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−.

Highlights

  • Groundwater is indispensable for human survival and sustaining societal development

  • The results showed four anthropogenic and natural factors affecting the groundwater chemistry during the wet and dry seasons in the Hulan area

  • The geogenic Fe and Mn contamination were primarily influenced by agricultural activities during the wet season, and derived from infiltration of anthropogenic sources for their spatial distribution during the dry season

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Summary

Introduction

Groundwater is indispensable for human survival and sustaining societal development. It is a ubiquitous source of water for domestic, agricultural, and industrial purposes. During the past few decades, climate change has gradually exacerbated the pressure on the hydrologic system and induced potential risks for drinking water safety, in semi-arid and arid regions with considerable seasonal groundwater recharge and discharge [4,5]. There is an urgent need to quantify potential pollution sources and evaluate hydrogeochemical processes affecting groundwater quality for its sustainable application [6]. Natural climate change and seasonal variation dynamically impact groundwater recharge, runoff, and discharge conditions.

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