在微尺度上对地基质和相邻管道之间的水交换进行数值模拟
Jiao Li1, Douqiang Yang1, Guanping An1
1School of Environmental Science and Engineering, Southwest Jiaotong University, Chengdu, 611756, Sichuan, China.
Scientific reports
|March 6, 2025
概括
在地系统中微量级的水交换是使用合数值模型来澄清的. 矩阵异质性显著影响管道和多孔介质之间的水流.
科学领域:
- 水文地质学 水文地质学
- 地质科学 地质科学
- 环境科学 环境科学
背景情况:
- 在微尺度上的石水媒介中的水交换是不太了解的.
- 岩系统表现出复杂的多层次的水流动力学.
研究的目的:
- 为了研究岩管道和周围矩阵之间的微量水交换.
- 量化矩阵异质性对水交换动态的影响.
主要方法:
- 应用斯托克斯 - 布林克曼方程对配对矩阵透和导管流量.
- 使用数字核心技术来描述矩阵微异质性和液压性能.
- 开发一个微尺度数值模型,用于矩阵-管道交换水.
主要成果:
- 在不同的矩阵样本中观察到液压性能的显著变化.
- 流速和压力梯度的可视化显示了水交换接口的特征.
- 在交换流量和管道入口速度之间发现了线性正相关性,由液压头差异驱动.
- 与同质模型相比,微异质矩阵结构对水交换有显著的影响.
结论:
- 卡斯特矩阵的异质性是影响微尺度水交换的关键因素.
- 开发的模型为石水动态提供了新的视角.
- 这些发现为预测和管理石水资源提供了宝贵的见解.
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