Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4676755 | Cold Regions Science and Technology | 2007 | 7 Pages |
Abstract
Based on literature results, the temperature of an iceberg around the Grand Banks of Newfoundland is shown to vary from about 0 °C at the water–ice interface to approximately − 20 °C in the interior. This temperature variation affects the strength of the ice. A review of the strength of iceberg ice shows that its uniaxial compressive strength is 1.7 times less than other freshwater ice at a strain-rate of 10− 3 s− 1, probably due to pre-existing healed cracks or flaws. Using an activation energy of 80 kJ/mol., the uniaxial compressive strength of iceberg ice is shown to vary from 5 MPa at 0 °C near the surface, to 8.5 MPa at − 20 °C, 10–20 m inside the iceberg.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Stephen J. Jones,