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Record #112828:

The effect of deformation on fabric development in columnar sea ice / E. Stander, Bernard Michel.

Title: The effect of deformation on fabric development in columnar sea ice / E. Stander, Bernard Michel.
Author(s): Stander, E.
Michel, Bernard.
Date: 1991.
Publisher: St. John's, Newfoundland: Memorial University of Newfoundland, Ocean Engineering Research Centre
In: POAC'91 : the 11th International Conference on Port and Ocean Engineering under Arctic Conditions, September 24-28, 1991, St. John's, Canada. (1991.), Vol.1.
Abstract: Reviews observations on development of aligned columnar (S3 or C3) sea ice, in which ice crystals share unique, usually horizontal, c-axis alignment, which can complicate ice/structure interactions as strength of this ice type varies with function of geometry and direction of imposed deformation. Experiments test hypothesis that c-axis alignment can be influenced in this way, and discusses results in relation to previously published models.
Notes:

In: POAC'91 : the 11th International Conference on Port and Ocean Engineering under Arctic Conditions, September 24-28, 1991, St. John's, Canada. Vol.1. / D.B. Muggeridge, D.B. Colbourne, H.M. Muggeridge, eds.

Keywords: 551.32 -- Glaciology.
551.322 -- Ice and snow.
551.326 -- Floating ice.
539.37 -- Ice, plastic and viscous deformation.
548.2 -- Ice, granular structure. Anisotropy.
551.326.7 -- Sea ice.
E6 -- Glaciology: floating ice.
SPRI record no.: 112828

MARCXML

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245 14 ‡aThe effect of deformation on fabric development in columnar sea ice /‡cE. Stander, Bernard Michel.
260 ## ‡aSt. John's, Newfoundland :‡bMemorial University of Newfoundland, Ocean Engineering Research Centre,‡c1991.
300 ## ‡ap. 527-540 :‡bill., diags., table.
500 ## ‡aIn: POAC'91 : the 11th International Conference on Port and Ocean Engineering under Arctic Conditions, September 24-28, 1991, St. John's, Canada. Vol.1. / D.B. Muggeridge, D.B. Colbourne, H.M. Muggeridge, eds.
520 3# ‡aReviews observations on development of aligned columnar (S3 or C3) sea ice, in which ice crystals share unique, usually horizontal, c-axis alignment, which can complicate ice/structure interactions as strength of this ice type varies with function of geometry and direction of imposed deformation. Experiments test hypothesis that c-axis alignment can be influenced in this way, and discusses results in relation to previously published models.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.322 -- Ice and snow.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a539.37 -- Ice, plastic and viscous deformation.‡2udc
650 07 ‡a548.2 -- Ice, granular structure. Anisotropy.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
700 1# ‡aMichel, Bernard.
773 0# ‡7nnam ‡aD.B. Muggeridge, D.B. Colbourne, H.M. Muggeridge, eds. ‡tPOAC'91 : the 11th International Conference on Port and Ocean Engineering under Arctic Conditions, September 24-28, 1991, St. John's, Canada. ‡dSt. John's, Newfoundland : Memorial University of Newfoundland, Ocean Engineering Research Centre, 1991. ‡gVol.1. ‡wSPRI-112387
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