The symbiotic system of sulfate-reducing bacteria and clay-sized fraction of purplish soil strengthens cadmium fixation through iron-bearing minerals

文献类型： 外文期刊

第一作者： Li, Jie

作者： Li, Jie;Du, Hongxia;Ma, Ming;Rennenberg, Heinz;Zhao, Wancang;Guan, Yaobing

作者机构： Southwest Univ, Coll Resources & Environm, Ctr Mol Ecophysiol CMEP, Chongqing 400715, Peoples R China;Southwest Univ, Sch Geog Sci, Chongqing Key Lab Karst Environm, Chongqing 400715, Peoples R China;Ningxia Acad Agr & Forestry Sci, Guyuan Branch, Guyuan 756002, Peoples R China

关键词： Sulfate reducing bacteria; Purplish soil; Clay minerals; Fe-bearing minerals; Fixation of cadmium

期刊名称：SCIENCE OF THE TOTAL ENVIRONMENT （ 2021影响因子：10.753； 五年影响因子：10.237 ）

ISSN： 0048-9697

年卷期： 2022 年 820 卷

页码：

收录情况： SCI

摘要： The microbe-clay mineral system is widely known to reduce the fluidity of heavy metals through biomineralization, thus mitigating soil pollution stemming from heavy metals. Here, we investigated the effect of mineral distinction on the solidification of cadmium (Cd) using sulfate-reducing bacteria (SRB) to construct symbiotic systems with purplish soil, clay-sized fraction of purple soil (Clay(-csp)), clay particles of amorphous iron (Fe) oxide (Clay(-ox)), clay particles removing crystalline Fe oxide (Clay(-CBD)), and residues of Clay(-CBD) treated by hydrochloric acid (Clay(-HCl)). The difference in Cd morphology among purplish soil, Clay(-csp), and Clay(-ox) indicated that the fixation of Cd in soil was largely determined by Fe oxides. The content of Cd in Clay(-csp) decreased by 66.7% after the removal of amorphous Fe, confirming that clay easily adsorbed infinitive Fe oxides in purple soil. In the system of SRB and Clay(-ox), carbonate-bound Cd (F2) decreased by 14.85% and residual Cd (F5) increased by 14% fromthe retardation to late decline phase, eventually forming iron-sulfur (Fe-S) compounds. Based on the correlation analyses of Cd and Fe in amorphous-bound state and Fe-manganese (Mn) oxidation state in simulation experiments, it is demonstrated that Fe-Mn oxides control the behavior of Cd in soil clay, and SRB-mediated Fe-bearing minerals promote the transformation of Cd fromactivated to stable state.

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