| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6439341 | Geochimica et Cosmochimica Acta | 2012 | 25 Pages |
Abstract
The carbonation of plagioclase at stagnant conditions is slow compared to olivine at temperatures around 200 °C. However, industrial operations involving high fluid flows of CO2-water mixtures induce gradients in pH or solute concentrations, which may lead to increased reaction rates and changes in porosity/permeability.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
I.A. Munz, Ã. Brandvoll, T.A. Haug, K. Iden, R. Smeets, J. Kihle, H. Johansen,