Sentence examples for stress rate of from inspiring English sources

Many are playing their cards close to their chests but, in general, lenders seem to be applying a "stress rate" of between6%and7% 7%, says Peter Gettins at mortgage broker London & Country.

Numerical data for the skin friction, couple stress, rate of heat and mass transfer have also been tabulated for various values of the thermophysical parameters.

Fatigue tests were applied to the specimens at a stress rate of 0.05 and frequency of 0.42 Hz in accordance with the ASTM-D 2992 standard.

The loading force was controlled with a stress rate of about 30 MPa/s before bar yielding and beyond that transferred to displacement control with a strain rate of about 0.002 s.

The constitutive equations are taken to be tau =lambda tau_{y}+ 1-lambda )bar{k}(-dot{gamma })^{n};qquad tau >tau_{y}, quad 0< lambda < 1, (5) where τ, γ̇, (tau_{y}), k̄ and n denote shear stress, rate of deformation, yield stress, consistency index and flow behaviour index, respectively, along with (tau =vert tau_{rz} vert =- tau_{rz}).

Although there are four parameters of interest in the present problem, the effects of viscous dissipation parameter which is characterized by the Eckert number Ec, magnetic parameter M, and Prandtl number Pr on the surface shear stress, rate of heat transfer, velocity, and temperature are focused.

Based on the strain and stress rates of Sumatra Fault calculated from the GPS measurements in Indonesia and its close vicinity, Aydan (2008) predicted an earthquake of magnitude 8.7 in the offshore area of Siberut and Sipora islands, with a rupture length of 400 450 km and an epicentre about 260 km away from the west coast of Sumatra.

There was, however, no difference in the overall stress rating of these events in relapsers and non-relapsers.

This value is coincident with a corresponding stressing rate of 3 kPa/year estimated from GPS data.

We calculate here the variation in stressing rate as 0.5×rigidity× (a variation in differential strain rate), that is, the variation in stressing rate of shear stress.

We estimated a spatial variation in the stressing rate of 15 18 kPa/year in the crust from that of coda Q in the analyzed region.