Abstract
Stress change experiments during compressive creep tests at high stresses on polycrystalline MgO at 1596 K have shown that the creep rate at any instant during transient and steady state creep is predicted by the ratio,r/h, wherer is the rate of recovery (=−∂σ/t6t) andh is the coefficient of strain hardening (=∂σ/∂ε). Over most of transient and steady state creep, whenh is constant and the decrease in creep rate,\(\dot \in\), is a direct result of a decrease inr, the variation of the creep strain,ε, with time,t, is accurately described as
whereε 0 is the instantaneous strain on loading,ε T the transient creep strain,m relates to the rate of exhaustion of transient creep and\(\dot \in _s\) is the steady creep rate. Deviations from this equation occur during the initial 10 to 15% of the transient creep life, whenh increases rapidly.
The variations in\(\dot \in\),r andh during transient and steady state creep are explained in terms of a model for creep in which the rate-determining process is the diffusion controlled growth of the three-dimensional dislocation network within subgrains to form dislocation sources allowing slip to occur.
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Birch, J.M., Wilshire, B. Transient and steady state creep behaviour of polycrystalline MgO. J Mater Sci 9, 871–875 (1974). https://doi.org/10.1007/BF00570377
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DOI: https://doi.org/10.1007/BF00570377