1) core-to-sludge ratio
岩心岩粉比
2) stone dust
岩粉
1.
Based on the experiment data of stone dust suppression of propagation of coal dust continuous explosion at DMT research institute of Germany,this paper studies the problems such as,partial inertia effect of stone dust with one time explosion and repeated explosion of coal dust.
根据在德国DMT研究院进行的煤尘连续爆炸时岩粉隔爆效果的实验数据,分析与探讨了在煤尘的一次爆炸和重复爆炸时,岩粉局部惰化效果等问题。
3) Siltstone
[英]['siltstəun] [美]['sɪlt,ston]
粉岩
4) sandstone core
砂岩岩心
1.
The pore structure,oil and water flow mechanics including the lithology of sandstone core,electricity curve and relative permeability curve were characterized by fractal.
砂岩岩心不仅孔隙结构具有分形特征,而且油、水在岩石内部渗流过程中岩电特性曲线和油、水相对渗透率曲线也具有分形特征。
5) core
[英][kɔ:(r)] [美][kɔr]
岩心
1.
Primary research on lateral accretion with horizontal well core samples;
水平井岩心侧积夹层初探
2.
Core Test of Profile Control and Displacemrnt by Combining Weak Gel with Microbe;
弱凝胶与微生物调驱联作技术岩心试验研究
3.
Experimental research of the transmission characteristic of low frequency hydrodynamic oscillation in cores;
低频水力振动在岩心中的传播特性实验
6) cores
[英][kɔ:] [美][kor]
岩心
1.
This is due to the skin effect of cores.
实测的岩石压缩系数数值普遍偏高,甚至高于地层原油的压缩系数,该现象是由于岩心的表皮效应所致。
2.
A method for determining oil and water saturations in cores by volume?_CT scanner was developed on the basis of X_ray hardening treatment,X_ray drifting correction,martix transformation of imagines and position correction of CT images with volume?_CT technology.
对CT图像进行了X射线硬化处理、X射线漂移校正、图像矩阵变换及体积CT位置校正 ,研究出用体积CT对岩心流体饱和度进行测量的技术。
3.
The changes of relative permeability for oil phase,kro, and for water phase, krw, determined at 80℃ in oil displacement experiments on cores by formation water (FW) of Caoqiao, Shengli, and 1% solutions of anionic surfactants HD1 and HD2 in FW (HD1, HD2 solution) are investigated.
通过岩心流动实验,测定了80℃时胜利草桥某井地层水、两种磺酸盐类阴离子表面活性剂HD 1和HD 2的1%地层水溶液驱油时,油相和水相相对渗透率kro和krw的变化。
补充资料:粉砂岩
粉砂岩 siltstone 由粒径为0.0625~0.0039毫米(mm)的粉砂的含量占50%以粉砂岩标本的一种碎屑沉积岩。除粉砂以外其它由砂、粘土或化学沉淀物组成。按粒度划分为粗粉砂岩(0.0625~0.0312mm)和细粉砂岩(0.0312~0.0039mm)。按碎屑成分划分为石英粉砂岩、长石粉砂岩、岩屑粉砂岩(少见)和它们间的过渡类型。根据胶结物成分划分为粘土质粉砂岩、铁质粉砂岩、钙质粉砂岩和白云质粉砂岩。黄土也是一种疏松的或半固结的粉砂质沉积物。粉砂岩多形成于河漫滩、三角洲、潟湖和海洋的较深水部位。
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