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Record #93328:
- #93328
Main publication details
MARC recordExperimental study on distribution of brine drainage channels in sea ice / Toshiyuki Kawamura.
| Title: | Experimental study on distribution of brine drainage channels in sea ice / Toshiyuki Kawamura. |
| Author(s): | Kawamura, Toshiyuki. |
| 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. 2. |
| Abstract: | Growth of brine drainage channels affects mechanical properties of sea ice. At low ice-growth rate, brine was drained from whole growing interface and channels were not shaped. At higher growth rates, definite channels formed on favoured grain boundaries at almost constant intervals. Channel interval tended to decrease with increasing c-axis inclination angle of adjacent grains to horizontal plane. Brine channels were formed initially at intersection of grain boundary and protrusion on ice-water interface. |
| Notes: | In: Proceedings, the 9th International Symposium on Ice, 23-27 August 1988, Sapporo, Japan. Vol. 2. / Hiroshi Saeki, Ken-ichi Hirayama, eds. |
| Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.7 -- Sea ice. 54 -- Chemistry. E6 -- Glaciology: floating ice. |
| SPRI record no.: | 93328 |
LDR 01634naa#a2200000#a#4500 001 SPRI-93328 005 20231202114422.0 007 ta 008 231202s1988####ne#a###|#####|0||#0#eng#d 035 ## ‡aSPRI-93328 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aKawamura, Toshiyuki. 245 10 ‡aExperimental study on distribution of brine drainage channels in sea ice /‡cToshiyuki Kawamura. 260 ## ‡a[Delft] :‡bInternational Association for Hydraulic Research, Committee on Ice Problems,‡c1988. 300 ## ‡ap. 219-228 :‡bill., table. 500 ## ‡aIn: Proceedings, the 9th International Symposium on Ice, 23-27 August 1988, Sapporo, Japan. Vol. 2. / Hiroshi Saeki, Ken-ichi Hirayama, eds. 520 3# ‡aGrowth of brine drainage channels affects mechanical properties of sea ice. At low ice-growth rate, brine was drained from whole growing interface and channels were not shaped. At higher growth rates, definite channels formed on favoured grain boundaries at almost constant intervals. Channel interval tended to decrease with increasing c-axis inclination angle of adjacent grains to horizontal plane. Brine channels were formed initially at intersection of grain boundary and protrusion on ice-water interface. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a54 -- Chemistry.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 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. 2. ‡wSPRI-93033 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231202