Zhang Yaxian, Li Hua, Gong Libo, Dong Guowen, Shen Liang, Wang Yuanpeng, Li Qingbiao
Department of Chemical and Biochemical Engineering, College of Chemistry and Chemical Engineering, Xiamen University, Xiamen 361005, China.
Department of Chemical and Biochemical Engineering, College of Chemistry and Chemical Engineering, Xiamen University, Xiamen 361005, China.
J Environ Sci (China). 2017 Jul;57:329-337. doi: 10.1016/j.jes.2017.01.007. Epub 2017 Feb 5.
The purpose of this study is to investigate the effects of nano-sized or submicro FeO/FeO on the bioreduction of hexavalent chromium (Cr(VI)) and to evaluate the effects of nano-sized FeO/FeO on the microbial communities from the anaerobic flooding soil. The results indicated that the net decreases upon Cr(VI) concentration from biotic soil samples amended with nano-sized FeO (317.1±2.1mg/L) and FeO (324.0±22.2mg/L) within 21days, which were approximately 2-fold of Cr(VI) concentration released from blank control assays (117.1±5.6mg/L). Furthermore, the results of denaturing gradient gel electrophoresis (DGGE) and high-throughput sequencing indicated a greater variety of microbes within the microbial community in amendments with nano-sized FeO/FeO than the control assays. Especially, Proteobacteria occupied a predominant status on the phylum level within the indigenous microbial communities from chromium-contaminated soils. Besides, some partial decrease of soluble Cr(VI) in abiotic nano-sized FeO/FeO amendments was responsible for the adsorption of nano-sized FeO/FeO to soluble Cr(VI). Hence, the presence of nano-sized FeO/FeO could largely facilitate the mobilization and biotransformation of Cr(VI) from flooding soils by adsorption and bio-mediated processes.
本研究的目的是调查纳米级或亚微米级FeO/FeO对六价铬(Cr(VI))生物还原的影响,并评估纳米级FeO/FeO对厌氧淹水土壤微生物群落的影响。结果表明,在21天内,添加纳米级FeO(317.1±2.1mg/L)和FeO(324.0±22.2mg/L)的生物土壤样品中Cr(VI)浓度的净下降,约为空白对照试验中释放的Cr(VI)浓度(117.1±5.6mg/L)的2倍。此外,变性梯度凝胶电泳(DGGE)和高通量测序结果表明,与对照试验相比,添加纳米级FeO/FeO的微生物群落中微生物种类更多。特别是,变形菌门在受铬污染土壤的原生微生物群落的门水平上占据主导地位。此外,非生物纳米级FeO/FeO添加剂中可溶性Cr(VI)的部分下降是由于纳米级FeO/FeO对可溶性Cr(VI)的吸附。因此,纳米级FeO/FeO的存在可以通过吸附和生物介导过程极大地促进淹水土壤中Cr(VI)的迁移和生物转化。