相对稳定的压力效应和时间增长的热收缩控制 希伯地热场变形
Guoyan Jiang1, Andrew J Barbour2, Robert J Skoumal3
1School of Geodesy and Geomatics, Hubei Luojia Laboratory, Wuhan University, Wuhan, China. gyjiang@whu.edu.cn.
Nature communications
|June 17, 2024
概括
地热运行可能会导致土壤沉降,原因是流体退出和热收缩,挑战现有的流体注入表面升起模型. 这些因素也影响了地震活动.
科学领域:
- 地质物理学 地质物理学
- 地热能源 地热能源
- 地球科学 地球科学 地球科学
背景情况:
- 地热场变形,包括沉降和地震性,是复杂的,由于地质因素和数据限制,人们对其了解甚少.
- 在Heber地热场 (HGF) 中观察到的沉降与盐注入所预期的表面提升相矛盾.
- 升起和沉降之间的短暂反转使地热运作的解释变得复杂.
研究的目的:
- 确定控制高温电流中的地热场变形的物理过程.
- 为了解释尽管注射了液体,但观察到的异常沉降.
- 阐明流体压力与热效应对表面移位和地震性的相互作用.
主要方法:
- 来自希伯地热场十年的变形数据的分析. 希伯地热场.
- 流体动力学的建模,包括从高产量生产井的吸收效应.
- 评估热收缩和对操作变化的可弹性反应.
主要成果:
- 高产量生产井抽出液体,导致周围低注入区域的沉降.
- 由冷却驱动的热收缩随着时间的推移变得占主导地位,超过了压力效应.
- 沉降异常归因于液体吸收和热收缩的联合作用.
结论:
- 这项研究表明,液体吸收和热收缩是地热沉降的关键驱动因素,而不仅仅是注入.
- 热收缩显著影响长期的表面移位和地震性趋势.
- 压力效应导致地热场变形的快速,短期变化.
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