Ramped Temperature CO2 Evolution for Permafrost and Kolyma River Dissolved Organic Carbon
Rogers, Jennifer A
Kellerman, Anne M
Chanton, Jeffrey P
Spencer, Robert G M
This dataset is the CO2 (ppm) produced as a function of increasing temperature combustion of dissolved organic
carbon at a constant 5°C per minute ramped rate with a constant flow-through of oxygen. Dissolved organic
carbon samples were gathered from a permafrost thaw stream and the Kolyma River in northeastern Siberia and
subjected to microbial incubation degradation before investigation by ramped pyrolysis oxidation. Data is used to
create a thermogram followed by inverse modeling to garner chemical composition based on thermostability.
Samples were analyzed to determine the contribution of permafrost dissolved organic carbon to the Kolyma River.
How to cite this dataset:
Rogers, J. A., Galy, V., Kellerman, A. M., Chanton, J. P., Zimov, N., Spencer, R. G. M., 2020. Ramped Temperature CO2 Evolution for Permafrost and Kolyma River Dissolved Organic Carbon, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111617.
DOI Creation Date:
Creative Commons Attribution-ShareAlike 4.0 International [CC BY-SA 4.0]
National Science Foundation: ANT‐120
National Science Foundation: PLR‐150
National Science Foundation: DMR-164
The State of Florida
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Arctic, Kolyma River
User Contributed Keyword(s):
dissolved organic carbon, combustion, ramped pyrolysis oxidation, CO2
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