在正常负荷下,通过自然粗断裂的流量进行实验和数值分析
Paolo Trinchero1, Liangchao Zou2, Miquel de La Iglesia1,3
1AMPHOS 21 Consulting S.L., Carrer de Veneçuela, 103, 08019, Barcelona, Spain.
Scientific reports
|March 7, 2024
概括
了解破碎岩石中的合水力机械 (HM) 过程是核废物处理的关键. 这项研究表明,将液压孔径调整为机械孔径的1/5,可以改善在不同负载下自然断裂的流量预测.
科学领域:
- 地质科学 地质科学
- 水文地质学 水文地质学
- 岩石机械学 岩石机械学
背景情况:
- 废核燃料的深层地质储存库依赖于破碎的晶体岩石.
- 在这些构成中,流量和溶解物运输由自然断裂网络控制.
- 断裂异质性和可变的正常负荷 (例如,冰化) 显著影响水力机械 (HM) 过程.
研究的目的:
- 在单个自然断裂中分析和建模水力机械实验.
- 了解当地立方体法的适用性和正常负载对通道的影响.
- 改进各种地下应用的大规模离散断裂网络模型的参数化.
主要方法:
- 通过激光扫描获得了初始断裂孔径,并通过CFD建模定义了相当的初始孔径.
- 使用高分辨率接触模型模拟装载阶段的机械效应.
- 使用经过修改的雷诺兹方程运行了地下水流动模拟,使用计算的断裂孔径.
主要成果:
- 当地立方法,没有修正,大大高估了流量.
- 将液压孔口设置为机械孔口的1/5,可以合理地近似跨载荷周期的实验流量.
- 观察到流体流量导通与应用正常负载之间存在正相关性.
结论:
- 明确区分机械和液压孔径对于在破裂岩石中准确的流量建模至关重要.
- 这些发现增强了对自然断层中合的HM过程的理解,改善了核废物处理和其他地下应用的模型.
- 正常负载直接影响断裂内的道行为.
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