Mineralogical and geochemical analysis of Fe-phases in drill-cores from the Triassic Stuttgart Formation at Ketzin CO2 storage site before CO2 arrival
| Autor: | Hilke Würdemann, Aude Picard, Laura Mariana Wehrmann, Patrick Meister, Christoph Vogt, Christian März, Monika Kasina, Anna Lichtschlag, Laura Wagenknecht, Dieter Pudlo, Susanne Bock |
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| Rok vydání: | 2017 |
| Předmět: |
010504 meteorology & atmospheric sciences
Soil Science Mineralogy engineering.material 010502 geochemistry & geophysics 01 natural sciences microbial activity chemistry.chemical_compound Environmental Chemistry Chlorite 0105 earth and related environmental sciences Earth-Surface Processes Water Science and Technology Total organic carbon Global and Planetary Change CO_{2} capture and storage (CCS) sCO_{2} Fe-mineralogy Geology Supercritical CO2 Pollution Petroleum reservoir Silicate Diagenesis Microbial activity chemistry Illite Ketzin engineering Pyrite CO2 capture and storage (CCS) Clay minerals Stuttgart formation |
| Zdroj: | Environmental Earth Sciences ENVIRONMENTAL EARTH SCIENCES |
| DOI: | 10.1007/s12665-017-6460-9 |
| Popis: | Reactive iron (Fe) oxides and sheet silicate-bound Fe in reservoir rocks may affect the subsurface storage of CO_{2} through several processes by changing the capacity to buffer the acidification by CO_{2} and the permeability of the reservoir rock: (1) the reduction of three-valent Fe in anoxic environments can lead to an increase in pH, (2) under sulphidic conditions, Fe may drive sulphur cycling and lead to the formation of pyrite, and (3) the leaching of Fe from sheet silicates may affect silicate diagenesis. In order to evaluate the importance of Fe-reduction on the CO_{2} reservoir, we analysed the Fe geochemistry in drill-cores from the Triassic Stuttgart Formation (Schilfsandstein) recovered from the monitoring well at the CO_{2} test injection site near Ketzin, Germany. The reservoir rock is a porous, poorly to moderately cohesive fluvial sandstone containing up to 2-4 wt% reactive Fe. Based on a sequential extraction, most Fe falls into the dithionite-extractable Fe-fraction and Fe bound to sheet silicates, whereby some Fe in the dithionite-extractable Fe-fraction may have been leached from illite and smectite. Illite and smectite were detected in core samples by X-ray diffraction and confirmed as the main Fe-containing mineral phases by X-ray absorption spectroscopy. Chlorite is also present, but likely does not contribute much to the high amount of Fe in the silicate-bound fraction. The organic carbon content of the reservoir rock is extremely low ( |
| Databáze: | OpenAIRE |
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