Many studies have focused on hydrological and geochemical fluxes from land to the ocean via groundwater discharge, however few have assessed groundwater flow in deltaic settings. Hydrological budgets indicate that 1,000 to 5,000 m3s-1 of water flow from the Mississippi River (MR) to its delta (MRD) via subterranean pathways, however the spatial and geological controls on these processes are less known. This study suggests that deltaic lithofacies of paleoenvironments related to the delta cycle allow for groundwater to discharge out of the MR main channel and into the MRD through organic sediment-rich and silt-sand overbank and mouth bar facies. This study employs geophysical data, including chirp sonar subbottom profiling and continuous resistivity profiling (CRP), to detect the location of these sediments in Barataria Bay, a coastal bay located in the MRD. Chirp data indicate paleochannel features in the MRD, whereas CRP data indicate freshwater seepage into MRD embayments during high river stage events. Analyses of bulk properties of sediment cores are used to characterize delta facies sediments and determine variability in hydraulic conductivity values, which range from 10-7 to 10-2 ms-1. These geophysical and sediment core data show the potential for groundwater flux through deltaic sediments, and will contextualize geochemical tracer data collected by project collaborators. Results indicate that groundwater discharge in the MRD is directly controlled by the geological constraints of the delta region. These results illustrate the potential for substantial groundwater fluxes in other large river deltas, and present implications for urban and coastal infrastructure planning, as many large global deltas sustain significant populations.
