Forsterite dissolution and magnesite precipitation at conditions relevant for deep saline aquifer storage and sequestration of carbon dioxide
Top Cited Papers
- 16 February 2005
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 217 (3-4), 257-276
- https://doi.org/10.1016/j.chemgeo.2004.12.013
Abstract
No abstract availableKeywords
This publication has 36 references indexed in Scilit:
- Factors affecting the dissolution kinetics of volcanic ash soils: dependencies on pH, CO2, and oxalateApplied Geochemistry, 2004
- Carbon dioxide reaction processes in a model brine aquifer at 200 °C and 200 bars: implications for geologic sequestration of carbonApplied Geochemistry, 2003
- An improved model calculating CO2 solubility in pure water and aqueous NaCl solutions from 273 to 533 K and from 0 to 2000 barChemical Geology, 2003
- Aquifer disposal of acid gases: modelling of water–rock reactions for trapping of acid wastesApplied Geochemistry, 2000
- Sequestration of CO2 in geological media: criteria and approach for site selection in response to climate changeEnergy Conversion and Management, 2000
- Precipitation of calcium and magnesium carbonates from homogeneous supersaturated solutionsJournal of Crystal Growth, 1998
- Olivine dissolution kinetics at near-surface conditionsChemical Geology, 1992
- Control of dissolution rates of orthosilicate minerals by divalent metal–oxygen bondsNature, 1992
- CO2 SOLUBILITY IN WATER AND BRINE UNDER RESERVOIR CONDITIONSChemical Engineering Communications, 1990
- Adsorption of Gases in Multimolecular LayersJournal of the American Chemical Society, 1938