Errors in the solutions of a set of equations representing an experimental system: a case study for the simultaneous determination of 13C/12C, 17O/16O and 18O/16O abundance ratios as CO2+
Abstract
The relationships between experimental-cum-input errors ([not partial differential]Ri's) and the errors ([not partial differential]Em's) of solutions (Em's), corresponding to a somewhat generalized and representative experimental case of any given three simultaneous equations (fi({Em}) = Ri (i, m = 1, 2, 3)), are worked out. It is shown that the [not partial differential]Em's are, however, solutions of the corresponding characteristic differential relationships, fi({[not partial differential]Em}) = [not partial differential]Ri (i, m = 1, 2, 3). Verification of this finding, and/or its implication that derived parameters might turn out better or even worse representative of the investigating system than corresponding experimental quantities, is provided in terms of simultaneous determination of carbon and oxygen isotopic abundance ratios (Em's) via isotopic CO2+ abundance ratios (Ri's). The CO2+-system offers not just (required) 3 but 15 different Ri = fi({Em}) = fi(E13/12, E17/16, E18/16) relationships. In addition, the well-known oxygen-systems based formula, (with R[alpha] and [beta] as chosen constants), is often used to represent the CO2+-system. All such relevant relationships are discussed, and it is shown how can different typical sets of their combinations of required three be solved for the desired Em's. It is demonstrated how the desired results (solutions: Em's) vary with input errors, and examined whether the rate of such variations are governed by the choice of the required three representative equations (monitors) and/or by the (magnitudes of) Em's themselves. Essentially, more than providing a hitherto unexamined but required background for accurate simultaneous determination of 13C/12C, 17O/16O and 18O/16O abundance ratios as CO2+, it is clarified that acceptable accuracy in measurements alone cannot ensure the conclusions of indirect experimental studies to be always valid. The fundamental requirement is shown to be the [`]a priori' examining of the role of computational step involved in defining the errors ([not partial differential]Em's) in desired results (Em's), and hence to accordingly design the experiment to be carried out. It is thus in the case of working CO2+-system pointed out that "", if employed as a monitor, acts as however a purely theoretical tool, and shown how the process of evaluation of corresponding results itself sets the guideline for correctly choosing its parameters (R[alpha] and [beta]) and yielding the desired results equally as accurate as, or even more accurate than, the measurements involved.
- Publication:
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International Journal of Mass Spectrometry
- Pub Date:
- October 2004
- DOI:
- Bibcode:
- 2004IJMSp.237..135D
- Keywords:
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- Carbon;
- Oxygen;
- Isotopic analysis;
- Error;
- Error propagation