| 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. ?? 1973. |
| Genre: | Article |
| ProdID: | 70009773 |
| Citation Author: | Luce, R. W.; Parks, G. A. |
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| Citation End Page: | 153 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Chemical Geology |
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| Citation Number Of Pages: | 7 |
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| Citation Publisher: | Elsevier |
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| Citation Search Results Text: | Point of zero charge of weathered forsterite; 1973; Article; Journal; Chemical Geology; Luce, R. W.; Parks, G. A. |
| Citation Start Page: | 147 |
| Citation Volume: | 12 |
| Citation Year: | 1973 |
| Type: | citation/reference |
| Text: | Point of zero charge of weathered forsterite; 1973; Article; Journal; Chemical Geology; Luce, R. W.; Parks, G. A. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1016/0009-2541(73)90112-5 |
| Date Other: | Mon, 1 Jan 1973 00:00 -0600 |
| Publisher: | Elsevier |
