Abiotic and biotic controls on soil organo–mineral interactions: develo** model structures to analyze why soil organic matter persists

D Dwivedi, J Tang, N Bouskill… - … in Mineralogy and …, 2019 - pubs.geoscienceworld.org
Soil organic matter (SOM) represents the single largest actively cycling reservoir of terrestrial
organic carbon, accounting for more than three times as much carbon as that present in the …

[HTML][HTML] Relationship between soil CO2 fluxes and soil moisture: Anaerobic sources explain fluxes at high water content

L Fairbairn, F Rezanezhad, M Gharasoo, CT Parsons… - Geoderma, 2023 - Elsevier
Soil moisture is a known environmental factor influencing carbon dioxide (CO 2) emissions
and therefore represents an important variable in predictive models. Establishing …

Warming promotes soil CO2 and CH4 emissions but decreasing moisture inhibits CH4 emissions in the permafrost peatland of the Great **ng'an Mountains

B Lu, L Song, S Zang, H Wang - Science of The Total Environment, 2022 - Elsevier
Permafrost peatlands, as large soil carbon pools, are sensitive to global warming. However,
the effects of temperature, moisture, and their interactions on carbon emissions in the …

Microbe-iron interactions control lignin decomposition in soil

C Liao, W Huang, J Wells, R Zhao, K Allen… - Soil Biology and …, 2022 - Elsevier
Lignin decomposition is critically linked to terrestrial carbon (C) cycle due to the enormous C
mass of lignin and its importance in controlling overall rates of litter decomposition …

Global hotspots and trends in microbial-mediated grassland carbon cycling: a bibliometric analysis

X **ang, T Yao, B Man, D Lin, C Li - Frontiers in Microbiology, 2024 - frontiersin.org
Grasslands are among the most widespread environments on Earth, yet we still have poor
knowledge of their microbial-mediated carbon cycling in the context of human activity and …

Microbial sensitivity to temperature and sulfate deposition modulates greenhouse gas emissions from peat soils

R AminiTabrizi, N Graf‐Grachet, RK Chu… - Global Change …, 2023 - Wiley Online Library
Peatlands are among the largest natural sources of atmospheric methane (CH4) worldwide.
Microbial processes play a key role in regulating CH4 emissions from peatland ecosystems …

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, Y Song, L Sun, C Song, X Wang, X Ma… - Applied Soil …, 2020 - Elsevier
Peatlands in permafrost region are large carbon pools sensitive to global warming.
However, the effects of increased temperature on carbon emissions and associated …

Increasing organic carbon biolability with depth in yedoma permafrost: ramifications for future climate change

JK Heslop, M Winkel… - Journal of …, 2019 - Wiley Online Library
Permafrost thaw subjects previously frozen organic carbon (OC) to microbial decomposition,
generating the greenhouse gases (GHG) carbon dioxide (CO2) and methane (CH4) and …

Quantifying pH buffering capacity in acidic, organic-rich Arctic soils: Measurable proxies and implications for soil carbon degradation

J Zheng, EC Berns-Herrboldt, B Gu, SD Wullschleger… - Geoderma, 2022 - Elsevier
Dynamic pH change promoted by biogeochemical reactions in Arctic tundra soils can be a
major control on the production and release of CO 2 and CH 4, which contribute to rising …

Limitations of the Q10 Coefficient for Quantifying Temperature Sensitivity of Anaerobic Organic Matter Decomposition: A Modeling Based Assessment

Q Wu, R Ye, SD Bridgham, Q ** - Journal of Geophysical …, 2021 - Wiley Online Library
The Q10 coefficient is the ratio of reaction rates at two temperatures 10° C apart, and has
been widely applied to quantify the temperature sensitivity of organic matter decomposition …