Evaluating the influencing factors of groundwater evolution in rapidly urbanizing areas using long-term evidence

IF 3 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Feng-jie Li , Yang Liu , Nusrat Nazir , Ramamoorthy Ayyamperumal
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Abstract

Groundwater ionic components evolution can simultaneously characterize the process of natural environment and anthropogenic activities on groundwater. In order to reveal the long-term evolution mechanism and influencing factors of urban groundwater in the context of rapid urbanization and industrialization. Studies carried out in Lanzhou, a region in Northwest China known for interconnection of anthropogenic activities and groundwater systems, sought to explore the mechanisms influencing the evolution of groundwater ionic components within the last 20 years. Hydrochemical analysis methods and integrated groundwater ion source analysis methods were utilized to isolate natural and anthropogenic factors in the evolution of groundwater ions, and subsequently combined with LULC to analyze the correlation between the type and intensity of land changes on groundwater ion components. The results show that, the ionic composition of groundwater was dominated by ion exchange and mineral weathering, river recharge, industrial activities, urban activities, and agricultural activities in 26%, 10%, 23%, 25%, and 16% of the sample sites respectively in 2002. However, in 2022, the proportion of sites dominated by these five categories is 20%, 18%, 12%, 40%, and 10%, respectively. Further combining the yearly trends in LULC, it is concluded that the decrease of cultivated land area and the significant increase of urban construction land in Lanzhou are closely related to the groundwater evolution process in Lanzhou in the past 20 years. Today's agricultural activities no longer dominate the ionic fraction of groundwater in Lanzhou, but increased population density and urban sewage discharge due to rapid and intensive urbanization are the main factors influencing the ionic fraction of groundwater.

利用长期证据评估快速城市化地区地下水演变的影响因素
地下水离子成分演变可同时表征自然环境和人类活动对地下水的影响过程。为了揭示快速城市化和工业化背景下城市地下水的长期演变机制和影响因素。在兰州(中国西北地区以人为活动与地下水系统相互关联而著称的地区)开展的研究试图探索近 20 年来地下水离子成分演变的影响机制。利用水化学分析方法和地下水离子源综合分析方法,分离出地下水离子演变过程中的自然因素和人为因素,并结合 LULC 分析了土地变化类型和强度对地下水离子组分的相关性。结果表明,2002 年,分别有 26%、10%、23%、25% 和 16%的样本点的地下水离子成分以离子交换和矿物风化、河流补给、工业活动、城市活动和农业活动为主。而到了 2022 年,以这五类活动为主的站点比例分别为 20%、18%、12%、40% 和 10%。结合土地利用、土地利用变化(LULC)的逐年变化趋势,可以得出结论:兰州耕地面积的减少和城市建设用地的大幅增加与兰州近 20 年的地下水演变过程密切相关。如今,农业活动已不再主导兰州地下水的离子组分,但人口密度的增加和快速密集的城市化带来的城市污水排放是影响地下水离子组分的主要因素。
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来源期刊
Physics and Chemistry of the Earth
Physics and Chemistry of the Earth 地学-地球科学综合
CiteScore
5.40
自引率
2.70%
发文量
176
审稿时长
31.6 weeks
期刊介绍: Physics and Chemistry of the Earth is an international interdisciplinary journal for the rapid publication of collections of refereed communications in separate thematic issues, either stemming from scientific meetings, or, especially compiled for the occasion. There is no restriction on the length of articles published in the journal. Physics and Chemistry of the Earth incorporates the separate Parts A, B and C which existed until the end of 2001. Please note: the Editors are unable to consider submissions that are not invited or linked to a thematic issue. Please do not submit unsolicited papers. The journal covers the following subject areas: -Solid Earth and Geodesy: (geology, geochemistry, tectonophysics, seismology, volcanology, palaeomagnetism and rock magnetism, electromagnetism and potential fields, marine and environmental geosciences as well as geodesy). -Hydrology, Oceans and Atmosphere: (hydrology and water resources research, engineering and management, oceanography and oceanic chemistry, shelf, sea, lake and river sciences, meteorology and atmospheric sciences incl. chemistry as well as climatology and glaciology). -Solar-Terrestrial and Planetary Science: (solar, heliospheric and solar-planetary sciences, geology, geophysics and atmospheric sciences of planets, satellites and small bodies as well as cosmochemistry and exobiology).
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