Sulfate enhances the dissimilatory arsenate-respiring prokaryotes-mediated mobilization, reduction and release of insoluble arsenic and iron from the arsenic-rich sediments into groundwater.

Dissimilatory arsenate-respiring prokaryotes (DARPs) play key roles in the mobilization and release of arsenic from mineral phase into groundwater; however, little is known about how environmental factors influence these processes. This study aimed to explore the effects of sulfate on the dissolution and release of insoluble arsenic. We collected high-arsenic sediment samples from different depths in Jianghan Plain. Microcosm assays indicated that the microbial communities from the samples significantly catalyzed the dissolution, reduction and release of arsenic and iron from the sediments. Remarkably, when sulfate was added into the microcosms, the microorganisms-mediated release of arsenic and iron was significantly increased. To further explore the mechanism of this finding, we isolated a novel DARP, Citrobacter sp. JH001, from the samples. Arsenic release assays showed that JH001 can catalyze the dissolution, reduction and release of arsenic and iron from the sediments, and the presence of sulfate in the microcosms also caused a significant increase in the JH001-mediated dissolution and release of arsenic and iron. Quantitative PCR analysis for the functional gene abundances showed that sulfate significantly increased the arsenate-respiring reductase gene abundances in the microcosms. Thus, it can be concluded that sulfate significantly enhances the arsenate-respiring bacteria-mediated arsenic contamination in groundwater.