NSF LogoNSF Award Abstract - #0221791 AWSFL008-DS3

BE/CBC: Biogeochemistry of Fe(III) and Sulfate Reduction in Extreme Acidic
Environments

NSF Org CHE
Latest Amendment Date July 11, 2003
Award Number 0221791
Award Instrument Standard Grant
Program Manager Janice M. Hicks
CHE DIVISION OF CHEMISTRY
MPS DIRECT FOR MATHEMATICAL & PHYSICAL SCIEN
Start Date September 15, 2002
Expires August 31, 2007 (Estimated)
Expected Total Amount $1590000 (Estimated)
Investigator Richard F. Yuretich yuretich@geo.umass.edu (Principal Investigator current)
Sarina J. Ergas (Co-Principal Investigator current)
Allan Feldman (Co-Principal Investigator current)
David P. Ahlfeld (Co-Principal Investigator current)
Klaus Rudolf L. Nuesslein (Co-Principal Investigator current)
Sponsor U of Massachusetts Amherst
408 Goodell Building
Amherst, MA 010033285 413/545-0698
NSF Program 1972 ELECTROCHEMISTRY & SURFACE CHE
Field Application
Program Reference Code 0000,1689,OTHR,

Abstract

Professor Richard Yuretich of the University of Massachusetts Amherst and coworkers are supported by the Biocomplexity-Coupled Biogeochemical Cycles program to study the microbiology, hydrology and environmental science of acid mine drainage (AMD) sites. The team will study the processes of Fe(III) and sulfate reduction in an AMD site in western Massachusetts through field studies, modeling and laboratory experiments, and will quantify the roles of acidophilic and acid-tolerant anaerobic microorganisms. Changes in hydrology and geochemistry of the stream and groundwater will be monitored as a function of distance from the AMD source. Sediment from the stream and surrounding aquifer will be examined for anaerobic microorganisms, for iron and sulfate reducing microorganisms and for the metabolic potential of these species. A variety of molecular genetic probes and polymerase chain reactions (PCR) will be used in the identification of species. Additional experiments will involve in situ microcosms in the laboratory that will be modeled in order to study attenuation. International collaboration will enable comparisons with similar mines in the United Kingdom. K12 teachers in training will act as research assistants, and real pedagogical work will be done on the effects of teaching style.

Acid mine drainage results from the oxidation of pyrite and other sulfide minerals in streams and shallow groundwater. Much research has been directed toward understanding the formation of these conditions, however, the biogeochemistry of natural attenuation is relatively unknown. Organisms discovered here might have global significance in the reduction of iron and sulfate in other environments. Knowledge about microbial cycling of iron and sulfur can be applied to other ecosystems.


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