Coupling scales in process‐based soil organic carbon modeling including dynamic aggregation

• Published in: Journal of plant nutrition and soil science 2024-02, Vol.187 (1), p.130-142
• Main Authors: Zech, Simon, Prechtel, Alexander, Ray, Nadja
• Format: Article
• Language: English
• Subjects: Biodegradation; Carbon dioxide; Carbon sequestration; carbon turnover; Cellular automata; cellular automaton method; diffusion equation mechanistic image‐based modeling; Environmental changes; Environmental conditions; Environmental degradation; Mathematical models; Microorganisms; Occlusion; Organic carbon; Organic matter; Organic soils; Oxygen; Particulate organic matter; pore‐scale model; Soil organic matter; Soil profiles; Soil properties; soil structure dynamics; Soils; upscaling
• ISSN: 1436-8730; 1522-2624
• DOI: 10.1002/jpln.202300080

Background Carbon storage and turnover in soils depend on the interplay of soil architecture, microbial activities, and soil organic matter (SOM) dynamics. For a fundamental understanding of the mechanisms that drive these processes, not only the exploitation of advanced experimental techniques down to the nanoscale is necessary but also spatially explicit and dynamic image‐based modeling at the pore scale. Aim We present a modeling approach that is capable of transferring microscale information into macroscale simulations at the profile scale. This enables the prediction of future developments of carbon fluxes and the impact of changes in the environmental conditions linking scales. Method We consider a mathematical model for CO2 transport across soil profiles (macroscale), which is informed by a pore‐scale (microscale) model for C turnover. It allows for the dynamic, self‐organized re‐arrangement of solid building units, aggregates and particulate organic matter (POM) based on surface interactions, realized by a cellular automaton method, and explicitly takes spatial effects on POM turnover such as occlusion into account. We further include the macroscopic environmental conditions water saturation, POM content, and oxygen concentration. Results The coupled simulations of macroscopic transport and pore‐scale carbon and aggregate turnover reveal the complex, nonlinear interplay of the underlying processes. Limitations by diffusive transport, oxygen availability, texture‐dependent occlusion and turnover of OM drive CO2 production and carbon storage. Conclusions This emphasizes the need for such micro–macro models exchanging information on different scales to investigate and quantify the effects of structural changes, variations in environmental conditions, or degradation processes on carbon turnover.