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Real adsorbed layer models

Heterogeneous catalytic reactions are the combinations of interrelated physical and chemical elementary acts in reaction mixture - catalyst systems. Here one should discriminate between microscopic and macroscopic kinetics. [Pg.61]

In this connection kinetic models can also be separated into microscopic and macroscopic models. The relations between these models are established through statistical physics equations. Microscopic models utilize the concepts of reaction cross-sections (differential and complete) and microscopic rate constants. An accurate calculation of reaction cross-sections is a problem of statistical mechanics. Macroscopic models utilize macroscopic rates. [Pg.61]

To determine the latter, a function for the energy distributions between molecules must be known. A detailed consideration of the relations between macroscopic and microscopic parameters can be found in refs. 48 and 49. [Pg.61]

It has been known for a fairly long time that the reaction rate must depend on the law of energy distribution between reacting molecules. Apparently it was Marcelin who first realized this in 1915 [48, p. 149]. Experiments with molecular beams in the 1960s and 1970s revealed that, in gas-phase systems, a wide variety of reactions take place that cannot be interpreted without [Pg.61]

The degree of non-equilibrium is determined by the ratio of microscopic rates of reaction to relaxation. Here relaxation is treated as restoration of the Boltzmann distribution due to various physical processes of energy exchange. [Pg.62]


The microscopic characteristics of a real adsorbate layer have been considered [33, 34] by separating the x, y and z components of the electric field at the interface (Fig.4), and applying the Lorentz oscillator model to microscopically represent the adsorbate in the three-layer model. For the case of external reflection at a vacuum/semi-conducting, where Ss is real (no absorption) and isotropic, we can write ... [Pg.525]

In real adsorbed layers, the kinetics is more complicated, as the active sites could have different activity associated with various defects. Similarly to the treatment of adsorption, we will present here a special model of surface nonuniformity, which was developed by M. Temkin. The rate of sorption on an ideal surface is given by ... [Pg.129]

Phase transitions in adsorbed layers often take place at low temperatures where quantum effects are important. A method suitable for the study of phase transitions in such systems is PIMC (see Sec. IV D). Next we study the gas-liquid transition of a model fluid with internal quantum states. The model [193,293-300] is intended to mimic an adsorbate in the limit of strong binding and small corrugation. No attempt is made to model any real adsorbate realistically. Despite the crudeness of the model, it has been shown by various previous investigations [193,297-300] that it captures the essential features also observed in real adsorbates. For example, the quite complex phase diagram of the model is in qualitative agreement with that of real substances. The Hamiltonian is given by... [Pg.98]

Figure 8. A selfsimilar picture for an adsorbed polymer layer around a sphere, derived from the model of de Gennes for flat surfaces (left), and the corresponding real life picture (right). tfe define the thickness 5 of the adsorbed layer by the location of the last layer which contains loops. Figure 8. A selfsimilar picture for an adsorbed polymer layer around a sphere, derived from the model of de Gennes for flat surfaces (left), and the corresponding real life picture (right). tfe define the thickness 5 of the adsorbed layer by the location of the last layer which contains loops.
A serious drawback of lattice gas models is their inadequacy to describe properly the commensurate - incommensurate phase transitions, often observed in real systems [144 - 150]. The possibility of the formation of incommensurate phases results directly from the finitness of potential berriers between adjacent potential minima and from the off-lattice motion of adsorbed particles. Although attempts have been made to extend the lattice-gas models and include the possibility of the formation of incommensurate solid phases [151,152], but it is commonly accepted (and intuitively obvious) that the continuous-space theories are much better suited to describe behaviour of adsorbed films exhibiting incommensurate phases. Theoretical calculations of the gas - solid potential for a variety of systems [88] have shown that, in most cases, the lateral corrugation is rather low. Nevertheless, it appears to have a very big influence on the behaviour of adsorbed layers. [Pg.614]

It is apparent that real food emulsions are likely to behave in a more complex way than are simple model systems studied in the laboratory. This may be especially important when lecithins are present in the formulation. Although these molecules are indeed surfactants, they do not behave like other small-molecule emulsifiers. For example, they do not appear to displace proteins efficiently from the interface, even though the lecithins may themselves become adsorbed (123). They certainly have the capability to alter the conformation of adsorbed layers of caseins, although the way in which they do this is not fully clear it is possibly because they can fill in gaps between adsorbed protein molecules (124). In actual food emulsions, the lecithins in many cases contain impurities, and the role of these (which may also be surfactants) may confuse the way that lecithin acts (125). It is possible also for the phospholipids to interact with the protein present to form vesicles composed of protein and lecithin, independently of the oil droplets in the emulsion. The existence of such vesicles has been demonstrated (126), but their functional properties await elucidation. [Pg.222]

Very few data are available at the moment on two-dimensional melts or analog systems on computers. However, we expect that here model (b) is closer to the real situation. Since the perturbation parameter (is of order unity, the chains still have a radius comparable with Ro. Thus the two-dimensional concentration associated with one chain is c = N// o a . A single chain is enough to build up a c value comparable with the total concentration, and the chains must be somewhat segregated. It is to be hoped that future experiments using chains on adsorbed layers (or chains trapped in lamellar systems such as lipid -I- water), will be able to probe these questions. [Pg.61]

Brunauer (see Refs. 136-138) defended these defects as deliberate approximations needed to obtain a practical two-constant equation. The assumption of a constant heat of adsorption in the first layer represents a balance between the effects of surface heterogeneity and of lateral interaction, and the assumption of a constant instead of a decreasing heat of adsorption for the succeeding layers balances the overestimate of the entropy of adsorption. These comments do help to explain why the model works as well as it does. However, since these approximations are inherent in the treatment, one can see why the BET model does not lend itself readily to any detailed insight into the real physical nature of multilayers. In summary, the BET equation will undoubtedly maintain its usefulness in surface area determinations, and it does provide some physical information about the nature of the adsorbed film, but only at the level of approximation inherent in the model. Mainly, the c value provides an estimate of the first layer heat of adsorption, averaged over the region of fit. [Pg.653]

A number of the assumptions used in the BET theory have been questioned for real samples [6]. One assumption states that all adsorption sites are energetically equivalent, which is not the case for normal samples. The BET model ignores lateral adsorbate interactions on the surface, and it also assumes that the heat of adsorption for the second layer and above is equal to the heat of liquefaction. This assumption is not valid at high pressures and is the reason for using adsorbate pressures less than 0.35. In spite of these concerns, the BET method has proven to be an accurate representation of surface area for the majority of samples [9,10]. [Pg.259]

Such a comparison has formed the basis, for example, for the assertion that the double layer can be emersed essentially intact from solution /8/. A common ambiguity, although for different reasons, in both emersion and UHV model experiments is the difference in the amount of solvent present either at the emersed or synthesized interface, compared to the in-situ situation. In the UHV the total amount of solvent adsorbed, and its distribution into the first and subsequent layers, can in many instances directly be determined, but this information is difficult to obtain and not yet available for the emersed and the real interface. To gather such missing pieces in the interfacial puzzle is the motivation for the work described in this paper. One important prerequisite for any model of the double layer is, for example, the density of solvent molecules in the inner layer as a function of the charge on the interfacial capacitor. [Pg.56]

The determination of the specific surface area of a zeolite is not trivial. Providers of zeolites typically give surface areas for their products, which were calculated from gas adsorption measurements applying the Brunauer-Emmet-Teller (BET) method. The BET method is based on a model assuming the successive formation of several layers of gas molecules on a given surface (multilayer adsorption). The specific surface area is then calculated from the amount of adsorbed molecules in the first layer. The space occupied by one adsorbed molecule is multiplied by the number of molecules, thus resulting in an area, which is assumed to be the best estimate for the surface area of the solid. The BET method provides a tool to calculate the number of molecules in the first layer. Unfortunately, it is based on a model assuming multilayer formation. Yet, the formation of multilayers is impossible in the narrow pores of zeolites. Specific surface areas of zeolites calculated by the BET method (often termed BET surface area) are therefore erroneous and should not be mistaken as the real surface areas of a material. Such numbers are more related to the pore volume of a zeolite rather than to their surface areas. [Pg.101]

To convert hw into real film thickness a three-layer film model with estimated values for the thickness and refractive index of the two adsorbed surfactant layers was assumed [159,277,278] (see Section 2.1-3). A thickness of 0.76 nm and a refractive index of 1.41 were... [Pg.175]

Also, the variation in the C parameter along the isotherm serve to account for the different shapes of the isotherms. From a mathematical point of view, the C constant of the BET equation is intimately related to the shape of the isotherm. A detailed analysis of this can be found in the book by Grengg and Sing [2], according to which when the C constant is lower than 2 the BET equation affords a convex curve, with the shape of the Type III isotherm. However, when the C constant is above 2 the curve acquires the shape of the Type V isotherm. What is absolutely clear is that the most important consequence of C changing with the surface coverage is that this circumvents one of the most important criticisms that have been made about the BET model. Now, the adsorption heat in the first layer changes with the amount adsorbed, as happens in real systems. [Pg.384]

The studies presented here are based essentially on the principle of comparison of the thermodynamic characteristics of adsorption measured on a number of organoderivatives of layer silicates and silica, with the data obtained from the molecular statistic calculations involving the portions of surface, which model the real surface of the materials studied. These surface portions were chosen on the basis of the adsorbent structure analysis and complex physico-chemical studies of the modifying layers structure. [Pg.539]

To be converted catalytically or photocatalytically involving a solid aerosol that is not covered by a water layer, atmospheric components have to be adsorbed onto their surface. Experimental data on adsorption for real atmospheric aerosols, or their models under natural conditions, are still very scarce. However, as suggested by the estimates made in Ref. 2 with CO2 and H2S as particular examples, even at a very low pressures of a trace component (e.g. 10" bar for H2S) they still may be adsorbed on a solid aerosol with a high enough coverage 0. [Pg.227]

This idea is a consequent transfer of the three-dimensional van der Waals equation into the interfacial model developed by Cassel and Huckel (cf. Appendix 2B.1). The advantages of Frumkin s position is a more realistic consideration of the real properties of a two-dimensional surface state of the adsorption layer of soluble surfactants. This equation is comparable to a real gas isotherm. This means that the surface molecular area of the adsorbed molecules are taken into consideration. Frumkin (1925) additionally introduced, on the basis of the van der Waals equation, the intermolecular interacting force of adsorbed molecules represented by a . [Pg.49]


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