Vector Analysis of Ice Fabric Data

The mechanical properties of ice are strongly affected by crystal texture and c-axis alignment. In this report we develop a general quantitative method for analysis of uniaxial crystal orientation data. These data are represented as unit vectors from the origin with endpoints on the surface of a uni...

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Bibliographic Details
Main Authors: Ferrick, Michael G., Claffey, Kerran J.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
Format: Text
Language:English
Published: 1992
Subjects:
ICE
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA250832
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA250832
id ftdtic:ADA250832
record_format openpolar
spelling ftdtic:ADA250832 2023-05-15T16:37:18+02:00 Vector Analysis of Ice Fabric Data Ferrick, Michael G. Claffey, Kerran J. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1992-03 text/html http://www.dtic.mil/docs/citations/ADA250832 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA250832 en eng http://www.dtic.mil/docs/citations/ADA250832 Approved for public release; distribution is unlimited. DTIC AND NTIS Snow Ice and Permafrost Numerical Mathematics *SEA ICE *ICE MECHANICS EIGENVALUES CRYSTALS SPHERES ICE FORMATION ALIGNMENT VARIABLES SURFACES ICE ERRORS VECTOR ANALYSIS STANDARDS OCEANS EQUATIONS TEXTURE STRUCTURES MECHANICAL PROPERTIES COMPARISON AST42 WU01 COMPRESSIVE STRENGTH SCHMIDT NETS PE61102A Text 1992 ftdtic 2016-02-22T16:19:04Z The mechanical properties of ice are strongly affected by crystal texture and c-axis alignment. In this report we develop a general quantitative method for analysis of uniaxial crystal orientation data. These data are represented as unit vectors from the origin with endpoints on the surface of a unit sphere. An orthogonal least-squares error measure is used to develop equations that define the closest plane and line through the data. The resulting eigenvalue problem is identical to that obtained by other investigators using different methods. However, we identify an implicit assumption in the method, and observe that the error measure represents physical distance and quantifies the goodness-of-fit of the idealized structures to the data. For comparison, a parallel development is presented of classical dependent-variable least squares. A method is developed to transform the data and the results for viewing on Schmidt nets drawn in the best plane and the predominant basal plane of a sample, in addition to the standard xy-plane. Applications of the analysis to sea ice samples include both numerical and Schmidt net presentations of results. C-axis orientation, Orthogonal least-squares, Sea ice, Crystal fabric analysis, Schmidt nets. Text Ice permafrost Sea ice 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
Numerical Mathematics
*SEA ICE
*ICE MECHANICS
EIGENVALUES
CRYSTALS
SPHERES
ICE FORMATION
ALIGNMENT
VARIABLES
SURFACES
ICE
ERRORS
VECTOR ANALYSIS
STANDARDS
OCEANS
EQUATIONS
TEXTURE
STRUCTURES
MECHANICAL PROPERTIES
COMPARISON
AST42
WU01
COMPRESSIVE STRENGTH
SCHMIDT NETS
PE61102A
spellingShingle Snow
Ice and Permafrost
Numerical Mathematics
*SEA ICE
*ICE MECHANICS
EIGENVALUES
CRYSTALS
SPHERES
ICE FORMATION
ALIGNMENT
VARIABLES
SURFACES
ICE
ERRORS
VECTOR ANALYSIS
STANDARDS
OCEANS
EQUATIONS
TEXTURE
STRUCTURES
MECHANICAL PROPERTIES
COMPARISON
AST42
WU01
COMPRESSIVE STRENGTH
SCHMIDT NETS
PE61102A
Ferrick, Michael G.
Claffey, Kerran J.
Vector Analysis of Ice Fabric Data
topic_facet Snow
Ice and Permafrost
Numerical Mathematics
*SEA ICE
*ICE MECHANICS
EIGENVALUES
CRYSTALS
SPHERES
ICE FORMATION
ALIGNMENT
VARIABLES
SURFACES
ICE
ERRORS
VECTOR ANALYSIS
STANDARDS
OCEANS
EQUATIONS
TEXTURE
STRUCTURES
MECHANICAL PROPERTIES
COMPARISON
AST42
WU01
COMPRESSIVE STRENGTH
SCHMIDT NETS
PE61102A
description The mechanical properties of ice are strongly affected by crystal texture and c-axis alignment. In this report we develop a general quantitative method for analysis of uniaxial crystal orientation data. These data are represented as unit vectors from the origin with endpoints on the surface of a unit sphere. An orthogonal least-squares error measure is used to develop equations that define the closest plane and line through the data. The resulting eigenvalue problem is identical to that obtained by other investigators using different methods. However, we identify an implicit assumption in the method, and observe that the error measure represents physical distance and quantifies the goodness-of-fit of the idealized structures to the data. For comparison, a parallel development is presented of classical dependent-variable least squares. A method is developed to transform the data and the results for viewing on Schmidt nets drawn in the best plane and the predominant basal plane of a sample, in addition to the standard xy-plane. Applications of the analysis to sea ice samples include both numerical and Schmidt net presentations of results. C-axis orientation, Orthogonal least-squares, Sea ice, Crystal fabric analysis, Schmidt nets.
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
format Text
author Ferrick, Michael G.
Claffey, Kerran J.
author_facet Ferrick, Michael G.
Claffey, Kerran J.
author_sort Ferrick, Michael G.
title Vector Analysis of Ice Fabric Data
title_short Vector Analysis of Ice Fabric Data
title_full Vector Analysis of Ice Fabric Data
title_fullStr Vector Analysis of Ice Fabric Data
title_full_unstemmed Vector Analysis of Ice Fabric Data
title_sort vector analysis of ice fabric data
publishDate 1992
url http://www.dtic.mil/docs/citations/ADA250832
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA250832
genre Ice
permafrost
Sea ice
genre_facet Ice
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA250832
op_rights Approved for public release; distribution is unlimited.
_version_ 1766027590410174464