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Record #166539:
Simulations of an isotopic fractionation by freezing in an open system / Yoshinori Iizuka.
Title: | Simulations of an isotopic fractionation by freezing in an open system / Yoshinori Iizuka. |
Author(s): | Iizuka, Yoshinori. |
Date: | 2003. |
In: | Chinese Journal of Polar Science. (2003.), Vol. 14(1) (2003) |
Abstract: | Presents model for isotopic fractionation by freezing in an open system designed to examine regelation beneath Hamna Glacier, Sôya drainage, East Antarctica. One-dimensional model assumes near equilibrium and zero boundary layer thickness. Describes simulations for nine ratios of freezing to water input rates, which show clear distinction between closed and open systems. Uses model to analyse a measured isotopic curve from Hamna basal ice. Concludes this ice formed in an open system with a freezing/water input ratio of 10/4. |
Notes: | Chinese Journal of Polar Science. Vol. 14(1) :57-64 (2003). |
Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.22 -- Glaciers: Hamna Glacier. 551.322 -- Ice and snow. 54.027 -- Isotope analysis. 536.421.4 -- Freezing. 539.6 -- Ice, adhesion and friction. Regelation. 519.673 -- Modelling. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. (*73) -- Dronning Maud Land. |
SPRI record no.: | 166539 |
LDR 01605naa#a2200000#a#4500 001 SPRI-166539 005 20230401204055.0 007 ta 008 230401s2003####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-166539 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aIizuka, Yoshinori. 245 10 ‡aSimulations of an isotopic fractionation by freezing in an open system /‡cYoshinori Iizuka. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2003. 300 ## ‡ap. 57-64 :‡bill., diags., tables. 500 ## ‡aChinese Journal of Polar Science. Vol. 14(1) :57-64 (2003). 520 3# ‡aPresents model for isotopic fractionation by freezing in an open system designed to examine regelation beneath Hamna Glacier, Sôya drainage, East Antarctica. One-dimensional model assumes near equilibrium and zero boundary layer thickness. Describes simulations for nine ratios of freezing to water input rates, which show clear distinction between closed and open systems. Uses model to analyse a measured isotopic curve from Hamna basal ice. Concludes this ice formed in an open system with a freezing/water input ratio of 10/4. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.22 -- Glaciers: Hamna Glacier.‡2udc 650 07 ‡a551.322 -- Ice and snow.‡2udc 650 07 ‡a54.027 -- Isotope analysis.‡2udc 650 07 ‡a536.421.4 -- Freezing.‡2udc 650 07 ‡a539.6 -- Ice, adhesion and friction. Regelation.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*73) -- Dronning Maud Land.‡2udc 773 0# ‡7nnas ‡tChinese Journal of Polar Science. ‡gVol. 14(1) (2003) ‡wSPRI-143545 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230401