Acoustic lance: Newinsituseafloor velocity profiles
作者:
S. S. Fu,
R. H. Wilkens,
L. N. Frazer,
期刊:
The Journal of the Acoustical Society of America
(AIP Available online 1996)
卷期:
Volume 99,
issue 1
页码: 234-242
ISSN:0001-4966
年代: 1996
DOI:10.1121/1.414506
出版商: Acoustical Society of America
关键词: ACOUSTIC MEASUREMENTS;ATTENUATION;OCEANOGRAPHY;SEA BED;SEDIMENT−WATER INTERFACES;UNDERWATER
数据来源: AIP
摘要:
The acoustic lance is an instrument developed to obtaininsitucompressional wave velocity and attenuation (Q−1) profiles for a sedimentary layer of several meters thickness at the sediment–seawater interface. The self‐contained instrument consists of ten independent recording channels with a linear array of receivers embedded in the seafloor below a broadband acoustic source. It providesinsiturecording of full waveforms to determine interval velocity and attenuation. The system can be attached to a gravity corer or to a specially designed probe. A comprehensive experiment was carried out in Mid‐Atlantic Ridge sediment ponds where the lance madeinsitumeasurements, and core samples were recovered. Core data agree well withinsitudata in one location, but disagree in other locations. Lance data indicate that the sediment ponds have similarinsituvelocity distributions, with an acoustic channel much thinner than that predicted by earlier investigators.
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