Linking microscale processes and macroscale fluxes using soil properties in a process-rich simulation.
Researchers from Pacific Northwest National Laboratory (PNNL) coupled fundamental soil properties with microbial physiology in a pore-scale simulation to predict how microbial respiration will vary under different moisture conditions.
By modeling soil microbial respiration response to moisture using a more fundamental understanding of the system, scientists from PNNL can improve our predictions of how different soils will respond biogeochemically to drought and inundation events like floods and extreme weather.
DOE’s PNNL researchers have observed for a long time a “sweet spot” where soils respire the most carbon dioxide when they aren’t too wet or too dry. However, the location of this zone seemed to vary across different soil types and it was difficult to predict.
In this study, scientists captured the underlying physical controls and microbial physiology in a computer simulation and generated a range of different respiration-moisture curves across different soil types. This demonstrated the distribution of these different moisture responses across soils and how those differences can be explained by specific soil properties. The findings will help us develop better models for soil biogeochemistry.
Contacts (BER PM)
Terrestrial Ecosystems Program, DOE BER
Pacific Northwest National Lab
This research was supported by the National Key R&D Program of China and DOE’s Office of Science, Biological and Environmental Research (BER) Division through the Terrestrial Ecosystem Science (TES) program.
Yan, Z., B. Bond-Lamberty, K. Todd-Brown, V. Bailey, S. Li, C. Liu, C Liu, “A moisture function of soil heterorophic respiration incorporating microscale processes.” Nature Communications volume 9(1) Article number: 2562 (2018). [DOI:10.1038/s41467-018-04971-6]
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