Abstract
Coastal ecosystems have been largely ignored in Earth system models but are important zones for carbon and nutrient processing. Interactions between water, microbes, soil, sediments, and vegetation are important for mechanistic representation of coastal processes and ecosystem function. To investigate the role of these feedbacks, we used a reactive transport model (PFLOTRAN) that has the capability to be connected to the Energy Exascale Earth System Model (E3SM). PFLOTRAN was used to incorporate redox reactions and track chemical species important for coastal ecosystems as well as define simple representations of vegetation dynamics. Our goal was to incorporate oxygen flux, salinity, pH, sulfur cycling, and methane production along with plant-mediated transport of gases and tidal flux. Using porewater profile and incubation data for model calibration and evaluation, we were able to create depth-resolved biogeochemical soil profiles for saltmarsh habitat and use this updated representation to simulate direct and indirect effects of elevated CO2 and temperature on subsurface biogeochemical cycling. We found that simply changing the partial pressure of CO2 or increasing temperature in the model did not fully reproduce observed changes in the porewater profile, but the inclusion of plant or microbial responses to CO2 and temperature manipulations was more accurate in representing porewater concentrations. This indicates the importance of characterizing tightly coupled vegetation-subsurface processes for developing predictive understanding and the need for measurement of plant-soil interactions on the same time scale to understand how hotspots or moments are generated.
Original language | English |
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Article number | e2023JG007633 |
Journal | Journal of Geophysical Research: Biogeosciences |
Volume | 129 |
Issue number | 3 |
DOIs | |
State | Published - Mar 2024 |
Funding
Funding for this project was provided by the US Department of Energy, Office of Science, Office of Biological and Environmental Research, Environmental System Science programme under award numbers DE‐SC0014413, DE‐SC0019110, DE‐SC0021131, and DE‐SC0021112. Additional support was provided by COMPASS‐FME, a multi‐institutional project supported by the U.S. Department of Energy, Office of Science, Biological and Environmental Research as part of the Environmental System Science Program, the Smithsonian Institution, and the National Science Foundation Long‐Term Research in Environmental Biology Program (DEB‐0950080, DEB‐1457100, DEB‐1557009, DEB‐2051343). Funding for this project was provided by the US Department of Energy, Office of Science, Office of Biological and Environmental Research, Environmental System Science programme under award numbers DE-SC0014413, DE-SC0019110, DE-SC0021131, and DE-SC0021112. Additional support was provided by COMPASS-FME, a multi-institutional project supported by the U.S. Department of Energy, Office of Science, Biological and Environmental Research as part of the Environmental System Science Program, the Smithsonian Institution, and the National Science Foundation Long-Term Research in Environmental Biology Program (DEB-0950080, DEB-1457100, DEB-1557009, DEB-2051343).
Funders | Funder number |
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Smithsonian Institution | |
U.S. Department of Energy | |
COMPASS-FME | |
Environmental System Science programme | |
Office of Science | |
National Science Foundation Long-Term Research in Environmental Biology Program | |
National Science Foundation Long‐Term Research in Environmental Biology Program | DEB‐1557009, DEB‐2051343, DEB‐0950080, DEB‐1457100 |
Biological and Environmental Research | DE‐SC0019110, DE‐SC0014413, DE‐SC0021131, DE‐SC0021112 |
Keywords
- coastal systems
- earth system models
- plant-soil-water interactions