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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #84471:

Outward flux of vapour from frozen soils at Mayo, Yukon, Canada: results and interpretation / Michael W. Smith, C.R. Burn.

Title: Outward flux of vapour from frozen soils at Mayo, Yukon, Canada: results and interpretation / Michael W. Smith, C.R. Burn.
Author(s): Smith, Michael W.
Burn, C. R.
Date: 1987.
In: Cold Regions Science and Technology. (1987.), Vol. 13(2) (1987)
Abstract: At site where permafrost was present, ouflow ceased by March. At other site, where there was only seasonal frost, flow continued throughout season. Magnitude of fluxes first examined in terms of soil vapour diffusion, but this was shown to be inadequate. However, observations were shown to be consistent with liquid transport through frozen soil.
Notes:

Cold Regions Science and Technology. Vol. 13(2) :143-152 (1987).

Keywords: 551.345 -- Permafrost. Cryopedology.
536 -- Heat.
551.343.7 -- Frost, soil moisture and surface water, effect on movement of.
E8 -- Glaciology: frost action and permafrost.
(*41) -- Canada.
(*430) -- Yukon Territory.
SPRI record no.: 84471

MARCXML

LDR 01319naa#a2200000#a#4500
001 SPRI-84471
005 20220929155518.0
007 ta
008 220929s1987####xx#a##|##|###|0||#0|eng#d
035 ## ‡aSPRI-84471
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aSmith, Michael W.
245 10 ‡aOutward flux of vapour from frozen soils at Mayo, Yukon, Canada :‡bresults and interpretation /‡cMichael W. Smith, C.R. Burn.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1987.
300 ## ‡ap. 143-152 :‡billus., diags., tables.
500 ## ‡aCold Regions Science and Technology. Vol. 13(2) :143-152 (1987).
520 3# ‡aAt site where permafrost was present, ouflow ceased by March. At other site, where there was only seasonal frost, flow continued throughout season. Magnitude of fluxes first examined in terms of soil vapour diffusion, but this was shown to be inadequate. However, observations were shown to be consistent with liquid transport through frozen soil.
650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc
650 07 ‡a536 -- Heat.‡2udc
650 07 ‡a551.343.7 -- Frost, soil moisture and surface water, effect on movement of.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*41) -- Canada.‡2udc
651 #7 ‡a(*430) -- Yukon Territory.‡2udc
700 1# ‡aBurn, C. R.
773 0# ‡7nnas ‡tCold Regions Science and Technology. ‡gVol. 13(2) (1987) ‡wSPRI-59075
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220929