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Simulation studies on cases of velocity tracking and trajectory tracking verify the effectiveness of the proposed methodology.
This study investigates two cases of velocity predictions for North Sea chalk: fluid substitution of compressional velocity (vP) and estimation of shear velocity (vS).
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The Navier-type solution is obtained for the case of velocity feedback using modal filtering.
In the three different velocity ratio cases, the case of velocity ratio equal to 1/100 has the best deposition efficiency and the most uniform deposition distribution.
Figure 4 shows the effect of the radiation parameter K on the velocity and temperature profiles at different values of the velocity slip factor (S_{f}) in the case of velocity profiles (see Figure 4(a)), and thermal slip factor in the case of temperature profiles (see Figure 4(b)).
Figure 3 depicts the effect of the magnetic parameter M on the velocity and temperature profiles at different values of the velocity slip factor (S_{f}) in the case of velocity profiles (see Figure 3(a)), and thermal slip factor in the case of temperature profiles (see Figure 3(b)).
Figure 2 shows the influence of Casson parameter β on the velocity and the temperature profiles at different values of the Forchheimer parameter Λ in the case of velocity profiles (see Figure 2(a)), and thermal slip factor (S_{T}) in the case of temperature profiles (see Figure 2(b)).
Such distribution allows to represent variables that are only defined for positive values and that can be concentrated mainly in one value, as it is the case of velocities' magnitudes in far range of interactions.
where we introduced the factor α to take energy dissipation into account [7]. Figure 5 displays two cases of the velocity dependence of e; we find these to be representative for the entire range of stiffness and adhesion values investigated.
Because we examined only one station for one earthquake, it is important to collect case studies of velocity changes at different depths for different situations.
Similarity solutions for pressure gradient driven flow over a stretching boundary were analyzed by Riley and Weidman [14] for the case of external velocity and boundary velocity being proportional to the same powers of the downstream coordinate.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com