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Strong azimuthal anisotropy in the NoMelt upper mantle that decreases with depth through the lithosphere (Lin et al. 2016) suggests a greater degree of shearing and fabric alignment at shallow depths.
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The degree of shear thinning, however, is best described using a logarithmic function.
Higher xanthan concentration raised the absolute solution viscosity and increased the degree of shear thinning.
The degree of shear cracking damage in a specimen was quantified by the amount of shear deformation.
For example, the degree of shear connection (ηtest) = 0.390 for 675 mm shear span is shown in Figure 18.
In the current model, the degree of shear strain concentration was influenced by the assumption of rheology.
The apparent/physical viscosity ratio is shown to increase as the degree of shear-thinning increases.
A method to consider the effect of the degree of shear connection on the strength reduction factor is proposed.
The model considers independent variables that measure the degree of shear and flexural damage separately.
The beams were designed based on Australian guidelines with a degree of shear connection equal to 0.79.
The degree of shear strain concentration is controlled by the weakening effect due to nonlinear relation between shear strain rate and stress (power-law rheology).
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