Microbial Sulfate Reduction Kinetics of an Acid Mine
Drainage Site, Davis Mine, Rowe, MA
Caryl
Ann Becerra, University of Massachusetts, Amherst,
Microbiology Department, 639 North Pleasant Street,
Amherst, MA 01003, Tel: 413-545-1204, Email: cbecerra@microbio.umass.edu
Acid
mine drainage is one of the largest widespread
environmental problems which is exarcerbated by mining
activities. Methods
to prevent AMD production and methods to remediate AMD are
both time consuming and expensive.
Promoting the natural attenuation of sites affected
by AMD offers a more cost-effective strategy for the
mining industry.
Davis
Mine in Rowe, Massachusetts is an acid mine drainage site
where natural attenuation is occurring.
The natural attenuation at this site may be due to
the dilution of unpolluted water into the area and/or
microbial activity such as sulfate reduction.
In previous studies, sulfate-reducing bacteria (SRB)
were found at this site.
The main goal of the study is to determine the
contribution of microbial sulfate reduction to the natural
attenuation observed at Davis Mine using several
techniques to measure sulfate reduction activity.
Microbial sulfate reduction rates are determined
through microcosm studies with amended Davis mine water
and SRB media buffered at pH 3.
A sediment core depth analysis of sulfate reduction
rates was also determined for Well 14, Well 15, and C2
using radio-isotopes of sulfate.
By
determining the rate of sulfate reduction and the
abundance and diversity of SRB’s in AMD site, we can
provide estimates of their likely importance in other
global settings. Besides
the remediation of AMD, this research will provide new
information for developing remediation strategies of other
acidic metal contaminated industrial waste streams.
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