Jiang Xia, Yediler Ayfer, Yufang Song, Sun Tieheng, Kettrup Antonius
Institute of Applied Ecology, Chinese Academy of Sciences, P.O. Box 417, Shenyang 110015, PR China.
Chemosphere. 2005 Nov;61(5):741-51. doi: 10.1016/j.chemosphere.2005.03.098. Epub 2005 Jul 12.
The aim of this work was to evaluate the effect of linear alkylbenzene sulfonate (LAS, 200 mg l(-1)) on the fate of phenanthrene in a model ecosystem "water-lava-hydrophytes-air". The experiments were conducted using two closed cultivation chamber systems. Rushes (Juncus effesus) were selected as a representative hydrophyte. Five hundred micrograms per liter of phenanthrene in a culture solution containing a 14C-activity of 75 microCi per chamber was applied (i) to investigate the degradation of the labeled test substance and the transfer processes within the system; (ii) to determine the mass-balance possible and (iii) to detect the occurrence of volatile test substances, their volatile metabolites and the degradation end-product CO2 in the gas phase. Most of the applied 14C-activity was found in the plant (41-45%), in which approximately 95% was associated with plant roots and approximately 5% with shoots. The 14C-activity recovered in the form of VOCs and CO2 was measured in lava (18-29%, 8-11%), and in the culture solution (10-14% and 1%), respectively. Majority of the applied 14C-activity existed in two forms, i.e. (1) polar metabolites (26%), of which 91% were found in plant roots, and (2) un-extractable residues (23%), most of which were in plant roots (40%) and bounded to lava (58%). The presence of LAS significantly increased the volatilization of phenanthrene and its metabolites, inhibited its mineralization and decreased the level of 14C-activity in lava. Moreover, LAS reduced the phenanthrene level in plant roots.
本研究旨在评估线性烷基苯磺酸盐(LAS,200毫克/升)对菲在“水-熔岩-水生植物-空气”模型生态系统中归宿的影响。实验使用了两个封闭培养箱系统。灯心草(Juncus effesus)被选为代表性水生植物。向每个培养箱中含有75微居里14C活性的培养液中施加每升500微克的菲,以(i)研究标记测试物质的降解及系统内的转移过程;(ii)确定可能的质量平衡;(iii)检测气相中挥发性测试物质、其挥发性代谢物及降解终产物二氧化碳的存在情况。大部分施加的14C活性存在于植物中(41%-45%),其中约95%与植物根系相关,约5%与地上部分相关。以挥发性有机化合物和二氧化碳形式回收的14C活性分别在熔岩(18%-29%,8%-11%)和培养液(10%-14%和1%)中测得。大部分施加的14C活性以两种形式存在,即(1)极性代谢物(26%),其中91%存在于植物根系中,(2)不可提取残留物(23%),其中大部分存在于植物根系中(40%)并与熔岩结合(58%)。LAS的存在显著增加了菲及其代谢物的挥发,抑制了其矿化,并降低了熔岩中14C活性水平。此外,LAS降低了植物根系中的菲含量。