文摘
Sediment organic matter heterogeneity in sediments isshown to impact the sorption behavior of contaminants.We investigated the sorptive properties as well as thecomposition of organic matter in different subsamples (mainlygrain size fractions) of the Canadian River Alluvium(CRA). Organic petrography was used as a new tool todescribe and characterize the organic matter in thesubsamples. The samples studied contained many differenttypes of organic matter including bituminous coal particles.Differences in sorption behavior were explained basedon these various types of organic matter. Subsamplescontaining predominately coaly, particulate organic mattershowed the highest Koc, the highest nonlinearity ofsorption isotherms and the slowest sorption kinetics. Soilsubsamples with organic matter present as organiccoatings around the quartz grains evidenced the lowestKoc, the most linear sorption isotherms and the fastest sorptionkinetics, which was not limited by slow intraparticlediffusion. Due to the high sorption capacity of the coalyparticles even when it is present as only a small fractionof the composite organic content (<3%) causes Kocvalues which are much higher than expected for soil organicmatter (e.g. Koc - Kow relationships). The results showthat the identification and quantification of the coaly particleswithin a sediment or soil sample is a prerequisite inorder to understand or predict sorption behavior of organicpollutants.