在以上研究的基础上，本实验室通过对各种盐逆境，特别是碳酸盐逆境(carbonate stress)，进行系统的 分析和研究，提出了通过：强化植物细胞的pH调控系统、强化活性氧的解毒系统、提高植物细胞的电子传
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sodium carbonate stress 碳酸钠胁迫
And the strong karstification in the same direction as layer and cataclasis create by tectonic stress are the control factors of Ordovician carbonate karst reservoir development.
而强烈的顺层岩溶作用和构造应力引发的破裂作用是轮古东地区奥陶系碳酸盐岩岩溶型储层发育的主控因素。
This paper presented an evaluation method of carbonate fractured reservoirs, which is a numerical simulation method for the an ciend structural stress field.
本文提出了碳酸盐岩裂缝性储层的一种新评价方法——古构造应力场数值模拟法。
It was showed that the continuous rotation of principal stress induced the development of pore water pressure in carbonate sand.
结果表明，主应力方向的连续旋转导致了钙质砂中孔隙水压力的增长。
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