Journal of the American Ceramic Society · 1962 · 75 citations · 2 references
Natural SciencesMaterials EngineeringMaterials ScienceCeramicsMechanical Behavior Of MaterialsSolid MechanicsDeformation MechanismsFlow BehaviorFracture MechanicsPlastic DeformationPlasticityStress-strain BehaviorBrittle FailureBrittle Fracture BehaviorMaterial Flow PropertiesPlastic FlowStrain-rate SensitivityTemperature Dependence Of DeformationTensile DeformationYield Stress
The tensile deformation of sapphire was studied as a function of the temperature and of the strain rate. The ranges of the two variables were approximately 1200° to 1700°C and 10 −3 to 10 −1 in. per in. per minute. The work showed the existence of a relatively sharp temperature transition between completely brittle fracture and massive plastic flow, the specific transition temperature being sensitively related to the strain rate. For the limits of the rate range used, the transition temperature increased from approximately 1270° to 1520°c. In going through a range of only a few degrees of temperature near the transition, it was possible to obtain either no plastic flow on the low‐temperature side or a relatively large amount of the order of a 100% extension on the high‐temperature side. The stress‐strain relation for plastic flow was found to be characterized by a pronounced yield‐point drop; i.e., the stress required to initiate macroscopic flow was approximately double that required for subsequent flow. The magnitudes of both the upper and lower yield stresses were temperature sensitive and both decreased approximately exponentially with increasing temperature for a given strain rate. An inverse dependency of a similar kind was found for the effect of strain rate under conditions of isothermal testing. On the other hand, the fracture stress before yielding was found to be essentially independent of both temperature and strain rate, lying in a scatter band of approximately 16,000 to 20,000 psi. As the testing temperature at a given strain rate was lowered, the plastic yield stress therefore rose sharply. The transition temperature between ductile and brittle behavior was interpreted to correspond to the temperature at which the upper yield stress equaled the fracture stress. Since the lower yield stress was only half the upper yield stress, extensive flow then became possible whenever the transition temperature for yielding was exceeded.
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