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Abstract:
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A surf zone sediment transport study was conducted in Jamaica Beach , Texas ,
using new oceanographic equipment . A mini -sled was constructed and outfitted with an
instrument package that consisted of two velocimeters , one current profiler , three OBS's
(Optical Back Scatter ) , and a Sequoia Instruments LISST (Laser in situ Scatteroineter
and Transinissoineter ) . This instrumented sled was used to measure sand concentration
and flow velocity across the surf zone . Using these two parameters we were able to
determine longshore sand transport .
The study provided an accurate measurernent of sand transport on a muddy coast .
Previous methods for measuring total longshore sediment transport did not quantify the
effect that mud -sized particles would have on OBS's . To circumvent this issue we used
the LISST to measure sand concentration in the water . The LISST can measure sand
concentration despite the presence of mud .
During this study it appeared that sand transport peaks 10 cm above the sea
bottom . The measured total longshore transport rate closely matched results from one
equation for determining total longshore transport (Kamphius , 199 1 ) . The CERC
equation was also compared to the measured result . |