Effects of Fe(III) chemical speciation on dissimilatory Fe(III) reduction by Shewanella putrefaciens

被引:71
作者
Haas, JR [1 ]
Dichristina, TJ
机构
[1] Western Michigan Univ, Dept Chem & Environm Studies, Kalamazoo, MI 49008 USA
[2] Georgia Inst Technol, Sch Biol, Atlanta, GA 30332 USA
关键词
D O I
10.1021/es0109287
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Shewanella putrefaciens, a heterotrophic member of the gamma-proteobacteria is capable of respiring anaerobically on Fe(III) as the sole terminal electron acceptor (TEA). Recent genetic and biochemical studies have indicated that anaerobic Fe(Ill) respiration by S. putrefaciens requires outermembrane targeted secretion of respiration-linked Fe(III) reductases. Thus, the availability of Fe(III) to S. putrefaciens may be governed by equilibrium chemical speciation both in the solution phase and at the bacterial cell-aqueous or cell-mineral interface. In the present study, effects of Fe(III) speciation on rates of bacterial Fe(III) reduction have been systematically examined by cultivating S. putrefaciens anaerobically on a suite of Fe(III)organic complexes as the sole TEA. The suite of Fe(III)organic complexes spans the range of stability constants normally encountered in natural water systems and includes Fe(III) complexed to citrate, 5-sulfosalicylate, NTA, salicylate, tiron, and EDTA. Rates of bacterial Fe(III) reduction in the presence of dissolved chelating agents correlate with the thermodynamic stability constants of the Fe(III)-organic complexes, implying that chemical speciation governs Fe(III) bioavailability. Equilibrium Fe(III) sorption experiments measured the reversible coordination of Fe(III) with S. putrefaciens as a function of cell/Fe(III) concentration, time, and activity of competing chelating agents. Results show that S. putrefaciens readily sorbs dissolved Fe(III) but that adsorption is restricted by the presence of strong Fe(III)-chelating agents. Our results indicate that dissimilatory Fe(III) reduction by S. putrefaciens is controlled by equilibrium competition for Fe(III) between dissolved organic ligands and strongly sorbing functional groups on the cell surface.
引用
收藏
页码:373 / 380
页数:8
相关论文
共 35 条
[1]  
[Anonymous], PRINCIPLES APPL AQUA
[2]  
Beliaev AS, 1998, J BACTERIOL, V180, P6292
[3]  
CHATTOPADHYAYA MC, 1982, J INDIAN CHEM SOC, V59, P1416
[4]   A comparison of the thermodynamics of metal adsorption onto two common bacteria [J].
Daughney, CJ ;
Fein, JB ;
Yee, N .
CHEMICAL GEOLOGY, 1998, 144 (3-4) :161-176
[5]   Mineral transformation associated with the microbial reduction of magnetite [J].
Dong, HL ;
Fredrickson, JK ;
Kennedy, DW ;
Zachara, JM ;
Kukkadapu, RK ;
Onstott, TC .
CHEMICAL GEOLOGY, 2000, 169 (3-4) :299-318
[6]  
Dzombak D.A., 1990, SURFACE COMPLEXATION
[7]   A chemical equilibrium model for metal adsorption onto bacterial surfaces [J].
Fein, JB ;
Daughney, CJ ;
Yee, N ;
Davis, TA .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1997, 61 (16) :3319-3328
[8]   Experimental study of uranyl adsorption onto Bacillus subtilis [J].
Fowle, DA ;
Fein, JB ;
Martin, AM .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2000, 34 (17) :3737-3741
[9]  
Gaspard S, 1998, APPL ENVIRON MICROB, V64, P3188
[10]   Thermodynamics of U(VI) sorption onto Shewanella putrefaciens [J].
Haas, JR ;
Dichristina, TJ ;
Wade, R .
CHEMICAL GEOLOGY, 2001, 180 (1-4) :33-54