title: Velocity dispersion and attenuation in granular marine sediments: comparison of measurements with predictions using acoustic models.
abstract: The large velocity dispersion recently reported could be explained by a gap stiffness model incorporated into the Biot model (the BIMGS model) proposed by the author. However, at high frequencies, some measured results have been reported for negative velocity dispersion and attenuation proportional to the first to fourth power of frequency. In this study, first, it is shown that the results of velocity dispersion and attenuation calculated using the BIMGS model are consistent with the results measured in two kinds of water-saturated sands with different grain sizes, except in the high-frequency range. Then, the velocity dispersion and attenuation in six kinds of water-saturated glass beads and four kinds of water-saturated silica sands with different grain sizes are measured in the frequency ranges of 80-140 and 300-700 kHz. The measured results are compared with those calculated using the BIMGS model plus some acoustic models. It is shown that the velocity dispersion and attenuation are well predicted by using the BIMGS model in the range of kd ≤ 0.5 (k: wavenumber in water, d: grain diameter) and by using the BIMGS model plus multiple scattering effects in the range of kd ≥ 0.5 in which negative velocity dispersion appears.
authors.affiliation: Poro-Acoustics Laboratory, 1115-22 Miyakami, Shimizu, Shizuoka, Shizuoka 424-0911, Japan. mk45@nifty.com
authors.forename: Masao
authors.initials: M
authors.lastname: Kimura
mesh_terms: D055119:Elastic Modulus; D019015:Geologic Sediments / Q000737:chemistry*; D005844:Geology / Q000379:methods*; D008962:Models, Theoretical; D009038:Motion; D009792:Oceans and Seas; D010316:Particle Size; D016062:Porosity; D012815:Signal Processing, Computer-Assisted; D013016:Sound; D013997:Time Factors; D014465:Ultrasonics; D014783:Viscosity; D014867:Water
chemical_list: D014867:Water