Author:
Mellor Malcolm,Testa Richard
Abstract
Uniaxial compressive creep tests on fine-grained polycrystalline ice indicate that secondary strain-rate is proportional toσ1.8, whereσis applied stress, for the range 0.1 <σ< 0.5 kgf/cm2(10 <σ< 50 kN/m2). On the basis of the present tests, earlier results suggesting linear viscous behaviour at low stress are believed to be invalid.
Publisher
Cambridge University Press (CUP)
Cited by
54 articles.
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