Desorption behavior of U(VI) from kaolinite and hematite by Shewanella putrefaciens cells and extracellular polymeric substances

被引:2
作者
Huang, Feng-Yu [1 ]
Zhang, Hai-Ling [2 ]
Feng, Su [3 ]
Ding, Huan-Huan [2 ]
Cheng, Meng-Xi [2 ]
Liu, Wei-Dong [2 ]
Yi, Fa-Cheng [1 ]
Wang, Zhe [1 ]
Wang, Yong-Peng [2 ]
Huang, He-Xiang [2 ]
机构
[1] Southwest Univ Sci & Technol, Coll Environm & Resources, Mianyang 621010, Sichuan, Peoples R China
[2] China Acad Engn Phys, Inst Mat, Jiangyou 621907, Sichuan, Peoples R China
[3] Sichuan Univ, Coll Life Sci, Minist Educ, Key Lab Bioresources & Ecoenvironm, Chengdu 610065, Sichuan, Peoples R China
基金
国家重点研发计划; 中国国家自然科学基金;
关键词
Uranium (U); Desorption; Minerals; Shewanella putrefaciens; Extracellular polymeric substances (EPS); BACILLUS-SUBTILIS; AQUEOUS-SOLUTION; HEAVY-METALS; URANIUM VI; ATR-FTIR; ADSORPTION; BACTERIA; KINETICS; SORPTION; MINERALS;
D O I
10.1007/s10967-021-07919-1
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
The desorption of U(VI) from minerals by microorganisms and their extracellular polymeric substances (EPS) was characterized with Shewanella putrefaciens (S. putrefaciens) as a typical bacterial strain, while kaolinite and alpha-Fe2O3 as typical minerals. Based on the results, EPS contributed significantly to U(VI) desorption from minerals. Two kinds of mechanisms should be mainly involved in U(VI) desorption, including the competition for the adsorption sites of minerals between U(VI) and bacterial cells or EPS, and the formation of stable U(VI)-bacterial cells or U(VI)-EPS complexes. Desorption kinetics indicated that the desorption process of U(VI) on minerals was a complex heterogeneous diffusion and chemical desorption process.
引用
收藏
页码:1555 / 1569
页数:15
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