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Record #126224:
- #126224
Main publication details
MARC recordThe growth condition of a segregated ice layer and the segregation potential / Yoshisuke Nakano, Kazuo Takeda.
| Title: | The growth condition of a segregated ice layer and the segregation potential / Yoshisuke Nakano, Kazuo Takeda. |
| Author(s): | Nakano, Yoshisuke. Takeda, Kazuo. |
| Date: | 1993. |
| In: | CRREL Special Report. (1993.), Vol. 93-22 (1993) |
| Abstract: | Growth condition of segregated ice layer in freezing soil can be described accurately by model of frozen fringe in which gradients of temperature and unfrozen water pressure are two independent driving forces of water. Segregation potential theory of soil freezing was examined by using this model and empirical findings. Accuracy of theory in predicting growth of final ice layer can be improved if neglected term of pressure gradient is restored in equation of water flow. |
| Notes: | CRREL Special Report. Vol. 93-22 :250-255 (1993). |
| Keywords: | 551.34 -- Geocryology. Frozen ground. 551.345 -- Permafrost. Cryopedology. 536.421.4 -- Freezing. 551.345.2 -- Permafrost, formation and decay. 519.673 -- Modelling. 536.65 -- Ice, latent heat. E8 -- Glaciology: frost action and permafrost. |
| SPRI record no.: | 126224 |
LDR 01429naa#a2200000#a#4500 001 SPRI-126224 005 20230922221127.0 007 ta 008 230922s1993####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-126224 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aNakano, Yoshisuke. 245 14 ‡aThe growth condition of a segregated ice layer and the segregation potential /‡cYoshisuke Nakano, Kazuo Takeda. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 250-255 :‡bdiags. 500 ## ‡aCRREL Special Report. Vol. 93-22 :250-255 (1993). 520 3# ‡aGrowth condition of segregated ice layer in freezing soil can be described accurately by model of frozen fringe in which gradients of temperature and unfrozen water pressure are two independent driving forces of water. Segregation potential theory of soil freezing was examined by using this model and empirical findings. Accuracy of theory in predicting growth of final ice layer can be improved if neglected term of pressure gradient is restored in equation of water flow. 650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc 650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc 650 07 ‡a536.421.4 -- Freezing.‡2udc 650 07 ‡a551.345.2 -- Permafrost, formation and decay.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a536.65 -- Ice, latent heat.‡2udc 650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local 700 1# ‡aTakeda, Kazuo. 773 0# ‡7nnas ‡tCRREL Special Report. ‡gVol. 93-22 (1993) ‡wSPRI-36510 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230922