About This Item
- Full text of this item is not available.
- Abstract PDFAbstract PDF(no subscription required)
Share This Item
The AAPG/Datapages Combined Publications Database
Houston Geological Society Bulletin
Abstract
THE 1997 NATIONAL GROUND WATER ASSOCIATION'S HENRY DARCY DISTINGUISHED LECTURE:
Abstract: Water, Microbes, and Rocks: The
Geochemical
Ecology of Contaminated Ground Water
Geochemical
Ecology of Contaminated Ground WaterBy
Dept. of Geological Sciences,
Univ. of Texas at Austin
When an organic substance, either natural or anthropogenic, infiltrates into
an aquifer it becomes a component of a dynamic bio-
geochemical
system. From the
perspective of the subsurface microbe, these compounds may be benign, toxic, or
a rich source of carbon in an otherwise carbon-poor environment. Microbes
consume this carbon, producing energy, cell mass, and geochemically reactive
byproducts. The transformation of organic toxicants
by native microorganisms, sometimes
known as intrinsic bioremediation,
is considered one of the most promising
remediation approaches for contaminated
ground water. From a geologic perspective,
however, rapid metabolic transformation
of organic substances also results
in dramatic changes in the
geochemical
ecology of that aquifer, changing the
native microbial consortia, aquifer mineralogy
and permeability, vadose-zone gas
composition, and water chemistry.
This lecture will examine the geology and
geochemistry of microbial transformation
of hydrocarbons using laboratory experiments,
geochemical
modeling, and field
observations of contaminated aquifers,
including results from the collaborative
U.S. Geological Survey's Bemidji
research program. Hydrocarbon degradation
produces bicarbonate, acidity, and
organic waste products, potentially changing
the bulk geochemistry of the aquifer
over wide areas, or more subtly, producing
reactive micro-environments near
attached microbes. How does oil degrade
in ground water, what are the degradation
byproducts, and what is the nature of the
micro-environment created around an
attached microbe? Are these biogeochemical
reactions a significant contribution to
subsurface mineral diagenesis? Is mineral
weathering enhanced only by
surface
colonizing
microbes, or do microbes affect equilibria by altering "bulk" pore-water
chemistry? Do microbes colonize mineral
surfaces in order to leach necessary nutrients,
or is colonization controlled by
surface
charge and
surface
roughness? The
goal of this lecture is to examine the
geochemical
consequences of subsurface
microbial processes.
End_of_Record - Last_Page 10---------------