Field demonstration of CO2 leakage detection in potable aquifers with a pulselike CO2-release test.
This study presents two field pulselike CO2-release tests to demonstrate CO2 leakage detection in a shallow aquifer by monitoring groundwater pH, alkalinity, and dissolved inorganic carbon (DIC) using the periodic groundwater sampling method and a fiber-optic CO2 sensor for real-time in situ monitoring of dissolved CO2 in groundwater. Measurements of groundwater pH, alkalinity, DIC, and dissolved CO2 clearly deviated from their background values, showing responses to CO2 leakage. Dissolved CO2 observed in the tests was highly sensitive in comparison to groundwater pH, DIC, and alkalinity. Comparison of the pulselike CO2-release tests to other field tests suggests that pulselike CO2-release tests can provide reliable assessment of geochemical parameters indicative of CO2 leakage. Measurements by the fiber-optic CO2 sensor, showing obvious leakage signals, demonstrated the potential of real-time in situ monitoring of dissolved CO2 for leakage detection at a geologic carbon sequestration (GCS) site. Results of a two-dimensional reactive transport model reproduced the geochemical measurements and confirmed that the decrease in groundwater pH and the increases in DIC and dissolved CO2 observed in the pulselike CO2-release tests were caused by dissolution of CO2 whereas alkalinity was likely affected by carbonate dissolution.
Bureau of Economic Geology, The University of Texas at Austin , Austin, Texas 78759, United States.
Changbing
C
Yang
Susan D
SD
Hovorka
Jesus
J
Delgado-Alonso
Patrick J
PJ
Mickler
Ramón H
RH
Treviño
Straun
S
Phillips
D002245:Carbon Dioxide / Q000737:chemistry*; D057965:Carbon Sequestration; D057231:Climate Change; D060587:Groundwater / Q000737:chemistry*; D060753:Water Quality; D014881:Water Supply
D002245:Carbon Dioxide