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利用新型综合权重水质指数(IWQI)和驱动力分析对交口灌区地下水质量进行评估。

Groundwater quality assessment using a new integrated-weight water quality index (IWQI) and driver analysis in the Jiaokou Irrigation District, China.

机构信息

School of Water and Environment, Chang'an University, Xi'an 710054, Shaanxi, China; Key Laboratory of Subsurface Hydrology and Ecological Effects in Arid Region of the Ministry of Education, Chang'an University, Xi'an 710054, Shaanxi, China.

School of Water and Environment, Chang'an University, Xi'an 710054, Shaanxi, China; Key Laboratory of Subsurface Hydrology and Ecological Effects in Arid Region of the Ministry of Education, Chang'an University, Xi'an 710054, Shaanxi, China.

出版信息

Ecotoxicol Environ Saf. 2021 Apr 1;212:111992. doi: 10.1016/j.ecoenv.2021.111992. Epub 2021 Jan 30.

Abstract

Groundwater is an important water resource in arid and semi-arid regions. The impact of human activities on groundwater is increasing. After 60 years running, the groundwater quality and its formation mechanism are imperative questions needed to be answered in Jiaokou Irrigation District, Guanzhong Basin, China. In this study, the quality of groundwater in Jiaokou Irrigation District was assessed by a new integrated-weight water quality index (IWQI), and the groundwater chemistry is studied through integrated statistical, geostatistical and hydrogeochemical approaches. The patterns for the average anion and cation concentrations were HCO > SO > Cl > NO > CO > NO, and Na > Mg Ca > K > NH, respectively. Statistics showed that the major water chemistry types were HCONa, SO·Cl-Na, and Cl·SO-Na. A new integrated-weight water quality index (IWQI) was proposed based on the entropy-weighted method and CRITIC method and showed excellent performance for explaining and evaluating the groundwater quality. The IWQI results show 65.33% of groundwater, mainly distributed in the central and western parts of this study area, was unsuitable for drinking. Furthermore, SO, HCO, Cl, NO, and Na had more important effects on groundwater quality. The weathering process affecting groundwater quality in the study area is carbonate dissolution, followed by silicate weathering and evaporite dissolution, whereas the major geochemical processes include the dissolution and precipitation of calcite, as well as the dissolution of dolomite and gypsum (anhydrite). Cation exchange also plays an important role in the hydrogeochemical evolution of groundwater with a long residence time. Anthropogenic activities affecting groundwater quality included long-term irrigation infiltration and excessive use of fertilizers. The findings and the results of the study can improve understanding of the processes driving groundwater chemistry in Jiaokou Irrigation District, and can be used for reference to other similar regions in the world.

摘要

地下水是干旱半干旱地区的重要水资源。人类活动对地下水的影响日益增加。在中国关中盆地交口灌区,经过 60 年的运行,地下水水质及其形成机制是亟待回答的问题。本研究采用新的综合权重水质指数(IWQI)评价交口灌区地下水水质,并采用综合统计、地质统计学和水化学方法研究地下水化学。平均阴离子和阳离子浓度的模式分别为 HCO > SO > Cl > NO > CO > NO 和 Na > Mg > Ca > K > NH。统计结果表明,主要水化学类型为 HCONa、SO·Cl-Na 和 Cl·SO-Na。基于熵权法和 CRITIC 法提出了一种新的综合权重水质指数(IWQI),该指数在解释和评价地下水水质方面表现出优异的性能。IWQI 结果表明,65.33%的地下水,主要分布在研究区的中西部地区,不适合饮用。此外,SO、HCO、Cl、NO 和 Na 对地下水质量的影响更大。影响研究区地下水质量的风化过程是碳酸盐溶解,其次是硅酸盐风化和蒸发盐溶解,而主要的地球化学过程包括方解石的溶解和沉淀,以及白云石和石膏(硬石膏)的溶解。阳离子交换在具有长停留时间的地下水水化学演化中也起着重要作用。影响地下水水质的人为活动包括长期灌溉入渗和过度施肥。本研究的发现和结果可以提高对交口灌区地下水化学驱动过程的认识,并为世界其他类似地区提供参考。

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