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Applications of a total dissolved gas pressure probe in ground water studies
Authors:Manning Andrew H  Solomon D Kip  Sheldon Amy L
Institution:Department of Geology and Geophysics, University of Utah, Salt Lake City, UT 84112;(801) 585-1538;fax (801) 581-7065;;Department of Geological Sciences, SUNY-Geneseo, 1 College Circle, Geneseo, NY 14454;(716) 245-5988;;Now at U.S. Geological Survey, P. O. Box 25046, Mail Stop 973;Denver, CO 80225;(303) 236-1812;fax (303) 236-3200;
Abstract:Measurements of dissolved gases have numerous applications in ground water hydrology, and it is now possible to measure the total dissolved gas pressure in situ using a probe. Dissolved gas pressure is measured by submerging a headspace volume with a gas-permeable membrane, allowing dissolved gases in the water to equilibrate with gases in the headspace, then measuring the pressure in the headspace with a pressure transducer. Total dissolved gas pressure (TGP) probes have many potential uses in ground water studies employing dissolved gases, including: (1) determining approximate excess air levels, which may provide information about the time and location of recharge; (2) screening wells for air contamination, which can compromise the accuracy of dissolved gas tracer techniques: (3) detecting a trapped gas phase, which can significantly reduce hydraulic conductivity and impede the transport of dissolved solutes and gases; (4) enabling the use of gas-filled passive diffusion samplers for determining accurate dissolved gas concentrations; and (5) determining relative concentrations of CH4 and CO2 when they are known to be highly abundant. Although TGP probes designed for surface water have been available for several years, TGP probes suitable for ground water applications have only recently become available. Herein we present what are, to our knowledge, the first reported ground water dissolved gas data collected using a TGP probe. We also explain the basic operating principles of these probes and discuss the potential applications listed.
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