Measurement of labile Cu in soil using stable isotope dilution and isotope ratio analysis by ICP-MS |
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Authors: | Annette L. Nolan Yibing Ma Enzo Lombi Mike J. McLaughlin |
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Affiliation: | (1) Centre for Environmental Contaminants Research, CSIRO Land and Water, PMB 2, Glen Osmond, SA 5064, Australia;(2) Present address: National Measurement Institute, PO Box 385, Pymble, NSW 2073, Australia;(3) Institute of Soil and Fertilizers, Chinese Academy of Agricultural Sciences, Beijing, China;(4) Soil and Land Systems, School of Earth and Environmental Sciences, The University of Adelaide, PMB 1, Glen Osmond, SA 5064, Australia |
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Abstract: | Isotope dilution is a useful technique to measure the labile metal pool, which is the amount of metal in soil in rapid equilibrium (<7 days) with the soil solution. This is normally performed by equilibrating soil with a metal isotope, and sampling the labile metal pool by using an extraction (E value), or by growing plants (L value). For Cu, this procedure is problematic for E values, and impossible for L values, due to the short half-life of the 64Cu radioisotope (12.4 h), which makes access and handling very difficult. We therefore developed a technique using enriched 65Cu stable isotope and measurement of 63Cu/65Cu ratios by quadrupole inductively coupled plasma mass spectrometry (ICP-MS) to measure labile pools of Cu in soils using E value techniques. Mass spectral interferences in detection of 63Cu/65Cu ratios in soil extracts were found to be minimal. Isotope ratios determined by quadrupole ICP-MS compared well to those determined by high-resolution (magnetic sector) ICP-MS. E values determined using the stable isotope technique compared well to those determined using the radioisotope for both uncontaminated and Cu-contaminated soils. |
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Keywords: | Soil Copper Labile pool Isotope dilution Isotope ratios ICP-MS |
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