在岩石盐中通过变形辅助的液体透
Soheil Ghanbarzadeh1, Marc A Hesse2, Maša Prodanović1
1Department of Petroleum and Geosystems Engineering, The University of Texas at Austin, 200 East Dean Keeton Street, Austin, TX 78712, USA.
概括
变形可以使岩盐中的液体流动,即使低于静态透值. 这一发现对于设计核废物储存库来防止泄漏至关重要.
科学领域:
- 地质学
- 地质学
- 材料科学
背景情况:
- 核废物的深层地质储存依赖于岩盐的低透性来隔离地下水.
- 透值通常限制静态岩盐中的流体流动.
研究的目的:
- 调查变形是否可以克服岩盐的静态透值.
- 评估核废物仓库设计对流体流动的影响.
主要方法:
- 在合成盐样本上进行静态实验,使用X射线微图学.
- 分析墨西哥湾盐矿的碳化合物分布情况.
主要成果:
- 在静态盐样本中确认了透值的存在.
- 观察到的碳化合物分布表明透发生在变形盐的静态值以下的孔隙.
- 被确定为变形辅助的透机制.
结论:
- 变形可以在静态值以下的孔隙中促进液体透.
- 核废物仓库的设计必须考虑到由变形驱动的流体透.
- 在变形的地质环境中,静态透值可能不足以限制流体流动.
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