College of Geology and Environment, Xi'an University of Science and Technology, Xi'an, China.
Environ Sci Pollut Res Int. 2020 Jun;27(17):22046-22064. doi: 10.1007/s11356-020-08645-z. Epub 2020 Apr 14.
Groundwater depletion becomes a prominent issue due to the fast-growing water demand in semiarid and arid regions, which poses serious hydrogeological problems and restrains regional sustainable development. Groundwater dynamic response mechanism analysis and quantity vulnerability assessment are useful methods for groundwater protection and management. This paper analyzed the spatial and temporal variation of groundwater level in Xi'an, and studied the response characteristic of groundwater dynamic to its driving forces in different periods under the influence of human activities. Considering both hydrological settings and human disturbances, a modified evaluation system based on fuzzy comprehensive evaluation method and DRYTECL model was proposed to assess groundwater quantity vulnerability. In order to make the results more reasonable and in line with actual situation of the study area, a weighting system that builds on subjective and objective weights was put forward as well. The results show that groundwater level sharply dropped in the last few decades, and the spatial autocorrelation of groundwater level has gotten weaker, suggesting that the contribution of natural factors to groundwater-level variation decreased. Land use, exploitation, and other human activities had a great influence on groundwater dynamic by changing the discharge and recharge condition of groundwater, and the response characteristic of groundwater level to precipitation, runoff, and exploitation varied with time and hydrogeological conditions. Groundwater quantity vulnerability map showed 63.8% of the study area fell within moderate-to-high quantity risk, which indicated that groundwater depletion mainly occurred in highly urbanized areas. The single-parameter sensitivity analysis showed that the exploitation is the most sensitive factor to groundwater quantity vulnerability, the real effects of land use on groundwater quantity risk are greater than its theoretical effects, and net recharge is important to groundwater recovery.
由于半干旱和干旱地区对水的需求快速增长,地下水枯竭成为一个突出问题,这给地下水带来了严重的水文地质问题,并制约了区域的可持续发展。地下水动态响应机制分析和数量脆弱性评估是保护和管理地下水的有用方法。本文分析了西安地区地下水位的时空变化,研究了人类活动影响下不同时期地下水动态对驱动力的响应特征。考虑到水文条件和人为干扰,提出了一种基于模糊综合评价法和 DRYTECL 模型的改进评价体系,对地下水数量脆弱性进行评估。为了使结果更加合理,符合研究区的实际情况,提出了一种基于主客观权重的权重体系。结果表明,近几十年来,地下水位急剧下降,地下水位的空间自相关减弱,表明自然因素对地下水位变化的贡献减小。土地利用、开采等人类活动通过改变地下水的排泄和补给条件,对地下水动态产生了很大的影响,地下水位对降水、径流量和开采量的响应特征随时间和水文地质条件而变化。地下水数量脆弱性图显示,研究区 63.8%的地区处于中高强度数量风险,这表明地下水枯竭主要发生在高度城市化地区。单参数敏感性分析表明,开采是对地下水数量脆弱性最敏感的因素,土地利用对地下水数量风险的实际影响大于其理论影响,净补给对地下水恢复很重要。