2011-2020年中国地下水状况:动态演变,影响因素和可持续发展
1College of Geographic Science and Tourism, Jilin Normal University, Siping 136000, China.
Heliyon
|July 29, 2024
概括
中国北部和西部的地下水位更深,受降水和人类活动的影响. 可持续管理对于国家水源安全和经济发展至关重要.
科学领域:
- 水文学的水文学
- 环境科学 环境科学
- 水资源管理 水资源管理
背景情况:
- 地下水对于生态平衡和资源安全至关重要,但对环境和人类影响敏感.
- 了解地下水的动态和影响因素对于可持续发展至关重要.
- 以前的研究已经强调了地下水的重要性,但缺乏对中国大陆的全面时空分析.
研究的目的:
- 分析2011-2020年中国大陆地下水深度的时空演变.
- 调查地下水变化,降水和其他影响因素之间的相关性.
- 评估地下水利用的可持续性及其对供水的贡献.
主要方法:
- 利用了来自地下水动态月度报告,中国水资源公报和省级水资源公报的数据.
- 分析了地下水深度的时间和时空演变趋势.
- 与降水,土地使用,人类活动和用水模式相关的地下水变化.
主要成果:
- 与中国南部和东部地区相比,中国北部和西部的地下水深度明显更大.
- 西北河流盆地表现出最深的地下水 (17.61-21.10米),而东南河流盆地则是最浅的 (1.61-5.19米).
- 降水,土地利用,人类活动和工业/农业用水被确定为影响地下水变化的关键因素.
结论:
- 在总供水中,地下水的总百分比下降了.
- 优化资源分配和工业调整导致了更协调的地下水利用.
- 该研究为确保国家水安全和促进可持续发展提供了科学基础.
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