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1)  Electroporation
电生孔
2)  immunity cell electroporation
细胞电生孔
3)  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
4)  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
5)  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。
6)  secondary porosity
次生孔隙
1.
The secondary porosity type of the clastic rock storage in Ordos Basin;
鄂尔多斯盆地碎屑岩储集体中的次生孔隙类型
2.
Relationship between development of salt layers and the secondary porosity of deep reservoirs in Bonan sag;
渤南洼陷膏盐层发育与深层储层次生孔隙发育的关系
3.
The controlling factors and processes for the formation of the secondary porosity of the deep-seated reservoir rocks in the Bonan depression,Shandong;
影响渤南洼陷深部储层次生孔隙形成的因素及其作用
补充资料:望月婆罗门引 史尚书生朝 强村丛书校孔荭谷
【诗文】:
太平有象,老人星、喜照滹阳。前衔曾近文昌。寿乐堂名今年余庆,新到五花堂。看鸡鸣问寝,鳞次称觞。白眉最良。八州督,汉侯王。院院琼林玉树,画戟清香。一椿五桂,更休说、燕山窦十郎。谈麈上,白日羲


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