Pakdeesusuk Usarat, Freedman David L, Lee Cindy M, Coates John T
Department of Environmental Engineering and Science, Clemson University, Clemson, South Carolina 29634-0919, USA.
Environ Toxicol Chem. 2003 Jun;22(6):1214-20.
Lake Hartwell is a U.S. Army Corps of Engineers reservoir system located on the state line between South Carolina and Georgia, USA. The lake was contaminated with an estimated 200 metric tons of polychlorinated biphenyls ([PCBs]; mainly Aroclor 1016 and 1254), and the entire Twelve Mile Creek watershed and the Seneca River arm of Lake Hartwell were placed on the National Priorities List. Monitored natural attenuation was chosen as a remedy for the contaminated sediment. The relatively warm temperature of Lake Hartwell and lack of significant cocontaminants along with the PCBs distinguish this site from others that have been studied for microbially mediated reductive dechlorination. Microcosm studies were conducted with sediment from two locations in the Twelve Mile Creek arm and confirmed the presence of indigenous microorganisms capable of reductively dechlorinating Aroclor 1254, which contains predominantly tetra-, penta-, and hexachlorobiphenyl. The average number of total chlorines per biphenyl decreased from 4.8 to 4.9 to 2.9 to 3.0, following 250 to 260 d of incubation. The maximum observed dechlorination rates were 0.29 to 0.87 microg-atoms Cl- per gram sediment dry weight per week. The onset of dechlorination activity correlated strongly with maximum methanogenesis, which occurred without a lag in samples from the site that showed signs of in situ fermentation activity. Dechlorination occurred primarily at the meta and para positions (58-63% removal), with no apparent decrease in ortho chlorines. This most closely resembles pattern M, characterized by preferential removal of unflanked and flanked meta chlorines. The microcosm results are consistent with sediment cores analyzed from the same locations, which indicate accumulation with depth of the same ortho- and para-substituted congeners. It therefore appears that the success of monitored natural attenuation for Lake Hartwell will hinge on covering the recalcitrant PCBs with a sufficient amount of uncontaminated sediment to isolate them from the food chain.
哈特韦尔湖是美国陆军工程兵团的一个水库系统,位于美国南卡罗来纳州和佐治亚州的州界线上。该湖受到约200公吨多氯联苯([PCBs];主要是氯丹1016和1254)的污染,整个十二英里溪流域以及哈特韦尔湖的塞内卡河分支被列入国家优先污染名单。监测自然衰减被选为受污染沉积物的补救措施。哈特韦尔湖相对较高的温度以及除多氯联苯外没有显著的共污染物,这使得该场地与其他已研究微生物介导的还原脱氯的场地有所不同。对十二英里溪分支两个地点的沉积物进行了微观研究,证实存在能够对主要含有四氯、五氯和六氯联苯的氯丹1254进行还原脱氯的本土微生物。在培养250至260天后,每联苯的总氯平均数从4.8降至4.9再降至2.9至3.0。观察到的最大脱氯速率为每克沉积物干重每周0.29至0.87微克原子氯。脱氯活性的开始与最大产甲烷作用密切相关,在显示原位发酵活性迹象的场地样本中,产甲烷作用没有滞后地发生。脱氯主要发生在间位和对位(去除率为58 - 63%),邻位氯没有明显减少。这与模式M最为相似,其特征是优先去除无侧链和有侧链的间位氯。微观研究结果与从相同地点分析的沉积物岩芯一致,沉积物岩芯表明相同的邻位和对位取代同系物随深度积累。因此,哈特韦尔湖监测自然衰减的成功似乎将取决于用足够数量的未受污染沉积物覆盖顽固的多氯联苯,使其与食物链隔离。