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Record #174455:

Soil deformation within the seabed due to ice-scouring / Ryo Ishikawa.

Title: Soil deformation within the seabed due to ice-scouring / Ryo Ishikawa.
Author(s): Ishikawa, Ryo.
Date: 2005.
Publisher: Mombetsu: Okhotsk Sea & Cold Ocean Research Association
In: Proceedings of the 20th International Symposium on Okhotsk Sea and Sea Ice, Mombetsu, Hokkaido, Japan, 20-25 February 2005. (2005.),
Abstract: Presents model experiments related to "sub-scour deformation", stress transmission or soil deformation within seabed below sea ice that occurs as deformed sea ice such as ice ridge comes into contact with seabed. Describes use of steel model ice keel in test tank. Finds stress within seabed does not depend on drift speed by on attack angle, and that model ice with smaller attack angle causes deformation over larger area through restriction/compression of large amount of soil in front of inclined ice surface.
Notes:

In: Proceedings of the 20th International Symposium on Okhotsk Sea and Sea Ice, Mombetsu, Hokkaido, Japan, 20-25 February 2005 / Okhotsk Sea & Cold Ocean Research Association.

Keywords: 551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.321.8 -- Glaciological model experiments.
551.326.37 -- Pressure ridges.
621.644 -- Pipelines.
551.326.3 -- Floating ice, structure and surface features.
624.145 -- Floating ice, engineering aspects.
624.145.2 -- Floating ice, damage.
624.145.4 -- Floating ice, protection.
E6 -- Glaciology: floating ice.
SPRI record no.: 174455

MARCXML

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001 SPRI-174455
005 20220930162303.0
007 ta
008 220930s2005####ja#a###|#####|0||#0#eng#d
035 ## ‡aSPRI-174455
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aIshikawa, Ryo.
245 10 ‡aSoil deformation within the seabed due to ice-scouring /‡cRyo Ishikawa.
260 ## ‡aMombetsu :‡bOkhotsk Sea & Cold Ocean Research Association,‡c2005.
300 ## ‡ap. 193-200 :‡bdiags., table.
500 ## ‡aIn: Proceedings of the 20th International Symposium on Okhotsk Sea and Sea Ice, Mombetsu, Hokkaido, Japan, 20-25 February 2005 / Okhotsk Sea & Cold Ocean Research Association.
520 3# ‡aPresents model experiments related to "sub-scour deformation", stress transmission or soil deformation within seabed below sea ice that occurs as deformed sea ice such as ice ridge comes into contact with seabed. Describes use of steel model ice keel in test tank. Finds stress within seabed does not depend on drift speed by on attack angle, and that model ice with smaller attack angle causes deformation over larger area through restriction/compression of large amount of soil in front of inclined ice surface.
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.321.8 -- Glaciological model experiments.‡2udc
650 07 ‡a551.326.37 -- Pressure ridges.‡2udc
650 07 ‡a621.644 -- Pipelines.‡2udc
650 07 ‡a551.326.3 -- Floating ice, structure and surface features.‡2udc
650 07 ‡a624.145 -- Floating ice, engineering aspects.‡2udc
650 07 ‡a624.145.2 -- Floating ice, damage.‡2udc
650 07 ‡a624.145.4 -- Floating ice, protection.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
773 0# ‡7c2am ‡aOkhotsk Sea & Cold Ocean Research Association. ‡tProceedings of the 20th International Symposium on Okhotsk Sea and Sea Ice, Mombetsu, Hokkaido, Japan, 20-25 February 2005. ‡dMombetsu : Okhotsk Sea & Cold Ocean Research Association, 2005. ‡wSPRI-171671
916 ## ‡a2006/02/08 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220930 ‡bRF