CO_(2)咸水层封存过程中土著微生物的生物地球化学行为进展研究  

Research Progress on Biochemical Behavior of Indigenous Microorganisms During CO_(2) Sequestration Process in Deep Saline Aquifers

作　　者：李晨阳 尚永正 王聪 刘刚 刘兆煐 Li Chen-yang;Shang Yong-zheng;Wang Cong;Liu Gang;Liu Zhao-ying

机构地区：[1]吉林建筑大学松辽流域水环境教育部重点实验室,吉林长春130118 [2]中国市政工程东北设计研究总院有限公司,吉林长春130000 [3]吉林省师泽环保科技有限公司,吉林长春130000 [4]吉林省长春生态环境监测中心,吉林长春130000

出　　处：《化工设计通讯》2022年第6期176-177,共2页Chemical Engineering Design Communications

基　　金：吉林省教育厅十三五科学研究规划项目(JJKH20200268KJ)。

摘　　要：CO_(2)地质封存技术是目前被认为有效减少温室气体排放量及应对气候变暖最有效、最直接的技术,而深部咸水层是CO_(2)地质储存的理想储层。CO_(2)注入咸水层后对土著微生物群落结构与多样性会产生较大影响,而某些特定微生物会反作用于CO_(2)地质封存过程,从而起到积极作用。CO_(2) geological storage technology is currently considered as the most effective and direct technology to reduce greenhouse gas emissions and cope with climate warming,and deep salt water layer is an ideal reservoir for CO_(2) geological storage.When CO_(2) is injected into the brackish water layer,the structure and diversity of the indigenous microbial community will be greatly affected,and some specific microorganisms will react on the CO_(2) geological storage process and play an active role.

关 键 词：CO_(2)地质封存技术 咸水层 土著微生物 

分 类 号：P632.4[天文地球—地质矿产勘探]