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Kinetic model for the heterogeneous reaction

For the present case the reaction rates will be the sum of homogeneous and heterogeneous reaction rates. [Pg.69]

The batch reactor model at isothermal conditions for each species can now be written as [Pg.70]

Cao and Cbo are the initial concentrations of acetic acid and methanol in kmol/m respectively. [Pg.70]

Fc shape factor, assumed to be unity for spherical particles, g acceleration due to gravity, cm/s  [Pg.83]

Ramchandran P. and Chaudhari R. V., Three Phase Catalytic Reactors , Garden branch science publishers. New York, (1983) [Pg.84]


To obtain a simple kinetic model for this heterogeneous reaction, it has to be assumed that the concentration of hydrogen as a reactant, in terms of partial pressure, is constant, and that the hydrogen is thoroughly mixed with the reaction mass to avoid external mass-transfer limitations. Consequently, experiments were carried out in which the speed of the stirrer was varied from 600 to 1800 rpm. For stirrer speeds up to 1200 rpm, a strong dependence of the rate of reaction on the stirrer speed was found. For stirrer speeds above 1200 rpm, no significant increase in the reaction rate was found therefore, a speed of 1200 rpm was... [Pg.223]

The kinetics and equilibrium of autocatalyzed and ion exchange resin (Amberlyst-15) catalyzed esterification of acetic acid with methanol and hydrolysis of methyl acetate were studied by Popken et. al. (2000) in a temperature range of 303 - 343 K. The homogeneous reaction has been described with a simple power-law model. To compare pseudo-homogeneous and adsorption-based kinetic models for the heterogeneously catalyzed reaction, independent binary liquid phase adsorption experiments were used to estimate the adsorption equilibrium constants to keep the number of adjustable parameters the same for each model. [Pg.177]

In DESIGNER, different ways of taking account of heterogeneous reaction kinetics are available, depending on the reaction rate and character. One further possibility is to use a detailed model for the heterogeneous catalyst mass transfer... [Pg.385]

Let us state the conclusions of this section. We have shown that, in terms of the law of acting surfaces (without any additional assumptions), it is possible to construct sufficiently simple kinetic models for the qualitative interpretation of self-oscillations in the rates of heterogeneous catalytic reactions. [Pg.303]

Further development of kinetic models for the OCM process followed the path of addition of a limited number of heterogeneous steps (first of all— initiation or generation of primary methyl radicals) to homogeneous schemes of methane oxidation (Aparicio et al, 1991 Hatano et al, 1990 McCarty et al, 1990 Shi et al, 1992 Vedeneev et al, 1995 Zanthoff and Baerns, 1990). There was certain logic in such an approach since the most efficient OCM catalysts are almost exclusively oxides with no transition metal ions (some Mn-contain-ing oxide systems are the only exception), any reactions in adsorbed layers at such temperatures can be neglected. In the framework of such models some substantial features of the process could be described. For instance, they predicted the limit in the C2-hydrocarbon yield close to that reliably observed experimentally over the most efficient catalysts (20-25%). [Pg.216]

The above thermochemical values were used to fill the heterogeneous module of the kinetic scheme for the OCM reaction over a model Li/MgO catalyst with corresponding kinetic parameters (see Table III). In combination with a scheme of homogeneous methane oxidation, this set of reactions forms the desired micro-kinetic description. It allowed us to re-consider specific features of the OCM process and to obtain some unexpected results. [Pg.221]

Simple chemical oxidation of arsenite by ferric iron at acid pH has been questioned by Barrett et al. (37). They found experimentally that Fe could not oxidize As02 chemically at pH 1.3 at either 70 or 45°C in the presence of a mixed culture capable of growing on Fe and pyrite (FeS2). However, when they added pyrite to the reaction mixture, the bacteria did promote oxidation of arsenite at 45°C. They explained the effect of the pyrite as a heterogeneous catalyst, the role of the bacteria being the regeneration of a clean catalytic surface on the pyrite and the reoxidation of Fe + generated in the oxidation of arsenite by Fe. Mandl and Vyskovsky (38) developed a kinetic model for the catalytic role of pyrite in this form of bacterial arsenite oxidation by Fe. They performed the experiments on which they based their model with T. ferrooxidans strain CCM 4253. [Pg.324]

The simulator is able to treat different heterogeneous reaction kinetics, depending on the reaction rate and its character. For example, a detailed model for the heterogeneous catalyst mass-transfer efficiency can be used, which is based on the approach of [99]. When applying this type of kinetic model, the intrinsic kinetics data are needed (see Section 10.3.1). Another way is the pseudohomoge-neous approach with effective kinetics expressions, by which the kinetics description is introduced as source terms into the balance equations (see Eqs. (10.3) and (10.4)). [Pg.341]

The design and experimental results for some typical applications of a high temperature, high speed constant volume adsorber-reactor have been presented. Preliminary experiments indicate that adsorption studies can provide a better insight into transport mechanisms and the role of adsorption in heterogeneous catalysis thereby assisting the development of improved kinetic models for these complex reactions. [Pg.59]

It is clear that the experimental curves, measured for solid-state reactions under thermoanalytical study, cannot be perfectly tied with the conventionally derived kinetic model functions (cf. previous table lO.I.), thus making impossible the full specification of any real process due to the complexity involved. The resultant description based on the so-called apparent kinetic parameters, deviates from the true portrayal and the associated true kinetic values, which is also a trivial mathematical consequence of the straight application of basic kinetic equation. Therefore, it was found useful to introduce a kind of pervasive des-cription by means of a simple empirical function, h(a), containing the smallest possible number of constant. It provides some flexibility, sufficient to match mathematically the real course of a process as closely as possible. In such case, the kinetic model of a heterogeneous reaction is assumed as a distorted case of a simpler (ideal) instance of homogeneous kinetic prototype f(a) (1-a)" [3,523,524]. It is mathematically treated by the introduction of a multiplying function a(a), i.e., h(a) =f(a) a(a), for which we coined the term [523] accommodation function and which is accountable for a certain defect state (imperfection, nonideality, error in the same sense as was treated the role of interface, e.g., during the new phase formation). [Pg.322]

The novelty in the aforementioned studies is the use of a comprehensive numerical model for the investigation of catalytic microscale reactors which includes, for the first time in the literature, detailed heterogeneous and homogeneous chemical reaction mechanisms, two-dimensional treatment for both the gas and solid wall phases and surface radiation heat transfer, under both steady and transient (quasisteady) conditions. Moreover, a validated chemical kinetics model for the coupled catalytic and gas-phase combustion of propane (a fuel of particular interest for portable applications) is presented for the first time. [Pg.120]

In this chapter we consider the problem of the kinetics of the heterogeneous reactions by which minerals dissolve and precipitate. This topic has received a considerable amount of attention in geochemistry, primarily because of the slow rates at which many minerals react and the resulting tendency of waters, especially at low temperature, to be out of equilibrium with the minerals they contact. We first discuss how rate laws for heterogeneous reactions can be integrated into reaction models and then calculate some simple kinetic reaction paths. In Chapter 26, we explore a number of examples in which we apply heterogeneous kinetics to problems of geochemical interest. [Pg.232]

Most standard chemical engineering tests on kinetics [see those of Car-berry (50), Smith (57), Froment and Bischoff (19), and Hill (52)], omitting such considerations, proceed directly to comprehensive treatment of the subject of parameter estimation in heterogeneous catalysis in terms of rate equations based on LHHW models for simple overall reactions, as discussed earlier. The data used consist of overall reaction velocities obtained under varying conditions of temperature, pressure, and concentrations of reacting species. There seems to be no presentation of a systematic method for initial consideration of the possible mechanisms to be modeled. Details of the methodology for discrimination and parameter estimation among models chosen have been discussed by Bart (55) from a mathematical standpoint. [Pg.319]

In a recent survey [19] it was noted that a realistic model for catalytic oxidation reactions must include equations describing the evolution of at least two concentrations of surface substances and account for the slow variation in the properties of the catalyst surface (e.g. oxidation-reduction). For the synchronization of the dynamic behaviour for various surface domains, it is necessary to take into consideration changes in the concentrations of gas-phase substances and the temperature of the catalyst surface. It is evident that, in the hierarchy of modelling levels, such models must be constructed and tested immediately after kinetic models. On the one hand, the appearance of such models is associated with the experimental data on self-oscillations in reactors with noticeable concentration variations of the initial substances and products (e.g. ref. 74) on the other hand, there was a gap between the comprehensively examined non-isothermal models with simple kinetics and those for the complex heterogeneous catalytic reactions... [Pg.269]

Analysis of the simplest non-linear kinetic models (in particular, of kinetic models for heterogeneous catalysis). The aim is to select the simplest non-linear kinetic models to carry out the most complete investigation of their steady-state and relaxation characteristics. The obtained systems of typical relationships facilitates the interpretation of complex reactions, including simpler "typical units. [Pg.385]

Heterogeneously catalyzed reactions are usually studied under steady-state conditions. There are some disadvantages to this method. Kinetic equations found in steady-state experiments may be inappropriate for a quantitative description of the dynamic reactor behavior with a characteristic time of the order of or lower than the chemical response time (l/kA for a first-order reaction). For rapid transient processes the relationship between the concentrations in the fluid and solid phases is different from those in the steady-state, due to the finite rate of the adsorption-desorption processes. A second disadvantage is that these experiments do not provide information on adsorption-desorption processes and on the formation of intermediates on the surface, which is needed for the validation of kinetic models. For complex reaction systems, where a large number of rival reaction models and potential model candidates exist, this give rise to difficulties in model discrimination. [Pg.103]

A different model [11] that can be used to obtain the kinetics equation for a pyrolytic reaction is adapted from the theory developed for the kinetics of heterogeneous catalytic reactions. This theory is described in literature for various cases regarding the determining step of the reaction rate. The case that can be adapted for a pyrolytic process in solid state is that of a heterogeneous catalytic reaction with the ratedetermining step consisting of a first-order unimolecular surface reaction. For the catalytic reaction of a gas, this case can be written as follows ... [Pg.44]


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