thickness of the cement and the location of the fluid layer.
     第二类产生于套管与地层之间,称水泥层斯通利波,当水泥胶结不好或无水泥时,必有此波存在,它的相速度和衰减与水泥厚度、流体层的位置有密切关系。
短句来源
     Earthquake tsunami is the result of interaction between the solid layer and the fluid layer of Earth’s surface.
     地震海啸的产生是地球表面固体层和流体层相互作用的结果.
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  相似匹配句对
     FRACTURE FLUID
     压裂液
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     and fluid mud.
     高浓度悬沙层和浮泥层?
短句来源
     FLUID THERAPY
     液体疗法
     THE MANTLE FLUID AND METALLOGENY
     地幔流体与成矿作用
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     sliding layer (D);
     D滑移带层 ;
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  the fluid layer
Stress-free, isothermal boundaries are assumed at the horizontal boundaries of the fluid layer.
      
The fluid layer is bounded from below by a rigid boundary and from above by a deformable free surface.
      
It is observed that the fluid layer with suspended particles heated from below is more stable compared to the classical fluid layer without suspended particles.
      
The results indicate that the stability of the system is significantly affected by both throughflow and internal heat generation in the fluid layer.
      
The temporal development of thermal disturbances in the fluid layer heated isothermally from below is investigated, based on propagation theory.
      
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In this paper, the roughly-cemented oil and gas-bearing sandstone is regarded as a viscous or viscoelastic fluid. A model of viscous (or vis-coelastic)fluid layer intercalated with elastic solids is set up. The reflection and transmission coefficients for simple harmonic plane SH wave on the fluid layer are determined. They are categorized to the function of frequency dependence,

本文把胶结极差的含油气砂岩看成粘性或粘弹性流体,建立弹性固体中粘性(或粘弹性)流体夹层模型,求出了平面SH简谐波在流体层上的反射系数与透射系数,它们是与频率有关的函数.

The Stoneley period equation is derived from full sonic well - logging.The Stoneley phase velocities, attenuation as well as its waveform are numerically calculated and their curves are plotted respectively for no and little cement in a well. The characteristics of various curves are analysed and it is found that there are two types of Stoneley waveform in cased wells: the frist generates between the fluid and the case in the well; the second occurs between the case and formation. When there is no or little...

The Stoneley period equation is derived from full sonic well - logging.The Stoneley phase velocities, attenuation as well as its waveform are numerically calculated and their curves are plotted respectively for no and little cement in a well. The characteristics of various curves are analysed and it is found that there are two types of Stoneley waveform in cased wells: the frist generates between the fluid and the case in the well; the second occurs between the case and formation. When there is no or little cement in the well, the second Stoneley wave must exist, its velocity and attenuation depends on the thickness of the cement and the location of the fluid layer. When there is more cement in the well, this wave disappears. Therefore, the propagating feature of Stoneley wave can reflect the cement quality.

根据套管井声波全波测井理论,导出了斯通利波久期方程,数值计算并绘制了斯通利波在无水泥和水泥胶结不好时的相速度、衰减以及波形曲线,详细分析了各种曲线的特点,指出套管井中具有两类斯通利波:第一类产生于井中流体与套管之间,称套管斯通利波,它的相速度和衰减与套管外有无水泥没有关系;第二类产生于套管与地层之间,称水泥层斯通利波,当水泥胶结不好或无水泥时,必有此波存在,它的相速度和衰减与水泥厚度、流体层的位置有密切关系。当水泥胶结好时,此波消失.因而从理论上证实了斯通利波在套管井中的传播特性能够反映水泥胶结质量。

Based on the geodynamics,we consider that when the fluid layer under the rock layer moves,and the transport and accumulation of momentum energy excess a faulting threshold value of rock,an earthquake takes place.From the nonlinear equations of fluid mechanics,we derive a simplified nonlinear solution of momentum,corresponding the accumulation of the energy.From this we then can also derive a chaos equation,and chaos should correspond to the earthquake.Further,combining the Carlson Langer...

Based on the geodynamics,we consider that when the fluid layer under the rock layer moves,and the transport and accumulation of momentum energy excess a faulting threshold value of rock,an earthquake takes place.From the nonlinear equations of fluid mechanics,we derive a simplified nonlinear solution of momentum,corresponding the accumulation of the energy.From this we then can also derive a chaos equation,and chaos should correspond to the earthquake.Further,combining the Carlson Langer model,the magnitude period formula of the earthquake may be obtained,hence some results can be calculated quantitatively.Moreover,many external causes of the earthquake are only the initial conditions of this nonlinear system.

在实验中观察到,在激波作用下非晶合金晶化成纳米晶体。本文试图对这一现象给出初步的理论上的解释。非晶合金内部微观不均匀,分布着大量微小有序原子集团(cluster)和位错。在激波作用下,位错运动,而cluster阻碍激波的传播,使位错堆积于cluster周围。激波与cluster周围局域应力场相互作用使得cluster旋转,而cluster周围的高应力应变能使类液区(intercluster)原子切变沉积于cluster上,cluster长大成为微晶,非晶合金晶化。

 
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