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Record #93076:

The indentation and arrest stress intensity factors of first year columnar sea ice / B.L. Parsons, J.B. Snellen, D.B. Muggeridge.

Title: The indentation and arrest stress intensity factors of first year columnar sea ice / B.L. Parsons, J.B. Snellen, D.B. Muggeridge.
Author(s): Parsons, B. L.
Snellen, J. B.
Muggeridge, D. B.
Date: 1988.
Publisher: [Delft]: International Association for Hydraulic Research, Committee on Ice Problems
In: Proceedings, the 9th International Symposium on Ice, 23-27 August 1988, Sapporo, Japan. (1988.), Vol. 1.
Abstract: Samples collected from Allen Bay, near Resolute Bay, NWT, Canada, in April 1987. Initiation stress intensity factor was found to increase with decreasing loading rate, but arrest stress intensity factor is time-independent. Crack growth length depends on drop from initiation to arrest value during event but showed no dependence on load rate. Arrest was observed in brine drainage channels and not at grain boundaries. Results show that arrest stress intensity factor should be used in crack length predictions during indentation phenomena, not critical stress intensity factor. Crack growth in ice is unstable, dynamic, and supplies significant kinetic energy to ice.
Notes:

In: Proceedings, the 9th International Symposium on Ice, 23-27 August 1988, Sapporo, Japan. Vol. 1. / Hiroshi Saeki, Ken-ichi Hirayama, eds.

Keywords: 624.145.5 -- Floating ice, bearing strength.
551.32 -- Glaciology.
551.326 -- Floating ice.
539.42 -- Ice, tensile strength.
539.56 -- Ice, fragility and brittleness.
E6 -- Glaciology: floating ice.
SPRI record no.: 93076

MARCXML

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100 1# ‡aParsons, B. L.
245 14 ‡aThe indentation and arrest stress intensity factors of first year columnar sea ice /‡cB.L. Parsons, J.B. Snellen, D.B. Muggeridge.
260 ## ‡a[Delft] :‡bInternational Association for Hydraulic Research, Committee on Ice Problems,‡c1988.
300 ## ‡ap. 502-511 :‡bdiags.
500 ## ‡aIn: Proceedings, the 9th International Symposium on Ice, 23-27 August 1988, Sapporo, Japan. Vol. 1. / Hiroshi Saeki, Ken-ichi Hirayama, eds.
520 3# ‡aSamples collected from Allen Bay, near Resolute Bay, NWT, Canada, in April 1987. Initiation stress intensity factor was found to increase with decreasing loading rate, but arrest stress intensity factor is time-independent. Crack growth length depends on drop from initiation to arrest value during event but showed no dependence on load rate. Arrest was observed in brine drainage channels and not at grain boundaries. Results show that arrest stress intensity factor should be used in crack length predictions during indentation phenomena, not critical stress intensity factor. Crack growth in ice is unstable, dynamic, and supplies significant kinetic energy to ice.
650 07 ‡a624.145.5 -- Floating ice, bearing strength.‡2udc
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a539.42 -- Ice, tensile strength.‡2udc
650 07 ‡a539.56 -- Ice, fragility and brittleness.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
700 1# ‡aSnellen, J. B.
700 1# ‡aMuggeridge, D. B.
773 0# ‡7nnam ‡aHiroshi Saeki, Ken-ichi Hirayama, eds. ‡tProceedings, the 9th International Symposium on Ice, 23-27 August 1988, Sapporo, Japan. ‡d[Delft] : International Association for Hydraulic Research, Committee on Ice Problems, 1988. ‡gVol. 1. ‡wSPRI-93033
917 ## ‡aUnenhanced record from Muscat, imported 2019
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