Sentence examples for traction change from inspiring English sources

Exact(5)

TD1 consists of the traction change due to the direct contribution propagated from the slip region, and also the perturbations due to the heterogeneities, e.g. reflected terms from the material interfaces, and refracted terms propagating through the high-velocity zone.

An instantaneous traction change is represented by the combination of a direct term calculated from the boundary-based method and a residual term calculated from the differences between two solutions of the domain-based methods.

The first term on the right-hand side of Eq. (1) is the instantaneous or the radiation damping term, representing the instantaneous effect of the slip on the traction change at the same element of the source and the receiver.

Figure 4 also shows the seismic ray traces of the S-wave, S and (S), corresponding to model D1 and D2, respectively, and travel times, 13.15 s and 14.12sat−6 km, are also marked on the velocity and traction change.

In this method, instantaneous traction change is represented by the combination of a direct term calculated by a boundary-based method for a homogeneous full space, and a residual term calculated from the differences between two solutions for a target heterogeneity model and for a homogeneous full space model by a domain-based method.

Similar(54)

Let TB, TD1, and TD2 be the traction changes calculated from the boundary-based method and two domain-based methods, respectively.

Figure 4 shows the calculated velocities in the normal component to the fault, and the calculated shear traction changes on the fault plane.

For example, it may intervene to brake a fast-moving vehicle by responding to traction changes depending on different road surfaces to within 5 10 ms for the safety of the driver.

Fig. 4. Characteristics of perturbation terms calculated from the differences between solutions from the target model (D1) and the layered model (D2); velocities in normal component and shear traction changes observed along the fault plane (top).

Discrete consolidation is well demarcated but non-uniform with traction changes that likely represent fibrosis.

"You need a good all-around package with strong, straight line speed and stability, decent traction and change of direction, but also good low-speed performance tempered with that".

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