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Pressure variations in the fluid deflect the diaphragm, which causes changes in the tension in the wire.The wire is regularly plucked by an electromagnet and the natural frequency of vibration is recorded.EPA Grant Number: R834386 Title: Integrated Design, Modeling, and Monitoring of Geologic Sequestration of Anthropogenic Carbon Dioxide to Safeguard Sources of Drinking Water Investigators: Mc Pherson, Brian J. , Goel, Ramesh , Solomon, Douglas Kip Institution: University of Utah EPA Project Officer: Klieforth, Barbara I Project Period: December 1, 2009 through November 30, 2012 (Extended to November 30, 2013) Project Period Covered by this Report: March 16, 2010 through March 15,2011 Project Amount: 9,567 RFA: Integrated Design, Modeling, and Monitoring of Geologic Sequestration of Anthropogenic Carbon Dioxide to Safeguard Sources of Drinking Water (2009) RFA Text | Recipients Lists Research Category: Drinking Water , Water geologic sequestration (GS) demonstration sites to develop an "Aquifer Risk Assessment Framework," or ARAF.
Therefore, we stopped the monitoring at pm immediately after the recharge period and began to record pressure and temperature manually.
Additionally, we will examine alternative natural sites that leak CO such as the Crystal Geyser in Utah, to provide context regarding what attributes may compromise storage sites and to evaluate the nature and processes of leakage.
We will use simulations to evaluate a range of possible injection scenarios, and use results to evaluate what engineering conditions will minimize risks.
In detail, our observation using the piezometer installed at a depth of 16 m indicated that both pressure and temperature regularly dropped during the eruption period.
In the absence of eruption activity, both the pressure and temperature stayed at consistent levels (0.15 MPa and 17.3°C).