Point of zero charge of weathered forsterite
Chemical Geology
By: R.W. Luce and George A. Parks
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Abstract
The point of zero charge of forsterite shifts from an estimated 8.9 for the unaltered mineral to 8.4 and 8.0, respectively, after being weathered artificially for 1 h and 4 h. These results corroborate the presence of magnesium-deficient surfaces on the weathered minerals, also indicated by chemical analyses of the solutions. H+ and OH− are shown to be potential-determining ions in this system
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Point of zero charge of weathered forsterite |
| Series title | Chemical Geology |
| DOI | 10.1016/0009-2541(73)90112-5 |
| Volume | 12 |
| Issue | 2 |
| Year Published | 1973 |
| Language | English |
| Publisher | Elsevier |
| Description | 7 p. |
| First page | 147 |
| Last page | 153 |
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