在灌农业地区使用地表地下水学建模估计地下水储存损失
Salam A Abbas1, Ryan T Bailey2, Jeremy T White3
1Department of Civil and Environmental Engineering, Colorado State University, Fort Collins, CO, 80521, USA. salam.a.abbas@colostate.edu.
Scientific reports
|March 12, 2025
概括
由于灌需求,密西西比河流平原的地下水位正在下降. 本研究量化了地下水储存和流量的长期变化,强调了需要当地管理解决方案的需要.
科学领域:
- 水文学 水文学
- 水文地质学 水文地质学
- 水资源管理 水资源管理
背景情况:
- 密西西比河流平原 (MAP) 的农业灌对地下水资源产生重大影响.
- 由于大量灌,在MAP中观察到长期地下水位下降.
研究的目的:
- 用水文模型量化MAP内地下水储存的长期变化.
- 在各种气候条件下分析地下水水位,充电和排放的趋势.
主要方法:
- 使用土壤和水资源评估工具 (SWAT+) 水文模型与gwflow模块.
- 模拟地下水储存和地表水的相互作用,以物理基础,空间分布的方式.
- 应用了线性定量回归来分析从1982年到2020年的潮湿,干燥和平均条件的趋势.
主要成果:
- 在所有条件下 (-18.0至-28.0毫米/年) 观察到地下水头部显著下降趋势.
- 干旱条件显示,充电 (-5.5毫米/年) 和地下水排放 (-5.5毫米/年) 显著下降.
- 平均条件表明充电量 (-6毫米/年) 和地下水排放量 (-9.3毫米/年) 的下降.
结论:
- 由于灌需求,MAP的地下水资源面临重大压力.
- 长期趋势表明地下水位和流量大幅下降.
- 在MAP中,地方管理策略对于可持续的地下水资源管理至关重要.
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