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2011 - 2020年中国地下水状况:动态演变、影响因素与可持续发展

China's groundwater situation in 2011-2020: Dynamic evolution, Influencing Factors, and sustainable development.

作者信息

Du Huishi

机构信息

College of Geographic Science and Tourism, Jilin Normal University, Siping 136000, China.

出版信息

Heliyon. 2024 Jul 4;10(13):e34097. doi: 10.1016/j.heliyon.2024.e34097. eCollection 2024 Jul 15.

Abstract

Groundwater plays important roles in resource security and ecological maintenance and is sensitive to changes in the natural environment and human activities. It is of paramount importance to investigate the dynamic evolution trend of groundwater and its affecting factors and sustainable development. This paper takes mainland China as the study area, using data sourced from the , the , and the . The temporal and space-time evolution trend of groundwater depth in 2011-2020 is determined, along with the correlation between variations in groundwater resources and precipitation, the factors affecting these changes, and the sustainability of groundwater use. The results are as follows: (1) The northern and western regions of mainland China had a greater depth of groundwater compared to the southern and eastern regions. The largest groundwater depth is in the Northwest Rivers Basin (Nw RB), which can reach 17.61-21.10 m, and the shallowest groundwater depth is in the Southeast Rivers Basin (Se RB), only 1.61-5.19 m. (2) Regarding the factors affecting the changes in groundwater resources, precipitation, land use pattern, human activities, and industrial and agricultural water use are highlighted. (3) Overall, the percentage of groundwater in the total water supply has declined. The optimization of groundwater resource allocation and the adjustment of industrial structure have resulted in the coordinated utilization of groundwater resources. The research establishes a scientific foundation for ensuring national water security and promoting sustainable economic and social development.

摘要

地下水在资源安全和生态维护方面发挥着重要作用,并且对自然环境和人类活动的变化较为敏感。研究地下水的动态演变趋势及其影响因素以及可持续发展至关重要。本文以中国大陆为研究区域,使用来自[具体数据源1]、[具体数据源2]和[具体数据源3]的数据。确定了2011 - 2020年地下水水位的时空演变趋势,以及地下水资源变化与降水之间的相关性、影响这些变化的因素和地下水利用的可持续性。结果如下:(1)中国大陆的北部和西部地区地下水水位比南部和东部地区更深。最大地下水水位出现在西北河流域(Nw RB),可达17.61 - 21.10米,最浅的地下水水位在东南河流域(Se RB),仅为1.61 - 5.19米。(2)关于影响地下水资源变化的因素,降水、土地利用模式、人类活动以及工农业用水受到关注。(3)总体而言,地下水在总供水中的占比有所下降。地下水资源配置的优化和产业结构的调整实现了地下水资源的协调利用。该研究为保障国家水安全和促进经济社会可持续发展奠定了科学基础。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0419/11283028/26df18689bd8/gr1.jpg

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