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Absolute 13C/12C Isotope Amount Ratio for Vienna Pee Dee Belemnite from Infrared Absorption Spectroscopy
Adam J Fleisher1,2, Hongming Yi1,2,3, Abneesh Srivastava1
1Material Measurement Laboratory, National Institute of Standards and Technology, Gaithersburg, MD, USA.
Stable carbon isotope ratio measurements are advancing with a new infrared spectroscopy method. This technique offers SI-traceable isotope analysis and improves CO2 source apportionment studies.
Area of Science:
- Geochemistry
- Analytical Chemistry
- Metrology
Background:
- Stable isotope ratio measurements rely on reference standards, historically the Vienna Pee Dee Belemnite (VPDB) scale.
- The original VPDB standard is depleted, and current reference materials face issues of exhaustion and compositional instability.
- This mirrors challenges in metrology, such as the redefinition of the International System of Units.
Purpose of the Study:
- To report an accurate, independent measurement of the stable carbon isotope ratio of VPDB.
- To validate infrared absorption spectroscopy as a fundamentally accurate method for isotope analysis.
- To support ongoing efforts to redefine the VPDB scale and advance SI-traceable isotope measurements.
Main Methods:
- Utilizing infrared absorption spectroscopy for direct measurement of the stable carbon isotope ratio.
- Employing a calibration-free approach to enhance accuracy and traceability.
- Comparing results with values derived from mass spectrometry.
Main Results:
- An accurate value for the stable carbon isotope ratio was determined using infrared absorption spectroscopy.
- The results align with recently reported mass spectrometry data, validating the new approach.
- The findings support the development of SI-traceable isotope analysis.
Conclusions:
- Infrared absorption spectroscopy provides a reliable, calibration-free method for stable carbon isotope ratio determination.
- This advancement aids in establishing SI-traceable isotope standards and improving CO2 source apportionment.
- The method holds potential for enhancing isotopic tracer studies and mass balance calculations.
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