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Table decomposition models

Fig. 2 Model calculation for the CO decomposition. Model parameters Mean residence time, state of mixedness (described with Bodenstein number Bo) and temperature, Oj concentration 2 Vol% and H2O concentration 15 Vol%, Kinetic data see Table I... Fig. 2 Model calculation for the CO decomposition. Model parameters Mean residence time, state of mixedness (described with Bodenstein number Bo) and temperature, Oj concentration 2 Vol% and H2O concentration 15 Vol%, Kinetic data see Table I...
Table 1, Decomposition Models Used to Fit a Year-Long Litterbag Study of Spartina alterniflora Decomposition in a Salt Marsh Creek... [Pg.370]

In this work, atmospheric particles (PM 10 and PM 2.5) were collected by a dichotomos air sampler. Several leaching procedures were investigated for decomposition of heavy metals. The digests were pre-concentrated with sodium diethyldithiocarbamate. The determinations were canted out on a Vartan Model AA-220 atomic absorption spectrometer. The instrarment was equipped with a GTA-110 graphite furnace system. Table 1 shows the concentrations of heavy metals associated with PM 10 and PM 2.5 particles. Table 1. Concentrations of heavy metals in PM 10 and PM 2.5 atmospheric particles (ng/m )... [Pg.237]

From plotting of 1/r versus 1/C, the reaction rate constant, k and adsorption constant, K can be obtained. Fig. 3 indicates that photocatalytic decomposition of 4-NP is in good agreement with L-H model. In the present work, the values of k and K in the presence of H2O2 were found to be higher than those in the absence of H2O2, as shown in Table 1. [Pg.255]

The so-called Tucker3 model is defined by the decomposition of a three-way table X into a three-way core matrix Z and three two-way loading matrices A, B, C (one for each mode) ... [Pg.154]

If possible, two-way ANOVA should be applied doing repetitions at each level. In case of double measurements the 2ab model represented in Tables 5.5 and 5.6 is taken as the basis of evaluation and variance decomposition. [Pg.130]

Literature data for the suspension polymerization of styrene was selected for the analysi. The data, shown in Table I, Includes conversion, number and weight average molecular weights and initiator loadings (14). The empirical models selected to describe the rate and the instantaneous properties are summarized in Table II. In every case the models were shown to be adequate within the limits of the reported experimental error. The experimental and calculated Instantaneous values are summarized in Figures (1) and (2). The rate constant for the thermal decomposition of benzoyl peroxide was taken as In kd 36.68 137.48/RT kJ/(gmol) (11). [Pg.204]

For fitting such a set of existing data, a much more reasonable approach has been used (P2). For the naphthalene oxidation system, major reactants and products are symbolized in Table III. In this table, letters in bold type represent species for which data were used in estimating the frequency factors and activation energies contained in the body of the table. Note that the rate equations have been reparameterized (Section III,B) to allow a better estimation of the two parameters. For the first entry of the table, then, a model involving only the first-order decomposition of naphthalene to phthalic anhydride and naphthoquinone was assumed. The parameter estimates obtained by a nonlinear-least-squares fit of these data, are seen to be relatively precise when compared to the standard errors of these estimates, s0. The residual mean square, using these best parameter estimates, is contained in the last column of the table. This quantity should estimate the variance of the experimental error if the model adequately fits the data (Section IV). The remainder of Table III, then, presents similar results for increasingly complex models, each of which entails several first-order decompositions. [Pg.119]

By slowly increasing the complexity of the models in this fashion, it was hoped that a model could be obtained that was just sufficiently complex to allow an adequate fit of the data. This conscious attempt to select a model that satisfies the criteria of adequate data representation and of minimum number of parameters has been called the principle of parsimonious parameterization. It can be seen from the table that the residual mean squares progressively decrease until entry 4. Then, in spite of the increased model complexity and increased number of parameters, a better fit of the data is not obtained. If the reaction order for the naphthalene decomposition is estimated, as in entry 5, the estimate is not incompatible with the unity order of entry 4. If an additional step is added as in entry 6, no improvement of fit is obtained. Furthermore, the estimated parameter for that step is negative and poorly defined. Entry 7 shows yet another model that is compatible with the data. If further discrimination between these two remaining rival models is desired, additional experiments must be conducted, for example, by using the model discrimination designs discussed later. The critical experiments necessary for this discrimination are by no means obvious (see Section VII). [Pg.121]

The mixed-potential model demonstrated the importance of electrode potential in flotation systems. The mixed potential or rest potential of an electrode provides information to determine the identity of the reactions that take place at the mineral surface and the rates of these processes. One approach is to compare the measured rest potential with equilibrium potential for various processes derived from thermodynamic data. Allison et al. (1971,1972) considered that a necessary condition for the electrochemical formation of dithiolate at the mineral surface is that the measmed mixed potential arising from the reduction of oxygen and the oxidation of this collector at the surface must be anodic to the equilibrium potential for the thio ion/dithiolate couple. They correlated the rest potential of a range of sulphide minerals in different thio-collector solutions with the products extracted from the surface as shown in Table 1.2 and 1.3. It can be seen from these Tables that only those minerals exhibiting rest potential in excess of the thio ion/disulphide couple formed dithiolate as a major reaction product. Those minerals which had a rest potential below this value formed the metal collector compoimds, except covellite on which dixanthogen was formed even though the measured rest potential was below the reversible potential. Allison et al. (1972) attributed the behavior to the decomposition of cupric xanthate. [Pg.9]

Fig. 1.30 Arrhenius plots for dehydrogenation of MgH (Tego Magnan ) nulled for 20 h and catalyzed by 5 wt% Ni (tests were done in the temperature range 275-375°C using a nonactivated powder). Arrhenius plots were obtained using various models of decomposition process (Table 1.6)... Fig. 1.30 Arrhenius plots for dehydrogenation of MgH (Tego Magnan ) nulled for 20 h and catalyzed by 5 wt% Ni (tests were done in the temperature range 275-375°C using a nonactivated powder). Arrhenius plots were obtained using various models of decomposition process (Table 1.6)...
To evaluate further the CAMD results, a number of atomic and chemical parameters from each structure (number of atoms, fractions of aromatic carbon and hydrogen, weight fraction or each atomic species, empirical formula) were compared with the original literature for each structure. This provided a useful check on the accuracy of the computer models. Results of the computer analyses for the four coal structures are given in Table I. The total numbers of atoms only appear as guides to the size and complexity of each structure, and bear no relationship to the size of a "coal molecule" or a decomposition product. [Pg.162]

Kempter50 studied the thermal decomposition of 88% dense NbC cylinders from 2273 to 3473 K in 1 atm of He. Data at 3273 K will be used to test our diffusion-coupled vaporization mass loss model. We transposed the cylindrical geometry into an equivalent slab by dividing the volume by the average vaporizing area. One face of the cylinder was not included in the calculation because it rested on a NbC pedestal in the furnace. Table 3.13. summarizes analytical X-ray data for average C/Nb compositions. [Pg.51]

Figure 8.17 reveals that the decomposition of dioxins and furans undergoes reduction because the best fit is for the correlation between kinetic rate constants and ELUMO therefore, the compounds act as electrophilic agents. Figure 8.17 presents the correlation between the kinetic rate constants and log P for chlorinated dioxins and furans. It indicates that the higher the hydrophobicity of a given chlorinated dioxin or furan, the less reactive it will be. Table 8.11 summarizes the QSAR models for the dioxins and furans studied. [Pg.331]

In general, as can be seen from the actual parameters for dihydrogen peroxide decomposition (Table 3), manganese catalases are less active than their heme iron counterparts. Catalytic rates comparable to these are a target for functional models of the Mn enzyme. [Pg.377]

In this table, we provide solubility parameters for some liquid solvents that can be used as modifiers in supercritical fluid extraction and chromatography. The solubility parameters (in MPa1/2) were obtained from reference 3, and those in cal1/2cm 3/2 were obtained by application of Equation 4.1 for consistency. It should be noted that other tabulations exist in which these values are slightly different, since they were calculated from different measured data or models. Therefore, the reader is cautioned that these numbers are for trend analysis and separation design only. For other applications of cohesive parameter calculations, it may be more advisable to consult a specific compilation. This table should be used along with the table on modifier decomposition, since many of these liquids show chemical instability, especially in contact with active surfaces. [Pg.266]

Noble gas clathrates will not now form on the Earth, as can be seen from the air pressure decomposition temperatures in Table 2.7. They might, however, form in cooler regions of the primitive solar nebula (see Limine Stevenson, 1985). Sill and Wilkening (1978) note that for pressures in a plausible model nebula, pure ice clathrates of Ar, Kr, and Xe could form at 40, 45, and 62 K, respectively. [Pg.61]


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