中国天山北坡昌吉绿洲地下水位动态特征及成因

Water Supply Pub Date : 2024-07-19 DOI:10.2166/ws.2024.165
Xin Hu, Wu Bin, Gao Fan, Mingliang Du
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引用次数: 0

摘要

地下水位动态反映了地下水补给和排泄之间的关系以及地下水资源的变化。为了有效地管理和保护地下水资源,有必要分析地下水水位的时空变化及其根本原因。研究结果表明,研究区域的地下水位有所下降,尤其是在灌溉区。具体而言,从 2000 年到 2020 年,地下水水深 50 米的区域增加了 167.38%。结果表明,研究区域的地下水位有所下降,尤其是在灌溉区。人类活动,如为扩大耕地面积而抽取地下水,是导致平原地区地下水位下降的主要因素。因此,根据研究结果,我们需要努力开发非传统水资源以缓解地下水资源匮乏的问题,进一步加强水资源监测和调控,大力发展节水措施和抗旱作物,提高公众节水意识,确保地下水资源的合理利用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characteristics and causes of groundwater level dynamics in the Changji oasis on the northern slopes of the Tianshan Mountains, China
Groundwater level dynamics reflect the relationship between groundwater recharge and discharge, and changes in groundwater resources. To effectively manage and protect groundwater resources, it is necessary to analyze spatial and temporal changes in groundwater levels and the underlying reasons. Results indicate that groundwater levels in the study area have declined, particularly in the irrigation area. Specifically, from 2000 to 2020, the area with groundwater levels <10 m deep decreased by 71.41%, the area with groundwater levels within the range of 10–50 m increased by 26.19%, and the area >50 m deep increased by 167.38%. Results indicate that groundwater levels in the study area have declined, particularly in the irrigation area. Human activities, such as groundwater extraction for cropland expansion, are the primary factors contributing to declining groundwater levels in the plains. Therefore, based on the research results, we need to make efforts to develop non-traditional water resources to alleviate the scarcity of groundwater resources, further strengthen water resources monitoring and regulation, vigorously develop water-saving measures and drought-resistant crops, raise public awareness of water conservation, to ensure the rational utilization of groundwater resources.
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