Measurement of the viscoelastic properties of water-saturated clay sediments.
Approved for public release, distribution unlimited === The complex shear modulus of both kaolin-water and bentonite-water mixtures has been determined in the laboratory. The method involved measuring the reaction on a torsional elastic wave propagated down a metal rod when the rod was immersed in s...
Main Author: | |
---|---|
Other Authors: | |
Language: | en_US |
Published: |
Monterey, California. Naval Postgraduate School
2014
|
Online Access: | http://hdl.handle.net/10945/40051 |
id |
ndltd-nps.edu-oai-calhoun.nps.edu-10945-40051 |
---|---|
record_format |
oai_dc |
spelling |
ndltd-nps.edu-oai-calhoun.nps.edu-10945-400512015-05-06T03:58:51Z Measurement of the viscoelastic properties of water-saturated clay sediments. Cohen, Steven Robert Wilson, O.B. Naval Postgraduate School (U.S.) Approved for public release, distribution unlimited The complex shear modulus of both kaolin-water and bentonite-water mixtures has been determined in the laboratory. The method involved measuring the reaction on a torsional elastic wave propagated down a metal rod when the rod was immersed in sediment. Observations were made over the frequency range two to forty-three kHz. Dispersed sediments behaved like Newtonian liquids. Undispersed sediments, however, were viscoelastic in character, and their shear moduli exhibited no dependence on frequency. For undispersed kaolin mixtures, a typical result is (21.6 + i 1.2) x 1,000 dynes per square centimeter at 32 percent concentration. In bentonite, a modulus of (4.6 + i 2.0) x 10,000 dynes per square centimeter at 19 percent concentration is representative. 2014-03-27T21:10:22Z 2014-03-27T21:10:22Z 1968-06 Thesis http://hdl.handle.net/10945/40051 en_US This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. As such, it is in the public domain, and under the provisions of Title 17, United States Code, Section 105, it may not be copyrighted. Monterey, California. Naval Postgraduate School |
collection |
NDLTD |
language |
en_US |
sources |
NDLTD |
description |
Approved for public release, distribution unlimited === The complex shear modulus of both kaolin-water and bentonite-water mixtures has been determined in the laboratory. The method involved measuring the reaction on a torsional elastic wave propagated down a metal rod when the rod was immersed in sediment. Observations were made over the frequency range two to forty-three kHz. Dispersed sediments behaved like Newtonian liquids. Undispersed sediments, however, were viscoelastic in character, and their shear moduli exhibited no dependence on frequency. For undispersed kaolin mixtures, a typical result is (21.6 + i 1.2) x 1,000 dynes per square centimeter at 32 percent concentration. In bentonite, a modulus of (4.6 + i 2.0) x 10,000 dynes per square centimeter at 19 percent concentration is representative. |
author2 |
Wilson, O.B. |
author_facet |
Wilson, O.B. Cohen, Steven Robert |
author |
Cohen, Steven Robert |
spellingShingle |
Cohen, Steven Robert Measurement of the viscoelastic properties of water-saturated clay sediments. |
author_sort |
Cohen, Steven Robert |
title |
Measurement of the viscoelastic properties of water-saturated clay sediments. |
title_short |
Measurement of the viscoelastic properties of water-saturated clay sediments. |
title_full |
Measurement of the viscoelastic properties of water-saturated clay sediments. |
title_fullStr |
Measurement of the viscoelastic properties of water-saturated clay sediments. |
title_full_unstemmed |
Measurement of the viscoelastic properties of water-saturated clay sediments. |
title_sort |
measurement of the viscoelastic properties of water-saturated clay sediments. |
publisher |
Monterey, California. Naval Postgraduate School |
publishDate |
2014 |
url |
http://hdl.handle.net/10945/40051 |
work_keys_str_mv |
AT cohenstevenrobert measurementoftheviscoelasticpropertiesofwatersaturatedclaysediments |
_version_ |
1716803347564986368 |