Anaerobic Fe(II)-Oxidizing Bacteria Show As Resistance and Immobilize As during Fe(III) Mineral Precipitation

被引:194
作者
Hohmann, Claudia [1 ]
Winkler, Eva [1 ]
Morin, Guillaume [2 ]
Kappler, Andreas [1 ]
机构
[1] Univ Tubingen, Ctr Appl Geosci, Tubingen, Germany
[2] Univ Paris 06, CNRS, UMR 7590, Inst Mineral & Phys Milieux Condenses, F-75015 Paris, France
关键词
FERROUS IRON; SURFACE-CHEMISTRY; REDUCING BACTERIA; ARSENIC RELEASE; WATER INTERFACE; STRAIN ANA-3; WEST-BENGAL; FERRIHYDRITE; REDUCTION; OXIDE;
D O I
10.1021/es900708s
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
More than 100 million individuals worldwide are exposed to arsenic-contaminated water, making the investigation of arsenic mobility in aquatic systems of utmost importance. Iron (hydr)oxides play a key role in preventing arsenic release in aquifers and soils due to their strong arsenic sorption and are even used to remove arsenic in water treatment Neutrophilic Fe(II)-oxidizing bacteria produce Fe(III) minerals and therefore have the potential to affect arsenic mobility. In the present study, we demonstrate that the metabolism of anaerobic nitrate-reducing and phototrophic Fe(II)-oxidizing bacteria is not significantly affected by arsenate concentrations of up to 500 mu M (37.5 mg/L). Even in the presence of the more toxic arsenic species, arsenite, cell metabolism was significantly impaired only at the highest arsenite concentration (500 mu M) for one of the Fe(II)-oxidizers. All Fe(II)-oxidizing bacteria tested effectively immobilized arsenic during Fe(II) oxidation (>96%), lowering the remaining dissolved arsenic concentrations to values close to or even lower than the current drinking water limit of 10 mu g/L Since the minerals formed by these bacteria included highly crystalline Fe(III) minerals that are hardly reducible by Fe(III)-reducing bacteria, stimulation of arsenic immobilization by Fe(II)-oxidizing bacteria can potentially support water treatment systems or even be applied as an effective remediation strategy.
引用
收藏
页码:94 / 101
页数:8
相关论文
共 45 条
[11]   SURFACE-CHEMISTRY OF FERRIHYDRITE .2. KINETICS OF ARSENATE ADSORPTION AND COPRECIPITATION [J].
FULLER, CC ;
DAVIS, JA ;
WAYCHUNAS, GA .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1993, 57 (10) :2271-2282
[12]   Physiology of phototrophic iron(II)-oxidizing bacteria: implications for modern and ancient environments [J].
Hegler, Florian ;
Posth, Nicole R. ;
Jiang, Jie ;
Kappler, Andreas .
FEMS MICROBIOLOGY ECOLOGY, 2008, 66 (02) :250-260
[13]   Role of metal-reducing bacteria in arsenic release from Bengal delta sediments [J].
Islam, FS ;
Gault, AG ;
Boothman, C ;
Polya, DA ;
Charnock, JM ;
Chatterjee, D ;
Lloyd, JR .
NATURE, 2004, 430 (6995) :68-71
[14]   Fe(III) mineral formation and cell encrustation by the nitrate-dependent Fe(II)-oxidizer strain BoFeN1 [J].
Kappler, A. ;
Schink, B. ;
Newman, D. K. .
GEOBIOLOGY, 2005, 3 (04) :235-245
[15]   Geomicrobiological cycling of iron [J].
Kappler, A ;
Straub, KL .
MOLECULAR GEOMICROBIOLOGY, 2005, 59 :85-108
[16]   Formation of Fe(III)-minerals by Fe(II)-oxidizing photoautotrophic bacteria [J].
Kappler, A ;
Newman, DK .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2004, 68 (06) :1217-1226
[17]   Arsenite oxidase, an ancient bioenergetic enzyme [J].
Lebrun, E ;
Brugna, M ;
Baymann, F ;
Muller, D ;
Lièvremont, D ;
Lett, MC ;
Nitschke, W .
MOLECULAR BIOLOGY AND EVOLUTION, 2003, 20 (05) :686-693
[18]   Dissimilatory Fe(III) and Mn(IV) reduction [J].
Lovley, DR ;
Holmes, DE ;
Nevin, KP .
ADVANCES IN MICROBIAL PHYSIOLOGY, VOL. 49, 2004, 49 :219-286
[19]   Determination of intrinsic bacterial surface acidity constants using a donnan shell model and a continuous pKa distribution method [J].
Martinez, RE ;
Smith, DS ;
Kulczycki, E ;
Ferris, FG .
JOURNAL OF COLLOID AND INTERFACE SCIENCE, 2002, 253 (01) :130-139
[20]  
Meharg AA, 2003, ENVIRON SCI TECHNOL, V37, P229, DOI 10.1021/es0259842