Modeling impacts of saltwater intrusion on methane and nitrous oxide emissions in tidal forested wetlands

• Published in: Ecological applications 2023-07, Vol.33 (5), p.e2858-n/a
• Main Authors: Wang, Hongqing, Dai, Zhaohua, Krauss, Ken W., Trettin, Carl C., Noe, Gregory B., Burton, Andrew J., Ward, Eric J.
• Format: Article
• Language: English
• Subjects: Biogeochemistry; blue carbon; Carbon; Carbon Dioxide - analysis; Carbon sequestration; Carbon sinks; Climate change; Climate change mitigation; Coastal aquifers; DeNitrification‐DeComposition (DNDC); Drought; Emission; Emissions; Forested wetlands; Forests; Geomorphology; Methane; Net Primary Productivity; Nitrous Oxide; oligohaline marshes; Organic carbon; Organic soils; Pore water; River systems; Rivers; Saline water; Saline water intrusion; Salinity; Salinity effects; Salt water intrusion; Savannahs; Seawater; Soil - chemistry; Soil dynamics; Soil salinity; Soil water; soil water level; Soils; soil‐borne greenhouse fluxes; Synergistic effect; tidal forests; Water levels; Wetlands
• ISSN: 1051-0761; 1939-5582
• DOI: 10.1002/eap.2858

Emissions of methane (CH4) and nitrous oxide (N2O) from soils to the atmosphere can offset the benefits of carbon sequestration for climate change mitigation. While past study has suggested that both CH4 and N2O emissions from tidal freshwater forested wetlands (TFFW) are generally low, the impacts of coastal droughts and drought‐induced saltwater intrusion on CH4 and N2O emissions remain unclear. In this study, a process‐driven biogeochemistry model, Tidal Freshwater Wetland DeNitrification‐DeComposition (TFW‐DNDC), was applied to examine the responses of CH4 and N2O emissions to episodic drought‐induced saltwater intrusion in TFFW along the Waccamaw River and Savannah River, USA. These sites encompass landscape gradients of both surface and porewater salinity as influenced by Atlantic Ocean tides superimposed on periodic droughts. Surprisingly, CH4 and N2O emission responsiveness to coastal droughts and drought‐induced saltwater intrusion varied greatly between river systems and among local geomorphologic settings. This reflected the complexity of wetland CH4 and N2O emissions and suggests that simple linkages to salinity may not always be relevant, as non‐linear relationships dominated our simulations. Along the Savannah River, N2O emissions in the moderate‐oligohaline tidal forest site tended to increase dramatically under the drought condition, while CH4 emission decreased. For the Waccamaw River, emissions of both CH4 and N2O in the moderate‐oligohaline tidal forest site tended to decrease under the drought condition, but the capacity of the moderate‐oligohaline tidal forest to serve as a carbon sink was substantially reduced due to significant declines in net primary productivity and soil organic carbon sequestration rates as salinity killed the dominant freshwater vegetation. These changes in fluxes of CH4 and N2O reflect crucial synergistic effects of soil salinity and water level on C and N dynamics in TFFW due to drought‐induced seawater intrusion.