An Examination of a Subsurface Impact on a Floating Ice Sheet.

An examination is made of the influence that various parameters impose upon the structural dynamics of a floating ice sheet due to the initial impact of a large mass. The Ritz method is employed to formulate a simple shape function to approximate a solution of the plate equation, subsequently used t...

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Bibliographic Details
Main Author: Conley, Judy A.
Other Authors: NAVAL SURFACE WARFARE CENTER CARDEROCK DIV BETHESDA MD
Format: Text
Language:English
Published: 1997
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA338293
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA338293
id ftdtic:ADA338293
record_format openpolar
spelling ftdtic:ADA338293 2023-05-15T16:37:24+02:00 An Examination of a Subsurface Impact on a Floating Ice Sheet. Conley, Judy A. NAVAL SURFACE WARFARE CENTER CARDEROCK DIV BETHESDA MD 1997-11 text/html http://www.dtic.mil/docs/citations/ADA338293 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA338293 en eng http://www.dtic.mil/docs/citations/ADA338293 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost *ICE *FLOATING BODIES FUNCTIONS VOLUME GLOBAL INERTIA IMPACT DYNAMICS PARAMETERS STRUCTURAL PROPERTIES MASS DISPLACEMENT FORMULATIONS SHAPE POTENTIAL ENERGY HEMISPHERES SUBSURFACE COLLISIONS CRUSHING Text 1997 ftdtic 2016-02-19T21:52:00Z An examination is made of the influence that various parameters impose upon the structural dynamics of a floating ice sheet due to the initial impact of a large mass. The Ritz method is employed to formulate a simple shape function to approximate a solution of the plate equation, subsequently used to represent the static displacement, obtain bending stiffness, and appropriate the fundamental frequency by the principle of minimum potential energy. Fluid inertia is incorporated by assuming the mass of a hemispherical volume of fluid, associated with the effective radius of the displaced shape, distributed as a function of the displaced shape of the plate. A dynamic formulation of a two degree-of-freedom system is made and shown equivalent to two separate one degree-of-freedom systems because of the huge disparity between the two masses due to the fluid inertia influence. Each separate system provides solutions for different issues of the study. An inelastic collision represents the global impact loading influencing the general bending of the ice plate. The local crushing deformation on the underside of the ice plate, found using both a Hertz contact solution and linear approximation, depicts the initial impact force. The influence of parameters for each system is quantified. Text Ice Ice Sheet 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
*ICE
*FLOATING BODIES
FUNCTIONS
VOLUME
GLOBAL
INERTIA
IMPACT
DYNAMICS
PARAMETERS
STRUCTURAL PROPERTIES
MASS
DISPLACEMENT
FORMULATIONS
SHAPE
POTENTIAL ENERGY
HEMISPHERES
SUBSURFACE
COLLISIONS
CRUSHING
spellingShingle Snow
Ice and Permafrost
*ICE
*FLOATING BODIES
FUNCTIONS
VOLUME
GLOBAL
INERTIA
IMPACT
DYNAMICS
PARAMETERS
STRUCTURAL PROPERTIES
MASS
DISPLACEMENT
FORMULATIONS
SHAPE
POTENTIAL ENERGY
HEMISPHERES
SUBSURFACE
COLLISIONS
CRUSHING
Conley, Judy A.
An Examination of a Subsurface Impact on a Floating Ice Sheet.
topic_facet Snow
Ice and Permafrost
*ICE
*FLOATING BODIES
FUNCTIONS
VOLUME
GLOBAL
INERTIA
IMPACT
DYNAMICS
PARAMETERS
STRUCTURAL PROPERTIES
MASS
DISPLACEMENT
FORMULATIONS
SHAPE
POTENTIAL ENERGY
HEMISPHERES
SUBSURFACE
COLLISIONS
CRUSHING
description An examination is made of the influence that various parameters impose upon the structural dynamics of a floating ice sheet due to the initial impact of a large mass. The Ritz method is employed to formulate a simple shape function to approximate a solution of the plate equation, subsequently used to represent the static displacement, obtain bending stiffness, and appropriate the fundamental frequency by the principle of minimum potential energy. Fluid inertia is incorporated by assuming the mass of a hemispherical volume of fluid, associated with the effective radius of the displaced shape, distributed as a function of the displaced shape of the plate. A dynamic formulation of a two degree-of-freedom system is made and shown equivalent to two separate one degree-of-freedom systems because of the huge disparity between the two masses due to the fluid inertia influence. Each separate system provides solutions for different issues of the study. An inelastic collision represents the global impact loading influencing the general bending of the ice plate. The local crushing deformation on the underside of the ice plate, found using both a Hertz contact solution and linear approximation, depicts the initial impact force. The influence of parameters for each system is quantified.
author2 NAVAL SURFACE WARFARE CENTER CARDEROCK DIV BETHESDA MD
format Text
author Conley, Judy A.
author_facet Conley, Judy A.
author_sort Conley, Judy A.
title An Examination of a Subsurface Impact on a Floating Ice Sheet.
title_short An Examination of a Subsurface Impact on a Floating Ice Sheet.
title_full An Examination of a Subsurface Impact on a Floating Ice Sheet.
title_fullStr An Examination of a Subsurface Impact on a Floating Ice Sheet.
title_full_unstemmed An Examination of a Subsurface Impact on a Floating Ice Sheet.
title_sort examination of a subsurface impact on a floating ice sheet.
publishDate 1997
url http://www.dtic.mil/docs/citations/ADA338293
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA338293
genre Ice
Ice Sheet
permafrost
genre_facet Ice
Ice Sheet
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA338293
op_rights APPROVED FOR PUBLIC RELEASE
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