Articles | Volume 16, issue 3
https://doi.org/10.5194/bg-16-663-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-16-663-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
04 Feb 2019
Research article |
| 04 Feb 2019
| 04 Feb 2019
Modeling anaerobic soil organic carbon decomposition in Arctic polygon tundra: insights into soil geochemical influences on carbon mineralization
Jianqiu Zheng
Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN
37931, USA
Peter E. Thornton
Environmental Sciences Division, Oak Ridge National Laboratory, Oak
Ridge, TN 37931, USA
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, TN 37931, USA
Scott L. Painter
Environmental Sciences Division, Oak Ridge National Laboratory, Oak
Ridge, TN 37931, USA
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, TN 37931, USA
Baohua Gu
Environmental Sciences Division, Oak Ridge National Laboratory, Oak
Ridge, TN 37931, USA
Stan D. Wullschleger
Environmental Sciences Division, Oak Ridge National Laboratory, Oak
Ridge, TN 37931, USA
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, TN 37931, USA
Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN
37931, USA
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, TN 37931, USA
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Cited
18 citations as recorded by crossref.
- Increasing Organic Carbon Biolability With Depth in Yedoma Permafrost: Ramifications for Future Climate Change J. Heslop et al. 10.1029/2018JG004712
- Theoretical Constraints on Fe Reduction Rates in Upland Soils as a Function of Hydroclimatic Conditions S. Calabrese et al. 10.1029/2020JG005894
- Limitations of the Q10 Coefficient for Quantifying Temperature Sensitivity of Anaerobic Organic Matter Decomposition: A Modeling Based Assessment Q. Wu et al. 10.1029/2021JG006264
- Simulated Hydrological Dynamics and Coupled Iron Redox Cycling Impact Methane Production in an Arctic Soil B. Sulman et al. 10.1029/2021JG006662
- Multi-scale temporal variation in CH4 and CO2 exchange and associated biophysical controls from two wetlands in Northeast China L. Sun et al. 10.1016/j.agrformet.2023.109818
- Representing methane emissions from wet tropical forest soils using microbial functional groups constrained by soil diffusivity D. Sihi et al. 10.5194/bg-18-1769-2021
- Microbe-iron interactions control lignin decomposition in soil C. Liao et al. 10.1016/j.soilbio.2022.108803
- Quantifying pH buffering capacity in acidic, organic-rich Arctic soils: Measurable proxies and implications for soil carbon degradation J. Zheng et al. 10.1016/j.geoderma.2022.116003
- Microscale heterogeneity controls macroscopic soil heterotrophic respiration by regulating resource availability and environmental stress Z. Yan et al. 10.1007/s10533-023-01044-9
- Warming promotes soil CO2 and CH4 emissions but decreasing moisture inhibits CH4 emissions in the permafrost peatland of the Great Xing'an Mountains B. Lu et al. 10.1016/j.scitotenv.2022.154725
- Temporal, Spatial, and Temperature Controls on Organic Carbon Mineralization and Methanogenesis in Arctic High-Centered Polygon Soils T. Roy Chowdhury et al. 10.3389/fmicb.2020.616518
- Abiotic and Biotic Controls on Soil Organo–Mineral Interactions: Developing Model Structures to Analyze Why Soil Organic Matter Persists D. Dwivedi et al. 10.2138/rmg.2019.85.11
- Assessment of Four Near‐Surface Soil Freeze/Thaw Detection Algorithms Based on Calibrated Passive Microwave Remote Sensing Data Over China W. Shao & T. Zhang 10.1029/2019EA000807
- Effects of warming on carbon emission and microbial abundances across different soil depths of a peatland in the permafrost region under anaerobic condition L. Jiang et al. 10.1016/j.apsoil.2020.103712
- Anaerobic respiration pathways and response to increased substrate availability of Arctic wetland soils M. Philben et al. 10.1039/D0EM00124D
- Revisiting diffusion-based moisture functions: why do they fail? J. Zheng et al. 10.1016/j.soilbio.2021.108525
- Relationship between soil CO2 fluxes and soil moisture: Anaerobic sources explain fluxes at high water content L. Fairbairn et al. 10.1016/j.geoderma.2023.116493
- Thermodynamic control on the decomposition of organic matter across different electron acceptors J. Zheng et al. 10.1016/j.soilbio.2024.109364
18 citations as recorded by crossref.
- Increasing Organic Carbon Biolability With Depth in Yedoma Permafrost: Ramifications for Future Climate Change J. Heslop et al. 10.1029/2018JG004712
- Theoretical Constraints on Fe Reduction Rates in Upland Soils as a Function of Hydroclimatic Conditions S. Calabrese et al. 10.1029/2020JG005894
- Limitations of the Q10 Coefficient for Quantifying Temperature Sensitivity of Anaerobic Organic Matter Decomposition: A Modeling Based Assessment Q. Wu et al. 10.1029/2021JG006264
- Simulated Hydrological Dynamics and Coupled Iron Redox Cycling Impact Methane Production in an Arctic Soil B. Sulman et al. 10.1029/2021JG006662
- Multi-scale temporal variation in CH4 and CO2 exchange and associated biophysical controls from two wetlands in Northeast China L. Sun et al. 10.1016/j.agrformet.2023.109818
- Representing methane emissions from wet tropical forest soils using microbial functional groups constrained by soil diffusivity D. Sihi et al. 10.5194/bg-18-1769-2021
- Microbe-iron interactions control lignin decomposition in soil C. Liao et al. 10.1016/j.soilbio.2022.108803
- Quantifying pH buffering capacity in acidic, organic-rich Arctic soils: Measurable proxies and implications for soil carbon degradation J. Zheng et al. 10.1016/j.geoderma.2022.116003
- Microscale heterogeneity controls macroscopic soil heterotrophic respiration by regulating resource availability and environmental stress Z. Yan et al. 10.1007/s10533-023-01044-9
- Warming promotes soil CO2 and CH4 emissions but decreasing moisture inhibits CH4 emissions in the permafrost peatland of the Great Xing'an Mountains B. Lu et al. 10.1016/j.scitotenv.2022.154725
- Temporal, Spatial, and Temperature Controls on Organic Carbon Mineralization and Methanogenesis in Arctic High-Centered Polygon Soils T. Roy Chowdhury et al. 10.3389/fmicb.2020.616518
- Abiotic and Biotic Controls on Soil Organo–Mineral Interactions: Developing Model Structures to Analyze Why Soil Organic Matter Persists D. Dwivedi et al. 10.2138/rmg.2019.85.11
- Assessment of Four Near‐Surface Soil Freeze/Thaw Detection Algorithms Based on Calibrated Passive Microwave Remote Sensing Data Over China W. Shao & T. Zhang 10.1029/2019EA000807
- Effects of warming on carbon emission and microbial abundances across different soil depths of a peatland in the permafrost region under anaerobic condition L. Jiang et al. 10.1016/j.apsoil.2020.103712
- Anaerobic respiration pathways and response to increased substrate availability of Arctic wetland soils M. Philben et al. 10.1039/D0EM00124D
- Revisiting diffusion-based moisture functions: why do they fail? J. Zheng et al. 10.1016/j.soilbio.2021.108525
- Relationship between soil CO2 fluxes and soil moisture: Anaerobic sources explain fluxes at high water content L. Fairbairn et al. 10.1016/j.geoderma.2023.116493
- Thermodynamic control on the decomposition of organic matter across different electron acceptors J. Zheng et al. 10.1016/j.soilbio.2024.109364
Latest update: 19 Apr 2024
Short summary
Arctic warming exposes soil carbon to increased degradation, increasing CO2 and CH4 emissions. Models underrepresent anaerobic decomposition that predominates wet soils. We simulated microbial growth, pH regulation, and anaerobic carbon decomposition in a new model, parameterized and validated with prior soil incubation data. The model accurately simulated CO2 production and strong influences of water content, pH, methanogen biomass, and competing electron acceptors on CH4 production.
Arctic warming exposes soil carbon to increased degradation, increasing CO2 and CH4 emissions....
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