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通过矩阵分解法测定威斯康星州谢博伊根河沉积物中的多氯联苯同系物和脱氯情况。

PCB congeners and dechlorination in sediments of Sheboygan River, Wisconsin, determined by matrix factorization.

作者信息

Bzdusek Philip A, Lu Jianhang, Christensen Erik R

机构信息

Department of Civil Engineering and Mechanics and Center for Great Lakes Studies, University of Wisconsin-Milwaukee, Milwaukee, Wisconsin 53201, USA.

出版信息

Environ Sci Technol. 2006 Jan 1;40(1):120-9. doi: 10.1021/es050083p.

Abstract

Nine sediment cores were collected from the Sheboygan River Inner Harbor, WI, and analyzed for polychlorinated biphenyl (PCB) congeners. Total PCBs ranged from approximately 0 to 161 mg/g. Positive matrix factorization (PMF) was applied to the PCB data setto determine source profiles. Two factors were determined to be significant. One factor resembled the original approximated PCB mixture of 50% Aroclor 1248 and 50% Aroclor 1254 and the other factor was a dechlorinated version of the mixture. An anaerobic dechlorination model was applied to the dechlorinated source profiles to quantify possible dechlorination pathways. It was found that dechlorination process H' provided the best fit for an individual process, and H' + M provides the best fit for combined processes. PMF source contributions, and plots of PCB concentration versus congener for individual samples, provide evidence of enhanced dechlorination at high concentrations (>40 ppm) and small amounts of dechlorination at low concentrations (<3 ppm). In addition, downward migration of lower chlorinated PCBs in core SR1a has occurred. Remediation dredging in the Upper Sheboygan River in 1989 and 1990 reintroduced PCBs to the water column and selective transport of PCB 18 is observed in core SR7.

摘要

从威斯康星州谢博伊根河内港采集了9个沉积物岩芯,并对多氯联苯(PCB)同系物进行了分析。总多氯联苯含量范围约为0至161毫克/克。对多氯联苯数据集应用正矩阵因子分解(PMF)来确定源特征。确定有两个因子具有显著性。一个因子类似于原始的近似多氯联苯混合物,即50%的Aroclor 1248和50%的Aroclor 1254,另一个因子是该混合物的脱氯版本。将厌氧脱氯模型应用于脱氯源特征,以量化可能的脱氯途径。结果发现,脱氯过程H'最适合单个过程,而H'+M最适合组合过程。PMF源贡献以及单个样品的多氯联苯浓度与同系物的关系图,提供了高浓度(>40 ppm)时脱氯增强和低浓度(<3 ppm)时少量脱氯的证据。此外,在岩芯SR1a中,低氯代多氯联苯出现了向下迁移。1989年和1990年在上谢博伊根河进行的修复疏浚将多氯联苯重新引入水柱,并且在岩芯SR7中观察到了多氯联苯18的选择性迁移。

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