Information is presented on the failure behavior of columnar-grained ice during compressive creep and constant strain rate tests. The role of crack formation in establishing the failure condition is briefly described. Breakdown of structure is responsible for a marked change in the creep behavior of ice in the stress range of 10 to 12 kg/sq cm. A ductile-to-brittle transition is observed at a strain rate of about 0.005/min. The upper yield stress in constant strain rate tests is shown to increase in rate of strain up to the ductile-to-brittle transition.

  • Authors:
    • Gold, L W
  • Publication Date: 1970-11

Media Info

Subject/Index Terms

Filing Info

  • Accession Number: 00032121
  • Record Type: Publication
  • Source Agency: Engineering Index
  • Files: TRIS
  • Created Date: Apr 21 1973 12:00AM