OCCURRENCES AT MINERAL BACTERIA INTERFACE DURING OXIDATION OF ARSENOPYRITE BY THIOBACILLUS-FERROOXIDANS

被引:53
作者
FERNANDEZ, MGM
MUSTIN, C
DEDONATO, P
BARRES, O
MARION, P
BERTHELIN, J
机构
[1] UNIV HENRI POINCARE NANCY 1,CTR PEDOL BIOL,CNRS,UPR 6831,VANDOEUVRE NANCY,FRANCE
[2] ENSG,INPL,ENVIRONNEMENT & MINERAL LAB,CNRS,URA 235,VANDOEUVRE NANCY,FRANCE
关键词
ARSENOPYRITE; THIOBACILLUS FERROOXIDANS; ADHERING BACTERIA; SURFACE-OXIDIZED PHASES; FERRIC ARSENATE; SULFUR;
D O I
10.1002/bit.260460103
中图分类号
Q81 [生物工程学(生物技术)]; Q93 [微生物学];
学科分类号
071005 ; 0836 ; 090102 ; 100705 ;
摘要
The combination of an improved bacterial desorption method, scanning electron microscopy (SEM), diffuse reflectance and transmission infrared Fourier transform spectroscopy, and a desorption-leaching device like high-pressure liquid chromatography (HPLC) was used to analyze bacterial populations (adhering and free bacteria) and surface-oxidized phases (ferric arsenates and elemental sulfur) during the arsenopyrite biooxidation by Thiobacillus ferrooxidans. The bacterial distribution, the physicochemical composition of the leachate, the evolution of corrosion patterns, and the nature and amount of the surface-oxidized chemical species characterized different behavior for each step of arsenopyrite bioleaching. The first step is characterized by a slow but strong adhesion of bacteria to mineral surfaces, the appearance of a surface phase of elemental sulfur, the weak solubilization of Fe(ll), As(III), and As(V), and the presence of the first corrosion patterns, which follow the fragility zones and the crystallographic orientation of mineral grains. After this short step, growth of the unattached bacteria begins, while ferrous ions in solution are oxidized by them. Ferric ions produced by the bacteria can oxidize the sulfide directly and are regenerated by Fe(ll) bacterial oxidation. At this time, a bioleaching cycle takes place and a coarse surface phase of ferric arsenate (FeAsO(4)xH(2)O where x approximate to 2) and deep ovoid pores appear. At the end of the bioleaching cycle, the high concentration of fe(lll) and As(V) in solution promotes the precipitation of a second phase of amorphous ferric arsenate (FeAsO4.xH(2)O where x approximate to 4) in the leachate. Then the biooxidation process ceases: The bacteria adhering to the mineral surfaces are coated by the ferric arsenates and the concentration of Fe(lll) on the leachate is found to have decreased greatly. Both oxidation mechanisms (direct and indirect oxidation) have been stopped. (C) 1995 John Wiley and Sons, Inc.
引用
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页码:13 / 21
页数:9
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