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Other arrows show the directions of the forces associated with the so-called normal stresses σ11 and σ22, which in the absence of motion of the fluid would both be equal, by Pascal's law, to -p. Now σ12 is clearly zero when the rate of variation of velocity, ∂v1/∂x2, is zero, for then there is no slip, and presumably it increases monotonically as ∂v1/∂x2 increases.
Therefore, we have measured the variation of velocity as a function of the simulation time.
Open image in new window Fig. 6 Velocity/depth model showing the variation of velocity with depth for primary events.
The variation of velocity along time τ for different values of K and ξ is shown in Figure 4.
The variation of velocity along τ for different values ξ and M is studied in Figure 5.
Figure 14 Variation of velocity (pmb{f' eta)}) for different values of slip parameter (pmb{k_{2}}).
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Variations of velocity within a fluid result in the transport of momentum, which is normally referred to as viscous flow.
Presence of anisotropic symmetry affects the magnitude as well as directional variations of velocity of qS1-wave.
The presence of anisotropic symmetries have a very significant effect on the variations of velocity with propagation direction.
To see the spatial variations of velocity changes, we need to consider sensitivity kernels (e.g., Pacheco and Snieder 2005).
Results on the variations of velocity and temperature profiles with geometrical parameters, at different temperature and velocity, for heat transfer by free and forced convection techniques are presented.
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