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Record #94182:
Physical and chemical characteristics of the active layer and near-surface permafrost in a disturbed homogeneous Picea nariana stand, Fort Norman, N.W.T., Canada / K.E. Evans, G.P. Kershaw, B.J. Gallinger.
Title: | Physical and chemical characteristics of the active layer and near-surface permafrost in a disturbed homogeneous Picea nariana stand, Fort Norman, N.W.T., Canada / K.E. Evans, G.P. Kershaw, B.J. Gallinger. |
Author(s): | Evans, K. E. Kershaw, G. P. Gallinger, B. J. |
Date: | 1988. |
Publisher: | Trondheim: Tapir Publishers |
In: | Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. (1988.), Vol. 1. |
Abstract: | Examines moisture content, pH, cation exchange capacity, and concentrations of Ca, Mg, and K. Probing of active layer to determine depth to permafrost indicated mean increase of 17% after one full growing season following tree canopy removal. Results confirm that variability among soil and near-surface permafrost characteristics is high both areally and with depth. |
Notes: | In: Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. Vol. 1. / Kaare Senneset, ed. |
Keywords: | 551.343 -- Periglacial processes. Thermokarst. 551.345 -- Permafrost. Cryopedology. 53 -- Physics. 54 -- Chemistry. E8 -- Glaciology: frost action and permafrost. (*41) -- Canada. (*440) -- Northwest Territories. |
SPRI record no.: | 94182 |
LDR 01596naa#a2200000#a#4500 001 SPRI-94182 005 20230401044113.0 007 ta 008 230401s1988####no#ab##|#####|0||#0#eng#d 035 ## ‡aSPRI-94182 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aEvans, K. E. 245 10 ‡aPhysical and chemical characteristics of the active layer and near-surface permafrost in a disturbed homogeneous Picea nariana stand, Fort Norman, N.W.T., Canada /‡cK.E. Evans, G.P. Kershaw, B.J. Gallinger. 260 ## ‡aTrondheim :‡bTapir Publishers,‡c1988. 300 ## ‡ap. 568-573 :‡bdiags., tables, map. 500 ## ‡aIn: Permafrost. Fifth International Conference. August 2-5, 1988. Proceedings. Vol. 1. / Kaare Senneset, ed. 520 3# ‡aExamines moisture content, pH, cation exchange capacity, and concentrations of Ca, Mg, and K. Probing of active layer to determine depth to permafrost indicated mean increase of 17% after one full growing season following tree canopy removal. Results confirm that variability among soil and near-surface permafrost characteristics is high both areally and with depth. 650 07 ‡a551.343 -- Periglacial processes. Thermokarst.‡2udc 650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc 650 07 ‡a53 -- Physics.‡2udc 650 07 ‡a54 -- Chemistry.‡2udc 650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local 651 #7 ‡a(*41) -- Canada.‡2udc 651 #7 ‡a(*440) -- Northwest Territories.‡2udc 700 1# ‡aKershaw, G. P. 700 1# ‡aGallinger, B. J. 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# ‡a20230401