| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4699934 | Chemical Geology | 2010 | 15 Pages |
Abstract
âºSolutes controlled by binary mixing between silicate and trace carbonate weathering. âºCl/Ca ratios indicate host metavolcanic rocks are an important source of Cl. âºOxidation of sulfide mineralization accounts for 60% of the dissolved sulfate. âºSulfide oxidative weathering accounts for ~ 20% of the cation flux in the watershed. âºCation denudation and CO2 consumption rates similar to watersheds in western Canada.
Related Topics
Physical Sciences and Engineering
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Geochemistry and Petrology
Authors
Matthew I. Leybourne, Wayne D. Goodfellow,