地表水-灌回流主导着地下水补充,地下水年龄和酸盐动态在流盆地含水层
Mariachiara Caschetto1, Elisa Sacchi2, Daniele L Pinti3
1Department of Earth and Environmental Sciences, University of Milano-Bicocca, Italy.
Water research
|June 26, 2025
概括
地表水灌大大补充了含水层,并影响了地下水的年龄和酸盐水平. 密集的灌稀释了酸盐,而较少的密集灌可以增加由于土壤浸.
科学领域:
- 水文地质学 水文地质学
- 环境科学 环境科学
- 农业科学 农业科学
背景情况:
- 地表水灌对农业至关重要,但影响地下水补充和污染物运输.
- 灌回流在含水层动态和酸盐污染中的确切作用尚不清楚.
- 了解这些过程对于灌地区的可持续水资源管理至关重要.
研究的目的:
- 调查地表水灌回流对地下水补充,流量和酸盐污染的影响.
- 量化灌回流对意大利波平原地下水层补充的贡献.
- 分析灌方式对地下水表面年龄和酸盐度的影响.
主要方法:
- 用于地下水充电 (稳定同位素,Cl/Br比) 和年龄测定 (CFC,SF6,3H-3He,贵气) 的标志物.
- 从64点监测网络中分析了长期平均酸盐度.
- 与灌强度相关联的水文地质数据,以评估对地下水的影响.
主要成果:
- 地表水灌回流是波平原灌区的主导充电源 (中位数为64.4%).
- 密集灌使地下水年龄恢复,并通过混合年轻水来改变流动路径.
- 地下水中酸盐度最初随着灌而增加,但由于稀释和冲洗,在密集的实践下下降.
结论:
- 地表水灌返回流量显著控制地下水的补充,年龄和酸盐动态.
- 稀释和冲洗等水文地质过程是地下水中酸盐水平的短期关键驱动因素.
- 研究结果为全球类似灌地区的水资源管理提供了宝贵的参考.
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