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Wave paths

The laser-Doppler anemometer measures local fluid velocity from the change in frequency of radiation, between a stationary source and a receiver, due to scattering by particles along the wave path. A laser is commonly used as the source of incident illumination. The measurements are essentially independent of local temperature and pressure. This technique can be used in many different flow systems with transparent fluids containing particles whose velocity is actually measured. For a brief review or the laser-Doppler technique see Goldstein, Appl. Mech. Rev., 27, 753-760 (1974). For additional details see Durst, MeUing, and Whitelaw, Principles and Practice of Laser-Doppler Anemometry, Academic, New York, 1976. [Pg.889]

The variation of r and f through 3.0 GPa and 5.4 GPa shock waves is shown in Fig. 7.7 [38]. This figure shows clearly that the shock-wave path is in the dislocation drag regime (r > f). The mechanical threshold stress f increases from 10 MPa to 80 MPa in the 5.4 GPa shock thus from (7.37)... [Pg.233]

Figure 12 shows a schematic view of sound waves traveling through a two layered system of soil over bedrock. A seismic source produces sound waves which travel in all directions into the ground. The seismic method is only concerned with the wave paths shown in Figure 12. One of these waves, the direct wave, travels parallel to the ground s surface in the surface layer. Figure 12 shows a schematic view of sound waves traveling through a two layered system of soil over bedrock. A seismic source produces sound waves which travel in all directions into the ground. The seismic method is only concerned with the wave paths shown in Figure 12. One of these waves, the direct wave, travels parallel to the ground s surface in the surface layer.
Uniform coverage of the AW path is of some importance as well. In the case of a SAW, FPW, or APM delay line, the propagating wavefront is typically fairly linear a film that covers some parts of the wave path to a greater extent titan others causes parts of the wavefront to be delayed relative to others. The consequent loss of coherence of the propagating wavefiont adversely affects the signal-to-noise ratio. [Pg.347]

The electron wave path of phase contrast in a TEM is illustrated by Figure 3.24. The properties of electron waves exiting the specimen are represented by an object function, /(r), which includes the distributions of wave amplitude and phase, r is the position vector from the central optical axis. The object function may be represented as a function in Equation 3.3. [Pg.96]

Wave paths Reflection (XRD) Transmission (Laue) Transmission... [Pg.101]

Lu, J., Wakai, K., Takahashi, S., and Shimizu, S. "Acoustic Computer Tomographic Pyrometry for Two-Dimensional Measurement of Gases Taking into Account the Effect of Refraction of Sound Wave Paths." Measurement Science and Technology 11 (2000) 692-97. [Pg.116]

Another approach to modeling vibration looks at individual propagation paths. This can work well, especially in large contained spaces such as rooms. Figure 12.10 shows a singer and a listener in a simple room. Only the first few wave paths from the singer s mouth to the listener s ears are shown. [Pg.138]

However, the periodicity condition (4.518) for paths is to be maintained and properly implemented in approximating the effective-classical partition function (4.525) being, nevertheless, closely and powerfully related with the quantum beloved concept of stationary orbits defined/described by periodic quantum waves/paths. This way, the effective-classical path integral approach appears as the true quantum justification of the quantum atom and of the quantum stabilization of matter in general, providing reliable results without involving observables or operators relaying on special quantum postulates other than the variational principles - with universal (classical or quantum) value. [Pg.505]

This is very general equation that will be used further on. From the same figure we can extract another useful relationship between the q-vector and the wave path difference A accumulated along the distance between the particles. It is just a difference of two scalar products ... [Pg.80]

The same condition can easily be found by comparison of the wave path difference 2 /sim9 with wavelength X. [Pg.80]

Rosen (1971) is the only investigator known by the writer to have measured the temperature dependence of the elastic properties of ytterbium. Using an ultrasonic pulse technique (10 MHz) to determine acoustic wave velocities in polycrystalline ytterbium Rosen obtained the results given in figs. 8.85 and 8.86. He corrected the acoustic wave path length for thermal expansion. The values of E, G and d increase smoothly with decreasing temperature and approach the... [Pg.694]

No current flows in the medium (no conduction), no charges or more precisely no charge gradient exists in the medium, and the medium is assumed to be homogeneous for having a constant energetic absorption factor Uq all along the wave path. [Pg.554]

FIG U RE 12.9 In the femtolaboratory. The laser ray is reflected on a certain wave path with the help of mirrors. [Pg.333]

The representation of the radio wave path in Fig. 13.29 and the previous discussion have only considered a direct path between the receiver and transmitter. In reality, there are two major modes of propagation the skywave and the groundwave. The skywave refers to propagation via the ionosphere, which consists of several layers of ionized particles in the Earth s atmosphere from approximately 50 to several hundred kilometers in altitude. Some frequencies will be reflected by the ionosphere resulting in potentially longdistance propagation. This propagation mode is discussed in detail in a later section. [Pg.1519]

Figure 2. Rules for the use of the evolution curves in the composition triangles. For a given composition E in the triangle, and for k = 1,2, one can determine the portions of curves which connect E to other compositions by drawing only the acceptable parts, either by a continuous evolution (relaxation or ddtentes , full line) or by shocks (dotted line), a. Case where one connects point E to other points located on its right (downstream). Such a point is called a left point, b. Case when point E is connected to other points located on its left (upstream). Such a point is called a right point c. When one wants to connect a left point to a right point, one uses the results given in (a) and (b) together with the condition that a I -wave is followed by a 2-wave (path A and not path B). This makes an intermediate state appear (Sedqui and Cuy, 2001 with permission from Elsevier). Figure 2. Rules for the use of the evolution curves in the composition triangles. For a given composition E in the triangle, and for k = 1,2, one can determine the portions of curves which connect E to other compositions by drawing only the acceptable parts, either by a continuous evolution (relaxation or ddtentes , full line) or by shocks (dotted line), a. Case where one connects point E to other points located on its right (downstream). Such a point is called a left point, b. Case when point E is connected to other points located on its left (upstream). Such a point is called a right point c. When one wants to connect a left point to a right point, one uses the results given in (a) and (b) together with the condition that a I -wave is followed by a 2-wave (path A and not path B). This makes an intermediate state appear (Sedqui and Cuy, 2001 with permission from Elsevier).

See other pages where Wave paths is mentioned: [Pg.132]    [Pg.795]    [Pg.75]    [Pg.117]    [Pg.336]    [Pg.337]    [Pg.420]    [Pg.577]    [Pg.661]    [Pg.98]    [Pg.143]    [Pg.110]    [Pg.199]    [Pg.199]    [Pg.209]    [Pg.226]    [Pg.325]    [Pg.364]    [Pg.212]    [Pg.172]    [Pg.3487]   
See also in sourсe #XX -- [ Pg.55 ]




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Straight Characteristics and Particle Paths in a Simple Wave

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