Sediment cores of up to 4 metres in depth have been collected from various locations around the coast of North Queensland. The location of the sites has been chosen on consideration of the potential for natural and anthropogenic input into the Great Barrier Reef Lagoon. Six possible sources of mercury in the sediments have been identified :-
Methodology for the digestion of sediment samples has been investigated. Digested samples were analysed by a Varian CGA-76 Cold Vapour Generator (CVG) coupled to a Varian Liberty 220 Inductively Coupled Plasma Atomic Emission Spectrometer (ICPAES) by a published method [2]. An appropriate method was developed for analysis of samples by CVG coupled to a Varian UltraMass Inductively Coupled Plasma Mass Spectrometer (ICPMS).
A comparison of results from a series of standard solutions run on both instruments will be presented. Limits of detection in solutions of standard Mercury Chloride was found to be around 10ppt for the ICPMS. Results from sediment digests will be presented. Limits of detection of mercury in digested solution were found to be 1ppb for ICPAES and 0.05ppb for ICPMS. The method and factors effecting precision and background level will be discussed.
Combined results indicate an anomalous concentration of mercury in certain levels of sediment from an area in the Great Barrier Reef Lagoon. The data will be presented and the results discussed.