Abstract
Monitoring changes in stable oxygen isotope ratios in molecular oxygen allows for studying many fundamental processes in bio(geo)chemistry and environmental sciences. While the measurement of ^{18}O/^{16}O ratios of mathrm {O}_{2} in gaseous samples can be carried out conveniently and from extracting moderately small aqueous samples for analyses by continuous-flow isotope ratio mass spectrometry (CF-IRMS), oxygen isotope signatures, updelta ^{18}O, could be overestimated by more than 6permille because of interferences from argon in air. Here, we systematically evaluated the extent of such Ar interferences on ^{18}O/^{16}O ratios of mathrm {O}_{2} for measurements by gas chromatography/IRMS and GasBench/IRMS and propose simple instrumental modifications for improved Ar and mathrm {O}_{2} separation as well as post-measurement correction procedures for obtaining accurate updelta ^{18}O. We subsequently evaluated the consequences of Ar interferences for the quantification of O isotope fractionation in terms of isotope enrichment factors, upepsilon _{mathrm {O}}, and ^{18}O kinetic isotope effects (^{18}O KIEs) in samples where mathrm {O}_{2} is consumed and Ar:mathrm {O}_{2} ratios increase steadily and substantially over the course of a reaction. We show that the extent of O isotope fractionation is overestimated only slightly and that this effect is typically smaller than uncertainties originating from the precision of updelta ^{18}O measurements and experimental variability. Ar interferences can become more relevant and bias upepsilon _{mathrm {O}} values by more than 2permille in aqueous samples where fractional mathrm {O}_{2} conversion exceeds 90%. Practically, however, such samples would typically contain less than 25 upmuM of mathrm {O}_{2} at ambient temperature, an amount that is close to the method detection limit of ^{18}O/^{16}O ratio measurement by CF-IRMS.Graphical abstract
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