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模拟地层的英文

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"模拟地层"怎么读用"模拟地层"造句

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  • simulated formation

例句与用法

  • Experimental study on the relations between rock resistivity and temperature in simulating in - situ conditions
    模拟地层条件下岩芯电阻率与温度关系的实验研究
  • 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) 。
  • A nonlinear transient flows model for stress - sensitive formation were built , and the one classical and two classical approximately solution and t column source solution in laplace domain were go by pedrosa , kikani , wang xiaodon , etc . the stress - sensitivity study main focus on tuziluoke and yinan2 gas fields in tarim basin : the core samples stress - sensitivity is analyzed by the servo tri - axes rock mechanics test system . the data points plot on the semi - log plot does not show a single linear curve but two or multiple stage linear curves . the main reason is that the different pore structure type has different capability to against the compress
    在前人研究的基础上,本文针对塔里木吐孜洛克和依南2两个气藏的压敏特性进行了深入的研究:利用引进于美国的全伺服三轴岩石力学实验系统,针对所研究工区的塔里木吐孜洛克气藏和伊南2气藏高压低渗的特点,对所选取的岩心进行了一系列模拟地层条件下的压力敏感性实验,获得了大量的实验数据。
  • Using the rock resistivity meter with simulating in - situ conditions , the relations between rock resistivity and temperature were observed from 6 sandstone samples with different porosity and permeability , while samples were brine water - saturated and subjected to certain confining pressure . it is found that the resistivities of water - saturated rock samples decrease in the form of power expression with the temperature increase . although the resistivity of brine water decreases with temperature in the same rule , it can not entirely account for the decreasing of rock resistivity . the cementation factor
    利用模拟地层条件岩芯电阻率测量仪,对6块孔隙度渗透率各不相同的砂岩岩芯,在一定围压条件下,岩芯完全饱和盐水时,考察了岩芯电阻率随温度的变化。发现饱和盐水岩芯的电阻率随温度升高,以幂函数形式下降。虽然岩芯中饱和盐水的电阻率同样随温度以幂函数形式下降,但岩芯电阻率的下降不能完全用岩芯饱和盐水的下降表征。
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