Improving a Biogeochemical Model to Simulate Microbial‐Mediated Carbon Dynamics in Agricultural Ecosystems. (14th November 2021)

• Record Type: Journal Article
• Authors: Deng, Jia; Frolking, Steve; Bajgain, Rajen; Cornell, Carolyn R.; Wagle, Pradeep; Xiao, Xiangming; Zhou, Jizhong; Basara, Jeffrey; Steiner, Jean; Li, Changsheng
• Is Part Of: Journal of advances in modeling earth systems. Volume 13:Number 11(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-11-14
• Subjects: SOC change -- CO2 flux -- SOM decomposition -- microbial physiology -- farming management practices -- biogeochemical modeling; Geological modeling -- Periodicals; Climatology -- Periodicals; Geochemical modeling -- Periodicals; 551.5011
• DOI: 10.1029/2021MS002752
• Languages: English
• ISSNs: 1942-2466

Abstract

Abstract: Soil microbes drive decomposition of soil organic matter (SOM) and regulate soil carbon (C) dynamics. Process‐based models have been developed to quantify changes in soil organic carbon (SOC) and carbon dioxide (CO2 ) fluxes in agricultural ecosystems. However, microbial processes related to SOM decomposition have not been, or are inadequately, represented in these models, limiting predictions of SOC responses to changes in microbial activities. In this study, we developed a microbial‐mediated decomposition model based on a widely used biogeochemical model, DeNitrification‐DeComposition (DNDC), to simulate C dynamics in agricultural ecosystems. The model simulates organic matter decomposition, soil respiration, and SOC formation by simulating microbial and enzyme dynamics and their controls on decomposition, and considering impacts of climate, soil, crop, and farming management practices (FMPs) on C dynamics. When evaluated against field observations of net ecosystem CO2 exchange (NEE) and SOC change in two winter wheat systems, the model successfully captured both NEE and SOC changes under different FMPs. Inclusion of microbial processes improved the model's performance in simulating peak CO2 fluxes induced by residue return, primarily by capturing priming effects of residue inputs. We also investigated impacts of microbial physiology, SOM, and FMPs on soil C dynamics. Our results demonstrated that residue or manure input drove microbial activity and predominantly regulated the CO2 fluxes, and manure amendment largely regulated long‐term SOC change. The microbial physiology had considerable impacts on the microbial activities and soil C dynamics, emphasizing the necessity of considering microbial physiology and activities when assessing soil C dynamics in agricultural ecosystems. Plain Language Summary: Soil microbes drive decomposition of soil organic matter (SOM) and regulate soil carbon (C) dynamics. Process‐based models are useful tools for quantifying changes in soil organic carbon (SOC) and carbon dioxide (CO2 ) fluxes in agricultural ecosystems. However, microbial processes related to SOM decomposition have not been, or are inadequately, represented in these models, limiting predictions of SOC responses to changes in microbial activities. We developed a microbial‐mediated decomposition model based on a widely used biogeochemical model, DeNitrification‐DeComposition (DNDC), to simulate C dynamics in agricultural ecosystems. The model simulates organic matter decomposition, soil respiration, and SOC formation by simulating microbial dynamics and controls on decomposition, and considering impacts of climate, soil, crop, and farming management practices (FMPs) on C dynamics. We also investigated impacts of microbial physiology, SOM, and FMPs on soil C dynamics. Our results demonstrated that residue or manure input drove microbial activity and predominantly regulated CO2 fluxes, and manure amendment largely regulated long‐term SOC change. The microbial physiology had considerable impacts on microbial activities and soil C dynamics, emphasizing the necessity of considering microbial physiology and activities when assessing soil C dynamics in agricultural ecosystems. These results provide insights in simulating microbial‐mediated soil C dynamics in agricultural ecosystems. Key Points: A biogeochemical model was improved to simulate microbe‐driven soil organic matter (SOM) decomposition and carbon dynamics in agricultural ecosystems The model simulates carbon dynamics by simulating both microbial controls and impacts of soil, crop, and farming management practices Carbon input drives microbial activity and exerts large impacts on carbon dynamics while microbes play a central role in decomposing SOM