| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5779250 | Procedia Earth and Planetary Science | 2017 | 4 Pages |
Abstract
A thermodynamic-kinetic model for interactions in water-rock systems has been modified to calculate water-rock interactions during fluid flow. We used published data on chemical composition of atmospheric precipitates at Hawaii and their abundance in Kaka Falls aria, the Island of Hawaii, a level of surface runoff, age and initial composition of basaltic tephra, mineralogical zoning of laterites, to adjust such a parameter of the model as a degree of exposure of the primary mineral surfaces to aqueous solution. The goal was to obtain an approximate agreement of scales of simulated and observed mineral alterations during certain time.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
M.V. Mironenko, E.V. Cherkasova,