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基于源解析的影响地下水质量的人为因素和自然因素的季节性和空间变异性。

Seasonal and Spatial Variability of Anthropogenic and Natural Factors Influencing Groundwater Quality Based on Source Apportionment.

机构信息

College of Water Sciences, Beijing Normal University, Beijing 100875, China.

Engineering Research Center of Groundwater Pollution Control and Remediation, Ministry of Education, Beijing 100875, China.

出版信息

Int J Environ Res Public Health. 2018 Feb 6;15(2):279. doi: 10.3390/ijerph15020279.

Abstract

Globally, groundwater resources are being deteriorated by rapid social development. Thus, there is an urgent need to assess the combined impacts of natural and enhanced anthropogenic sources on groundwater chemistry. The aim of this study was to identify seasonal characteristics and spatial variations in anthropogenic and natural effects, to improve the understanding of major hydrogeochemical processes based on source apportionment. 34 groundwater points located in a riverside groundwater resource area in northeast China were sampled during the wet and dry seasons in 2015. Using principal component analysis and factor analysis, 4 principal components (PCs) were extracted from 16 groundwater parameters. Three of the PCs were water-rock interaction (PC₁), geogenic Fe and Mn (PC₂), and agricultural pollution (PC₃). A remarkable difference (PC₄) was organic pollution originating from negative anthropogenic effects during the wet season, and geogenic F enrichment during the dry season. Groundwater exploitation resulted in dramatic depression cone with higher hydraulic gradient around the water source area. It not only intensified dissolution of calcite, dolomite, gypsum, Fe, Mn and fluorine minerals, but also induced more surface water recharge for the water source area. The spatial distribution of the PCs also suggested the center of the study area was extremely vulnerable to contamination by Fe, Mn, COD, and F.

摘要

全球范围内,地下水资源正受到快速社会发展的破坏。因此,迫切需要评估自然和人为增强源对地下水化学的综合影响。本研究旨在识别人为和自然影响的季节性特征和空间变化,通过来源分配来提高对主要水文地球化学过程的理解。2015 年,在湿季和干季采集了位于中国东北河畔地下水资源区的 34 个地下水点。利用主成分分析和因子分析,从 16 个地下水参数中提取了 4 个主成分(PC)。其中三个 PC 为水岩相互作用(PC₁)、地球成因的 Fe 和 Mn(PC₂)和农业污染(PC₃)。在湿季,PC₄ 表现出显著差异,是源自负向人为影响的有机污染,而在干季则是地球成因 F 的富集。地下水开采导致了水源区周围水力梯度较高的明显沉降漏斗。这不仅加剧了方解石、白云石、石膏、Fe、Mn 和氟化物的溶解,还导致了更多的地表水补给水源区。PC 的空间分布也表明,研究区中心极易受到 Fe、Mn、COD 和 F 的污染。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4f7c/5858348/eaf2dfe90cff/ijerph-15-00279-g001.jpg

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