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SWELLING PROPERTIES OF SOIL ORGANIC MATTER AND THEIR RELATION TO SORPTION OF NON-IONIC ORGANIC COMPOUNDS
Citation:
Lyon, W. AND D. Rhodes. SWELLING PROPERTIES OF SOIL ORGANIC MATTER AND THEIR RELATION TO SORPTION OF NON-IONIC ORGANIC COMPOUNDS. U.S. Environmental Protection Agency, Washington, D.C., EPA/600/2-91/033.
Description:
A method has been developed to measure the swelling properties of Concentrated natural organic materials in various organic liquids, and has been applied to various eat, pollen, chitin and cellulose samples. he swelling of these macromolecular aterials is rhe volumetric manifestation of bulk sorption, i.e., sorption by dissolution (or partitioning) of the sorbed liquids into the macromolecular solid phase. irect evidence for the existence of this category of sorbed materials has been obtained for soil organic materials by the present research; swelling in liquids has long been known in coals and polymers. ulk sorbed molecules are thought to be inaccessible to direct biological attack, and may represent a continuing source of low-level rebound contamination of groundwater at a polluted site. quilibration of bulk-sorbed molecules with liquid phases surrounding the particles is kinetically slow (diffusion limited) relative to sorption and fluid movement, and this sluggishness is probably responsible for some nonequilibrium sorption phenomena seen in soil column flow experiments. olecules with molar volumes greater than about 93 cm3 mol-1 appear to be strongly excluded from sorption inside the soil organic materials studied in this work. n contrast, cellulose excluded molecules with molar volumes greater than about 88 cm3 mol-1. xtensive bibliographies included.