THE ROLE OF A PERMEABLE SAND COLUMN IN MODIFYING TIDAL CREEK GEOCHEMISTRY AND LAND-DERIVED INPUTS TO THE COASTAL OCEAN
Our study site is Singleton Swash, one of fifteen major estuarine swashes located along the Grand Strand that drains 613 hectares (ha) of watershed into Long Bay. Discharge into the coastal ocean is through one primary tidal creek, whose main channel is heavily influenced by nearshore processes and is ever-changing. Erosion-deposition patterns dictate the main types of benthic interfaces across which sediment-water exchange occurs and, consequently, the rates of biogeochemical modification of land-derived inputs before they reach the ocean.
Our hypothesis is that estuarine swashes may mitigate land-derived inputs into the coastal ocean by exchanging matter across the sediment-water interface and incorporating the remineralized constituents into microphytobenthic primary producers. We are currently assessing the non-conservative behavior of materials which are subject to enhanced exchange across a permeable sediment-water interface. We are also documenting the role of microphytobenthic communities, assimilating inorganic nutrients regenerated in porewater and transported upwards. Upon completion of this project we hope to demonstrate whether interaction through exchange between the sediment and overlying water affects tidal creek geochemistry. If so, swashes should be considered as a filter for land-derived pollutants transported through the regional watersheds, and thus mitigating the impact of land-derived substances on the coastal ocean.