通过脆性到柔性过渡的透性划分及其对超临界地热水库的影响
Gabriel G Meyer1, Ghassan Shahin2, Benoît Cordonnier3
1Laboratory of Experimental Rock Mechanics, School of Architecture, Civil & Environmental Engineering, Ecole Polytechnique Fédérale de Lausanne, Lausanne, Switzerland. gabriel.meyer@epfl.ch.
Nature communications
|September 5, 2024
概括
超临界地热能能提供十倍的功率提升. 这项研究表明,半性岩石,而不仅仅是脆性岩石,可以显著增加透性,使地球地中的液体循环得到增强.
科学领域:
- 地热能源 地热能源
- 岩石机械学 岩石机械学
- 水文地质学 水文地质学
背景情况:
- 超临界地热资源 (≥400°C) 承诺比传统系统增加十倍的功率输出.
- 这些水库往往位于半可伸缩或可伸缩地区域,阻碍断裂形成并限制对液压性能的理解.
- 脆性-柔性过渡 (BDT) 通常被认为是流体循环的障碍.
研究的目的:
- 在超临界条件下研究岩石的复杂透性.
- 了解应变分离在不同变形模式下对岩石透性的影响.
- 挑战BDT限制地中流体循环的概念.
主要方法:
- 使用基于气体的三轴装置进行机械数据采集.
- 用于微观结构分析的高分辨率同步死后3D成像.
- 有限元模型模拟岩石变形和透性演变.
主要成果:
- 应变分离被确定为透性的主要控制.
- 在脆弱模式下,应变局部化发生在现有断层上,而不会显著增加散装透性.
- 在半柔性模式下,分布式应变增强了变形带和散体中的透性,导致超过十倍的增加.
结论:
- 在变形的半性岩石中,透性可以显著发展和增加.
- 脆性-柔性过渡并不代表在地中流体循环的最终切断.
- 这些发现支持在以前被忽视的半性岩层中增强地热系统的潜力.
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