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  • Presentation | B32B: Quantifying Rates and Coupling of Biogeochemical Cycles in Terrestrial Ecosystems I Oral
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  • B32B-02: An improved method for analyzing the 13C content of dissolved organic carbon in soil extracts in high-molarity salt solution
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  • Location Icon261-262
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Author(s):
Andrew Curtright, University of California Davis (First Author, Presenting Author)
Xia Zhu-Barker, University of Wisconsin Madison
William Horwath, University of California Davis


Understanding how carbon moves and changes in soil is key to addressing climate change and improving soil health. Researchers often use carbon-13 (13C) to trace where carbon goes in the environment. However, it’s been difficult and expensive to measure 13C in liquid soil extracts, where carbon is dissolved in water or salt solution. Current methods require highly specialized equipment or complicated steps that can lead to errors. In this study, we developed a simpler and more affordable method to measure 13C in soil extracts. Our technique works with commonly used salt solutions, reduces sample processing, and only requires a gas-phase analyzer. We tested this method and found it recovered more than 95% of the carbon, even at low concentrations, and could accurately detect different levels of 13C.



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