对Caprock泄漏评估的自然剪切和诱导拉伸断裂的分析和比较
Sahyuo Achuo Dze1,2, Tomos Phillips1,3, Reza Najafi-Silab2
1Lyell Centre, Heriot-Watt University, Edinburgh, UK.
概括
诱导的拉力和自然剪切断裂在低透性的卡普罗克表现出类似的流体流. 断裂开放模式对流量的影响小于所选择的估计方法,突出了流量分析中的不确定性.
科学领域:
- 地质科学 地质科学
- 岩石机械学 岩石机械学
- 水文地质学 水文地质学
背景情况:
- 了解地下裂中的流体流动对于地质应用至关重要.
- 区分自然和诱导骨折之间的流动特征仍然是一个挑战.
研究的目的:
- 为了比较实验室诱导的拉力断裂与自然剪切断裂中的流体流.
- 分析断裂几何和打开模式对流量的影响.
主要方法:
- 高分辨率的同步子成像,以创建3D断裂空隙几何形状.
- 对光圈分布,表面粗度和空间相关性的分析.
- 与平行板模型和直接数值模拟 (DNS) 进行测量传导性的比较.
主要成果:
- 诱导的拉力和自然剪切断裂显示在低透性的卡普罗克中具有相似的流量.
- 骨折异质性差异的影响小于预期.
- 流量估计方法比断裂打开模式带来了更多的不确定性.
结论:
- 卡普洛克断裂中的流体流动是相似的,无论它们是自然剪切还是诱导拉力.
- 直接的数值模拟和理论模型应该考虑方法诱导的不确定性.
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