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Ian D Clark

Publications and source records attributed to Ian D Clark.

2 recordsLinked to original sources

Using a simple high-performance liquid chromatography separation and fraction collection methodology to achieve compound-specific isotopic analysis for dissolved organic compounds.

A new application for the quantitative and isotopic analyses of dissolved inorganic and dissolved organic carbon compounds has been developed. Dissolved organic matter (DOM) in natural water samples can be separated on a high-performance liquid chromatography (HPLC) column and collected as fractions. Each discrete fraction can then be analyzed using the technique of St-Jean (Rapid Commun. Mass Spectrom. 2003; 17: 419-428) with a total inorganic carbon/total organic carbon (TIC/TOC) analyzer interfaced with a continuous-flow isotope ratio mass spectrometer. Experimental data using short-chain fatty acid standards (formic, acetic, and propionic acids) show that fraction recoveries of 100% are possible and that sample integrity is maintained. 13C-isotopic analyses of products prior to and subsequent to extraction and collection show no isotopic effects associated with the methodology, and errors are well within the accepted analytical uncertainty of the IRMS. Comparison of data from pure standards and organic-rich natural waters shows that quantitative analyses still need to be done with standards that more closely imitate the matrices of the samples, in order to acquire an appropriate calibration curve. Injections of organic-rich matrices on the HPLC column did not affect fraction recovery, nor did they create high background of partially retained organic compounds slowly released from the HPLC column, and hence 13C-isotopic results are relatively unaffected. The specific limitation on this methodology is the required use of carbon-free carrier solvents due to potential memory effects associated with the TIC/TOC analyzer. Further developments of this application could make routine compound-specific isotopic analyses (CSIA) for a wider range of organic materials possible.

Carbon Isotopes↗

Sources and circulation of water and arsenic in the Giant Mine, Yellowknife, NWT, Canada.

Recovery of gold from arsenopyrite-hosted ore in the Giant Mine camp, Yellowknife, NWT, Canada, has left a legacy of arsenic contamination that poses challenges for mine closure planning. Seepage from underground chambers storing some 237,000 tonnes of arsenic trioxide dust, has As concentrations exceeding 4000 ppm. Other potential sources and sinks of As also exist. Sources and movement of water and arsenic are traced using the isotopes of water and sulphate. Mine waters (16 ppm As; AsV/AsIII approximately 150) are a mixture of two principal water sources--locally recharged, low As groundwaters (0.5 ppm As) and Great Slave Lake (GSL; 0.004 ppm As) water, formerly used in ore processing and discharged to the northwest tailings impoundment (NWTP). Mass balance with delta18O shows that recirculation of NWTP water to the underground through faults and unsealed drillholes contributes about 60% of the mine water. Sulphate serves to trace direct infiltration to the As2O3 chambers. Sulphate in local, low As groundwaters (0.3-0.6 ppm As; delta34SSO4 approximately 4% and delta18OSO4 approximately -10%) originates from low-temperature aqueous oxidation of sulphide-rich waste rock. The high As waters gain a component of 18O-enriched sulphate derived from roaster gases (delta18OSO4) = + 3.5%), consistent with their arsenic source from the As2O3 chambers. High arsenic in NWTP water (approximately 8 ppm As; delta18OSO4 = -2%) derived from mine water, is attenuated to close to 1 ppm during infiltration back to the underground, probably by oxidation and sorption by ferrihydrite.

Arsenic↗