Journal
JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY
Volume 27, Issue 12, Pages 2123-2131Publisher
ROYAL SOC CHEMISTRY
DOI: 10.1039/c2ja30215b
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Funding
- Directorate For Geosciences
- Division Of Ocean Sciences [1131387] Funding Source: National Science Foundation
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Double spike techniques are widely used for measuring the isotopic composition of natural samples. In order to achieve the most accurate results by double spike analysis, it is important to choose an appropriate double-spike composition, analyte concentration, and spike to natural ratio (C-spk/C-nat) where C-nat is the concentration of a sample or standard with a natural abundance of the isotopes and C-spk is the concentration of an added spike with an unnatural isotope composition. Here, the effect of varying these parameters is explored using a Monte Carlo technique which simulates error from counting statistics, Johnson noise, and isobaric interferences. Typically, optimal spike composition and C-spk/C-nat are calculated under the constraint that total concentration of spike plus sample (C-spk + C-nat) must remain constant, so that as the amount of double spike is increased, the amount of sample is decreased. In practice, there is no reason for C-spk + C-nat to be held constant, because an analyst with a fixed quantity of sample may add any amount of spike to this sample as long as detector limits are not exceeded. Therefore, here, double spikes are here optimized while allowing C-spk and C-nat to vary independently. For thirty three different elements, this new approach of allowing C-spk and C-nat to vary independently led to a decrease in theoretical error of up to similar to 30% in the absence of isobaric interferences. In the presence of isobaric interferences, this approach can deliver even larger improvements in accuracy and precision. Theoretical error is then compared to observed error both for delta Fe-56 standards and for delta Fe-56, delta Zn-66, and delta Cd-114 measured in seawater. Theoretical error and measured error for real seawater samples are highly correlated, with 78%, 85%, and 96% of observed error in delta Fe-56, delta Zn-66, and delta Cd-114, respectively, accounted for using an error model which includes only Johnson noise and counting statistics. This confirms that such models, which minimize theoretical error, can be used to optimize spike composition, C-spk, and C-nat in order to increase accuracy and precision for analysis of natural samples.
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