Cited by 306Soil Carbon and Nitrogen DynamicsFire effects on ecosystemsSoil and Environmental Studies

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Stability of black carbon in soils across a climatic gradient

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Cheng, Chih‐Hsin, Lehmann, Johannes, Thies, Janice E., Burton, Sarah D.·2008·Journal of Geophysical Research: Biogeosciences

DOI 10.1029/2007jg000642

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Abstract

The recalcitrant properties of black carbon (BC) grant it to be a significant pool of stable organic C (OC) in soils. Up to now, however, the longevity of BC under different climates is still unclear. In this study, we used BC samples from historical charcoal blast furnace sites to examine the stability of BC across a climatic gradient of mean annual temperatures (MAT) from 3.9 to 17.2°C. The results showed that OC concentration and OC storage in the BC‐containing soils at a soil depth of 0–0.2 m were 9.0 and 4.7 times higher than those in adjacent soils, respectively. Organic C in the BC‐containing soils was more stable, with a significantly lower amount of the labile OC fraction (4.4 mg g−1 OC versus 27.5 mg g−1 OC) and longer half‐life of the recalcitrant OC fraction (59 years versus 9 years) than the adjacent soils determined by incubation experiments. The stability of BC was primarily due to its inherently recalcitrant chemical composition as suggested by short‐term incubation and solid state 13 C nuclear magnetic resonance spectra of isolated BC particles. A significant negative relationship between OC storage and MAT further indicated that OC storage was decreased with warmer climate. However, the lack of a relationship between MAT and BC mineralization suggested that the stability of the remaining BC was similar between sites with very different MAT. Despite the fact that warming or cooling result in immediate consequences for BC stocks, it may have little impact on the stability of remaining BC over the period studied.

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Beltrá, J. C. (2024) · Digital Repository (Polytechnic University of Cartagena) · doi:10.31428/10317/13763
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Nguyen, B. T. (2009) · eCommons (Cornell University)
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Asrat, Z., Fekadu, M., Woldu, Z., Demissew, S., Mekonnen, B., Opgenoorth, L., Miehe, G., & Zech, W. (2026) · Soil Systems · doi:10.3390/soilsystems10050058

Authors: Cheng, C., Lehmann, J., Thies, J. E., & Burton, S. D.
Affiliations: Cornell University (US)
Pacific Northwest National Laboratory (US)
ORCID: Cheng, Chih‐Hsin
Lehmann, Johannes
Thies, Janice E.
Burton, Sarah D.
Venue: Journal of Geophysical Research: Biogeosciences
Publisher: American Geophysical Union (AGU)
Published: 2008-06
Volume: 113
Issue: G2
ISSN: 0148-0227 (ISSN-L)
DOI: 10.1029/2007jg000642
OpenAlex: W2080826644
Cited by: 306
References: 47
Citations by year: 2026: 9 · 2025: 3 · 2024: 14 · 2023: 12 · 2022: 9 · 2021: 13 · 2020: 21 · 2019: 17 · 2018: 17 · 2017: 27 · 2016: 16 · 2015: 23 · 2014: 26 · 2013: 29 · 2012: 22
FWCI: 24.30
Type: journal article
Language: en
Open access: bronze
doi.org
Licence: onlinelibrary.wiley.com/termsAndConditions#vor (vor, 3 d)
Locations: Journal of Geophysical Research Atmospheres (publishedVersion)
Funders: Pacific Northwest National Laboratory
Topics: Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
Physical Sciences › Environmental Science › Global and Planetary Change › Fire effects on ecosystems
Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil and Environmental Studies
Keywords: black carbon, soil organic carbon, carbon stability, recalcitrant carbon, mean annual temperature, climate gradients, organic carbon storage, labile carbon, organic carbon mineralization, solid-state 13C NMR, soil warming

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Stability of black carbon in soils across a climatic gradient

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