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Record #126225:
- #126225
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MARC recordTime delay in the water--ice phase change during soil freezing / Wilko K.P. van Loon, Ies A. van Haneghem, Hennie P.A. Boshoven, Edo Gerkema, Ed Perfect.
| Title: | Time delay in the water--ice phase change during soil freezing / Wilko K.P. van Loon, Ies A. van Haneghem, Hennie P.A. Boshoven, Edo Gerkema, Ed Perfect. |
| Author(s): | Loon, Wilko K. P. van. Haneghem, Ies A. van. Boshoven, Hennie P. A. Gerkema, Edo. Perfect, Ed. |
| Date: | 1993. |
| In: | CRREL Special Report. (1993.), Vol. 93-22 (1993) |
| Abstract: | Heat fluxes that accompany in situ freezing of pore water were investigated by comparing two independent measurements close to 0°C isotherm: temperature and unfrozen water content. From both measurements, estimation of latent heat flux can be obtained. Calculations indicated that 0°C isotherm penetrated faster than corresponding rate of change in liquid water content. Concludes there is time delay in formation of pore ice, which can be related to time dependence of nucleation phenomena. |
| Notes: | CRREL Special Report. Vol. 93-22 :256-262 (1993). |
| Keywords: | 551.34 -- Geocryology. Frozen ground. 551.345 -- Permafrost. Cryopedology. 536.421.4 -- Freezing. 551.345.2 -- Permafrost, formation and decay. 536.65 -- Ice, latent heat. E8 -- Glaciology: frost action and permafrost. |
| SPRI record no.: | 126225 |
LDR 01550naa#a2200000#a#4500 001 SPRI-126225 005 20240419030441.0 007 ta 008 240419s1993####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-126225 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aTime delay in the water--ice phase change during soil freezing /‡cWilko K.P. van Loon, Ies A. van Haneghem, Hennie P.A. Boshoven, Edo Gerkema, Ed Perfect. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 256-262 :‡bdiags., tables. 500 ## ‡aCRREL Special Report. Vol. 93-22 :256-262 (1993). 520 3# ‡aHeat fluxes that accompany in situ freezing of pore water were investigated by comparing two independent measurements close to 0°C isotherm: temperature and unfrozen water content. From both measurements, estimation of latent heat flux can be obtained. Calculations indicated that 0°C isotherm penetrated faster than corresponding rate of change in liquid water content. Concludes there is time delay in formation of pore ice, which can be related to time dependence of nucleation phenomena. 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 ‡a536.65 -- Ice, latent heat.‡2udc 650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local 700 1# ‡aLoon, Wilko K. P. van. 700 1# ‡aHaneghem, Ies A. van. 700 1# ‡aBoshoven, Hennie P. A. 700 1# ‡aGerkema, Edo. 700 1# ‡aPerfect, Ed. 773 0# ‡7nnas ‡tCRREL Special Report. ‡gVol. 93-22 (1993) ‡wSPRI-36510 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419