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U.S. Department of Energy
Office of Scientific and Technical Information

Geochemical assessment of aquifer recharge effects in the southwest Denver basin

Technical Report ·
OSTI ID:6479321
Recharge of the Denver groundwater basin by injection recharge has been proposed as a result of increasing depletion of the water supply. However, injection recharge can cause physical and chemical changes in the geologic materials of the recharged aquifer, depending on the chemistry of both the host and injected waters, as well as the mineralogy of the aquifer's rock matrix. The Denver groundwater basin contains four principal bedrock aquifers, of which the Arapahoe aquifer is considered to be the best in terms of water quality and quantity. Some preliminary field injection tests have been undertaken using drinking water supplies. However, water that meets drinking water standards contains constituents which may react upon injection, resulting in aquifer damage. As a preliminary step in designing future field tests, analyses of aquifer water and Denver Water Board municipal drinking water were evaluated by a geochemical equilibrium computer model (PHREEQE), developed by the U.S. Geological Survey, to determine the potential for reaction. The results of these simulations confirm that the Arapahoe aquifer is a good candidate for injection recharge.
Research Organization:
Colorado State Univ., Fort Collins, CO (United States). Water Resources Research Inst.
OSTI ID:
6479321
Report Number(s):
PB-93-200384/XAB; COMPLETION--146; CNN: DI-14-08-0001-G1006; DI-14-08-0001-G1214
Country of Publication:
United States
Language:
English