Low Frequency In Situ Sediment Dispersion Estimates in the Presence of Discrete Layers and Gradients
Thursday, November 1, 2012 3:00 p.m. in ARL Auditorium
Dr. Charles W. Holland
Applied Research Laboratory
The Pennsylvania State University
One of the difficulties in validating sediment models has been the lack of reliable low frequency dispersion measurements. A reflection method is presented that yields in situ dispersion without sediment disturbance over a broad range of frequencies and can explicitly disentangle frequency-dependent effects of vertical structure, e.g., layers and gradients. Measurements on the outer shelf from 300—3000 Hz show that dispersion is a strong function of depth in the sediment column. The depth and frequency-dependent results generally agree well with independent measurements on core data. Cohesive sediments in the upper few meters exhibit a nearly frequency-independent sound speed and a nearly linear frequency dependence of attenuation. In the lower part of the sediment column the sediments are more granular: the lowest layer exhibits an attenuation with a peak frequency at 1100 Hz, where its dependence below and above trends to f^2 and f^(1/2), respectively. While Biot theory predicts this dependence, its underlying physical explanation, fluid flow through interstitial pores, does not seem plausible for this sediment, due to the unreasonable permeability value required. Viscous Grain Shearing theory also predicts this dependence, but it is not known whether the parameter values are reasonable.