1) primary interstice
初生孔隙
2) original porosity
初始孔隙度
1.
The original porosity lied on clastic size and lithofacies so that the original porosity of a sort clastic bed can be considered as the same, but the compaction process could be different from each other.
同种类的沉积岩石的初始孔隙度值可能相差不大,它们主要受碎屑颗粒大小和沉积相影响,但是其压实过程可能会存在较大的差异。
3) initial void ratio
初始孔隙比
1.
It was shown that ① For the rockfills with determined particle grading,the conversion between shear dilatancy and shrinkage of the samples depended upon a critical initial void ratio(e0)crit and critic.
基于不同初始孔隙比e0和不同固结压力σc情况下筑坝堆石料大型三轴固结排水剪切试验,分析了堆石料应力应变关系与体积应变关系以及剪胀率ζ与塑性剪应变εsp关系的变化规律。
2.
The study has shown that the transient modulus of MSW is changed when the organic content,the initial moisture,the initial void ratio or the degradation degree of MSW changing;and some changing laws due to influences of above-mentioned factors are obtained.
采用有代表性配比的人工配料垃圾土试样对瞬时模量变化规律进行了试验研究,结果表明:垃圾土有机质含量、初始含水率、初始孔隙比及降解程度的变化对瞬时模量都有影响,并得到了各影响因素下的变化规律。
4) secondary pores
次生孔隙
1.
Effectiveness of thermochemical sulfate reduction on oil and gas industry—a H_2S formation accelerating development of the secondary pores in reservoirs;
TSR(H_2S)对石油天然气工业的积极性研究——H_2S的形成过程促进储层次生孔隙的发育
2.
Distribution and genesis of secondary pores in Tertiary clastic reservoir in Southwestern Qaidam Basin;
柴西南地区第三系碎屑岩储集层次生孔隙分布及成因
3.
Genesis of heterogeneity of secondary pores in deep reservoir of Jiangling Depression;
江陵凹陷深层储层次生孔隙非均质性成因
5) primary pore
原生孔隙
1.
The pore types of the deep reservoir are divided into three types, namely, the primary pore, secondary pore, and mixing pore.
通过对胜利油区渤南洼陷深部储层特征的研究 ,提出了深部储层孔隙类型划分方案 ,将孔隙划分为原生孔隙、次生孔隙和混生孔隙三大类 ;将裂缝划分为构造缝、重力滑移缝、异常压力缝、成岩缝、原生缝、塑性变形面、溶蚀裂缝七大类 ,把裂缝型储层提到了与孔隙型储层同等重要的位置 ,强调了泥岩裂缝型储层的重要
6) primary porosity
原生孔隙
1.
From the analysis of thin section,it shows widely growing primary porosity and complicate secondary porosity in Shaximiao Fm of Middle Jurassic,Luodai Gas Field of the West Sichuan.
早成岩A期,压实作用和石英Ⅰ级次生加大使原生孔隙度迅速降低至10%~15%左右;早成岩B期,碳酸盐胶结物和硬石膏胶结物大量出现,孔隙度丧失至不足10%;到中成岩A期,由于强酸性水的存在,开始出现Ⅱ级石英加大边和自生高岭石沉淀;中成岩B期,溶蚀作用不断加强,对孔隙改善作用明显;整个中成岩阶段,孔隙不断的消长演化,孔隙度下降到4%~9%,并最终形成低孔低渗的致密性储层。
补充资料：催化剂孔隙度(degree of catalyst pole)
分子式：
CAS号：
性质：又称催化剂孔隙度(degree of catalyst pole)。多孔性催化剂颗粒内微孔的总体积，单位是ml/g。其大小由催化剂制备条件决定。
CAS号：
性质：又称催化剂孔隙度(degree of catalyst pole)。多孔性催化剂颗粒内微孔的总体积，单位是ml/g。其大小由催化剂制备条件决定。
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