[Migration and Transformation of Adsorbed Arsenic Mediated by Sulfate Reducing Bacteria]. 2019

Qian-Qian Jia, and Wei Li, and Ya-Nan Wang, and Jin-Ming Duan, and Yu-Can Liu
School of Environmental and Municipal Engineering, Xi'an University of Architecture & Technology, Xi'an 710055, China.

In the natural environment, arsenic (As) is mainly adsorbed on iron oxide minerals. The release of adsorbed arsenic from iron oxide minerals to the water is the main source of arsenic pollution. Microbes play a crucial role for this process. The purpose of this study was to investigate the effect of the sulfate-reducing bacteria Desulfovibrio vulgaris DP4 on the transformation and mobilization of As. The experimental results show that the released As concentration of the two systems is 0 μmol·L-1 at 0 h. Compared with the control, DP4 promotes the desorption of As(Ⅴ) before the 84 h incubation process. The released As concentration reaches the maximum value of 12.6 μmol·L-1 at 13 h, accounting for~79% of the initial total adsorbed As (16 μmol·L-1). The maximum released As concentration is~8.4 times higher than that of the control (1.5 μmol·L-1). After 84 hours, the concentration of the released As in the DP4 system is lower than the abiotic control, which suggests that the released As is readsorbed on the solid surface. During the incubation process, the As mobility is significantly correlated with Eh. The XRD results show that the crystallinity of the solid samples in the DP4 system decreases by~50%. In general, a lower crystallinity of the adsorbent indicates a higher adsorption capacity. This may be one important reason for the As readsorption after 84 h. In addition, the SEM shows that goethite is agglomerated by DP4 and the EDS results indicate that goethite is partially transformed to an Fe-S mineral. Based on XANES, arsenic-sulfur minerals were not detected in the solid phase, which further confirms the SEM-EDS results, that is, that Fe-S minerals formed in the solid phase, rather than As2S3 (AsS). The released As was readsorbed on the secondary iron mineral, resulting in a lower dissolved As concentration in the DP4 system than in the abiotic control. Furthermore, 19% As(Ⅲ) was detected in the solid phase while dissolved As(Ⅲ) was not determined during the incubation process. The results suggest that sulfate-reducing bacteria may directly reduce adsorbed As(Ⅴ) to As(Ⅲ).

UI MeSH Term Description Entries
D007501 Iron A metallic element with atomic symbol Fe, atomic number 26, and atomic weight 55.85. It is an essential constituent of HEMOGLOBINS; CYTOCHROMES; and IRON-BINDING PROTEINS. It plays a role in cellular redox reactions and in the transport of OXYGEN. Iron-56,Iron 56
D010084 Oxidation-Reduction A chemical reaction in which an electron is transferred from one molecule to another. The electron-donating molecule is the reducing agent or reductant; the electron-accepting molecule is the oxidizing agent or oxidant. Reducing and oxidizing agents function as conjugate reductant-oxidant pairs or redox pairs (Lehninger, Principles of Biochemistry, 1982, p471). Redox,Oxidation Reduction
D003901 Desulfovibrio A genus of gram-negative, anaerobic, rod-shaped bacteria capable of reducing sulfur compounds to hydrogen sulfide. Organisms are isolated from anaerobic mud of fresh and salt water, animal intestines, manure, and feces.
D001151 Arsenic A shiny gray element with atomic symbol As, atomic number 33, and atomic weight 75. It occurs throughout the universe, mostly in the form of metallic arsenides. Most forms are toxic. According to the Fourth Annual Report on Carcinogens (NTP 85-002, 1985), arsenic and certain arsenic compounds have been listed as known carcinogens. (From Merck Index, 11th ed) Arsenic-75,Arsenic 75
D013431 Sulfates Inorganic salts of sulfuric acid. Sulfate,Sulfates, Inorganic,Inorganic Sulfates
D016999 Sulfur-Reducing Bacteria A group of gram-negative, anaerobic bacteria that is able to oxidize acetate completely to carbon dioxide using elemental sulfur as the electron acceptor. Sulfur Reducing Bacteria

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