Xu Feng, Liang Xinmiao, Lin Bingcheng
Dalian Institute of Chemical Physics, Chinese Academy of Sciences, 161 Zhongshan Road, Dalian 116011, China.
J Environ Qual. 2002 Nov-Dec;31(6):1972-9. doi: 10.2134/jeq2002.1972.
Research efforts dealing with chemical transportation in soils are needed to prevent damage to ground water. Methanol-containing solvents can increase the translocation of nonionic organic chemicals (NOCs). In this study, a general log-linear retention equation, log k' = log k'w - Sphi (Eq. [1]), was developed to describe the mobilities of NOCs in soil column chromatography (SCC). The term phi denotes the volume fraction of methanol in eluent, k' is the capacity factor of a solute at a certain phi value, and log k'w and -S are the intercept and slope of the log k' vs. phi plot. Two reference soils (GSE 17204 and GSE 17205) were used as packing materials, and were eluted by isocratic methanol-water mixtures. A model of linear solvation energy relationships (LSER) was applied to analyze the k' from molecular interactions. The most important factor determining the transportation was found to be the solute hydrophobic partition in soils, and the second-most important factor was the solute hydrogen-bond basicity (hydrogen-bond accepting ability), while the less important factor was the solute dipolarity-polarizability. The solute hydrogen-bond acidity (hydrogen-bond donating ability) was statistically unimportant and deletable. From the LSER model, one could also obtain Eq. [1]. The experimental k' data of 121 NOCs can be accurately explained by Eq. [1]. The equation is promising to estimate the solute mobility in pure water by extrapolating from lower-capacity factors obtained in methanol-water mixed eluents.
需要开展有关土壤中化学物质迁移的研究工作,以防止对地下水造成损害。含甲醇的溶剂会增加非离子有机化合物(NOCs)的迁移。在本研究中,开发了一个通用的对数线性保留方程log k' = log k'w - Sphi(式[1]),用于描述NOCs在土壤柱色谱法(SCC)中的迁移率。术语phi表示洗脱液中甲醇的体积分数,k'是溶质在特定phi值下的容量因子,log k'w和 -S分别是log k'与phi关系图的截距和斜率。使用两种参考土壤(GSE 17204和GSE 17205)作为填充材料,并用等度甲醇 - 水混合物进行洗脱。应用线性溶剂化能关系(LSER)模型从分子相互作用分析k'。发现决定迁移的最重要因素是溶质在土壤中的疏水分配,第二重要因素是溶质的氢键碱性(氢键接受能力),而较不重要的因素是溶质的偶极矩 - 极化率。溶质的氢键酸度(氢键供体能力)在统计学上不重要且可忽略。从LSER模型中,也可以得到式[1]。121种NOCs的实验k'数据可以用式[1]准确解释。该方程有望通过从甲醇 - 水混合洗脱液中获得的较低容量因子进行外推,来估计溶质在纯水中的迁移率。