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Potential causes of organic carbon normalized partition coefficient (KOC) variability for organic compounds: A review

机译:有机化合物的有机碳归一化分配系数(KOC)变异性的潜在原因:综述

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Even though the most widely-used sorption model is the organic carbon normalized partition coefficient (KOC) partitioning model and this model provides a good approximation of sorption properties in many cases, it is unreasonable to expect such a simple model to accurately describe a process as complex as sorption of organic pollutants to soil. The one main shortcomings of the KOC model is; it assumes all organic matter is equally sorptive. Although some studies have reported correlations between KOC and particular C types, especially aromatic C and alkyl C. Here, alternative causes of KOC variability are reviewed. Sorption by soil minerals and blocking of sorption sites by minerals or by the lipid fraction of organic matter also altering the physical conformation of the soil organic matter are other possible of KOCvariability which is making it more sorptive.  
机译:即使使用最广泛的吸附模型是有机碳归一化分配系数(KOC)分配模型,并且该模型在许多情况下都能提供良好的吸附性能近似值,但期望这种简单模型能够准确地进行吸附是不合理的描述了一个过程,就像有机污染物吸附到土壤一样复杂。 KOC模型的主要缺点之一是:它假定所有有机物都具有同等吸收性。尽管一些研究报告了KOC与特定C类型之间的相关性,尤其是芳族C和烷基C。在此,对KOC变异性的其他原因进行了综述。土壤矿物质的吸附和矿物质或有机物质的脂质组分对吸附位点的阻塞也改变了土壤有机物的物理构象,这也是KOC变异性的另一种可能,这使其更具吸附性。  

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