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土壤性质对1-丁基-3-甲基咪唑类离子液体吸附/脱附行为的影响
引用本文:李月,雷思聪,石炎,邱宇平.土壤性质对1-丁基-3-甲基咪唑类离子液体吸附/脱附行为的影响[J].农业环境科学学报,2017,34(1):30-37.
作者姓名:李月  雷思聪  石炎  邱宇平
作者单位:污染控制与资源化研究国家重点实验室, 同济大学环境科学与工程学院, 上海 200092,污染控制与资源化研究国家重点实验室, 同济大学环境科学与工程学院, 上海 200092,污染控制与资源化研究国家重点实验室, 同济大学环境科学与工程学院, 上海 200092,污染控制与资源化研究国家重点实验室, 同济大学环境科学与工程学院, 上海 200092
基金项目:国家自然科学基金(21377093,21677108)
摘    要:研究了2 种咪唑类离子液体(ILs)—氯化1-丁基-3-甲基咪唑(Bmim]Cl])和1-丁基-3-甲基咪唑双三氟甲磺酰亚胺盐(Bmim](CF3SO22N])在16种土壤上的吸附/脱附规律,探讨了土壤理化性质对于吸附/脱附行为的影响。研究发现,Bmim]Cl]和Bmim](CF3SO22N]的土壤吸附系数与土壤阳离子交换量(CEC)呈正相关性,相关系数(R2)分别为0.842 9和0.835 3(P<0.05),表明土壤主要通过静电作用来吸附ILs,而与土壤总有机碳含量(TOC%)的R2 值仅分别为0.003 5和0.073 0(P< 0.01),说明ILs 与土壤有机质的疏水结合作用为相对次要。ILs 阴离子基团对吸附行为有一定的影响,但并不明显。ILs 吸附/脱附的迟滞系数(HI)均小于1,可能与(ILs)在土壤粘土/有机质上的不可逆结合有关。其中,CEC 和Bmim]Cl]和Bmim](CF3SO22N]的HI之间存在较大的相关性(R2分别为0.772 9,0.781 5,P<0.01),说明CEC 对迟滞行为有着不可忽视的影响。

关 键 词:土壤性质,离子液体,吸附,脱附
收稿时间:2016/9/28 0:00:00

Effects of Soil Characteristics on Sorption-Desorption of 1-butyl-3-methyl-imidazolium-based Ionic Liquids
LI Yue,LEI Si-cong,SHI Yan and QIU Yu-ping.Effects of Soil Characteristics on Sorption-Desorption of 1-butyl-3-methyl-imidazolium-based Ionic Liquids[J].Journal of Agro-Environment Science( J. Agro-Environ. Sci.),2017,34(1):30-37.
Authors:LI Yue  LEI Si-cong  SHI Yan and QIU Yu-ping
Institution:State Key Laboratory of Pollution Control and Resources Reuse, College of Environmental Science and Engineering, Tongji University, Shanghai 200092, China,State Key Laboratory of Pollution Control and Resources Reuse, College of Environmental Science and Engineering, Tongji University, Shanghai 200092, China,State Key Laboratory of Pollution Control and Resources Reuse, College of Environmental Science and Engineering, Tongji University, Shanghai 200092, China and State Key Laboratory of Pollution Control and Resources Reuse, College of Environmental Science and Engineering, Tongji University, Shanghai 200092, China
Abstract:Effects of soil characteristics on sorption-desorption of 1-butyl-3-methyl-imidazolium-based ionic liquids(Bmim]Cl] and Bmim](CF3SO2)2N])by sixteen natural soils were studied. The value of sorption coefficient Kd of Bmim]Cl] and Bmim](CF3SO2)2N] ranged from 2.5 to 15.9 L·kg-1 and 2.9 to 16.4 L·kg-1, respectively. The high positive correlation could be observed between the soil CEC and the Kd of Bmim]Cl] and Bmim](CF3SO2)2N](R2=0.842 9 and 0.835 3, P<0.05, respectively). In contrast, TOC exhibited the weak correlations with Kd(R2=0.003 5 and 0.073 0, P<0.01, respectively). It probably indicated that the electrostatic interaction between ILs cation and nega tively charged soil was the dominant sorption mechanism, while the hydrophobic interaction played the secondary role in ILs sorption.Addi tionally, IL anions showed an insignificant impact on the total sorption of ILs. The sorption-desorption hysteresis indexes(HI)of two ionic liquids by soils were less than 1, which was generally attributed to their irreversible binding to soil components such as clay minerals and soil organic matter. The high linear relationships between desorption HI and CEC were observed(R2 values for Bmim]Cl] and Bmim](CF3SO2)2N] were 0.772 9 and 0.781 5, P<0.01, respectively), showing CEC had a considerable influence on the sorption-desorption hysteresis of ionic liquids.
Keywords:soil properties  ionic liquids(ILs)  sorption  desorption
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