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Abiotic and Biotic Controls on Soil Organo–Mineral Interactions
Published: September 15, 2019
Posted: July 30, 2020

Kinetics, surface chemistry, microbial community structure, and other factors are key for predicting soil organic matter dynamics within a reactive transport modeling framework.

The Science
While there currently exists a suite of models representing soil organic matter (SOM) dynamics that span a range of complexity, some recent mechanistic models are more consistent with an emerging understanding of the persistence of SOM. Yet even these more recent models do not represent several processes that can be important for SOM dynamics. It is clear that next-generation models need to represent the full spectrum of quantitatively important mechanisms for determining SOM persistence—including rate-limited and equilibrium-based sorption, formation of soil aggregates, representative soil minerals, microbial community dynamics, and vegetation interactions—to accurately predict short- and long-term SOM dynamics.

The Impact
This study informs development of a robust predictive understanding of SOM dynamics. However, it is challenging to incorporate recommendations, such as mineral-associated organic matter and vegetation dynamics, in a reactive transport modeling framework. These emergent concepts require emergent technologies to appropriately characterize, e.g., molecular, soil, and root structure. Several technologies (e.g., FT-ICR-MS, NMR, STXM, and NEXAFS) are available today for such characterization, but these technologies have not yet been fully exploited nor have the resulting data/findings been fully incorporated into modeling studies. To enhance process understanding of SOM dynamics, streamlined coordination between technologies for characterization and emerging understanding for SOM modeling are needed.

Soils represent the largest store of actively cycling terrestrial organic carbon. This carbon is susceptible to release to the atmosphere as greenhouse gases, including carbon dioxide (CO2) and methane (CH4). However, significant gaps remain in understanding why certain soil organic matter (SOM) decomposes rapidly, and why thermodynamically unstable SOM can persist in soils for centuries. To fill this critical knowledge gap, a robust predictive understanding of SOM dynamics is essential, particularly for examining short-term and long-term changes in soil carbon storage and its feedback to climate. In this review paper, the authors argue that a representation of organic matter molecular structure, the activity of belowground communities, and mineral-associated organic matter (MAOM) are required to model SOM dynamics beyond first-order effects accurately. This argument is based on a review of the literature describing the current understanding of the main interacting biological, geochemical, and physical factors leading to SOM stabilization, and on an analysis of a suite of soil carbon models. The authors conclude by recommending several mechanisms that require implementation within the next generation of mechanistic models, including kinetic and equilibrium-based sorption, soil mineral surface chemistry, and vegetation dynamics to accurately predict short- and long-term SOM dynamics.

BER Program Manager
Paul Bayer
Department of Energy

Principal Investigator
Dipankar Dwivedi
Lawrence Berkeley National Laboratory

This material is based on work supported by the Office of Biological and Environmental Research (as part of the Watershed Function Scientific Focus Area), within the U.S. Department of Energy (DOE) Office of Science, and the Office of Advanced Scientific Computing (as part of the project “Deduce: Distributed Dynamic Data Analytics Infrastructure for Collaborative Environments”), within the DOE Office of Science, under Contract No. DE-AC02-05CH11231. Jinyun Tang acknowledges support from the Next-Generation Ecosystem Experiments (NGEE)–Arctic. The U.S. Department of Agriculture (USDA) National Institute of Food and Agriculture (NIFA) Postdoctoral Fellowship program supported Katerina Georgiou. Nicholas Bouskill acknowledges support from a DOE Early Career Research Project (#FP00005182). William Riley acknowledges support from the Terrestrial Ecosystem Science Scientific Focus Area of Berkeley Lab.

Dwivedi D, Tang J, Bouskill N, Georgiou K, Chacon SS, Riley WJ. "Abiotic and biotic controls on soil organo–mineral interactions: Developing model structures to analyze why soil organic matter persists." Reviews in Mineralogy and Geochemistry 85(1), 329–348  (2019). [DOI:10.2138/rmg.2019.85.11].

Topic Areas:

  • Research Area: Subsurface Biogeochemical Research
  • Research Area: Terrestrial Ecosystem Science
  • Research Area: Carbon Cycle, Nutrient Cycling
  • Cross-Cutting: Scientific Computing and SciDAC
  • Cross-Cutting: Early Career
  • Research Area: Next-Generation Ecosystem Experiments (NGEE)

Division: SC-33.1 Earth and Environmental Sciences Division, BER


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