ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
干热岩地应力测量评价方法与前沿挑战
  
关键词:hot dry rock (HDR)  in-situ stress measurement  evaluation method  hydraulic fracturing  reservoir development  induced earthquake
基金项目:中国地质调查局地质调查项目(编号: DD20190138; DD20221660);国家自然科学基金项目(编号: 42177175);中国地质科学院地质力学研究所基本科研业务费项目(编号: DZLXJK202204)
作者单位E-mail
许家鼎 中国地质科学院地质力学研究所 jdingxu@126.com 
张重远 中国地质科学院地质力学研究所
中国矿业大学(北京)力学与建筑学院 
zhchongyuan@126.com 
缑艳红 中国石油集团测井有限公司地质研究院  
高万里 中国地质科学院地质力学研究所  
何满潮 中国矿业大学(北京)力学与建筑学院  
陈群策 中国地质科学院地质力学研究所  
秦向辉 中国地质科学院地质力学研究所  
李少辉 中国地质科学院地质力学研究所
中国矿业大学(北京)力学与建筑学院 
 
孙东生 中国地质科学院地质力学研究所  
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摘要:
An Overview of the Measurement and Evaluation Methods of In-situ Stress and Its Frontier Challenges in Hot Dry Rock
      Reliable in-situ stress data can guide the development of hot dry rock (HDR) resources. In view of the difficulties involved in investigation of in-situ stress in deep reservoirs of HDR, this study summarizes and puts forward three types of investigation methods suitable for in-situ stress measurement and evaluation in HDR, based on borehole, core, and geology, and points out their basic principles, test instruments, application scenarios and advantages and disadvantages. Additionally, the HDR in-situ stress measurement and evaluation model is proposed taking the Gonghe HDR project in Qinghai, China, as an example. The main conclusions of the in-situ stress feature are shown, and its consistency with the result of hydraulic fracturing is verified. Subsequently, two frontier scientific issues related to in-situ stress in HDR development, namely reservoir fracture control and induced earthquake, are pointed out. Finally, the understanding of the in-situ stress measurement method of HDR is summarized, and its development trend and challenges are also assessed.
XU Jia-ding,ZHANG Chong-yuan,GOU Yan-hong,GAO Wan-li,HE Man-chao,CHEN Qun-ce,QIN Xiang-hui,LI Shao-hui,SUN Dong-sheng.2023.An Overview of the Measurement and Evaluation Methods of In-situ Stress and Its Frontier Challenges in Hot Dry Rock[J].Acta Geoscientica Sinica,44(1):200-210.
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