Datensatz

Zusammenfassung

Rock core samples of the Upper Triassic Stuttgart Formation from the Ketzin pilot CO2 storage site were exposed to pure CO2 and synthetic reservoir brine at simulated reservoir P-T conditions of 5 MPa and 40 °C. Autoclaves were opened and samples were taken after 15, 21, 24 and 40 months, respectively. The samples were analysed mineralogically and geochemically and compared to baseline data of untreated samples. XRD analyses with Rietveld refinement show no significant mineralogical changes for the studied intervals. On freshly broken rock fragments of the CO2-treated samples, corrosion textures were found on plagioclase, K-feldspar and anhydrite surfaces. BSE images of the respective twin samples show (intensified) alterations of feldspar minerals. EMPA data display a change in plagioclase composition from intermediate to almost pure albite endmember compositions after CO2 exposure. Inorganic fluid data show, besides others, highly increased calcium, potassium and sulfate concentrations [1]. The experimental observations were reproduced using the reactive geochemical modeling code PHREEQC. 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.