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Particles, heterogeneous reactions

When the volatile matter has left the particles, heterogeneous reactions, such as gasification with CO2 and H2O and char combustion, begin. Char combustion is a slower process than gas combustion and demands a higher temperature (> 800°C) to be complete. As long as oxygen is present combustion dominates, since gasification is slow. [Pg.749]

Heterogeneous reactions these various processes are cyclic and continuous, taking place in all sections of the boiler from the economizer to the condensate lines and including suspended ferric oxide and cupric oxide particles. Unless the hydrazine overfeed is extremely substantial (say, six to seven times theoretical), these latter reactions tend to predominate ... [Pg.492]

Fig. 20. Heterogeneous reactions occurring at oxidizer-particle-polymeric-binder interface (A6). Fig. 20. Heterogeneous reactions occurring at oxidizer-particle-polymeric-binder interface (A6).
The valence band structure of very small metal crystallites is expected to differ from that of an infinite crystal for a number of reasons (a) with a ratio of surface to bulk atoms approaching unity (ca. 2 nm diameter), the potential seen by the nearly free valence electrons will be very different from the periodic potential of an infinite crystal (b) surface states, if they exist, would be expected to dominate the electronic density of states (DOS) (c) the electronic DOS of very small metal crystallites on a support surface will be affected by the metal-support interactions. It is essential to determine at what crystallite size (or number of atoms per crystallite) the electronic density of sates begins to depart from that of the infinite crystal, as the material state of the catalyst particle can affect changes in the surface thermodynamics which may control the catalysis and electro-catalysis of heterogeneous reactions as well as the physical properties of the catalyst particle [26]. [Pg.78]

All vapourisation processes of solutions made of unstable substances are dangerous because the concentration of the unstable substance increases. In this category the heterogeneous reactions can be grouped together they lead to accidents because of compounds with too thin a particle size distribution. So it is possible to control the reaction of phenyllithium by using thick pieces of lithium. [Pg.151]

For heterogeneous reactions in the solid state, tests on small quantities with different particle size distributions can help the technician make the right decisions. [Pg.152]

Nevertheless, in the sensor study of heterogeneous reactions of singlet oxygen, it is better to employ selective sources that do not generate other active particles and produce though low, but stable concentrations of 02( ). These sources can be photochemical and chemical... [Pg.305]

Ehrenfreund P., et al. (2003). Physics and chemistry of icy particles in the universe answers from microgravity. Planetary and Space Science 51 473-494 Emeline A. V. (2003). Abiogenesis and photo-stimulated heterogeneous reactions in the interstellar medium and on primitive Earth. Relevance to the genesis of life.. Journal of Photochemistry and Photobiology C 3 203. [Pg.330]

Recall the diffusion controlled burning rate of a particle with fast heterogeneous reactions at the surface given by Eq. (9.29)... [Pg.527]

Char oxidation dominates the time required for complete burnout of a coal particle. The heterogeneous reactions responsible for char oxidation are much slower than the devolatilization process and gas-phase reaction of the volatiles. Char burnout may require from 30 ms to over 1 s, depending on combustion conditions (oxygen level, temperature), and char particle size and reactivity. Char reactivity depends on parent coal type. The rate-limiting step in char burnout can be chemical reaction or gaseous diffusion. At low temperatures or for very large particles, chemical reaction is the rate-limiting step. At... [Pg.25]

At low temperatures (T<1320 °C) and small particles, combustion regime (I) prevails [11,74,75]. Regime (I) is controlled by chemical kinetics intraparticle (reaction control), see Figure 55. The oxygen content is constant at any radius inside the particle since the rate of diffusion is fast compared to the rate of heterogeneous reaction. The particle then burns with reducing density and a constant diameter, see Figure 55. [Pg.130]

A review of research on the application of quantum mechanics to heterogeneous reactions is outside the scope of this article. Thus, the readers are referred to sources such as Surface Science, Vol. 156, which contains the proceedings of the Third International Meeting on Small Particles and Inorganic Clusters, Berlin, West Germany, July 9-13, 1984, and Supercomputer Research in Chemistry and Chemical Engineering, ACS Symposium Series No. 353, 1987. [Pg.175]

It should be noted that particles in the chemisorbed state may differ in nature from the corresponding molecules in the gaseous phase, representing not these molecules themselves, but just parts of them, which lead an independent existence on the surface. In other words, the very act of adsorption may in some cases be accompanied by dissociation of the molecule this may be considered an experimentally established fact. Such adsorption accompanied by dissociation, requires an activation energy, as was shown by Lennard-Jones (16) on the example of the Hj molecule. The mechanism of such dissociation, which is one of the simplest examples of a heterogeneous reaction has, however, until recently not been investigated. [Pg.203]

In this case the quantity n indicates how many times the number of reactive particles adsorbed per unit surface increases under illumination (other external conditions remaining the same). Evidently, the rate of the heterogeneous reaction in which these particles participate will be a function of fi and thus will be sensitive to illumination. If An = Ap = 0 (photo-electrically inactive absorption of light), then according to (41) m = 1, and illumination has no effect on the reaction rate. [Pg.245]

The particle surface may function as a catalytic site for heterogeneous reactions involving the generation or removal of gaseous pollutants (11, 15-17). [Pg.138]

Surface Chemical Analysis. Electron spectroscopy of chemical analysis (ESCA) has been the most useful technique for the identification of chemical compounds present on the surface of a composite sample of atmospheric particles. The most prominent examples Include the determination of the surface chemical states of S and N in aerosols, and the investigation of the catalytic role of soot in heterogeneous reactions involving gaseous SO2, NO, or NH3 (15, 39-41). It is apparent from these and other studies that most aerosol sulfur is in the form of sulfate, while most nitrogen is present as the ammonium ion. A substantial quantity of amine nitrogen also has been observed using ESCA (15, 39, 41). [Pg.146]

The surface layer composition may effect catalytic activity. Surface enrichments of trace metals, for example, may enhance the catalytic role of particles in heterogeneous reactions in the atmosphere involving gaseous pollutants such as SO2 (54, 55). [Pg.156]

The scope of kinetics includes (i) the rates and mechanisms of homogeneous chemical reactions (reactions that occur in one single phase, such as ionic and molecular reactions in aqueous solutions, radioactive decay, many reactions in silicate melts, and cation distribution reactions in minerals), (ii) diffusion (owing to random motion of particles) and convection (both are parts of mass transport diffusion is often referred to as kinetics and convection and other motions are often referred to as dynamics), and (iii) the kinetics of phase transformations and heterogeneous reactions (including nucleation, crystal growth, crystal dissolution, and bubble growth). [Pg.6]

The mathematical difficulty increases from homogeneous reactions, to mass transfer, and to heterogeneous reactions. To quantify the kinetics of homogeneous reactions, ordinary differential equations must be solved. To quantify diffusion, the diffusion equation (a partial differential equation) must be solved. To quantify mass transport including both convection and diffusion, the combined equation of flow and diffusion (a more complicated partial differential equation than the simple diffusion equation) must be solved. To understand kinetics of heterogeneous reactions, the equations for mass or heat transfer must be solved under other constraints (such as interface equilibrium or reaction), often with very complicated boundary conditions because of many particles. [Pg.83]


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See also in sourсe #XX -- [ Pg.332 ]




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ATMOSPHERIC FATES OF PARTICLE-ASSOCIATED PAHs HETEROGENEOUS REACTIONS

Heterogeneous reaction

Particle heterogeneous

Reaction heterogeneous reactions

Reaction particles

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