Determining the History and Sources of Contaminants in Sediments in the Tamar Estuary, Tasmania, Using 210Pb Dating and Stable Pb Isotope Analyses
Andrew Seen A E , Ashley Townsend B , Bonnie Atkinson A , Joanna Ellison C , Jennifer Harrison D and Henk Heijnis DA School of Chemistry, University of Tasmania, Launceston TAS 7250, Australia.
B Central Science Laboratory, University of Tasmania, Hobart TAS 7001, Australia.
C School of Geography and Environmental Studies, University of Tasmania, Launceston TAS 7250, Australia.
D Australian Nuclear Science and Technology Organisation (ANSTO), Menai NSW 2234, Australia.
E Corresponding author (e-mail: A.J.Seen@utas.edu.au).
Environmental Chemistry 1(1) 49-54 https://doi.org/10.1071/EN04011
Submitted: 22 March 2004 Accepted: 30 April 2004 Published: 30 June 2004
Environmental Context. Dating estuary sediments provides insights into the materials entering the estuary and can pinpoint when the contamination occurred. Heavy metal contamination is a known health risk but attributing it to a source can be contentious. For a sample sourced downstream of a city and a mining region, lead-210 dating and stable lead isotope analyses uncovered the sources of lead inputs. These methods quantified the extent that upstream mining activities and, for the first time, the extent that non-mining inputs (vehicles, industry) contributed to the estuary’s pollution.
Abstract. 210Pb dating and heavy metal analyses (Cd, Cu, Pb, Zn) have been combined to establish an historical profile of pollutant levels in sediments in the Tamar Estuary (Tasmania, Australia) over the past century. Heavy metal profiles through the core show a strong correlation with mining activities and industrialization during the past century, reflecting catchment disturbance in one of Australia’s earliest settled areas. A source apportionment of Pb in the sediment core using stable Pb isotope ratios (204Pb, 206Pb, 207Pb, 208Pb) shows that mine pollution has been contributing 10–25 mg kg–1 to Tamar Estuary sediments since the start of mining in the early 1890s, whilst non-mining inputs were not significant until post-1930 and became increasingly significant post-World War II. Since the 1950s–1960s, non-mining anthropogenic Pb inputs have become as significant as Pb from mining activities, although there does appear to be a decline in non-mining inputs during the past 20 years, which is consistent with findings elsewhere where reductions in atmospheric Pb levels have been observed and are attributed to the phasing-out of leaded gasoline. The source apportionment does, however, suggest that Pb from mine pollution at Storys and Aberfoyle Creeks continues to impact upon upper Tamar Estuary sediment quality.
Keywords. : contaminant deposition — geochemistry (inorganic) — lead — source characterization
Acknowledgements
The authors are grateful for the support of a University of Tasmania Institutional Research Grant Scheme Award and an AINSE Research Grant for this work. Dr Gregg Brunskill and Mr John Pfitzner are thanked for their contributions to understanding the unsupported 210Pb profile.
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