Brash Ice Behavior.

The behavior of brash ice, its formation and recommended vessel operating procedures are presented. Brash ice behaves as a Mohr-Coulomb solid below a critical strain rate or ship speed. Above this speed, fluidization of the medium occurs and the resistance appears to be that of a viscous, laminar fl...

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Bibliographic Details
Main Author: Greisman,Paul
Other Authors: COAST GUARD RESEARCH AND DEVELOPMENT CENTER GROTON CT
Format: Text
Language:English
Published: 1981
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA104152
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA104152
id ftdtic:ADA104152
record_format openpolar
spelling ftdtic:ADA104152 2023-05-15T16:37:09+02:00 Brash Ice Behavior. Greisman,Paul COAST GUARD RESEARCH AND DEVELOPMENT CENTER GROTON CT 1981-05 text/html http://www.dtic.mil/docs/citations/ADA104152 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA104152 en eng http://www.dtic.mil/docs/citations/ADA104152 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Civil Engineering Marine Engineering *Ice Fragments Channels(Waterways) Mechanical properties Ship hulls Interactions Resistance Laboratory tests Field tests *Brash ice Mohr-Coulomb theory Text 1981 ftdtic 2016-02-19T07:42:06Z The behavior of brash ice, its formation and recommended vessel operating procedures are presented. Brash ice behaves as a Mohr-Coulomb solid below a critical strain rate or ship speed. Above this speed, fluidization of the medium occurs and the resistance appears to be that of a viscous, laminar fluid. The optimum operating speed for a vessel in brash is at the viscous threshold, found here to be 0.12 sg.rt of gL) where g (32.2 fS-2) is the acceleration of gravity and L is the length of the vessel. Repeated passages through brash-filled channels to keep them unconsolidated are generally unadvisable due to the attendant enhancement of the accretion rates. The laboratory and field experiments employed in this study are presented. Laboratory tests in brash ice appear to yield very useful results that are good predictors of full-scale resistance. (Author) Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Civil Engineering
Marine Engineering
*Ice
Fragments
Channels(Waterways)
Mechanical properties
Ship hulls
Interactions
Resistance
Laboratory tests
Field tests
*Brash ice
Mohr-Coulomb theory
spellingShingle Snow
Ice and Permafrost
Civil Engineering
Marine Engineering
*Ice
Fragments
Channels(Waterways)
Mechanical properties
Ship hulls
Interactions
Resistance
Laboratory tests
Field tests
*Brash ice
Mohr-Coulomb theory
Greisman,Paul
Brash Ice Behavior.
topic_facet Snow
Ice and Permafrost
Civil Engineering
Marine Engineering
*Ice
Fragments
Channels(Waterways)
Mechanical properties
Ship hulls
Interactions
Resistance
Laboratory tests
Field tests
*Brash ice
Mohr-Coulomb theory
description The behavior of brash ice, its formation and recommended vessel operating procedures are presented. Brash ice behaves as a Mohr-Coulomb solid below a critical strain rate or ship speed. Above this speed, fluidization of the medium occurs and the resistance appears to be that of a viscous, laminar fluid. The optimum operating speed for a vessel in brash is at the viscous threshold, found here to be 0.12 sg.rt of gL) where g (32.2 fS-2) is the acceleration of gravity and L is the length of the vessel. Repeated passages through brash-filled channels to keep them unconsolidated are generally unadvisable due to the attendant enhancement of the accretion rates. The laboratory and field experiments employed in this study are presented. Laboratory tests in brash ice appear to yield very useful results that are good predictors of full-scale resistance. (Author)
author2 COAST GUARD RESEARCH AND DEVELOPMENT CENTER GROTON CT
format Text
author Greisman,Paul
author_facet Greisman,Paul
author_sort Greisman,Paul
title Brash Ice Behavior.
title_short Brash Ice Behavior.
title_full Brash Ice Behavior.
title_fullStr Brash Ice Behavior.
title_full_unstemmed Brash Ice Behavior.
title_sort brash ice behavior.
publishDate 1981
url http://www.dtic.mil/docs/citations/ADA104152
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA104152
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA104152
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766027447808032768