通过多维分析,研究地下水和异构性对热水力机械合的影响
Zhenming Shi1, Junliang Li1, Yong Zhi Zhao1
1Department of Geotechnical Engineering, Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, State Key Laboratory for Disaster Reduction in Civil Engineering, Tongji University, Shanghai, China.
本研究分析了多层,横向同otropic 介质中的热-水力-机械 (THM) 合,考虑地下水.
科学领域:
- 地质技术工程 地质技术工程
- 连续力学 连续力学
- 水文地质学 水文地质学
背景情况:
- 热水力机械 (THM) 合在分层横向同otropic 介质中至关重要.
- 了解地下水对THM行为的影响对于地质技术应用至关重要.
研究的目的:
- 为了研究分层横向同位素介质的THM合行为.
- 分析地下水位和横向同位素参数对THM反应的影响.
主要方法:
- 使用转换微分方程方程 (TDQM) 进行分析.
- 建立了考虑到地下水的合管理方程.
- 应用积分变换方法来导出普通微分方程.
- 将边界和连续性条件集成到全球矩阵方程中.
主要成果:
- 这项研究成功地模拟了THM合在层叠的横向同位素介质中.
- 地下水位显著影响THM的行为.
- 横向同otropy参数在系统的响应中起着关键作用.
结论:
- TDQM是一种有效的方法来分析这些媒体中的THM合.
- 地下水和材料特性极大地影响了层次横向同otropic 构成的热水力学行为.
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