Limitations of the Q 10 Coefficient for Quantifying Temperature Sensitivity of Anaerobic Organic Matter Decomposition: A Modeling Based Assessment-Reference-Cited by-同舟云学术

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Limitations of the Q 10 Coefficient for Quantifying Temperature Sensitivity of Anaerobic Organic Matter Decomposition: A Modeling Based Assessment

Published:2021-08 Issue:8 Volume:126 Page:
ISSN:2169-8953
Container-title:Journal of Geophysical Research: Biogeosciences
language:en
Short-container-title:J Geophys Res Biogeosci

Author:

Wu Qiong¹,Ye Rongzhong²³,Bridgham Scott D.³,Jin Qusheng¹^ORCID

Affiliation:

1. Department of Earth Science University of Oregon Eugene OR USA

2. Department of Plant and Environmental Sciences Pee Dee Research and Education Center Clemson University Florence SC USA

3. Institute of Ecology and Evolution University of Oregon Eugene OR USA

Funder

National Science Foundation

National Aeronautics and Space Administration

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JG006264

Reference87 articles.

1. Growth and extracellular enzyme production by strains of Bacillus species isolated from fermenting African locust bean, iru

2. Soil-carbon response to warming dependent on microbial physiology

3. Substrate Influences Temperature Sensitivity of Dissolved Organic Carbon (DOC) and Nitrogen (DON) Mineralization in Arid Agricultural Soils

4. Temperature Sensitivity as a Microbial Trait Using Parameters from Macromolecular Rate Theory

5. The Role of Microbial Community Composition in Controlling Soil Respiration Responses to Temperature

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1. Temperature sensitivity of aerobic and anaerobic organic carbon mineralization varies with climate and soil depth in riparian zones;Soil Biology and Biochemistry;2024-08

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