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新疆呼图壁地下储气库断层气体地球化学特征研究
引用本文:蒋雨函,高小其,张磊,许秋龙,汪成国,陈其峰,范雪芳. 新疆呼图壁地下储气库断层气体地球化学特征研究[J]. 中国地震, 2021, 37(4): 749-766
作者姓名:蒋雨函  高小其  张磊  许秋龙  汪成国  陈其峰  范雪芳
作者单位:应急管理部国家自然灾害防治研究院,地壳动力学重点实验室,北京 100085;新疆维吾尔自治区地震局,乌鲁木齐 830011;山东省地震局,济南 250014;山西省地震局,太原 030021
基金项目:国家重点研发计划(2019YFC1509203)、中国地震局地壳应力研究所中央级公益性科研院所基本科研业务专项(ZDJ2017-27)和中国大陆综合地球物理场观测仪器研发专项(J2218827)共同资助
摘    要:Rn、CO2、Hg、H2等断层气体被广泛应用于断层活动性以及断层结构特征的研究.当前,研究介质中压力变化与断层气间的关系是断层气映震研究的主要技术方法之一.新疆呼图壁地下储气库自建成以来,每年以周期性循环"注入/采出"模式运行,该运行模式带来的储气库气压变化会影响周围地区的地震活动.同时,这一定期加压存储与减压释放气体...

关 键 词:呼图壁储气库  断层气  气体地球化学  氢气    流动观测  连续观测
收稿时间:2021-02-19
修稿时间:2021-06-08

Geochemical Characteristics of Soil Gas along Faults in Hutubi Underground Gas Storage, Xinjiang
Jiang Yuhan,Gao Xiaoqi,Zhang Lei,Xu Qiulong,Wang Chengguo,Chen Qifeng,Fan Xuefang. Geochemical Characteristics of Soil Gas along Faults in Hutubi Underground Gas Storage, Xinjiang[J]. Earthquake Research in China, 2021, 37(4): 749-766
Authors:Jiang Yuhan  Gao Xiaoqi  Zhang Lei  Xu Qiulong  Wang Chengguo  Chen Qifeng  Fan Xuefang
Affiliation:Key Laboratory of Crustal Dynamics, National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, China;Earthquake Agency of Xinjiang Uygur Autonomous Region, Urumqi 830011, China;Shandong Earthquake Agency, Jinan 250014, China; Shanxi Earthquake Agency, Taiyuan 030021, China
Abstract:Earthquakes activities can cause the release of underground gas. Soil gases along faults such as radon, carbon dioxide, mercury and hydrogen are widely used in the study of fault activity and the characteristics of fault structure. At present, a great attention has been paid to study the relationship between pressure changes in the medium and gas along fault in studying fault gas reflection. Since the completion of Xinjiang Hutubi Underground Gas Storage, it has been operating in a cyclical "injection/production" mode every year. The gas storage pressure changes caused by such operation mode will have an impact on the seismic activity in the surrounding areas. At the same time of concerning the production and life safety of surrounding residents, this process of regular pressurized storage and decompression of gas release provides a natural testing ground for studying fault gas changes caused by stress changes. In this paper we carried out periodic fault gas measurement and continuous monitoring of fault gas at fixed points in Hutubi gas storage to obtain the fault gas Rn, CO2, Hg, H2 of the gas storage and the surrounding area during the repeated loading and unloading of the gas storage. Relatively high concentrations of Hg and H2 are observed in the gas storage area, with the maximum values of 190ng/m3 and 725.40ppm respectively. In terms of spatial distribution characteristics during the process of pressurized storage in the gas storage, the gas concentration near the injection and production wells in the gas storage area is higher than that outside the gas storage area. In addition, the long-term continuous observation results show that the H2 has a certain relationship with the pressure change of the gas storage, and has a certain effect on the gas storage, which suggests that the H2 response to changes in internal pressure is more sensitive. Our results show that analyzing the characteristics of gas changes caused by stress changes in Hutubi gas storage can provide geochemical scientific and technological support to help the survey and selection, construction, earthquake situation tracking and anomaly implementation of seismic stations.
Keywords:Hutubi gas storage  Fault gas  Gas geochemistry  Hydrogen  Mercury  Fault gas measurement  Continuous monitoring
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