21 Energy Resources in Sedimentary Basins
Tuesday, 6 September 2011
11:00 AM - 4:50 PM
A 125
RESERVOIR SANDSTONE SAMPLES FROM THE KETZIN PILOT SITE DURING LONG-TERM CO2-EXPOSURE EXPERIMENTS - MINERALOGICAL CHANGES AND GEOCHEMICAL MODELLING
Paper number: 21-2
Program: Theme Sessions
Time: 3:50 PM – 4:05 PM
Authors
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Axel LiebscherCentre for CO2 Storage, Potsdam, N/A
Abstract
The mineralogical-chemical measurements imply preferred dissolution of calcium out of plagioclase next to dissolution of K-feldspar and anhydrite. Due to the heterogeneous character of the Stuttgart Formation, which formed in a fluvial environment [2], it is often difficult to distinguish between natural variability and CO2-related changes. Additional data is needed to interconnect the indicated changes during the experiments and to better understand CO2-brine-rock interaction occurring within the Ketzin reservoir.
[1] Wandrey, et al. (2011). Monitoring petrophysical, mineralogical, geochemical and microbiological effects of CO2 exposure – Results of long-term experiments under in situ conditions. Energy Procedia 4, 3644-3650, doi:10.1016/j.egypro.2011.02.295.
[2] Förster et al. (2006). Baseline characterization of the CO2SINK geological storage site at Ketzin, Germany. Environ Geoscience, 13, 3, 145-161.