Geochemical detection of carbon dioxide in dilute aquifers
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* Corresponding author: Susan Carroll carroll6@llnl.gov
Chemistry, Materials, Earth and Life Sciences Division, Lawrence Livermore National Laboratory, Livermore CA 94550, USA
Geochemical Transactions 2009, 10:4 doi:10.1186/1467-4866-10-4
Published: 26 March 2009Additional files
Additional file 1:
Evolution of pH plume from a CO2 flux = 105 t/yr (62.5 t/m2/yr) and 0.3% hydraulic gradient.
Format: WMV Size: 3.8MB Download file
Additional file 2:
Evolution of pH plume from a CO2 flux = 103 t/yr (0.63 t/m2/yr) and 0.3% hydraulic gradient.
Format: WMV Size: 3.1MB Download file
Additional file 3:
Evolution of pH plume from a CO2 flux = 103 t/yr (0.63 t/m2/yr) and 0.1% hydraulic gradient.
Format: WMV Size: 3.1MB Download file
Additional file 4:
Evolution of pH plume from a CO2 flux = 103 t/yr (0.63 t/m2/yr) and 0.3% hydraulic gradient in a developed aquifer with sustained pumping (1893 L/min).
Format: WMV Size: 3.6MB Download file
