Skip to main content
ARS Home » Plains Area » Temple, Texas » Grassland Soil and Water Research Laboratory » Research » Publications at this Location » Publication #333638

Research Project: ENHANCED MODELS AND CONSERVATION PRACTICES FOR WATERSHED RESOURCE MANAGEMENT AND ASSESSMENT

Location: Grassland Soil and Water Research Laboratory

Title: Assessment of the denitrification process in alluvial wetlands at floodplain scale using the SWAT model

Author
item Sun, X - University Of Toulouse
item Bernard-jannin, L - University Of Toulouse
item Sauvage, S - University Of Toulouse
item Garneau, C - University Of Toulouse
item Arnold, Jeffrey
item Srinivasan, R - Texas A&m University
item Sanchez-perez, J - University Of Toulouse

Submitted to: Ecological Engineering
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: 6/22/2016
Publication Date: 7/9/2016
Publication URL: https://handle.nal.usda.gov/10113/5311364
Citation: Sun, X., Bernard-Jannin, L., Sauvage, S., Garneau, C., Arnold, J.G., Srinivasan, R., Sanchez-Perez, J.M. 2016. Assessment of the denitrification process in alluvial wetlands at floodplain scale using the SWAT model. Ecological Engineering. 103:344-358. doi:10.1016/j.ecoleng.2016.06.098.

Interpretive Summary: In many regions, flood plains support intensive agricultural activities. With high fertilizer application rates, groundwater under flood plains can experience elevated nitrate concentrations. Denitrification is an important process in nitrate pollution control. Denitrification is a process of nitrate reduction facilitated by microbial activity and influenced by organic carbon and soil moisture. In this study, a new model that represents the occurrence of denitrification in flood plain aquifers was developed. The new model was incorporated into the SWAT (Soil and Water Assessment Tool) watershed model and tested in the Garonne River flood plain in France. Model results matched measured data showing a denitrification rate equivalent to 40% of the nitrate applied as fertilizer. The new model represents an important advance in understanding and modeling of stream-aquifer interactions and denitrification rates in flood plain aquifers. It improves the accuracy of watershed models like SWAT, and ultimately improves land use decisions made in environmental assessments.

Technical Abstract: As alluvial plains support intensive agricultural activities, they often suffer from groundwater nitrate pollution. Denitrification is recognized as an important process in nitrate pollution control in riparian zones. In shallow aquifer zones influenced by recharged surface water, denitrification efficiently attenuates nitrate in groundwater as well, and the exchange between surface water and groundwater has a significant impact on the occurrence of denitrification. Denitrification is simulated in numerous models, however most models do not take into account the denitrification occurring in shallow aquifers or the influence of recharge surface water in the alluvial aquifer with organic carbon and bacteria to activate denitrification. In this study, a new module was developed that represents the occurrence of denitrification in the shallow aquifer of alluvial floodplains. Nitrate inputs in the shallow aquifer caused by the recharged river water through both lateral (river bank) and vertical (surface) infiltration and the influence of flooding on nitrate leaching were added to the Soil and Water Assessment Tool – Landscape Unit Darcy (SWAT-LUD) model. The influences of both dissolved organic carbon (DOC) and particulate organic carbon (POC) on denitrification were evaluated. The modified model was applied on an experimental site located in the floodplain of the Garoone River (southwest France). Results showed that the modified SWAT-LUD model was able to simulate the aquifer nitrate concentration in the near-bank zone (riparian zone) satisfactorily. The near-bank zone in the floodplain played the most important role in attenuating nitrate through denitrification with an annual denitrification rate of around 130 kg N-NO3-a-1y-1, representing about 40% of the nitrate input in this area. POC was more important than DOC in the denitrification process, especially in the near-bank zone where 98% of the nitrate was attenuated through POC consumption. Relationships between denitrification rates, groundwater levels and total input nitrate masses in the near-bank zone were determined. The results illustrated that groundwater levels were positively related to the denitrification rates in the near-bank zone. The absolute denitrification rate increased as the nitrate content increased, but the relative consumption rate by denitrification decreased.