Volatile selenium fluxes from selenium-contaminated sediments in an Australian coastal lake
Michael J. Ellwood A F , Larissa Schneider B E , Jaimie Potts C , Graeme E. Batley D , John Floyd C and William A. Maher B
+ Author Affiliations
- Author Affiliations
A Research School of Earth Sciences, Australian National University, Canberra, ACT 2601, Australia.
B Institute for Applied Ecology, University of Canberra, Kirinari Street, Bruce, ACT, 2600, Australia.
C New South Wales Office of Environment and Heritage, 59–61 Goulburn Street, Sydney, NSW 2000, Australia.
D CSIRO Land and Water, Lucas Heights, NSW 2234, Australia.
E Present address: Archaeology and Natural History, Australian National University, Canberra, ACT 2601, Australia.
F Corresponding author: michael.ellwood@anu.edu.au
Environmental Chemistry 13(1) 68-75 https://doi.org/10.1071/EN14228
Submitted: 23 October 2014 Accepted: 22 April 2015 Published: 27 August 2015
Environmental context. Methylation of sedimentary selenium to volatile dimethylselenide is a natural remediation process for contaminated aquatic systems. We present flux estimates for the loss of dimethylselenide from sediments of an anthropogenically affected lake and observe a 6-fold difference between late autumn–early winter and summer. The loss of dimethylselenide represents a significant sediment loss vector, of the same order as the diffusive loss flux for inorganic selenium across the sediment–water interface.
Abstract. Overflows from ash dams associated with the operation of coal-fired power stations in Lake Macquarie, NSW, Australia, have been a historical source of selenium to the lake. Although dissolved selenium concentrations have been marginally elevated, sediments are the major sink. Methylation of sedimentary selenium to volatile dimethylselenide (DMSe) is known to be a natural remediation process. Sediments from north of Wyee Bay and the Vales Point Power Station were the subject of field sampling and monitoring to determine the extent to which selenium is being lost to the atmosphere as DMSe. Flux estimates were obtained by trapping volatile selenium species using benthic domes, followed by analysis in the field using a fully automated cryogenic trapping system with atomic fluorescence detection. The detection limit of the system was 0.1 ng L–1 for DMSe and 1 ng L–1 for dimethyl diselenide (DMDSe). Measurements in both summer and late autumn–early winter showed a distinct seasonal difference, with a higher summer DMSe flux of 53 ± 25 ng Se m–2 h–1 (±s.d.) compared with 8 ± 5 ng Se m–2 h–1 in late autumn–early winter. No DMDSe was detected. These fluxes are similar to those measured in Europe and North America, and represent an annual loss of 1.3 kg of selenium per year from the nearby lake area. Lake-wide this would represent a significant loss to the atmosphere.
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