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Velocity denudation

The adsorbers are usually built of steel, and may be lagged or left unlagged the horizontal type is shown in Figure 28. The vapor-laden air is fed by the blower into one adsorber which contains a bed of 6- to 8-mesh activated carbon granules 12 to 30 inches thick. The air velocity through the bed is 40 to 90 feet per minute. The carbon particles retain the vapor only the denuded air reaches the exit, and then the exhaust line. The adsorption is allowed to continue until the carbon is saturated, when the vapor-laden air is diverted to the second adsorber, while the first adsorber receives low-pressure steam fed in below the carbon bed. The vapor is reformed and carried out by the steam. The two are condensed and if the solvent is not miscible with water, it may be decanted continuously while the water is run off similarly. After a period which may be approximately 30 or 60 minutes, all the vapor has been removed, the adsorbing power of the charcoal has been restored, and the adsorber is ready to function again, while adsorber No. 2 is steamed in turn. [Pg.300]

Rivers transport suspended sediments derived from the disintegration of basin surface layers. With reduced velocity, sediment is deposited in the river channel. The finest material is carried to the sea. It has been estimated that the average mechanical denudation rate for continents is 0.056 mm year (35). This is based on a total suspended load of 13.5 x 10 metric tons year (S). Presently, about two-thirds of the world s total suspended sediment load derives from Southern Asia and large Pacific Islands. Berner has estimated the increase in sediment loss in the U.S. and world since prehuman times to be approximately 200% (35). Current estimated erosion rate from the major land forms is provided in Table I. The relatively recent construction of large sediment trapping dams that normally caused sediment to be deposited in river valleys or transported to the ocean has drastically reduced sediment yields in great rivers. [Pg.251]

Animals continually exposed to concentrations between 100 and 600 ppm developed signs of peripheral neuropathy after 4-8 weeks in cats, the conduction velocity of the ulnar nerve was less than one-half of normal after exposure for 7-9 weeks. In these animals, histologic examination revealed focal denudation of myelin from nerve fibers with or without axonal swelling. In rats and monkeys, adverse effects on neurophysiological indicators of nervous system integrity were found with 9-month exposures to 100 ppm, 6 hours/day, 5 days/week. MBK neuropathies, however, occurred only after 4-month exposure at 1000 ppm. Four months of intermittent respiratory exposure of rats to 13 00 ppm caused severe symmetric weakness in the hind limbs. ... [Pg.460]

A prefired Pallflex 2500 QAST quartz filter (104-mm diameter) downstream of the denuder retained particle-phase PAHs together with other particulate matter at a face velocity of about 3 cm/s. The PUF retained vapor-phase PAH compounds that penetrated the denuder, together with those volatilized from the filter following collection in the particle state. The presence of a denuder is expected to enhance the extent of volatilization of PAHs from the filter relative to the unit without a denuder. The PAH concentrations volatilized during sampling from the unit without a denuder were referred to as the normal artifact, An. The corresponding concentrations from the unit with the denuder included An + Ae, where Ae indicates excess artifact caused by the presence of the denuder. The possibility that particle-phase PAH compounds could volatilize and be retained while within the denuder was not addressed. [Pg.40]

Rainfall is scarce and mild showers can be noticed during the months of May to September. The high velocity cold winds are common climatic feature of the area. Basically, there are two types of vegetation zones in the Lahaul valley (i) temperate zone (2400 to 3300 m), and (ii) alpine zone (above 3300 m) (Aswal and Mehrotra, 1994). Forest resources in the entire Lahaul valley are very sparse and scanty. The Chandra sub-valley has very few7 scattered trees of Betula utilis, Pinus wallichiana, Juniperus communis, J. indica, S. lindleyana and S. pycnostachya on almost denuded northern slopes southern slopes are almost barren. In the Pattan sub-valley, both the slope aspects have some patches of open forests. Juniperus macropoda is the most important tree species found on the south facing slopes. [Pg.53]

The velocity of this boundary and its relation with the chemical shock velocity can be determined by making a material balance on the retaining chemical the amount of chemical with concentration C, in the injected solution in the denuded water zone from x 3 to x b must equal the amount of chemical retained behind the front x 3. Mathematically,... [Pg.39]

An adherent layer of particles with a regular shape (with flat faces) is detached more rapidly than a layer of irregular particles. With an air velocity of 30 m/sec, within 0.25 sec from the moment at which the air stream starts to act, approximately 60% of an adherent layer of regularly shaped particles is detached, but only 20% are detached if the particles are irregularly shaped. The denudation rate can be calculated ... [Pg.335]

The denudation velocity is shown as a function of the parameter (FautP) in Fig. X.9. In Eq. (X.65), only the force of autohesion and the particle density are taken into account no consideration is given to the force of adhesion, even though Davies notes that dust is detached from polished brass surfaces more readily than from surfaces covered with Grade 0 emery paper [280]. [Pg.336]

In denudation all of the dust deposit is removed in approximately 0.5 sec. Hence the denudation velocity is the basic parameter defining this process. If - ad 0 aut the removal of large particles (diameter 2-4 mm) will depend solely on the air-flow velocity and will be observed along the boundary between the dust layer and the surface since the coefficient of friction will be greater for movement of particles along a surface of similar particles than for movement of particles along a solid (hard) surface [281]. [Pg.336]

Fig. X.9. Velocity of denudation of dust deposits on surface covered with Grade 0 emergy paper as a function of parameter (Fautp) r for adherent layer of regularly shaped particles (2) or irregularly shaped particles (1) dimensions of dust deposit 17.8 X 5.1 X 0.6 cm. Fig. X.9. Velocity of denudation of dust deposits on surface covered with Grade 0 emergy paper as a function of parameter (Fautp) r for adherent layer of regularly shaped particles (2) or irregularly shaped particles (1) dimensions of dust deposit 17.8 X 5.1 X 0.6 cm.
As we have demonstrated, the adhesion-type detachment of a layer of adherent particles (denudation) depends on the air-flow velocity, while autohesion-type detachment (erosion) depends on the flow velocity and the time during which the air stream is acting on the dust, as expressed in terms of arbitrary quantities. In many studies, unfortunately, no distinctions have been made as to the specific features of removal of the adherent particle layer, the time of detachment has not been recorded (this is usually a long period, greater than 5 min), and the results of detachment are evaluated solely in terms of the air-flow velocity. The following data relate to the flow velocities at which removal of the layer of adherent particles has been observed ... [Pg.338]

The removal of a layer of particles will depend on the relationship between the forces of adhesion and autohesion. Adhesion-type detachment of an adherent layer (denudation) is determined by the air-flow velocity and the adhesive force. Autohesion-type detachment (erosion) depends not only on the force of autohesion and the air velocity, but also on the time during which the air stream is acting on the surface. Consequently, the detachment of either a monolayer or layer of adherent particles, under otherwise equal conditions, is determined by the air-flow velocity. In turn, the air-flow velocity required for detachment of adherent particles will also be determined by the size of these particles. [Pg.348]

Jaroniec, M. Madey, R. Physical Adsorption on Heterogeneous Solids Elsevier Amsterdam, 1988. Katsanos, N.A. Gavril, D. Kapolos, J. Karaiskakis, G. Surface energy of solid catalysts measured by inverse gas chromatography. J. Colloid Interf. Sci. 2004,270,455-461. Topalova, I. Katsanos, N.A. Kapolos, J. Vasilakos, Ch. Simple measurement of deposition velocities and wall reaction probabihties in denuder tubes. Atm. Environ. 1994,28, 1791-1802. [Pg.2043]

Fig. VI.ll. Denudation velocity of dust deposits from a surface covered with emeiy paper of zero grain size as a function of the parameter to an adhering layer of regular (2) and... Fig. VI.ll. Denudation velocity of dust deposits from a surface covered with emeiy paper of zero grain size as a function of the parameter to an adhering layer of regular (2) and...

See other pages where Velocity denudation is mentioned: [Pg.242]    [Pg.215]    [Pg.23]    [Pg.246]    [Pg.345]    [Pg.87]    [Pg.33]    [Pg.78]    [Pg.371]    [Pg.51]    [Pg.335]    [Pg.215]    [Pg.217]    [Pg.220]    [Pg.462]    [Pg.158]    [Pg.453]   
See also in sourсe #XX -- [ Pg.216 , Pg.217 ]




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