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Record #162057:
- #162057
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MARC recordЗарождение и рост кристаллов льда на поверхности водоемов
| Title: | Зарождение и рост кристаллов льда на поверхности водоемов |
| Title, transliterated: | Zarozhdenie i rost kristallov lʹda na poverkhnosti vodoemov / V.N. Golubev. |
| Translated title: | Origin and propagation of ice crystals on a surface of water reservoirs. |
| Author(s): | Golubev, V. N. |
| Date: | 2002. |
| Language: | Russian. |
| In: | Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. (2002.), Vol. 92 (2002) |
| Abstract: | Discusses formation of ice on surface of water, finding condition of surface, whether calm or rough, together with hydrometeorological conditions, influences appearance and growth of ice crystals. Particles from atmosphere or soil become centres of crystallization. When supercooling of surface layer of water exceeds 0.1°C, formation of ice dendrites and needles is possible. Ice crust forms within 10⁴ s under radiate cooling. The ice formed on centres of crystallization when air temperature is low comes from condensation evaporated from vapour on surface of water. Defines three main types of ice-layer surface structure according to cooling, condition of water surface and source of crystallization centres. |
| Notes: | Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 92 :149-157 (2002). English summary and figure captions. |
| Keywords: | 551.322 -- Ice and snow. 548 -- Crystallography. 548.5 -- Ice crystals. 548.51 -- Ice crystal nuclei. 551.326 -- Floating ice. E6 -- Glaciology: floating ice. |
| SPRI record no.: | 162057 |
LDR 02252naa#a2200000#a#4500 001 SPRI-162057 005 20231207005118.0 007 ta 008 231207s2002####xx#a##|##|###|0||#0|rus#d 035 ## ‡aSPRI-162057 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡arus 100 1# ‡6880-01‡aGolubev, V. N. 242 10 ‡aOrigin and propagation of ice crystals on a surface of water reservoirs.‡yeng 245 10 ‡6880-02‡aZarozhdenie i rost kristallov lʹda na poverkhnosti vodoemov /‡cV.N. Golubev. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2002. 300 ## ‡ap. 149-157 :‡bdiags., table. 500 ## ‡aMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 92 :149-157 (2002). 500 ## ‡aEnglish summary and figure captions. 520 3# ‡aDiscusses formation of ice on surface of water, finding condition of surface, whether calm or rough, together with hydrometeorological conditions, influences appearance and growth of ice crystals. Particles from atmosphere or soil become centres of crystallization. When supercooling of surface layer of water exceeds 0.1°C, formation of ice dendrites and needles is possible. Ice crust forms within 10⁴ s under radiate cooling. The ice formed on centres of crystallization when air temperature is low comes from condensation evaporated from vapour on surface of water. Defines three main types of ice-layer surface structure according to cooling, condition of water surface and source of crystallization centres. 546 ## ‡aIn Russian. 546 ## ‡aRussian transliteration entered into original records using BGN/PCGN 1947 romanisation of Russian; Cyrillic text in MARC 880 field(s) reverse transliterated from this by automated process; BGN/PCGN 1947 text then upgraded to Library of Congress romanisation. 650 07 ‡a551.322 -- Ice and snow.‡2udc 650 07 ‡a548 -- Crystallography.‡2udc 650 07 ‡a548.5 -- Ice crystals.‡2udc 650 07 ‡a548.51 -- Ice crystal nuclei.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 773 0# ‡6880-03‡7nnas ‡tMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. ‡gVol. 92 (2002) ‡wSPRI-33585 880 1# ‡6100-01/(N‡aГолубев, В. Н. 880 10 ‡6245-02/(N‡aЗарождение и рост кристаллов льда на поверхности водоемов /‡cВ.Н. Голубев. 880 0# ‡6773-03/(N‡7nnas ‡tМатериалы Гляциологических Исследований. ‡gVol. 92 (2002) ‡wSPRI-33585 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231207