28 Applications of Hydrology and Biogeochemistry to Stormwater Management
Friday, 29 March 2019
8:00 AM - 12:00 PM
St. Matthews Room
THE ROLE OF A PERMEABLE SAND COLUMN IN MODIFYING TIDAL CREEK GEOCHEMISTRY AND LAND-DERIVED INPUTS TO THE COASTAL OCEAN
Paper number: 28-5
Program: Theme Sessions
Time: 9:20 AM – 9:40 AM
Authors
-
Angelos K. HannidesCoastal Carolina University, Conway, SC
Abstract
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.
Geological Society of America Abstracts with Programs. Vol. 51, No. 3
doi: 10.1130/abs/2019SE-327625
© Copyright 2019 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.