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Droplet measurements

Existing droplet measurement techniques may be classified into three broad categories (/) optical nonimaging techniques (2) imaging techniques and (3) nonoptical methods. A comprehensive review of these techniques are available (35—39). [Pg.333]

Gilbert, A.H., Goldstein, B. and Marom, G. (1990), A liquid droplet measurement technique as a means of assessing the interlaminar shear strength of fiber reinforced composites. Composites 21. 408-414. [Pg.39]

Not only do CCN affect the number of cloud droplets formed, but they also affect the size distribution of these droplets. This also affects cloud albedo and its sensitivity to changes in the number concentration (see Eqs. (JJ) and (KK)). Figure 14.47, for example, shows the size distribution for cloud droplets measured in urban and nonurban air around Denver, Colorado (Al-kezweeny et al., 1993). The median volume diameter was 14 jj,m for the urban air cloud, and this was only 50% of that of the much larger droplets in the... [Pg.812]

Some Water Droplet Measurements Inside Cooling Towers Martin, A. Barber, F. R. [Pg.291]

The mean turbulent velocity of eddies with size A in the inertial subrange of isotropic turbulence was assumed equal to the velocity of the neutrally buoyant droplets measured by Kuboi et al [53, 54]. Kuboi et al [53, 54] found that the turbulent velocity of droplets could be expressed by the Maxwell distribution function (9.32), thus the mean eddy velocity was approximated by ... [Pg.830]

Figure 5 Effect of Brownian motion on the measurement of the DSD in a sediment. Small droplets take part in chaotic thermal motion in a direction normal to the sediment plane. The histogram shows that a significant part of the smaller droplets are withdrawn from the DSD as measured in the sediment 67% of the droplets measured in the 1-pm class were not foimd within the sediment. Figure 5 Effect of Brownian motion on the measurement of the DSD in a sediment. Small droplets take part in chaotic thermal motion in a direction normal to the sediment plane. The histogram shows that a significant part of the smaller droplets are withdrawn from the DSD as measured in the sediment 67% of the droplets measured in the 1-pm class were not foimd within the sediment.
Figure 3,21 Results from (a) dynamic light scattering DJD vs. volume fraction of droplets), and (b) static light scattering (excess Rayleigh ratio vs. volume fraction of droplets) measurements at the emulsification... Figure 3,21 Results from (a) dynamic light scattering DJD vs. volume fraction of droplets), and (b) static light scattering (excess Rayleigh ratio vs. volume fraction of droplets) measurements at the emulsification...
Several methods to obtain and measure pL fluid volumes have been reviewed visual inspection measurement, electric measurement, and optical measurement. Visual inspection measurement captures a droplet image by microscope or stroboscope and measures the size of the droplet in the image to calculate its volume. The minimum volume of droplets can reach 10 pL, with a measurement accuracy of 0.1 pL. Coulometric and impedance methods were introduced as electric measurements, which measure the quantity of electricity or impedance of fluids to calculate the droplet volume. The minimum volume of droplets measurable with these methods is 30 pL, with 1 pL accuracy. Finally, optical measurement, especially the backscatter interferometric method, was introduced. This method measures the difference of light phase to calculate the velocity of a fluid and then calculates the volume. Flow rates from 0.833 to 1.66 nL/s were measured in experiments and the accuracy was 0.127 nL/s. [Pg.2734]


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See also in sourсe #XX -- [ Pg.122 ]

See also in sourсe #XX -- [ Pg.15 ]




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