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Author(s)
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Atlantic Oceanographic and Meteorological Laboratory, Ocean Chemistry Division, Miami, FL, USA.
Atlantic Oceanographic and Meteorological Laboratory, Ocean Chemistry Division, Miami, FL, USA.
Applied Research Center (ARC), Florida International University, Miami, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Florida Atlantic University, Civil Engineering Department, Boca Raton, FL, USA.
Atlantic Oceanographic and Meteorological Laboratory, Ocean Chemistry Division, Miami, FL, USA.
Atlantic Oceanographic and Meteorological Laboratory, Ocean Chemistry Division, Miami, FL, USA.
Applied Research Center (ARC), Florida International University, Miami, FL, USA.
In June, 2004 and February, 2007, in field tracer
studies were conducted on the Hollywood and South Central outfalls,
using sulfur hexafluoride (SF6)
as a tracer. The objective of these studies was to determine if the
tracer could be detected in the farfield at significant distance, and if
so, could this data be used to construct a model of the farfield plume.
Prior models for farfield plume movement do not appear to comport well
with the conditions in southeast Florida. Extensive research was
conducted in southeast Florida on 4 outfalls, which led to the
development of nearfield dilution equations for same. However farfield
modeling of outfall plumes was difficult to accomplish because the
tracers used are not detectable for significant distances. The SF6
resolved that problem and as a result the Hollywood outfall was used to
construct a model. Two methods were investigated for modeling the
plume, 1) the Eureqa formulation method and 2) the Gamma-Curve method.
The concentrations in the x-y
plane were first found by using the Eureqa formulation to calculate the
concentration at each grid point given its depth and the concentration
of the centerline at the same latitude. The plume models were generated
using MATLAB that matched with the results actually seen in the field.
Cite this paper
Bloetscher, F. , Pleitez, F. , Romah, T. , Albasri,
A. , Dickinson, C. , Sharif, H. , Matthews, K. , Nguyen, T. , Riche, L. ,
Youngman, F. , Carsey, T. , Stamates, J. and Proni, J. (2014) The
Use of SF6 and GIS to Study Farfield Modeling of Ocean Outfall Plumes in Florida. Journal of Environmental Protection, 5, 1037-1052. doi: 10.4236/jep.2014.511103.
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