Serrano Antonio, Gallego Mercedes, González José Luis
Department of Analytical Chemistry, Campus of Rabanales, University of Córdoba, E-14071 Córdoba, Spain.
Environ Pollut. 2006 Nov;144(1):203-9. doi: 10.1016/j.envpol.2005.12.031. Epub 2006 Feb 28.
A diesel fuel spill was simulated on a 12-m(2) plot of agricultural land, at a concentration of 1 Lm(-2) of soil. The natural attenuation of Volatile Aromatic Hydrocarbons (VAHs) was monitored at different soil depths over a period of 50 days. The natural attenuation of VAHs in the surface layer would be attributed to two processes, namely: volatilisation (mainly linked to the boiling point of each VAH, with t(1/2) from 2 to 71 min for benzene and p-isopropyltoluene, respectively); and dissipation (related to the boiling point as well as the analyte-soil matrix interaction, with t(1/2) from 2 to 169 h for benzene and p-isopropyltoluene, respectively). As expected, in the deeper layers, dissipation prevails over volatilisation. 50 days after the spill, only two VAHs were detected in the surface layer, at concentrations of 5-20 ngg(-1), which had disappeared after 80 days of the spill.
在一块12平方米的农田上模拟柴油泄漏,土壤中柴油浓度为1升/平方米。在50天的时间里,对不同土壤深度的挥发性芳烃(VAHs)的自然衰减情况进行了监测。表层VAHs的自然衰减可归因于两个过程,即:挥发(主要与每种VAH的沸点有关,苯和对异丙基甲苯的半衰期分别为2至71分钟);以及消散(与沸点以及分析物 - 土壤基质相互作用有关,苯和对异丙基甲苯的半衰期分别为2至169小时)。正如预期的那样,在较深层中,消散作用超过挥发作用。泄漏50天后,表层仅检测到两种VAHs,浓度为5 - 20纳克/克,在泄漏80天后这些VAHs消失了。