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Triple oxygen and hydrogen stable isotope composition of water in Murchison carbonaceous chondrite accessed by thermogravimetry-enabled laser spectroscopy
Chemical Geology ( IF 3.6 ) Pub Date : 2024-12-09 , DOI: 10.1016/j.chemgeo.2024.122557
Erik J. Oerter, Alexandre Garenne, Miguel Cisneros, George D. Cody, Michael Singleton, Conel M. O’D. Alexander

We have developed the capability to measure 17O/16O in H2O and OH of hydrous minerals by a technique using thermogravimetric analysis coupled with isotope ratio infrared spectroscopy (TGA-IRIS) on a suite of liquid water standards, terrestrial mineral standards, multi-mineral synthetic mixtures of terrestrial samples, and Murchison carbonaceous chondrite. This 17O/16O analytical capability is combined with the previously developed TGA-IRIS capability of 18O/16O, which enables us to calculate Δ`17O values. Additionally, we have made 2H/1H measurements by TGA-IRIS on the suite of materials. Analyses of 328 standard water samples sealed into silver tubes (0.25 μL, 174 VSMOW and 154 GISP) analyzed over the course of three years yielded δ18O values by TGA-IRIS with precision of ±0.30 ‰, δ17O of ±0.24 ‰, Δ`17O of ±0.126 ‰, and δ2H ± 7.5 ‰ (± 1 Std. Dev.). TGA-IRIS analyses of a suite of hydrous minerals (oxy-hydroxide, mica, serpentines, sulfide, phyllosillicates) yields similar precision. TGA-IRIS analyses of the CM2 carbonaceous chondrite Murchison resulted in δ18O, δ17O, Δ`17O, and δ2H values of the H2O and/or OH from its hydrous minerals. Δ`17O values of Murchison H2O range from 1.034 ‰ at 350 °C, to −0.368 ‰ at 650 °C, to −1.75 ‰ at 850 °C. TGA-IRIS can generate Δ`17O values of H2O and/or OH in hydrous materials that are well within the precision needed for the analysis of meteoritic samples, as well as samples returned from asteroids, such as Ryugu and Bennu.
更新日期:2024-12-09
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