Xie Mei, Yang Ze-Yu, Bao Lian-Jun, Zeng Eddy Y
State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China.
J Chromatogr A. 2009 May 22;1216(21):4553-9. doi: 10.1016/j.chroma.2009.03.075. Epub 2009 Apr 1.
A conventional solid-phase microextraction (SPME) method combined with liquid-liquid extraction was applied under equilibrium and nonequilibrium conditions to determine the partition coefficients (K(doc)) of 25 polychlorinated biphenyl congeners (PCBs) between Sigma-Aldrich humic acid (HA) and water. The values of log K(doc) determined with equilibrium SPME were linearly correlated with the logarithm of the octanol-water partition coefficients (K(ow)) for PCB congeners at logK(ow)< approximately 7.2, but the trends were disrupted for logK(ow) from approximately 7.2 to 8.18. In addition, short-term (5 min to 4 days) and long-term (5-44 days) uptake profiles of PCBs were established, from which a pseudo-equilibrium for sorption of PCBs was revealed at approximately 4 days of extraction. To understand this phenomenon, the uptake profiles were fitted with two equations (one equation is often used for pure water samples and the other one is applicable for samples containing complex matrices) derived from a first-order kinetics model. Subsequently, K(doc) values obtained through kinetic approaches were compared with those acquired from equilibrium SPME. The comparison of K(doc) values indicated that the pseudo-equilibrium was caused by the slow desorption of PCBs from HA rather than the biphasic desorption mechanism.
采用结合液-液萃取的传统固相微萃取(SPME)方法,在平衡和非平衡条件下测定了25种多氯联苯同系物(PCBs)在西格玛奥德里奇腐殖酸(HA)和水之间的分配系数(K(doc))。在logK(ow)<约7.2时,用平衡SPME测定的log K(doc)值与PCBs同系物的正辛醇-水分配系数(K(ow))的对数呈线性相关,但当logK(ow)从约7.2到8.18时,趋势被打乱。此外,还建立了PCBs的短期(5分钟至4天)和长期(5 - 44天)摄取曲线,从中发现在萃取约4天时PCBs的吸附达到了准平衡。为了解这一现象,摄取曲线用从一级动力学模型推导的两个方程(一个方程常用于纯水样品,另一个适用于含有复杂基质的样品)进行拟合。随后,将通过动力学方法获得的K(doc)值与从平衡SPME获得的值进行比较。K(doc)值的比较表明,准平衡是由PCBs从HA的缓慢解吸引起的,而不是双相解吸机制。