| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4699502 | Chemical Geology | 2012 | 14 Pages |
Abstract
⺠We realized CO2-rich brine percolation experiments at in situ condition through sandstone samples. ⺠Zeolite/chlorite rich sandstone is a good rock formation for CO2 storage as mineral phases. ⺠CO2 is sequestrated as carbonate and reduce carbon. ⺠Kaolinite precipitates as secondary mineral during CO2 rich-brine interactions. ⺠The precipitated minerals reduce strongly the permeability of the rock sample.
Related Topics
Physical Sciences and Engineering
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Geochemistry and Petrology
Authors
Linda Luquot, Muriel Andreani, Philippe Gouze, Pierre Camps,