Identifying the spatial pattern, driving factors and potential human health risks of nitrate and fluoride enriched groundwater of Ordos Basin, Northwest China

IF 10 1区 环境科学与生态学 Q1 ENGINEERING, ENVIRONMENTAL Journal of Cleaner Production Pub Date : 2022-11-20 DOI:10.1016/j.jclepro.2022.134289
Shen Qu , Limin Duan , Zheming Shi , Hairu Mao , Guangcai Wang , Tingxi Liu , Ruihong Yu , Xiaohong Peng
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引用次数: 10

Abstract

While the identification of the spatial patterns of fluoride (F) and nitrate (NO3) is important for groundwater management, these patterns remain poorly understood in the Ordos Basin. A total of 107 groundwater samples collected from phreatic aquifers were divided into three clusters using the self-organizing map (SOM). Cluster I, Cluster II and Cluster III represented the contaminated groundwater with different type and degree of pollution. On this basis, factor analysis (FA), together with classical hydrochemical diagrams reflected the major factors regulating the spatial characteristics of groundwater F and NO3. Firstly, water-rock interaction (carbonate precipitation, fluorite dissolution, and cation exchange) and evaporation were responsible for high groundwater NO3, F, hardness, and salinity. Secondly, anthropogenic inputs (agricultural activities and sewage) also contributed to high groundwater NO3 and F. Finally, the universal alkaline environment could regulate groundwater NO3 and F. Additionally, 68.22%, 37.38%, and 33.64% of samples showed higher total non-carcinogenic risk (HITotal > 1) for children, adult females, and adult males, respectively. Overall, the worst NO3 and F contamination and health risks were evident in the western part of the Ordos Basin. The results of this study can contribute to the sustainable development of groundwater and to the protection of public health in the Ordos Basin.

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鄂尔多斯盆地富硝、富氟地下水空间格局、驱动因素及潜在健康风险分析
虽然确定氟(F -)和硝态氮(NO3 -)的空间格局对地下水管理具有重要意义,但鄂尔多斯盆地对这些格局的了解仍然很少。利用自组织图(SOM)将107份地下含水层地下水样本划分为3个簇。聚类I、聚类II和聚类III分别代表不同类型和程度的污染地下水。在此基础上,因子分析(FA)结合经典水化学图反映了调节地下水F−和NO3−空间特征的主要因子。首先,水岩相互作用(碳酸盐沉淀、萤石溶解和阳离子交换)和蒸发是造成地下水NO3−、F−、硬度和盐度高的原因。其次,人为输入(农业活动和污水)也导致地下水NO3−和F−较高。最后,普遍碱性环境对地下水NO3−和F−具有调节作用。此外,68.22%、37.38%和33.64%的样本显示出较高的总非致癌风险(hittotal >1)分别为儿童、成年女性和成年男性。总体而言,鄂尔多斯盆地西部NO3−和F−污染和健康风险最严重。研究结果对鄂尔多斯盆地地下水资源的可持续发展和公众健康的保护具有重要意义。
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来源期刊
Journal of Cleaner Production
Journal of Cleaner Production 环境科学-工程:环境
CiteScore
20.40
自引率
9.00%
发文量
4720
审稿时长
111 days
期刊介绍: The Journal of Cleaner Production is an international, transdisciplinary journal that addresses and discusses theoretical and practical Cleaner Production, Environmental, and Sustainability issues. It aims to help societies become more sustainable by focusing on the concept of 'Cleaner Production', which aims at preventing waste production and increasing efficiencies in energy, water, resources, and human capital use. The journal serves as a platform for corporations, governments, education institutions, regions, and societies to engage in discussions and research related to Cleaner Production, environmental, and sustainability practices.
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