矩阵扩散控制 山丘斜坡地下水年龄和推断的储存动力学
Nicholas E Thiros1, Erica R Woodburn1, W Payton Gardner2
1Earth and Environmental Sciences Area, Lawrence Berkeley National Laboratory, Berkeley, California, USA.
Ground water
|March 29, 2025
概括
山区流域的地下水年龄是复杂的. 矩阵扩散对于准确建模年轻和旧的地下水混合物至关重要,特别是在基岩系统中,影响流域预测.
科学领域:
- 水文学的水文学
- 水文地质学 水文地质学
- 生物地质化学生物地质化学
背景情况:
- 地下水年龄分布为山区流域过程提供了关键的见解.
- 之前的研究表明,基岩流域中混合的年轻和旧的地下水,但潜在的机制仍然不清楚.
研究的目的:
- 通过使用集成的水文和粒子跟踪模型,模拟地下水在较低山坡上的年龄分布.
- 调查裂纹矩阵扩散在塑造地下水年龄分布中的作用.
- 将模型预测与观察到的环境跟踪数据 (3H和4He) 进行比较.
主要方法:
- 使用合的ParFlow-CLM集成水文和EcoSLIM粒子跟踪模型.
- 开发了一种基于卷积的方法,将断裂矩阵扩散纳入年龄分布.
- 进行蒙特卡洛分析以评估不确定矩阵和断裂参数.
主要成果:
- 矩阵扩散对于共同预测观察到的三 (3H) 和-4 (4He) 度至关重要.
- 仅靠偏向主导的模型无法复制观察到的年轻地下水和旧地下水的混合.
- 最适合的模型包括一个动态的基岩地下水库,在干旱期间储存损失很大.
结论:
- 断裂矩阵扩散对于理解基岩地下水中的环境跟踪数据至关重要.
- 动态的基岩地下水系统需要更深入地融入流域水生地化学模型.
- 准确地建模地下水的年龄,需要考虑向和矩阵扩散过程.
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