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Non-equilibrium model

To this point, we have emphasized that the cycle of mobilization, transport, and redeposition involves changes in the physical state and chemical form of the elements, and that the ultimate distribution of an element among different chemical species can be described by thermochemical equilibrium data. Equilibrium calculations describe the potential for change between two end states, and only in certain cases can they provide information about rates (Hoffman, 1981). In analyzing and modeling a geochemical system, a decision must be made as to whether an equilibrium or non-equilibrium model is appropriate. The choice depends on the time scales involved, and specifically on the ratio of the rate of the relevant chemical transition to the rate of the dominant physical process within the physical-chemical system. [Pg.401]

In contrast to kinetic models reported previously in the literature (18,19) where MO was assumed to adsorb at a single site, our preliminary data based on DRIFT results suggest that MO exists as a diadsorbed species with both the carbonyl and olefin groups being coordinated to the catalyst. This diadsorption mode for a-p unsaturated ketones and aldehydes on palladium have been previously suggested based on quantum chemical predictions (20). A two parameter empirical model (equation 4) where - rA refers to the rate of hydrogenation of MO, CA and PH refer to the concentration of MO and the hydrogen partial pressure respectively was developed. This rate expression will be incorporated in our rate-based three-phase non-equilibrium model to predict the yield and selectivity for the production of MIBK from acetone via CD. [Pg.265]

The material covered in the appendices is provided as a supplement for readers interested in more detail than could be provided in the main text. Appendix A discusses the derivation of the spectral relaxation (SR) model starting from the scalar spectral transport equation. The SR model is introduced in Chapter 4 as a non-equilibrium model for the scalar dissipation rate. The material in Appendix A is an attempt to connect the model to a more fundamental description based on two-point spectral transport. This connection can be exploited to extract model parameters from direct-numerical simulation data of homogeneous turbulent scalar mixing (Fox and Yeung 1999). [Pg.17]

Distillation columns are made to separate at least two different components. There are several different types of columns. The assumption of equilibrium between the liquid and vapour that leave each tray is still in common use to model tray distillation. The work of Krishna and Wesselingh shows, however, that non-equilibrium models give results that are very different from those obtained with the equilibrium assumption. [Pg.5]

Goltz, M.N., and P.V. Roberts. 1986. Interpreting organic solute transport data from a field experiment using physical non-equilibrium models. J. Contamin. Hydrol. 1 77-93. [Pg.301]

The three-phase nonequilibriimi model developed in our laboratory which includes kinetics, mass transfer and heat transfer models [6] is used to predict the yield and selectivity of EGME from the reaction of ethanol and EO. The model predicts fliat die conversion of EO would reach 94 % and 99 % selectivity to EGME at an operating pressure of 235 kPa and a reflux ratio of 2. The model predictions are in excellent agreement with experimental data (Table 2). This result shows that our three-phase non-equilibrium model could be used for the prediction of yield and selectivity in a CD process. [Pg.621]

Fig. 7.3 illustrates concentration profiles, calculated with the aid of three different models of FFF [16,19,20], and thus, substantially, a comparison of the non-equilibrium model with the dispersion model. The dimensionless mean concentration, C , in Fig. 7.3 is defined by the relationship... [Pg.504]

Calculations show that the model of a non-equilibrium surface layer is an alternative to kinetic-controlled adsorption models. On the basis of the purely diffusion-controlled adsorption mechanism the proper consideration of a non-equilibrium diffusion layer leads to a satisfactory agreement between theory and experimental data for various studied systems, systematically demonstrated for the short-chain alcohols [132], The non-equilibrium model is applicable in the concentration range from 10 to 10 mol/cm at different values of the Langmuir constant at- For l < 10 mol/cm a consideration of non-equilibrium layer effects is not necessary. For ai > 10 mol/cm and large surfactant concentration the Ay values calculated from the proposed theory do not compensate the discrepancy to the experimental data so that other mechanisms have to be taken into account. An empirical formula also proposed in [132] for the estimation of the non-equilibrium surface layer thickness leads to a better agreement with experimental data, however this expression restricts the validity of the non-equilibrium surface layer model as alternative to non-diffusional adsorption kinetics. [Pg.324]

In order to evaluate the differences in the approaches, we have performed calculations exploiting both equilibrium and non-equilibrium models within the PCM-IEF framework. All the computed frequencies and IR intensities we will report in the following are obtained in the harmonic approximation, no anharmonic effects have been considered. [Pg.31]

The results we have presented are suflBcient to show that the computar tional procedure gives frequencies emd intensities comparable with the experimental ones. The use of a non-equilibrium model for the C=0 stretch... [Pg.33]

The solubility isotherms obtained from the non-equilibrium models for all these systems are always satisfactory and all the different models used give very similar results. One may notice that the worst case is represented by the PSf-CH4 systems in which the NELF model slightly underestimates the experimental sorption data, especially at the higher pressure range, with an error, however, not exceeding 15%. [Pg.53]

Figure 2.4 Sorption isotherm for the systems CH4-PPO, CH4 PSf, and N2-PEMA the calculations of different non-equilibrium models (NELE, NE-SAFT, and NE-PHSC-SW) are also shown... Figure 2.4 Sorption isotherm for the systems CH4-PPO, CH4 PSf, and N2-PEMA the calculations of different non-equilibrium models (NELE, NE-SAFT, and NE-PHSC-SW) are also shown...
As in the previous cases, the non-equilibrium model gives quite good results in predicting the experimental data the ethylene content is in fact very well calculated and the slight underestimation of the CO2 content at the higher penetrant partial pressure can be attributed to the polymer swelling that probably occurs in such a condition and which... [Pg.59]

Now we are ready to test the hypothesis of nuclear synthesis by a-addition in an equilibrium process, which requires that the relative abundance of each nuclide within a common group must be directly related to its relative stability. The amazing reality is that, despite the imcertainty associated with the measurement of solar abundances, the correlation between nuclear stability and estimated abundance is totally convincing. The binding energy per nucleon and the reported abundance for the nuchdes in the A = 4m + 2 series, with Ne = 6, i.e. for the relevant isotopes of Ca to Kr, are shown in Figure 5.14 as a typical example. The correlation is unmistakable. There is no evidence of any discontinuity at Fe, as required by non-equilibrium models of nucleogenesis. [Pg.179]

This chapter is concerned solely with the modeling of RD processes. The widely used equilibrium stage model is described first, followed by a discussion of the variety of non-equilibrium models needed to model these complicated processes. A perspective on the use of these models in RD process design concludes this chapter. [Pg.217]


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See also in sourсe #XX -- [ Pg.54 , Pg.62 , Pg.71 , Pg.78 , Pg.85 , Pg.118 , Pg.127 , Pg.201 ]

See also in sourсe #XX -- [ Pg.54 , Pg.62 , Pg.71 , Pg.78 , Pg.85 , Pg.118 , Pg.127 , Pg.201 ]




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