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Record #94157:
- #94157
Main publication details
MARC recordA method for measuring the rate of water transport due to temperature gradients in unsaturated frozen soils / Yoshisuke Nakano, A.R. Tice.
| Title: | A method for measuring the rate of water transport due to temperature gradients in unsaturated frozen soils / Yoshisuke Nakano, A.R. Tice. |
| Author(s): | Nakano, Yoshisuke. Tice, A. R. |
| Date: | 1988. |
| Publisher: | Trondheim: Tapir Publishers |
| In: | Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. (1988.), Vol. 1. |
| Abstract: | When linear temperature distribution is imposed on closed soil column with initial uniform water content, redistribution of water occurs in column. As time increases, profile of water is stabilized to approach stationary condition, which is used to calculate rate of water movement due to temperature gradients. Theoretical justification of method is presented and feasibility is demonstrated by experiments with marine-deposited clay. |
| Notes: | In: Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. Vol. 1. / Kaare Senneset, ed. |
| Keywords: | 551.345.2 -- Permafrost, formation and decay. 551.341 -- Permafrost and frozen ground, equipment for investigating. E3 -- Glaciology: instruments and methods. |
| SPRI record no.: | 94157 |
LDR 01458naa#a2200000#a#4500 001 SPRI-94157 005 20230321141715.0 007 ta 008 230321s1988####no#a###|#####|0||#0#eng#d 035 ## ‡aSPRI-94157 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aNakano, Yoshisuke. 245 12 ‡aA method for measuring the rate of water transport due to temperature gradients in unsaturated frozen soils /‡cYoshisuke Nakano, A.R. Tice. 260 ## ‡aTrondheim :‡bTapir Publishers,‡c1988. 300 ## ‡ap. 412-417 :‡bdiags., table. 500 ## ‡aIn: Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. Vol. 1. / Kaare Senneset, ed. 520 3# ‡aWhen linear temperature distribution is imposed on closed soil column with initial uniform water content, redistribution of water occurs in column. As time increases, profile of water is stabilized to approach stationary condition, which is used to calculate rate of water movement due to temperature gradients. Theoretical justification of method is presented and feasibility is demonstrated by experiments with marine-deposited clay. 650 07 ‡a551.345.2 -- Permafrost, formation and decay.‡2udc 650 07 ‡a551.341 -- Permafrost and frozen ground, equipment for investigating.‡2udc 650 07 ‡aE3 -- Glaciology: instruments and methods.‡2local 700 1# ‡aTice, A. R. 773 0# ‡7nnam ‡aKaare Senneset, ed. ‡tPermafrost. Fifth International Conference. August 2-5, 1988. Proceedings. ‡dTrondheim : Tapir Publishers, 1988. ‡gVol. 1. ‡wSPRI-93838 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230321