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液体注入中断导致局部应力场的暂时变化,并在冰岛Krafla火山口诱导地震性
Elisabeth Glück1, Roberto Davoli2, Thorbjörg Ágústsdóttir3
1Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, IRD, Univ. Gustave Eiffel, ISTerre, Grenoble, France.
Scientific reports
|February 26, 2026
概括
在地热系统中注入液体可以引发地震. 在冰岛停止注射.
科学领域:
- 地质物理学 地质物理学
- 地热能源 地热能源
- 地震学 地震学
背景情况:
- 诱导性地震是地热能源生产的一个重要问题.
- 了解高温地热系统中的地震触发因素是复杂的.
- 冰岛东北部的克拉弗拉火山口是一个地质活跃的地区.
研究的目的:
- 研究人类活动与地热系统压力场变化之间的联系.
- 在液体注射中断期间分析地震异性变化.
- 了解引发注入井附近地震的机制.
主要方法:
- 对剪切波分裂现象的分析.
- 监测地震异质变化 (S波偏振和时间延迟).
- 地震事件与注入井活动的相关性.
主要成果:
- 在注射停止后,观察到快速S波偏振的90度翻转和S波时间延迟的减少.
- 这些变化恰逢罢工滑坡地震事件急剧增加.
- 恢复注射似乎恢复了之前的地震状态和异构性.
结论:
- 人为液体注射活动影响当地应力场和地震性.
- 地震异性变化与孔隙压力变化和断层激活有关.
- 需要进一步的研究才能充分理解这些复杂的相互作用.
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