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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #84684:
Preliminary measurements of terminal crack velocity in ice / B.L. Parsons, J.B. Snellen, B. Hill.
Title: | Preliminary measurements of terminal crack velocity in ice / B.L. Parsons, J.B. Snellen, B. Hill. |
Author(s): | Parsons, B. L. Snellen, J. B. Hill, B. |
Date: | 1987. |
In: | Cold Regions Science and Technology. (1987.), Vol. 13(3) (1987) |
Abstract: | Measurements made to determine if bifurcation of cracks propagating in first-year, shorefast sea ice in Allen Bay, near Resolute, Cornwallis Island, NWT, Canada, is possible mechanism influencing fragment size. Bifurcation was not observed in any samples, probably because of low crack velocity (20 m s⁻¹). Concludes that fragment size in ice is, instead, consequence of various stress fields developed. |
Notes: | Cold Regions Science and Technology. Vol. 13(3) :233-238 (1987). |
Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 539.56 -- Ice, fragility and brittleness. E6 -- Glaciology: floating ice. (*41) -- Canada. (*464.81) -- Cornwallis Island. |
SPRI record no.: | 84684 |
LDR 01318naa#a2200000#a#4500 001 SPRI-84684 005 20230603181831.0 007 ta 008 230603s1987####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-84684 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aParsons, B. L. 245 10 ‡aPreliminary measurements of terminal crack velocity in ice /‡cB.L. Parsons, J.B. Snellen, B. Hill. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1987. 300 ## ‡ap. 233-238 :‡billus., diags., table. 500 ## ‡aCold Regions Science and Technology. Vol. 13(3) :233-238 (1987). 520 3# ‡aMeasurements made to determine if bifurcation of cracks propagating in first-year, shorefast sea ice in Allen Bay, near Resolute, Cornwallis Island, NWT, Canada, is possible mechanism influencing fragment size. Bifurcation was not observed in any samples, probably because of low crack velocity (20 m s⁻¹). Concludes that fragment size in ice is, instead, consequence of various stress fields developed. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a539.56 -- Ice, fragility and brittleness.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*41) -- Canada.‡2udc 651 #7 ‡a(*464.81) -- Cornwallis Island.‡2udc 700 1# ‡aSnellen, J. B. 700 1# ‡aHill, B. 773 0# ‡7nnas ‡tCold Regions Science and Technology. ‡gVol. 13(3) (1987) ‡wSPRI-59075 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230603