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SUMMARY:Cracks in ice and their role in brittle compressive failure - Erla
 nd Schulson (Dartmouth College)
DTSTART:20171207T113000Z
DTEND:20171207T123000Z
UID:TALK96334@talks.cam.ac.uk
CONTACT:INI IT
DESCRIPTION:<span>Cracks--new and old\, short and long-- are ubiquitous fe
 atures within the arctic sea ice cover. How they form and the role they pl
 ay in mechanical behavior are important questions in ice mechanics. In thi
 s presentation\, emphasis will be placed on brittle compressive failure. T
 here\, cracks preferentially oriented with respect to the applied stress s
 tate can slide intermittently across opposing surfaces in contact\, activa
 ting in the process deformation mechanisms that can account for a number o
 f observations/characteristics of brittle compressive failure on scales sm
 all and large. One such scale-independent mechanism is the wing-crack cum 
 comb-crack mechanism: it can account for the axial splitting and shear fau
 lting modes of terminal failure\, conjugate faulting\, brittle compressive
  strength and\, upon consideration of crack-tip creep\, the transition fro
 m brittle to ductile behavior. Application of confining stress above a cri
 tical level\, set solely by the coefficient of kinetic friction\, suppress
 es frictional sliding and activates\, given a sufficiently high strain rat
 e and triaxial confinement\, a brittle-like mode of plastic failure govern
 ed by the different mechanism of adiabatic heating and dynamic recrystalli
 zation. These mechanisms will be described and questions arising addressed
 .<br> <br> </span>
LOCATION:Seminar Room 1\, Newton Institute
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