Tracing Organic Carbon Sources With Ramped Pyrolysis/Oxidation

Abstract Tracing sources of organic carbon (OC) is a critical aspect of studying surface carbon cycling. Previous methods, such as carbon and nitrogen isotopes, have struggled to separate different sources in some case studies. This study introduces a new approach for quantifying OC sources by using ramped pyrolysis/oxidation (RPO) thermograms without RPO‐fraction radiocarbon analysis. We applied matrix calculations to decompose thermograms into different endmembers contributions. This method was tested on two‐, three‐, and four‐endmember systems. The results show that the deviation in source contribution estimates is within 5%. The method was applied in tracing sources of particulate organic carbon (POC) of the Buha River, northeastern Tibetan Plateau. By analyzing the thermograms of riverine suspended sediments and their potential sources, the RPO‐based mixing model estimated that soil, vegetation, and rocks contributed approximately 89 ± 3%, 4 ± 3%, and 6 ± 3% of the POC, respectively. This study highlights the applicability of RPO in tracing OC sources.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-08-14
DOI
https://doi.org/10.1029/2025gl115321
Primary Topic
Geochemistry and Geologic Mapping
Type
article
Field-Weighted Citation Impact
0.00

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article

Tracing Organic Carbon Sources With Ramped Pyrolysis/Oxidation

Geophysical Research Letters
Geochemistry and Geologic Mapping
article

Tracing Organic Carbon Sources With Ramped Pyrolysis/Oxidation

article en

Abstract

Abstract Tracing sources of organic carbon (OC) is a critical aspect of studying surface carbon cycling. Previous methods, such as carbon and nitrogen isotopes, have struggled to separate different sources in some case studies. This study introduces a new approach for quantifying OC sources by using ramped pyrolysis/oxidation (RPO) thermograms without RPO‐fraction radiocarbon analysis. We applied matrix calculations to decompose thermograms into different endmembers contributions. This method was tested on two‐, three‐, and four‐endmember systems. The results show that the deviation in source contribution estimates is within 5%. The method was applied in tracing sources of particulate organic carbon (POC) of the Buha River, northeastern Tibetan Plateau. By analyzing the thermograms of riverine suspended sediments and their potential sources, the RPO‐based mixing model estimated that soil, vegetation, and rocks contributed approximately 89 ± 3%, 4 ± 3%, and 6 ± 3% of the POC, respectively. This study highlights the applicability of RPO in tracing OC sources.

Geophysical Research LettersVol. 52(16)
Shanghai Jiao Tong University (CN), Chinese Academy of Sciences (CN), Northwest University (CN), Institute of Earth Environment (CN)
National Natural Science Foundation of China, National Key Research and Development Program of China
Life in Land
Openalex Percentile: Top 63%
Geochemistry and Geologic Mapping
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