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Air inversion frequencies

Cavitation is the formation of gaseous cavities in a medium upon ultrasound exposure. The primary cause of cavitation is ultrasound-induced pressure variation in the medium. Cavitation involves either the rapid growth and collapse of a bubble (inertial cavitation) or the slow oscillatory motion of a bubble in an ultrasound field (stable cavitation). Collapse of cavitation bubbles releases a shock wave that can cause structural alteration in the surrounding tissue [13]. Tissues contain air pockets trapped in the fibrous structures that act as nuclei for cavitation upon ultrasound exposure. The cavitational effects vary inversely with ultrasound frequency and directly with ultrasound intensity. Cavitation might be important when low-frequency ultrasound is used, when gassy fluids are exposed, or when small gas-filled spaces are exposed. [Pg.319]

With experimental data for V as a function of 1/N, they were able to determine by inverse Laplace transform, the function fik) and the values of m for the Weibul distribution for Kibushi clay im = 1), TiOg im = 1), and Si02 im = 0.5). Such studies require that each powder have a reproducible initial packing, which can be achieved by fluidization with air. If the tap frequency is too high, consolidation will not take place so frequencies of 1 Hz are often used with an amplitude of tap of 1 cm. For these conditions, it is often found that p is achieved in 1000 to 2000 sec. [Pg.655]

Collapse of cavitation bubbles releases a shockwave that can cause structural alteration in the surrounding tissue. Tissues contain air pockets that are trapped in the fibrous structures and act as nuclei for cavitation upon US exposure. The cavitation effect varies inversely with US frequency and directly with US intensity. [Pg.171]

Numerous investigators have compared the aerosol droplet size of nebulized aerosols from ultrasonic and air-jet devices. " Because droplet size is inversely proportional to the acoustic frequency, smaller droplets are generated from ultrasonic devices with higher frequencies. Ultrasonic nebulizers with high operating frequencies (2-3 MHz) are capable of... [Pg.3857]

The frequency is independent of the medium in which radiation propagates, but the speed of light and the wavelength are inversely proportional to the refractive index (n) of the medium. This is to say, X = Xq I n and c = Cf I n. The refractive index of air is abont 0.03% greater than 1 (the refractive index of vacuum), and therefore it is often approximated as 1. [Pg.568]

The sound level experienced at a distance from an explosion can be heavily depended on transient atmospheric conditions (e.g. temperature inversions, wind shear, and even gusts of wind). The low frequency air pressure from a blast can cause vibration in buildings, in addition to its startle effect. Such vibration can give rise to concern about possible building damage at relatively low over-pressure levels. The subject has been investigated in depth by the United States Bureau of Mines, whose conclusions are summarised in [33.11]. [Pg.393]

Good evidence for the rapid motion and trapping of the soliton is demonstrated by a DNP experiment as shown in Figure 6.30 [146,173]. The dynamic nuclear polarization (DNP) experiments are carried out at 9 GHz between 1.5 and 300 K in cis [143,174] and irons PA [143,145,146,173,174]. At room temperature the pure Overhauser effect (OE) was observed in a -irans-PA without air or oxygen but a mixed solid state effect (SSE) together with OE was found in c/s-rich PA without air [143,174] and al -lrans-PA with air [146]. In particular, below 150 K, the mixed effect was observed, even in a -trans-PA without air [145,173], The OE is characteristic of dynamic interaction between nuclear spins and electron spins, with rapid motion, On the other hand, the SSE is of the static interaction between them. In other words, observation of the pure OE is clear evidence for the electron spin for motion with an inverse of the correlation time comparable with or larger than Wj,. At 300 K, the pure OE observed in all-/ra s-PA, is consistent with the conclusions for the neutral soliton to diffuse rapidly compared with 1/We as concluded from the ESR linewidth narrowed by motion [53] and the proton NMR 7Y ] [143] as a function of frequency over a broad range. [Pg.276]

For the absolute methods to be properly applied, the influence of material parameters has to be well known. This is usually not the case for fractures in concrete, where aggregates, reinforcement and air-filled pores are common. In addition, the sensor characteristics must be well known (this is not a problem in geophysics where seismometers with a flat response over the signal frequency range are usually used). Poor coupling of transducers also limits the application of these simple inversion techniques. [Pg.85]


See other pages where Air inversion frequencies is mentioned: [Pg.38]    [Pg.39]    [Pg.39]    [Pg.38]    [Pg.39]    [Pg.39]    [Pg.38]    [Pg.39]    [Pg.39]    [Pg.38]    [Pg.39]    [Pg.39]    [Pg.226]    [Pg.196]    [Pg.455]    [Pg.175]    [Pg.219]    [Pg.517]    [Pg.596]    [Pg.91]    [Pg.390]    [Pg.23]    [Pg.455]    [Pg.264]    [Pg.72]    [Pg.417]    [Pg.150]    [Pg.171]    [Pg.178]    [Pg.485]    [Pg.3836]    [Pg.838]    [Pg.53]    [Pg.261]    [Pg.3092]    [Pg.102]    [Pg.134]    [Pg.66]    [Pg.95]    [Pg.543]    [Pg.120]    [Pg.75]    [Pg.1300]    [Pg.13]    [Pg.254]    [Pg.319]   
See also in sourсe #XX -- [ Pg.39 ]

See also in sourсe #XX -- [ Pg.39 ]




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Inversions, air

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