Sources and enrichment processes of groundwater arsenite and arsenate in fissured bedrock aquifers in the Xunhua-Hualong basin, China

Although high arsenic (As) groundwater has been widely observed in sedimentary aquifers, arsenite (As(III)) and arsenate (As(V)) mobilization in fissured bedrock aquifers are less documented, and different mobilization be-haviors of As(III) and As(V) in groundwater from those aquifers are little known. Thus, geochemical and isotopic characteristics of high As groundwater in fissured bedrock aquifers in the Xunhua-Hualong basin were investi-gated. Results showed that fissured bedrock aquifer hosted high As groundwater. Total As concentrations in spring waters were up to 628 & mu;g/L being dominated by As(V) with high ORP values (from 87.2 to 212 mV). As (III) dominated dissolved As in deep groundwater (up to 22.5 & mu;g/L) with low ORP values (-217 and-288 mV). The positive correlation between As concentration and & delta;18O in spring water revealed that oxidation of As-bearing pyritic minerals in the fissured bedrock aquifers released As into groundwater. In deep groundwater under anoxic conditions recharged by shallow aquifers, high As groundwater usually had high concentrations of dissolved Fe, suggesting that reductive dissolution of Fe (oxyhydr)oxide minerals mobilized As into groundwater. Elevated concentrations of PO43-in high As spring water and deep groundwater indicated the competition adsorption between PO43-and As(V) (and As(III)). Insignificant correlations were observed between As(V) and pH, HCO3-, and Na+/Ca2+ in spring water, revealing that desorption induced by pH and HCO3- and cation exchange between Ca2+ and Na + had negligible effects on As(V) mobilization. However, alkaline pH caused the desorption of As (III), and the presence of HCO3- was conducive to As(III) desorption in deep groundwater. A conceptual model was established to explain As distribution in fissured bedrock aquifers, emphasizing contributions of mineral dissolution, desorption, and hydrogeological conditions to As mobilization. This paper highlights different mobilization behaviors of As(III) and As(V) in groundwater from fissured bedrock aquifers, requiring the different strategies to ensure the safety of drinking water in those areas.

Automated summary

This study investigated the geochemical and isotopic characteristics of high arsenic (As) groundwater in fissured bedrock aquifers in the Xunhua-Hualong basin. The results showed that the high As groundwater in the aquifers was dominated by As(III) and As(V), and their mobilization was influenced by the oxidation of As-bearing pyritic minerals and the reductive dissolution of iron (oxyhydr)oxide minerals. The migration of As in the fissured bedrock aquifers was controlled by mineral dissolution, desorption, and hydrogeological conditions.