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Updated: Jun 25, 2025

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在使用非参数统计测试的旁遮普州西南部长期季节性地下水位的时空趋势
Arvind Dhaloiya1, Jagdish Prasad Singh2, Anurag Malik3
1Department of Soil and Water Engineering, Punjab Agricultural University, Ludhiana, 141004, India. arvind-swe@pau.edu.
概括
旁遮普西南部的地下水位显示出显著的长期趋势. 虽然北部地区的地下水位下降,但南部地区的地下水位由于农业实践和地下水质量而上升.
科学领域:
- 水文学的水文学
- 环境科学 环境科学
- 地理空间分析的研究.
背景情况:
- 有效地管理地下水资源需要了解长期的地下水位 (GWL) 波动.
- 近几十年来,旁遮普西南部经历了大量的GWL变化.
研究的目的:
- 分析1973-2020年GWL的长期时空变化和趋势.
- 为了确定GWL在Punjab西南部变化的区域模式.
主要方法:
- 使用地理信息系统 (GIS) 进行空间分析.
- 使用的非参数统计测试:曼-肯德尔 (MK),Sens的斜率估计器 (SSE) 和创新趋势分析 (ITA).
- 分析了137个观测井的数据,考虑了季风前后的时间.
主要成果:
- 在季风季节前后都观察到显著的GWL趋势.
- MK和SSE测试显示,大约66%的水井在季风前和67%的季风后呈现上升趋势.
- 伊塔证实了约63.5% (季风前) 和65.7% (季风后) 井的增长趋势.
- 在研究区域的北部地区,GWL正在下降,但在研究区域的南部地区,GWL正在上升.
结论:
- 该研究强调了GWL趋势在旁遮普邦西南部的时空差异.
- 南方GWL的上升与农业活动和由于土壤盐度和水而减少的地下水利用有关.
- 结果为区域地下水管理和行动规划提供了关键的见解.
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