skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View a record

Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.

Please search for material in iDiscover for up-to-date information about the library collection.


Record #94382:

Secondary creep interpretations of ice rich permafrost. Secondary creep, permafrost soils, creep of ice / E.C. McRoberts.

Title: Secondary creep interpretations of ice rich permafrost. Secondary creep, permafrost soils, creep of ice / E.C. McRoberts.
Author(s): McRoberts, E. C.
Date: 1988.
Publisher: Trondheim: Tapir Publishers
In: Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. (1988.), Vol. 2.
Abstract: Presents results for temperatures from -0.8 to -4.0°C. Data are compared with recently published summaries of ice creep. For temperatures <-2°C, ice-creep data yield satisfactory constitutive relationship for creep in permafrost. At warmer temperatures, faster secondary creep rates are exhibited.
Notes:

In: Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. Vol. 2. / Kaare Senneset, ed.

Keywords: 551.345 -- Permafrost. Cryopedology.
539.37 -- Ice, plastic and viscous deformation.
E8 -- Glaciology: frost action and permafrost.
SPRI record no.: 94382

MARCXML

LDR 01256naa#a2200000#a#4500
001 SPRI-94382
005 20240329141915.0
007 ta
008 240329s1988####no#a###|#####|0||#0#eng#d
035 ## ‡aSPRI-94382
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aMcRoberts, E. C.
245 10 ‡aSecondary creep interpretations of ice rich permafrost. Secondary creep, permafrost soils, creep of ice /‡cE.C. McRoberts.
260 ## ‡aTrondheim :‡bTapir Publishers,‡c1988.
300 ## ‡ap. 1137-1142 :‡bdiags., tables.
500 ## ‡aIn: Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. Vol. 2. / Kaare Senneset, ed.
520 3# ‡aPresents results for temperatures from -0.8 to -4.0°C. Data are compared with recently published summaries of ice creep. For temperatures <-2°C, ice-creep data yield satisfactory constitutive relationship for creep in permafrost. At warmer temperatures, faster secondary creep rates are exhibited.
650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc
650 07 ‡a539.37 -- Ice, plastic and viscous deformation.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
773 0# ‡7nnam ‡aKaare Senneset, ed. ‡tPermafrost. Fifth International Conference. August 2-5, 1988. Proceedings. ‡dTrondheim : Tapir Publishers, 1988. ‡gVol. 2. ‡wSPRI-93838
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240329