To elucidate existence form of dioxins (PCDD/DFs and Co-PCBs), six samples of paddy (1), plowland (1), forest soils (2) and sea sediments (2) were separated into 6 particle-size fractions using the physical separation method
1), and particle-size distributions of dioxins associated with composition of soil organic matter were studied.
For most of the samples examined, the greastest proportion of dioxins was in the finest particle-size fraction (400- mesh), but for forest soils being in the large particle-size fraction (9-60 mesh) . Size-related accumulations of dioxins generally depended on the amounts of soil organic matter. However, a quantity and/or humification of humic acid also affected the relative enrichment of dioxins in finer particle fractions of paddy and plowland soils, which might be due to the interparticle redistribution of surfactant-soluble dioxins derived from pesticides. While for sediments a part of size distributions of dioxins might be complexed by a wide form of dioxin derived from soil particle, fly ash, wastewater and biological detritus, and for forest soils dioxins adsorbed on plant leaf
viaambient air involving fly ash and exhaust gas might directly affected their existence form. Furthermore, a relative enrichment of high-chlorinated PCDD/DFs and non-
orthoPCBs was found in the finer particle fractions associated with increasing amounts of humic acid, as compared to the other PCDD/DFs and Co-PCBs.
These observations indicate that the existence form of dioxins in soil and sediments is influenced by differences in characteristics of soil organic matter and/or emission source of dioxins, and their information is available to learn chemical and biological aspect and decomposition of dioxins.
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