[Distributions and Driving Factors of Hydrochemical Compositions in Different Types of Karst Groundwater in Qingjiang River Basin].

Q2 Environmental Science
Hao Xie, Hao-Yong Shen, Hai-Dao Zhang, Yong-Sheng Lin, Jun Li, Hui-Ya Liang, Zhi-Heng Wang, Tian-Long Zhu, Sheng-Zhang Zou
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引用次数: 0

Abstract

The karst groundwater resource is the key water supply for native residents and industrial and agricultural production in karst regions of southwest China and is even the only water supply for rural regions. Understanding the formation mechanism of hydrochemical compositions is practically imperative to the sustainable development and utilization of karst groundwater resources. The hydrochemical ions of 34 karst spring samples and 12 underground river water samples from the Qingjiang River Basin were measured and analyzed in this study. On the basis of investigating the distribution characteristics of hydrochemical components, methods such as hierarchical clustering analysis, Gibbs model, and relationships between hydrochemical components were used to comprehensively reveal the chemical genesis mechanism of karst groundwater from the perspectives of water-rock interaction and anthropogenic activities, especially in the disturbance mechanism of acidic pollutants on the natural dissolution of carbonate rocks. The results showed that the karst groundwater in the Qingjiang River Basin was weakly alkaline (7.12 ≤pH ≤ 8.69), and the overall water quality was good. Only the maximum concentration of NO3- in the karst spring (80.2 mg·L-1) exceeded the maximum acceptable limit for drinking purposes (10 mg·L-1 as N). The Ca2+ and HCO3- were identified as the dominant ions, associated with the main water phrase of HCO3-Ca·Mg in approximately 97.1% of karst spring samples and all underground river water samples. The dominant ions were derived from the strong dissolution of calcite, whereas Mg2+、SO42-, and F- were controlled by the weak dissolution of dolomite, gypsum, and fluorite, respectively. Karst groundwater NO3- was derived from the agricultural fertilizers and rainwater input, whereas the H2SO4 acid rain input was identified as another important source of karst groundwater SO42-. In addition, the carbonate rocks in the study area were mainly naturally dissolved; however, the input of exogenous acid by humans has changed the original karst hydrogeochemical evolution process and further decreased the carbonate sink flux of karst aquifers, accelerated the decrease rate of karst groundwater table, and increased the pollution risks of karst groundwater.

[清江流域不同类型岩溶地下水水化学成分分布及驱动因素分析]。
岩溶地下水资源是西南岩溶地区居民生活和工农业生产的关键水源,甚至是农村地区的唯一水源。了解水化学成分的形成机制对岩溶地下水资源的可持续开发利用具有重要的现实意义。对清江流域34个岩溶泉样和12个地下河样的水化学离子进行了测定和分析。在研究水化学成分分布特征的基础上,运用层次聚类分析、Gibbs模型、水化学成分间关系等方法,从水岩相互作用和人为活动的角度,特别是酸性污染物对碳酸盐岩自然溶蚀的干扰机制,全面揭示岩溶地下水的化学成因机制。结果表明:清江流域岩溶地下水呈弱碱性(7.12≤pH≤8.69),水质总体较好;仅喀斯特泉水中NO3-的最大浓度(80.2 mg·L-1)超过了饮用水可接受的最大限度(10 mg·L-1作为N)。在97.1%的岩溶泉样和所有地下河水样中,Ca2+和HCO3-为优势离子,与HCO3- ca·Mg主水相相关联。优势离子来源于方解石的强溶蚀作用,而Mg2+、SO42-和F-分别受白云石、石膏和萤石的弱溶蚀作用控制。岩溶地下水NO3-主要来源于农业肥料和雨水输入,而H2SO4酸雨输入是岩溶地下水SO42-的另一个重要来源。此外,研究区碳酸盐岩以自然溶解为主,但人类外源酸的输入改变了原有的岩溶水文地球化学演化过程,进一步降低了岩溶含水层的碳酸盐汇通量,加快了岩溶地下水位的下降速度,增加了岩溶地下水的污染风险。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
环境科学
环境科学 Environmental Science-Environmental Science (all)
CiteScore
4.40
自引率
0.00%
发文量
15329
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