1. Microbial Models for Simulating Soil Carbon Dynamics: A Review.
- Author
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Chandel, Aneesh Kumar, Jiang, Lifen, and Luo, Yiqi
- Subjects
CARBON in soils ,SOIL dynamics ,NONLINEAR equations ,PH effect ,SOIL microbiology - Abstract
Soils store the largest amount of carbon (C) in the biosphere, and the C pool in soil is critical to the global C balance. Numerous microbial models have been developed over the last few decades to represent microbial processes that regulate the responses of soil organic carbon (SOC) to climate change. However, the representation of microbial processes varies, and how microbial processes are incorporated into SOC models has not been well explored. Here, we reviewed 71 microbial models to characterize the microbial processes incorporated into SOC models and analyzed variations in mechanistic complexity. We revealed that (a) four processes (microbial‐mediated decomposition, mineral interaction, microbial necromass recycling, and active and dormant microbial dynamics) are commonly incorporated in microbial models, (b) ∼48% of models simulate only one microbial process (i.e., microbial‐mediated decomposition) and 35% of models simulate two microbial processes: for example, microbial‐mediated decomposition and mineral interaction, (c) more than 80% microbial models use nonlinear equations, such as forward Michaelis‐Menten kinetics, to represent SOC decomposition, (d) the concept of persistence of SOC due to its intrinsic properties has been replaced by organo‐mineral interaction (∼39% of microbial models) that protects SOC from decomposition, and (e) various temperature and moisture modifiers and pH effects have been used to explain the environmental effect on microbial processes. In the future, to realistically incorporate microbial processes into Earth System Models, it is imperative to identify experimental evidence on rate limitation processes and firmly ground model structure on the field and laboratory data. Plain Language Summary: Soil stores the largest amount of carbon (C) in land ecosystems and, thus, has the potential to regulate climate change. To understand soil C processes under climate change, researchers have developed numerous microbial models that focus on the role of microorganisms in soil organic carbon (SOC) decomposition. In this study, we reviewed 71 microbial models on how microbial processes are represented for their regulation of SOC dynamics. These models commonly include four processes: microbially mediated decomposition, mineral interaction, microbial necromass recycling, and dormancy of microbial activity. More than three‐fourths of the models use nonlinear equations to describe the decomposition of SOC. The concept of SOC stability has shifted from chemical‐based properties of SOC to interactions between SOC and minerals. Our review also revealed that microbial models vary greatly in representing environmental effects, such as temperature, soil moisture, and soil pH, on microbial processes. Finally, we recommend the use of data in guiding the future development of microbial models. Key Points: More than 70 microbial models have recently been developed to simulate soil carbon dynamicsDiversity in model structures and parameters indicates uncertainty in translating current knowledge of microbial processes into modelsData‐driven model development and parameterization are highly recommended to improve the prediction of microbial models [ABSTRACT FROM AUTHOR]
- Published
- 2023
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