U.S. Geological Survey Toxic Substances Hydrology Program--Proceedings
of the Technical Meeting, Colorado Springs, Colorado, September 20-24, 1993,
Water-Resources Investigations Report 94-4015
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Preliminary Assessment of Jet Fuel Contamination of an Atoll
Aquifer
by
Gordon W. Tribble (U.S. Geological Survey, Honolulu, Hawaii),
Roger W. Lee (U.S. Geological Survey, Austin, Texas), Duane S. Wydoski (U.S.
Geological Survey, Arvada, Colorado), Jill D. Torikai (U.S. Geological Survey,
Honolulu, Hawaii), and Charles D. Hunt, Jr. (U.S. Geological Survey, Honolulu,
Hawaii)
Abstract
Jet fuel spilled in 1991 on the atoll island of Diego Garcia (Chagos
Archipelago, Indian Ocean) has contaminated one of the fresh ground-water
lenses on the island. Freshwater lenses on the island are unconfined and
strongly influenced by tidal oscillations in sea level. The U.S. Geological
Survey is using a multidisciplinary approach to (1) evaluate contaminant
migration and, (2) determine the geochemical processes that affect contaminant
degradation. A network of water-level recorders is being used to determine
the effect of a hydraulic control scheme on the water-table configuration
and contaminant transport. The water table near the spill is 1 to 2 feet
above mean sea level and undergoes diurnal oscillations of as much as 4
feet in response to ocean tides.
Geochemical characterization of the aquifer will help to resolve
ambient and fuel-affected levels and types of microbial oxidation.
This information is useful to determine the need for, and
type of, remediation of residual contamination after efforts
to remove the fuel by pumping are completed. Initial data
from the first of three planned trips indicate that natural levels
of microbial oxidation are sufficient to deplete O2
in all aquifer waters. Concentrations of CO2, CH4,
and H2S indicate that the natural levels of microbial
oxidation are enhanced by the presence of hydrocarbon contaminants.
An evaluation of the rates, mechanisms, and limits of microbial
oxidation in the aquifer will require additional sampling and
physical measurements to assess hydraulic processes such as aquifer
properties and the response of ground-water flow to different
recharge and withdrawal conditions.
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