Historical deposition of persistent organic pollutants in Lake Victoria and two alpine equatorial lakes from East Africa: Insights into atmospheric deposition from sedimentation profiles

被引:14
作者
Arinaitwe, Kenneth [1 ]
Rose, Neil L. [2 ]
Muir, Derek C. G. [3 ]
Kiremire, Bernard T. [1 ]
Balirwa, John S. [4 ]
Teixeira, Camilla [3 ]
机构
[1] Makerere Univ, Dept Chem, Kampala, Uganda
[2] UCL, Environm Change Res Ctr, London, England
[3] Environm Canada, Aquat Contaminants Res Div, Burlington, ON L7R 4A6, Canada
[4] Natl Fisheries Resources Res Inst NaFIRRI, Jinja, Uganda
关键词
Atmospheric deposition; Sedimentation; Persistent organic pollutant; Lake Victoria; East Africa; Mountain lakes; FINAL GLOBAL SINK; SEA DWELLING FISH; ORGANOCHLORINE PESTICIDES; RWENZORI MOUNTAINS; SOUTH ATLANTIC; POINT-SOURCE; DEEP-SEA; RESIDUES; PCBS; AIR;
D O I
10.1016/j.chemosphere.2015.10.061
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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 Sigma DDTs, polychlorinated biphenyls (Sigma PCBs), hexachlorocyclohexanes (Sigma HCHs) and chlordanes (Sigma CHLs) were 390, 230, 210 and 120 ng m(-2) yr(-1). Higher fluxes of Sigma DDTs, Sigma PCBs, and Sigma CHLs 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, Sigma CHLs 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. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1815 / 1822
页数:8
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