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预测中性和离子化有机化合物的溶解有机碳分配和分布系数。

Predicting dissolved organic carbon partition and distribution coefficients of neutral and ionizable organic chemicals.

机构信息

Department of Science and High Technology (DiSAT), University of Insubria, Via Valleggio 11, Como, Italy.

出版信息

Sci Total Environ. 2019 Mar 25;658:1056-1063. doi: 10.1016/j.scitotenv.2018.12.282. Epub 2018 Dec 19.

DOI:10.1016/j.scitotenv.2018.12.282
PMID:30677970
Abstract

Estimating K (dissolved organic carbon/water partition coefficient) and D (dissolved organic carbon/water distribution coefficient) of neutral and ionizable organic chemicals is a crucial task for assessing mobility, modelling transport, environmental fate of a variety of chemicals and for evaluating their bioavailability in terrestrial and aquatic environments. A critical literature search of reliability-selected K and D values was performed to setup novel predictive relationships for K and D of neutral and ionizable organic chemicals. This goal was pursued by using: 1) LSER (linear solvation energy relationship) models to predict K for neutral chemicals using Abraham solute parameters calculated for different DOC sources (all DOC sources together, soil porewater, surface water, wastewater and Aldrich humic acid (HA)); 2) linear regressions for predicting D of organic acids from the octanol/water partition coefficient (Log K or Log P) and the dissociation constant (pKa), accounting separately for the contribution of the neutral and ionic fraction. The proposed models predicted Log K and D values within a root mean square deviation (RMSD) generally smaller than 0.3 log units.

摘要

估算中性和离子型有机化合物的 K(溶解有机碳/水分配系数)和 D(溶解有机碳/水分布系数)对于评估各种化学物质的迁移性、模拟迁移、环境归宿以及评估它们在陆地和水生环境中的生物可用性至关重要。本研究通过使用:1)线性溶剂化能量关系(LSER)模型,使用为不同 DOC 来源(所有 DOC 来源、土壤孔隙水、地表水、废水和 Aldrich 腐殖酸(HA))计算的 Abraham 溶质参数来预测中性化合物的 K 值;2)线性回归,根据辛醇/水分配系数(Log K 或 Log P)和离解常数(pKa)来预测有机酸的 D 值,分别考虑中性和离子部分的贡献,对中性和离子型有机化合物的 K 和 D 值进行预测。所提出的模型预测的 Log K 和 D 值的均方根偏差(RMSD)通常小于 0.3 个对数单位。

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