Sorption of non-ionic aliphatic molecules from aqueous solutions on clay minerals clay-organic studies--VII

Details Sorption of non-ionic aliphatic molecules from aqueous solutions on clay minerals clay-organic studies--VII Sorption of non-ionic aliphatic molecules from aqueous solutions on clay minerals clay-organic studies--VII

Nov 1963

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1963gecoa..27.1129b&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 27, Issue 11, pp.1129-1137

Computer Science

Scientific paper

Aqueous solutions of some non-ionic, aliphatic compounds are mixed with aqueous suspensions of kaolinite, gibbsite and montmorillonite. From the concentrations of the resulting organic solutions, the apparent sorptions of the organic molecules on the clay surfaces are determined. The results are expressed in m moles/m 2 of surface, molecules sorbed per 100 Å 2 , and as an equivalent number of packed organic layers. Gibbsite appears to sorb more organic material than does kaolinite, and kaolinite than montmorillonite. Tentative explanations are suggested. The steps involved in the sorption calculations are examined critically, and especially the consequences arising from the sorption of both water and organic molecules on the clay surfaces.

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