Groundwater flow and hydrogeochemical evolution in the Jianghan Plain, central China

Gan, Yiqun; Zhao, Ke; Deng, Yamin; Liang, Xing; Ma, Teng; Wang, Yanxin

Groundwater flow and hydrogeochemical evolution in the Jianghan Plain, central China | Flux d’eau souterraine et évolution hydrogéochimique dans la Plaine de Jianghan, Chine Centrale Flujo del agua subterránea y evolución hidrogeoquímica en la llanura de Jianghan, China central 江汉平原地下水径流和水文地球化学演化规律 Fluxo de águas subterrâneas e evolução hidrogeoquímica na planície de Jianghan, China central

2018

Hydrogeochemical analysis and multivariate statistics were applied to identify flow patterns and major processes controlling the hydrogeochemistry of groundwater in the Jianghan Plain, which is located in central Yangtze River Basin (central China) and characterized by intensive surface-water/groundwater interaction. Although HCO₃-Ca-(Mg) type water predominated in the study area, the 457 (21 surface water and 436 groundwater) samples were effectively classified into five clusters by hierarchical cluster analysis. The hydrochemical variations among these clusters were governed by three factors from factor analysis. Major components (e.g., Ca, Mg and HCO₃) in surface water and groundwater originated from carbonate and silicate weathering (factor 1). Redox conditions (factor 2) influenced the geogenic Fe and As contamination in shallow confined groundwater. Anthropogenic activities (factor 3) primarily caused high levels of Cl and SO₄ in surface water and phreatic groundwater. Furthermore, the factor score 1 of samples in the shallow confined aquifer gradually increased along the flow paths. This study demonstrates that enhanced information on hydrochemistry in complex groundwater flow systems, by multivariate statistical methods, improves the understanding of groundwater flow and hydrogeochemical evolution due to natural and anthropogenic impacts.

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