Acoustical and mass physical properties of deep ocean recent marine sediments

Eight cores obtained from the Monterey Submarine Fan in the Pacific Ocean 50 to 75 miles off Monterey, California, were sectioned to conduct vane shear, compressional wave speed, and viscoelastic measurements. After the cores were sectioned aboard ship utilizing a heated element technique, core sect...

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Main Author: Cepek, Robert Joseph.
Other Authors: NA
Language:en_US
Published: Monterey, California: U.S. Naval Postgraduate School 2013
Online Access:http://hdl.handle.net/10945/27926
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spelling ndltd-nps.edu-oai-calhoun.nps.edu-10945-279262014-11-27T16:17:05Z Acoustical and mass physical properties of deep ocean recent marine sediments Cepek, Robert Joseph. NA NA Oceanography Eight cores obtained from the Monterey Submarine Fan in the Pacific Ocean 50 to 75 miles off Monterey, California, were sectioned to conduct vane shear, compressional wave speed, and viscoelastic measurements. After the cores were sectioned aboard ship utilizing a heated element technique, core sections were immediately subjected to vane shear measurements utilizing a Wykeham- Farrance Vane Shear Machine modified to produce a graphical display of torque versus angle of blade rotation. Compressional wave speed measurements were also made aboard ship. Wet density, water content, porosity, and grain size distribution of sediment from core sections were determined later in the laboratory. The relationship of sediment shear strength to mass physical properties and compressional wave speed is discussed. No correlations were apparent between shear strength of the sediment and any single mass physical property or the compressional wave speed of the sediment. A critical discussion of the vane shear test is presented with recommendations for test improvement 2013-02-15T23:29:32Z 2013-02-15T23:29:32Z 1972 Thesis http://hdl.handle.net/10945/27926 ocn779497548 en_US Monterey, California: U.S. Naval Postgraduate School
collection NDLTD
language en_US
sources NDLTD
description Eight cores obtained from the Monterey Submarine Fan in the Pacific Ocean 50 to 75 miles off Monterey, California, were sectioned to conduct vane shear, compressional wave speed, and viscoelastic measurements. After the cores were sectioned aboard ship utilizing a heated element technique, core sections were immediately subjected to vane shear measurements utilizing a Wykeham- Farrance Vane Shear Machine modified to produce a graphical display of torque versus angle of blade rotation. Compressional wave speed measurements were also made aboard ship. Wet density, water content, porosity, and grain size distribution of sediment from core sections were determined later in the laboratory. The relationship of sediment shear strength to mass physical properties and compressional wave speed is discussed. No correlations were apparent between shear strength of the sediment and any single mass physical property or the compressional wave speed of the sediment. A critical discussion of the vane shear test is presented with recommendations for test improvement
author2 NA
author_facet NA
Cepek, Robert Joseph.
author Cepek, Robert Joseph.
spellingShingle Cepek, Robert Joseph.
Acoustical and mass physical properties of deep ocean recent marine sediments
author_sort Cepek, Robert Joseph.
title Acoustical and mass physical properties of deep ocean recent marine sediments
title_short Acoustical and mass physical properties of deep ocean recent marine sediments
title_full Acoustical and mass physical properties of deep ocean recent marine sediments
title_fullStr Acoustical and mass physical properties of deep ocean recent marine sediments
title_full_unstemmed Acoustical and mass physical properties of deep ocean recent marine sediments
title_sort acoustical and mass physical properties of deep ocean recent marine sediments
publisher Monterey, California: U.S. Naval Postgraduate School
publishDate 2013
url http://hdl.handle.net/10945/27926
work_keys_str_mv AT cepekrobertjoseph acousticalandmassphysicalpropertiesofdeepoceanrecentmarinesediments
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