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Point of zero charge of weathered forsterite

Chemical Geology

By:
and
DOI: 10.1016/0009-2541(73)90112-5

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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. ?? 1973.

Additional Publication Details

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
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Chemical Geology
First page:
147
Last page:
153