RESUMO
RATIONALE: A novel laser ablation-isotope ratio mass spectrometry (LA-IRMS) method for in situ analysis of sulfur isotopes in sulfides has been developed. Instead of the in situ reaction applied by the traditional laser microprobe, the analyte gas preparation in this method is separated temporally and spatially from the LA, resulting in improved precision and accuracy. METHODS: Our LA-IRMS system combines an ultraviolet LA system, an elemental analyzer (EA), a custom-built cryogenic concentration system, a continuous-flow interface, and an IRMS. The sulfide aerosol particles generated from LA were transferred by a helium carrier gas from the ablation cell into the reaction tube and were then converted into SO2 . Subsequently, SO2 was enriched in two cold traps and was finally introduced into the ion source of the IRMS through the continuous-flow interface. RESULTS: We measured three synthetic and four natural sulfide reference materials to test the performance of this method. Precisions of ±0.25-±0.48 and ±0.32-±0.64 (1SD, n = 5) for δ34 S values of synthetic and natural sulfide standards can be obtained for spot sizes ranging from 64 to 80 µm. Measured values and their recommended values showed a good linear relationship (R2 within 0.998 and 0.9995) with the slope of approaching unity (within 1.0509 and 1.1313). CONCLUSIONS: Data from the measurement of reference materials showed that the precision and accuracy of our method were satisfactory. This method is a powerful tool for in situ sulfur isotope measurement of sulfides and can be further applied to in situ carbon and oxygen isotope analyses.
RESUMO
RATIONALE: High-temperature phosphoric acid digestion combined with continuous-flow isotope ratio mass spectrometry (CF-IRMS) is one of the standard methods for the determination of carbon and oxygen isotopes in carbonate. However, the routine purification protocol has not been tested by samples with nitrate contamination. Here we show that the standard protocol is not capable of measuring such samples with satisfactory accuracy and precision. METHODS: We tested the low-temperature (25°C) phosphoric acid digestion method combined with CF-IRMS for the measurement of natural carbonate samples with ~1% nitrate concentration and nitrate-doped carbonate standards. We also recorded the Raman spectra of the gases extracted from the nitrate-doped carbonate standards to identify the gas species that affect the results. RESULTS: The accuracy and precision of δ18 O values for nitrate-doped carbonate standards digested at 72°C are much poorer than routine measurements. For the measurements of doped standards reacted at 25°C, the accuracy and precision of the δ13 C and δ18 O values are indistinguishable from normal results. Raman spectra demonstrate that NO2 generated from high-temperature digestion is the possible interference species for oxygen isotope measurement. CONCLUSIONS: Low-temperature digestion is a reliable method for the measurement of carbon and oxygen isotopes in nitrate-contaminated carbonate samples because the formation of NO2 can be largely reduced. This approach can be applied to some nitrate-rich speleothems, evaporites and other samples with nitrate contamination.