Titlebook: Bioavailability of Organic Chemicals in Soil and Sediment; Jose Julio Ortega-Calvo,John Robert Parsons Book 2020 The Editor(s) (if applica

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https://doi.org/10.1007/978-94-011-9399-3ype of soil organic matter, micronized Pahokee peat, by a single method, dynamic high-pressure flow-through column studies using controlled aqueous medium. This chapter collected these consistent . values obtained for a structurally diverse range of (non)polar, cationic, (perfluorinated) anionic, an

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https://doi.org/10.1007/978-3-476-03985-9carbon-based approaches. In particular, exploration of the influence of condensed aromatic structures in DOM, often referred to as dissolved black carbon, would probably yield better insights into their impact on the bioavailability of high molecular weight PAHs and other hydrophobic compounds. More

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https://doi.org/10.1007/978-3-322-94551-8uptake. The use of transpiration stream concentration factor (TSCF) predicted by the octanol-water partition coefficient (log .) has long been the dominant model; however, recent research has suggested a move away from these predictive relationships. Many studies have been conducted with approximate

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