作为对水表抽水的反应,过渡性流量吸收和耗尽的半分析模型
Bwalya Malama1, Ying-Fan Lin2, Kristopher L Kuhlman3
1Natural Resources Management and Environmental Sciences, California Polytechnic State University, San Luis Obispo, CA, 93407, USA.
Ground water
|July 4, 2024
概括
新的模型考虑了地下水抽取过程中流水水平的变化,改善了流水枯竭预测. 这项研究通过考虑过渡性溪流的抽取来加强可持续的地下水管理.
科学领域:
- 水文学的水文学
- 水文地质学 水文地质学
- 环境科学 环境科学
背景情况:
- 现有的流耗尽模型经常假设一个固定的流阶段,这是不现实的.
- 现场观测证实,在溪流附近抽取地下水导致溪流阶段下降 (下降).
- 这种限制可能导致对水的可用性进行不准确的预测.
研究的目的:
- 开发流耗尽的分析和半分析模型,其中包括过渡流阶段吸收.
- 解决目前使用固定流阶段条件的模型中的缺陷.
- 为评估地下水抽水对地表水资源的影响提供更准确的工具.
主要方法:
- 开发了基于流通道质量保存和有限流通道存储的新模型.
- 经过验证的模型与实地数据对比,测量了含水层和溪流的吸收.
- 分析模型结果以估计水表水力参数,溪床导电率和溪流通道储存.
主要成果:
- 新的模型准确地预测了流量枯竭与短暂的流量减少.
- 在无限流道存储条件下,模型缩小到现有的固定阶段模型.
- 模型简化为局限的含水层流量,当流量储存是可以忽略的时,没有流量边界.
- 将模型应用于现场数据,以估计关键的水文地质参数.
结论:
- 短暂的流量阶段减排是流量耗尽建模中的一个关键因素.
- 开发的模型提供了一个更现实的方法来预测流耗尽.
- 这些发现对可持续的地下水管理和水资源分配有重大影响.
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