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The energy dispersion in Equation 4 shows a nonparabolic relation with the wave vector.
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A similar situation has been established in [10] in relation with the discrete wave equation and in [11] in relation with the discrete heat equation (see [17 22]).
However, this decade has seen a shift in the relations with Europe, with the wave of change that swept the region with the beginning of the year.
The identification of various wave types is possible since each is characterized by its own dispersion relation, with the result that each wave type may be associated with characteristic features in the time frequency domain representation of a structural response.
Besides, the dispersion relation of the wave was obtained theoretically.
According to Watson [2], the ultrasound wave's frequency has relation with the depth reached by the ultrasonic waves in a specific biological tissue.
The relation with the experimentally reported cases of wave propagation at electrode/electrolyte interfaces is discussed to some extent.
Based on the energy dispersion of biased TGN, wave vector relation with the energy (E-k relation) shows overlap between the conduction and valence band structures, which can be controlled by a perpendicular external electric field [6, 39].
The northern wave pattern, produced by the upward-propagating migrating tide, is almost out of phase with the wave structure produced by in situ processes, while the southern wave pattern is out of phase relation in the pre-noon and in-phase relation in the post-noon period (compare Fig. 2 with Fig. 1, bottom).
The results show that the rock mass rating (RMR) and Q values have a close relation with P-wave velocity parameters, including P-wave velocity in field (VPF), P-wave velocity in the laboratory (VPL) and the ratio of VPF to VPL (i.e. KP = VPF/VPL).
Come crashing down with the wave.
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