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- W2049833614 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" @default.
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- W2049833614 date "1973-10-01" @default.
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- W2049833614 title "Point of zero charge of weathered forsterite" @default.
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- W2049833614 doi "https://doi.org/10.1016/0009-2541(73)90112-5" @default.
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