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直链烷基苯磺酸盐(LAS)对模型生态系统(水-熔岩-植物-空气)中14C-菲矿化、代谢及吸收的影响

Effect of linear alkylbenzene sulphonate (LAS) on the mineralization, metabolism and uptake of 14C-phenanthrene in a model ecosystem (water-lava-plant-air).

作者信息

Jiang Xia, Yediler Ayfer, Yufang Song, Sun Tieheng, Kettrup Antonius

机构信息

Institute of Applied Ecology, Chinese Academy of Sciences, P.O. Box 417, Shenyang 110015, PR China.

出版信息

Chemosphere. 2005 Nov;61(5):741-51. doi: 10.1016/j.chemosphere.2005.03.098. Epub 2005 Jul 12.

Abstract

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.

摘要

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。

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