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Size distribution of particles in the

The Carman-Kozeny equation relates the drop in pressure through a bed to the specific surface of the material and can therefore be used as a means of calculating S from measurements of the drop in pressure. This method is strictly only suitable for beds of uniformly packed particles and it is not a suitable method for measuring the size distribution of particles in the subsieve range. A convenient form of apparatus developed by Lea and Nurse 22 1 is shown diagrammatically in Figure 4.4. In this apparatus, air or another suitable gas flows through the bed contained in a cell (25 mm diameter, 87 mm deep), and the pressure drop is obtained from hi and the gas flowrate from h2. [Pg.203]

The model has been used to predict the sampling efficiency of the VE for a wide range of MMAD and GSD values typical of what might be encountered in cotton textile processing. These parameter values are for the actual size distribution of particles in the sampled air, and not for those collected on the membrane filter. These results are summarized in Table II. A remarkable feature of this model is that it predicts that the VE will collect significant amounts of particles with aerodynamic diameters greater than 30 pm. [Pg.68]

In the simulation mns, the design parameters were chosen as d = (u,D), i.e. the kinetic parameters of breakage and the classification function were fixed. The size distribution of particles in the feed stream was constant, selecting 0 for x = xmax/2 and 0.05 for x > xmax/2, while the initial size distribution of the material in the mill was the same in each run. The largest particle size was chosen xmax = 10-3 m, and the values of the kinetic parameters were Ks = 10-4, a = 1.00, /3 = 3.00, y = 0.60,

classification function jump function of the form... [Pg.275]

Zuikov and Soloviev (1979) studied the effect of monomer polarity on both the size and the size distribution of particles in the forming latexes. As a criterion of polarity they took the solubility of the monomer in water, which in this case has an independent significance as well. Polymerizations of styrene, methyl methacrylate, butyl methacrylate, and methyl acrylate... [Pg.258]

SCREEN ANALYSIS STANDARD SCREEN SERIES. Standard screens are used to measure the size (and size distribution) of particles in the size range between about 3 and 0.0015 in. (76 ram and 38 pm). Testing sieves are made of woven wire screens, the mesh and dimensions of which are carefully standardized. The openings are square. Each screen is identified in meshes per inch. The actual openings are smaller than those corresponding to the mesh numbers, however, because of the thickness of the wires. The characteristics of one common series, the Tyler standard... [Pg.931]

This is also known as photon correlation spectroscopy (PCS) or quasi-elastic light scattering (QELS). It uses scattered light to measure the rate of diffusion of protein particles in a sample. The data on molecular motion are digitally processed to yield a size distribution of particles in the sample, where the size is given by the mean Stokes radius or hydrodynamic radius of the protein particles this is the effective radius of a particle in its hydrated state. Clearly, the hydrodynamic radius depends on both mass and shape. [Pg.139]

Kaehler P., Bjornsen P.K., Lochte K., and Antia A. 1997. Dissolved organic matter and its utilization by bacteria during spring in the Southern Ocean. Deep-Sea Res. II44 341-353. Sheldon R.W., Prakash A., and Sutcliffe W.H. Jr. 1972. The size distribution of particles in the ocean. Limnol. Oceanogr. 17 327-340. [Pg.386]

FIGURE 4.4 Origins and size distribution of particles in the atmosphere. Of particular importance are fine particles, which typically have their origin in chemical processes, such as the conversion of gases (e.g., SO / NO / and NH3) to particles and the aggregation of ultra-fine particles (less than 0.1 pm in diameter). A peak also occurs in the vicinity of 10 pm due to the presence of coarse particles, which are typically produced by mechanical processes. Adapted from Wilson and Spengler (1996). [Pg.324]

Colloidal transition metals were prepared by reduction of the corresponding metal salts and by pulverizing the metallic mass. The colloidal metals prepared by the former procedure were generally superior to those prepared by the latter procedure in size and on the narrow size distribution of particles. In the preparation of colloidal metals in aqueous solution, natural poly-... [Pg.51]

Fig. 1. The size distribution of particles in an urban atmospheric dust showing the three size modes. Based on Whitby, 1977 4). Fig. 1. The size distribution of particles in an urban atmospheric dust showing the three size modes. Based on Whitby, 1977 4).
An illustration of the potential for improved resolution in the determination of size distributions with particles in the small size range is indicated in Figures 12 to ik. These results are for a polydisperse polystyrene (labelled 2D2) which has been doped by the addition (29% by mamber) of the Dow 380 X polystyrene standard. [Pg.19]

As discussed in Chapter 15, the size distribution of particles in an agglomeration process is essentially determined by a population balance that depends on the kinetics of the various processes taking place simultaneously, some of which result in particle growth and some in particle degradation. In a batch process, an equilibrium condition will eventually be established with the net rates of formation and destruction of particles of each size reaching an equilibrium condition. In a continuous process, there is the additional complication that the residence time distribution of particles of each size has an important influence. [Pg.139]

Laser diffraction is a fast alternative for analysis of the size distribution of particles in an aerosol cloud. The theory of laser diffraction is well understood [124,125]) but this technique requires special measures to test inhalation devices and to interpret the results correctly. One of the major problems is that flow adjustment through the inhaler is not possible. Furthermore, the presence of carrier particles from adhesive mixtures may disturb the measurement of the fine drug particles and the size distribution obtained is of an unknown dehvered mass fraction of the dose. These practical problems and limitations have been solved by the design of a new modular inhaler adapter for the Sympatec laser diffraction apparatus (Figure 3.6). [Pg.80]

Improved control devices now frequently installed on conventional coal-utility boilers drastically affect the quantity, chemical composition, and physical characteristics of fine-particles emitted to the atmosphere from these sources. We recently sampled fly-ash aerosols upstream and downstream from a modern lime-slurry, spray-tower system installed on a 430-Mw(e) coal utility boiler. Particulate samples were collected in situ on membrane filters and in University of Washington MKIII and MKV cascade impactors. The MKV impactor, operated at reduced pressure and with a cyclone preseparator, provided 13 discrete particle-size fractions with median diameters ranging from 0,07 to 20 pm with up to 6 of the fractions in the highly respirable submicron particle range. The concentrations of up to 35 elements and estimates of the size distributions of particles in each of the fly-ash fractions were determined by instrumental neutron activation analysis and by electron microscopy, respectively. Mechanisms of fine-particle formation and chemical enrichment in the flue-gas desulfurization system are discussed. [Pg.173]

FIGURE 9.33 Size distribution of particles in clouds (solid line) and below the clouds (dashed line), showing two modes (adapted from Hoppel et al., 1994). [Pg.380]

Particle size distribution refers to the distribution of particles in the soil matrix. In general, the three types of soil are sand, clay, and loam. Sand is soil composed of at least 70% sand clay is soil consisting of at least 35% clay and loam soil contains equal weights of sand, clay, and silt. Particular size or soil texture can affect the treatability of contaminated soil in two ways. The potential reaction sites are primarily limited to the surface of particles. The surface-to-volume ratio has a major impact on the nature and rate of reactions between the particle and the contaminant therefore, larger sandsized particles are less reactive than smaller clay-sized particles, particularly if reactions may occur between the sheets of clay minerals. [Pg.52]

Saltikov SA (1967) The determination of the size distribution of particles in an opaque material from a measurement of the size distribution of their sections. In Stereology. Elias H (ed) Springer-Verlag, New York, p 163-173... [Pg.214]

The size distribution of particles in soils and the experimental methods of obtaining them." Soil Science, 19 1-35. [Pg.524]

Particle dimension is crucial for the distribution of particles in the various regions of the human respiratory tract. The various mechanisms of clearance act differently for nano and micro-sized particles.1... [Pg.242]

The size distribution of particles in a wide variety of particulate systems is of paramount importance in the chemical processing industries. For example, the compacting and sintering behavior of metallurgical powders, the flow characteristics of granular material, the hiding power of paint (qv) pigments (qv), and the combustion efficiency of powdered coal (qv) and sprayed fluids, are all heavily influenced by the size of the constituent particles (see Flow... [Pg.126]


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