Effects of Sulfide Input on Arsenate Bioreduction and Its Reduction Product Formation in Sulfidic Groundwater

Int J Environ Res Public Health. 2022 Dec 17;19(24):16987. doi: 10.3390/ijerph192416987.

Abstract

Microbes have important impacts on the mobilization of arsenic in groundwater. To study the effects of sulfide on As(V) bioreduction in sulfidic groundwater, Citrobacter sp. JH012-1 isolated from sediments in the Jianghan Plain was used in a microcosm experiment. The results showed that sulfide significantly enhanced As(V) bioreduction as an additional electron donor. The reduction rates of As(V) were 21.8%, 34.5%, 73.6% and 85.9% under 0, 15, 75 and 150 µM sulfide inputting, respectively. The main products of As(V) bioreduction were thioarsenite and orpiment and the concentration of thioarsenite reached to 5.5 and 7.1 µM in the solution with the initial 75 and 150 µM sulfide, respectively. However, under 0 and 15 µM sulfide inputting, the dominant product was arsenite with no thioarsenite accumulation. The decrease in pH enhanced the bioreduction of As(V) and promoted the formation of thioarsenite and orpiment. In addition, the percentage of thioarsenite in total arsenic decreased with the decrease in the ratio of sulfur to arsenic, indicating that the formation of thioarsenite was limited by the concentration of initial sulfide. Therefore, the presence of sulfide had a significant effect on the transformation of arsenic in groundwater. This study provides new insights into the bioreduction of As(V) and the formation of thioarsenite in sulfidic groundwater.

Keywords: arsenic-reducing bacteria; groundwater; orpiment; sulfide; thioarsenite.

Publication types

  • Research Support, Non-U.S. Gov't

MeSH terms

  • Arsenamide
  • Arsenates
  • Arsenic* / metabolism
  • Groundwater*
  • Oxidation-Reduction
  • Sulfides

Substances

  • arsenic trisulfide
  • arsenic acid
  • Arsenates
  • Arsenic
  • Sulfides
  • Arsenamide

Grants and funding

This study was jointly supported by the National Natural Science Foundation of China (Grant Nos. 41572230 and 41172219), the Grant for Innovative Research Groups of the National Natural Science Foundation of China (41521001), and the Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) (122-G1323522145, CUG170103).