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The solutions are linear visco-elastic for low stresses (or strain-rates), becoming shear-thinning for larger stresses.
If the values of only some of the parameters are known, the remaining parameters when the edges are being designed can be chosen so that the conditions for low stresses are satisfied.
Semmrich et al. distinguished three differing response regimes: for low stresses, the creep compliance is approximately constant, showing a linear stress strain relation.
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Configuration I is better for sensing low stresses, whereas configuration II is better for sensing high stresses.
Although moisture content affects the fatigue life for high stress levels, this effect tends to disappear for low stress levels.
Especially for low stress amplitudes near the endurance limit, critical grain orientation and defects are both essential for cracks to initiate and propagate.
The method was particularly conservative for low stress ratios in the high-cycle regime and a procedure based on the use of the Goodman diagram was devised for correcting the Class B curve for mean stress.
Besides, it is experimentally shown that the self-heating curves are not dependent on the mean stress for low stress magnitudes while they are sensitive to the mean stress for higher stress magnitudes.
It is deduced that in the loading conditions used to determine the self-heating curves, the dissipative mechanisms imply recoverable strains (anelasticity) for low stress magnitudes and unrecoverable strains (inelasticity) for higher stress magnitudes.
Nevertheless, it is shown that fatigue crack initiation in the maximum shear plane seems to be the governing mechanism at the tip of the defect for low stress concentration defect.
Most importantly, the predicted dynamic behaviour shows a non-trivial and a priori unexpected dependence on the stress intensity; oscillations can be observed for low stress intensity for many parameter values that are in agreement with present data, while no oscillations are observed for high stress intensities.
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CEO of Professional Science Editing for Scientists @ prosciediting.com