Investigations into the PCDD contamination of topsoil, river sediments and kaolinite clay in Queensland, Australia

• Published in: Chemosphere (Oxford) 2002-03, Vol.46 (9), p.1335-1342
• Main Authors: Prange, Joelle A, Gaus, Caroline, Päpke, Olaf, Müller, Jochen F
• Format: Article
• Language: English
• Subjects: Aluminum Silicates - chemistry; Applied sciences; Australia; Australia, Queensland; Clay; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Environmental Monitoring; Exact sciences and technology; Freshwater; Geologic Sediments - chemistry; Kaolin - chemistry; Natural formation; Octachlorodibenzo- p-dioxin; PCDD/Fs; Pollution; Pollution sources. Measurement results; Pollution, environment geology; Polychlorinated Dibenzodioxins - analogs & derivatives; Polychlorinated Dibenzodioxins - analysis; Soil and sediments pollution; Soil Pollutants - analysis; Sources
• ISSN: 0045-6535; 1879-1298
• DOI: 10.1016/S0045-6535(01)00266-1

Recent findings of elevated PCDDs from an unknown source in the coastal marine environment of Queensland, Australia has instigated further investigations into the distribution of, and environments associated with the PCDD contamination. This study presents data for OCDD concentrations in the coastal, mountainous and inland environment of Queensland. Additionally, full 2,3,7,8-substituted polychlorinated dibenzo- p-dioxins and dibenzofuran (PCDD/F) profiles from different land-use types and environments in the coastal region were analysed. Distinct east–west gradients were detected in topsoil collected from various bushland regions with elevated OCDD concentrations confined to the coastal region. However, PCDD/F results from topsoil and river sediments collected in the Queensland coastal region suggest that elevated OCDD concentrations cannot be attributed to any of the environments, land-use or industry types investigated. PCDD/F congener profiles from select samples were remarkably similar to those previously described in marine sediments collected along the entire Queensland coastline. In addition, kaolinite clay samples from Queensland exhibited elevated OCDD concentrations, and PCDD/F profiles in these samples were similar to those detected in kaolinite clays elsewhere. Natural formation processes have been hypothesised as the source of elevated PCDDs in Queensland and other locations, where similar PCDD/F profiles and the general lack of anthropogenic sources are evident. This study presents additional data supporting this hypothesis and provides further information that may assist in the identification of the processes involved in the natural formation of PCDDs.