1976
DOI: 10.1016/0013-7944(76)90016-3
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Fracture in the compression of columnar gained ice

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Cited by 12 publications
(6 citation statements)
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“…Other arguments can be f0rmulated to explain Schwarz's results: sea ice fails most easily in tension by separation of the ice crystals along their long axis. This is what has been observed to happen in the uniaxial state of stress when a sample is loaded parallel to the direction of growth (which is also the direction of the long axes of the crystals) and subsequently fails by tensile strain perpendicular to the direction of load (Wu and others, 1976). is the compressive strength, a is the rate of stress application and b is an exp erimental constant equal to 0 .2 2).…”
mentioning
confidence: 58%
See 1 more Smart Citation
“…Other arguments can be f0rmulated to explain Schwarz's results: sea ice fails most easily in tension by separation of the ice crystals along their long axis. This is what has been observed to happen in the uniaxial state of stress when a sample is loaded parallel to the direction of growth (which is also the direction of the long axes of the crystals) and subsequently fails by tensile strain perpendicular to the direction of load (Wu and others, 1976). is the compressive strength, a is the rate of stress application and b is an exp erimental constant equal to 0 .2 2).…”
mentioning
confidence: 58%
“…Furthermore, ice temperature should not be overlooked as an important parameter in connection with the strain-rate. This has, as yet, not been investigated for sea ice, but from testing fresh-water ice (Carter, [1972]; Wu and others, 1976) we know that the relation between strength and strain-rate is temperature dependent. Due to the correlation between temperature and the brine volume of the ice, the strain-rate effect will also be a function of the brine volume.…”
Section: (D ) Temperaturementioning
confidence: 99%
“…The two populations appear to have different dependencies on strain-rate. There is evidence that grain-boundary cracks dominate in brittle fracture (Gold, 1972[a]; Wu and others, 1974). As the majority of cracks are transcrystalline for compressive creep at stress below 2 MN m -2 , there must be a transition in the c ha racteristics of the cracking activity.…”
Section: Ductile To Brittle Transitionmentioning
confidence: 99%
“…This type of failure can be observed in the laboratory if the specimen is constrained in a direction perpendicular to the applied load or if there is little or no friction between the specimen and the load pattern. Information is now becoming avai lable that, it is to be hoped, will allow the appropriate relationships to be established between the strength and deformation properties of ice measured at a laboratory scale and those that determine its behaviour when moving against a structure (Wu and others, 1974;Croasdale, 1974) . As shown by Wu and others, the stress immediately in front of the structure depends on the width of the structure and the thickness of the ice in addition to the properties of the ice under given conditions.…”
mentioning
confidence: 99%
“…D. J. GOODMAN: IS the author familiar with the paper of Wu and others (1976) who used ice to separate the specimen from the platens? Would he like to comment on this result?…”
Section: Discussionmentioning
confidence: 99%