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Spectral analyses of the pressure gage wave data were conducted and yielded one 

 direction per frequency. The correlations include immersed weight sediment 

 transport rate, I, versus longshore component of wave energy flux at breaking, 

 P£g. The most widely used correlation constant, K, in the relationship 

 I = KP^g is 0.77. The value determined from the data was K = 0.98, based on 

 the P£s values directed toward the trap. One feature of this type of trap is 

 the potential for overtrapping if the waves are directed nearly normal to shore. 



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