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Record #112859:
Freezing-rate effects on the physical characteristics of basal ice formed by net adfreezing / Bryn Hubbard.
Title: | Freezing-rate effects on the physical characteristics of basal ice formed by net adfreezing / Bryn Hubbard. |
Author(s): | Hubbard, Bryn. |
Date: | 1991. |
In: | Journal of Glaciology. (1991.), Vol. 37(127) (1991) |
Abstract: | Theoretical and empirical studies have indicated that many individual characteristics of ice formed by processes of net basal adfreezing may be sensitive to rate of propagation of freezing front through reservoir concerned. Effects of freezing rate on stable isotope chemistry and crystallography of ice, in addition to disposition and character of included debris and gas, are reported. Unidirectional freezing through cylindrical reservoir containing various water-sediment mixtures was conducted in laboratory, and resulting cores analyzed. Data lend support to inferences drawn from studies concerned with specific ice properties and idealized suite of characteristics is developed which may be diagnostic of basal ice formed by net freezing. |
Notes: | Journal of Glaciology. Vol. 37(127) :339-347 (1991). |
Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.22 -- Glaciers. 551.324.431 -- Land ice, accumulation. 539.6 -- Ice, adhesion and friction. Regelation. 519.673 -- Modelling. .000(410) -- British author. E5 -- Glaciology: land ice. |
SPRI record no.: | 112859 |
LDR 01698naa#a2200000#a#4500 001 SPRI-112859 005 20230327215923.0 007 ta 008 230327s1991####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-112859 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aHubbard, Bryn. 245 10 ‡aFreezing-rate effects on the physical characteristics of basal ice formed by net adfreezing /‡cBryn Hubbard. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 339-347 :‡bill., diags., tables. 500 ## ‡aJournal of Glaciology. Vol. 37(127) :339-347 (1991). 520 3# ‡aTheoretical and empirical studies have indicated that many individual characteristics of ice formed by processes of net basal adfreezing may be sensitive to rate of propagation of freezing front through reservoir concerned. Effects of freezing rate on stable isotope chemistry and crystallography of ice, in addition to disposition and character of included debris and gas, are reported. Unidirectional freezing through cylindrical reservoir containing various water-sediment mixtures was conducted in laboratory, and resulting cores analyzed. Data lend support to inferences drawn from studies concerned with specific ice properties and idealized suite of characteristics is developed which may be diagnostic of basal ice formed by net freezing. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.22 -- Glaciers.‡2udc 650 07 ‡a551.324.431 -- Land ice, accumulation.‡2udc 650 07 ‡a539.6 -- Ice, adhesion and friction. Regelation.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a.000(410) -- British author.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 37(127) (1991) ‡wSPRI-20534 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230327