Arinaitwe Kenneth, Rose Neil L, Muir Derek C G, Kiremire Bernard T, Balirwa John S, Teixeira Camilla
Chemistry Department, Makerere University, Kampala, Uganda.
Environmental Change Research Centre, University College London, London, UK.
Chemosphere. 2016 Feb;144:1815-22. doi: 10.1016/j.chemosphere.2015.10.061. Epub 2015 Nov 11.
Information on historical deposition of persistent organic pollutants (POPs) for African lakes is very limited. We investigated historical deposition trends and sources of POPs in sediment cores from Lakes Victoria (SC1), Bujuku (Buju2) and Mahoma (Maho2). The latter two lakes are situated in the Rwenzori mountain range in western Uganda. SC1 was taken from a central depositional area within the Ugandan part of the lake. Profiles in Buju2 and Maho2 were used as a reference for historical atmospheric deposition. For the post-1940 sediment deposits in SC1, average focusing factor-adjusted fluxes (FFFs) of ΣDDTs, polychlorinated biphenyls (ΣPCBs), hexachlorocyclohexanes (ΣHCHs) and chlordanes (ΣCHLs) were 390, 230, 210 and 120 ng m(-2) yr(-1). Higher fluxes of ΣDDTs, ΣPCBs, and ΣCHLs were observed in Buju2 and Maho2. The average FFF of HCB in Buju2 was the highest while the values for Maho2 and SC1 were similar. The endosulfan FFFs in SC1 were lower than in the alpine lake cores. Generally, Buju2 was a better reference for historical atmospheric deposition of POPs than Maho2 probably due to distortion of the latter's profile by Lake Mahoma's forested catchment. Profiles of p,p'-DDE, ΣCHLs and HCB in SC1 were consistent with atmospheric deposition while profiles of PCBs and HCHs were indicative of particle-bound loadings from additional sources. Profiles of endosulfans, DDTs, and chlordanes were consistent with influence of other factors such as anoxia, and dilution. Further studies of spatial resolution of historical deposition, especially in near-shore deposition areas of the lake are recommended.
关于非洲湖泊持久性有机污染物(POPs)历史沉积的信息非常有限。我们调查了维多利亚湖(SC1)、布朱库湖(Buju2)和马霍马湖(Maho2)沉积物岩芯中POPs的历史沉积趋势和来源。后两个湖泊位于乌干达西部的鲁文佐里山脉。SC1取自该湖乌干达部分的一个中央沉积区。Buju2和Maho2的岩芯剖面用作历史大气沉积的参考。对于SC1中1940年后的沉积物,滴滴涕总量(ΣDDTs)、多氯联苯(ΣPCBs)、六氯环己烷(ΣHCHs)和氯丹(ΣCHLs)的平均聚焦因子校正通量(FFFs)分别为390、230、210和120 ng m(-2) yr(-1)。在Buju2和Maho2中观察到更高的ΣDDTs、ΣPCBs和ΣCHLs通量。Buju2中六氯苯的平均FFFs最高,而Maho2和SC1的值相似。SC1中硫丹的FFFs低于高山湖泊岩芯。一般来说,Buju2比Maho2更适合作为POPs历史大气沉积的参考,这可能是由于马霍马湖森林覆盖的集水区使后者的剖面发生了扭曲。SC1中p,p'-滴滴伊、ΣCHLs和六氯苯的剖面与大气沉积一致,而多氯联苯和六氯环己烷的剖面表明有来自其他来源的颗粒结合负荷。硫丹、滴滴涕和氯丹的剖面与缺氧和稀释等其他因素的影响一致。建议进一步研究历史沉积的空间分辨率,特别是在湖泊近岸沉积区。