节点文献
深部含水灰岩层处置CO2作用机理探讨
Interaction Mechanism of Disposing CO2 in Deep Water-bearing Limestone
【摘要】 研究基于IS-100型高压气体等温吸附/解吸仪与自制密封反应器为实验平台,模拟了地质处置后CO2在不同压力和不同时间尺度下与深部含水灰岩的气-水-岩作用。实验结果表明:灰岩中钙离子在溶有CO2的溶液中极易析出;灰岩溶蚀速率随CO2注入压力的增高而呈线性增加;灰岩溶蚀量随时间的延长而增加,但溶蚀速率逐渐减小,并趋于稳定。
【Abstract】 The gas-water-rock action mechanism of CO2 with deep-water limestone after CO2 geological disposal at different pressures and different time scales is simulated on the base of IS-100 type high pressure gas isothermal adsorption/desorption instrument and self-made seal reaction tanks. The experiment results show that the calcium of limestone is easily precipitate in solution of CO2; the dissolution rate of limestone increased linearly with the increase of CO2 injection pressure; the amount of limestone dissolution increased with time, but the dissolution rate gradually decreased and stabilized.
【Key words】 geologic storage; gas-water-rock interaction; deep-water limestone;
- 【文献出处】 煤炭技术 ,Coal Technology , 编辑部邮箱 ,2017年03期
- 【分类号】X701;X141
- 【下载频次】61