首页|基于海口EGS场地的微震分析及震级预测

基于海口EGS场地的微震分析及震级预测

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近年随着地热能和增强型地热系统(EGS)的不断普及,越来越多的诱发微震事件也由此产生.为探讨地震活动的机制及查明实际工程中潜在的诱发微地震风险,笔者将位于海南省海口市的水力压裂场地作为研究区,通过收集相关地质和重磁勘探资料,建立二维地质模型,并模拟分析了断层面孔隙压力和孔隙弹性效应的时空演化过程,进行了诱发地震风险性评估和震级预测.结果表明:在研究区的流体注入会导致附近断层的应力发生改变,致使可能引起微小的断层活化现象,但由此产生的地震震级较小,工程风险较低.
Microseismic analysis and magnitude prediction based on EGS site in Haikou,Hainan
In recent years,with the continuous popularization of geothermal energy and enhanced geothermal systems(EGS),there has been an increase in the occurrence of induced microseismic events.To explore the mechanism of seismic activity and identify the potential risks of induced microseismicity in practical engineering,the authors took the hydraulic fracturing site in Haikou City,Hainan Province,as the study area.By collecting rel-evant geological and geophysical(gravity and magnetic)exploration data,a two-dimensional geological model was established,which was used to simulate and analyze the temporal and spatial evolution of the pore pressure and pore elasticity effects on the fault surface.Subsequently,an assessment of the risk of induced seismicity and a pre-diction of the magnitude of the seismicity were conducted.The results show that fluid injection in the study area will lead to changes in the stress on the nearby faults,which may cause minor fault activation phenomena,but the mag-nitude of the resulting earthquakes is low,resulting in a lower engineering risk.

EGSseismic activity ratemagnitude predictionHaikou

钱永胜、张延军、孙少游

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吉林大学建设工程学院,长春 130026

北京市市政工程设计研究总院有限公司,北京 100082

增强型地热系统 地震活动率 震级预测 海口

中国国家重点研发计划中国博士后科学基金

2019YFC06049052022M711291

2024

世界地质
吉林大学 东北亚国际地学研究与教学中心

世界地质

CSTPCD
影响因子:0.769
ISSN:1004-5589
年,卷(期):2024.43(1)
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