1) carbargillite
微泥质层
2) mudstone layer
泥质岩层
1.
Water is easily preserved in the pores and forms the undercompaction of the mudstone layer.
泥质岩层中的孔隙水在向外排运的过程中遵循低速非达西流动规律。
3) laminated shale
层状泥质
1.
Based on parallel conductance between laminated shale and dispersed shaly sands, and the assumption under which dispersed shaly sands are described with dual water conductivity model, a new dual water conductivity model for laminated and dispersed shaly sands is established.
基于层状泥质和分散泥质砂岩并联导电,采用双水电导率模型来描述分散泥质砂岩导电规律,建立了混合泥质砂岩双水电导率模型。
2.
Based on the hypothesis that the laminated shale and dispersed shaly sand are parallel conduction,and the conduction theory for 3-dimensional periodic array of charged spheres immersing in electrolyte,a new generalized double layer conductivity model is proposed for laminated and dispersed shale coexisting in shaly sand.
基于层状泥质与分散泥质砂岩并联导电理论,以及悬浮于电解液中三维周期排列带电球体导电理论,建立了分散泥质和层状泥质同时存在的混合泥质砂岩通用双电层电导率理论模型。
3.
Based on the parallel conductance between laminated shale and dispersed shaly sand,and new electric double layer conductivity model for dispersed shaly sand,then a new generalized electric double layer conductivity model is proposed for laminated and dispersed shaly sand interpretation.
基于层状泥质与分散泥质砂岩并联导电的理论,以及新的分散泥质砂岩双电层电导率模型,建立了分散泥质和层状泥质同时存在的混合泥质砂岩通用双电层电导率模型;分析了影响模型的因素。
4) shaly formation
泥质地层
1.
Determination of saturation exponent in shaly formation;
泥质地层中饱和度指数的确定
5) argillaceous sand
泥质砂层
6) muddy interbed
泥质夹层
1.
According to the lithology and physical properties of interbeds,the interbeds in the fluvial reservior could be divided into three types as muddy interbed,calcareous interbed and silty mud interbed.
根据夹层的岩性、物性特征,河流相储层中的夹层一般可分为泥质夹层、灰质(钙质)夹层和物性夹层,由于这3种夹层对流体运移影响程度不同,因此剩余油的分布也有差异。
补充资料：泥质陶
泥质陶 古代陶器的一种。早先的制陶，所用陶土不加淘洗。后来，人们学会选择陶土，并淘洗土中的杂质，此种经过选择、淘洗的陶器称为“泥质陶”，又名“细泥陶”。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条