| Citation: | ZHANG Xuefeng, YANG Jinhui, SHI Minshan. Analysis of Influencing Factors and Results Correction for Carbon and Oxygen Isotope Measurement of Soil Carbonates by Continuous-Flow Isotope Ratio Mass Spectrometry[J]. Rock and Mineral Analysis. DOI: 10.15898/j.ykcs.202505020112 |
Continuous-flow isotope ratio mass spectrometry has been widely employed for the analysis of carbon and oxygen isotopes in carbonates, operating on the principle of introducing CO2 generated from the phosphoric acid-carbonate reaction into an isotope ratio mass spectrometer for measurement. Water present in the phosphoric acid undergoes oxygen isotope exchange with the produced CO2 at a temperature-dependent rate. Due to matrix differences between soil samples and pure carbonate reference materials, a systematic evaluation is required to assess their respective responses to phosphoric acid concentration and the feasibility of standard material calibration. This study utilized a multifunctional online gas preparation system (Iso FLOW) coupled with an isotope ratio mass spectrometer (IRMS) to systematically compare the effects of different phosphoric acid concentrations and reaction temperatures on the