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The Effects of Bottomland
Hardwoods on the Water Quality of an Adjacent River
Richard Day, Barbara Kleiss, Terry Sicherman, and Brian
Hughes
U.S. Geological
Survey, Stephenson Center, Suite 129, 720 Gracern Road Columbia, South
Carolina, 29210-7651, USA
Abstract
The U.S. Geological
Survey is conducting a study to characterize daily water quality during
selected base flow and storm events upstream and downstream of extensive
bottomland hardwood wetland forests on the Cache River, Arkansas and the
Coosawhatchie River, South Carolina. The Cache River is located in an
area of intensive agriculture within the Lower Mississippi Alluvial Valley
and is characteristically turbid with a high suspended sediment load.
The Coosawhatchie River in coastal South Carolina is a braided, blackwater
river with a more forested watershed. Selected events are from3 to 8 consecutive
days and include low base flow, high base flow, and storm events. To quantify
these events, we are measuring physical parameters such as temperature,
pH, conductivity, and dissolved oxygen as well as water quality parameters,
including forms of nitrogen, phosphorus, and organic carbon, and suspended
sediments. Stream gages have been installed at both upstream and downstream
sites, and rating curves have been established to calculate stream flow
and loading rates of the chemical constituents. These water-quality data
will supplement concurrent biological and geochemical studies within the
bottomland hardwood sites adjacent to the Cache and Coosawhatchie Rivers
and help quantify the effects of the bottomland hardwood forests on water
quality of the adjacent river.
--- January 1997
To order SANT
NAWQA publications, please email or call:
Celeste A. Journey
SANT NAWQA Project Chief
cjourney@usgs.gov
(803) 750-6141
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