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Data Taylor type

For non-ideal systems the Maxwell-Stefan diffiisivities for multicomponent dense gases and liquids deviate from the Pick first law binary coefficients derived from kinetic theory and are thus merely empirical parameters [26], Hence, for non-ideal systems either Dn or Du must be fitted to experimental data. In the first approach the actual diffusivities Du are measured directly, thus this procedure requires no additional activity data. In the second approach the non-ideal effects are divided from the Maxwell-Stefan diffusivities. These are the binary Maxwell-Stefan coefficients, Du, that are fitted to experimental diffusivity data. The non-ideality corrections may be computed from a suitable thermodynamic model. These thermodynamic models generally contains numerous model parameters that have to be fitted to suitable thermodynamic data. This type of simulations were performed extensively by Taylor and Krishna [148]. The various forms of the multicomponent diffusion flux formulations are all of limited utility in describing multicomponent diffusion in non-ideal systems as they all contain a large number of empirical parameters that have to be determined experimentally. [Pg.300]

Similarly, many different types of functions can be used. Arden discusses, for example, the use of Chebyshev polynomials, which are based on trigonometric functions (sines and cosines). But these polynomials have a major limitation they require the data to be collected at uniform -intervals throughout the range of X, and real data will seldom meet that criterion. Therefore, since they are also by far the simplest to deal with, the most widely used approximating functions are simple polynomials they are also convenient in that they are the direct result of applying Taylor s theorem, since Taylor s theorem produces a description of a polynomial that estimates the function being reproduced. Also, as we shall see, they lead to a procedure that can be applied to data having any distribution of the X-values. [Pg.441]

Taylor has collected the above and similar data and compared the ratio of reactivities of the ortho and para positions of compounds of type 19 (expressed as log/odog/p) with the ratio of reactivities of the equivalent positions, a and c, in compounds of type 20 and found that the latter ratio was lower, i.e., a relative increase in the reactivity of the para position (c) has occurred upon ring formation. This fall in the ratio log fa log fc increases along the series X = S < 0 (< NH < CHg) in 20. As this trend parallels the increase in strain in the fused bridging ring it was argued that ring strain was the primary cause of the reduction in ratio. Position a is a-aromatic and position c is j8-aromatic therefore the above concept represents an extension by Taylor of an earlier explanation of the Mills-Nixon effect in indane. Further substitution... [Pg.213]

Diels-Alder reaction of onitrosobenzamide and 1,3-DIBF (no mp and spectral data given, only HRMS 93BSF101). Taylor and co-workers reported Diels-Alder type reactions of 1,3-DIBF and nitrosopyridines [82JOC552]. A Diels-Alder adduct of 1,3-DIBF and an azetidinone rearranges thermally to a ring opened product (92CJC2792). Whereas... [Pg.45]

In contrast to the relatively limited number of experimental approaches utilized to determine electron collisional information for C02 laser species, many different types of experiments have been employed in the determination of heavy particle rates as a function of temperature, for temperatures slightly below room temperature up to several thousand degrees. At room temperature, measurements have been obtained using sound absorption and/or dispersion as well as impact-tube and spectrophone techniques. High temperature rate data have been obtained primarily from shock tube experiments in which electron beam, infrared emission, schlieren, and interferometric diagnostic techniques are employed. For example, as many as 36 separate experiments have been conducted to determine the relaxation rate of the C02 bending mode in pure C02 [59]. The reader is referred to the review by Taylor and Bitterman [59] of heavy-particle processes of importance to laser applications for a detailed description and interpretation of available experimental and theoretical data. [Pg.440]

Figure 3 Ages of mare basalts and pyroclastic glasses show no correlation with Ti02. Age data are from previous compilations by BVSP (1981), Ryder and Spudis (1980), Fernandes et al. (2002a), and (for pyroclastic glasses) Shih et al. (2001), plus a lower limit cited for Apollo 17 VLT basalts by Taylor et al. (1991). The Ti02 data are averaged from the compilation of Haskin and Warren (1991). The five major Apollo basalt types are shown with small symbols because each point represents one of many available samples from the given locale, whereas each of the lunar meteorites represents (probably) our only sample from its locale. Figure 3 Ages of mare basalts and pyroclastic glasses show no correlation with Ti02. Age data are from previous compilations by BVSP (1981), Ryder and Spudis (1980), Fernandes et al. (2002a), and (for pyroclastic glasses) Shih et al. (2001), plus a lower limit cited for Apollo 17 VLT basalts by Taylor et al. (1991). The Ti02 data are averaged from the compilation of Haskin and Warren (1991). The five major Apollo basalt types are shown with small symbols because each point represents one of many available samples from the given locale, whereas each of the lunar meteorites represents (probably) our only sample from its locale.
Figure 5 Mare pyroclastic glasses tend to have far higher MgO, yet a similar range in Ti02, compared to crystalline mare basalts. For basalts, plotted data are averages of many literature analyses for basalt types (Table 2), except for lunar meteorites, which are individual rocks (shown with smaller filled squares). Other data sources are as cited by Arai and Warren (1999), i.e., primarily the compilation of Taylor et al. (1991) updated from Arai and Warren (1999) by adding lunar meteorites Dhofar 287 and NWA032 (but not the cumulate NWA773, 26 wt.% MgO, excluded because its composition is presumably unrepresentative of its magma type). Figure 5 Mare pyroclastic glasses tend to have far higher MgO, yet a similar range in Ti02, compared to crystalline mare basalts. For basalts, plotted data are averages of many literature analyses for basalt types (Table 2), except for lunar meteorites, which are individual rocks (shown with smaller filled squares). Other data sources are as cited by Arai and Warren (1999), i.e., primarily the compilation of Taylor et al. (1991) updated from Arai and Warren (1999) by adding lunar meteorites Dhofar 287 and NWA032 (but not the cumulate NWA773, 26 wt.% MgO, excluded because its composition is presumably unrepresentative of its magma type).
First-Order (NONMEM) Method. The first nonlinear mixed-effects modeling program introduced for the analysis of large pharmacokinetic data was NONMEM, developed by Beal and Sheiner. In the NONMEM program, linearization of the model in the random effects is effected by using the first-order Taylor series expansion with respect to the random effect variables r], and Cy. This software is the only program in which this type of linearization is used. The jth measurement in the ith subject of the population can be obtained from a variant of Eq. (5) as follows ... [Pg.2951]

For non-ideal systems, on the other hand, one may use either D12 or D12 and the corresponding equations above (i.e., using the first or second term in the second line on the RHS of (2.498)). In one interpretation the Pick s first law diffusivity, D12, incorporates several aspects, the significance of an inverse drag D12), and the thermodynamic non-ideality. In this view the physical interpretation of the Fickian diffusivity is less transparent than the Maxwell-Stefan diffusivity. Hence, provided that the Maxwell-Stefan diffusivities are still predicable for non-ideal systems, a passable procedure is to calculate the non-ideality corrections from a suitable thermodynamic model. This type of simulations were performed extensively by Taylor and Krishna [96]. In a later paper, Krishna and Wesselingh [49] stated that in this procedure the Maxwell-Stefan diffusivities are calculated indirectly from the measured Fick diffusivities and thermodynamic data (i.e., fitted thermodynamic models), showing a weak composition dependence. In this engineering approach it is not clear whether the total composition dependency is artificially accounted for by the thermodynamic part of the model solely, or if both parts of the model are actually validated independently. [Pg.306]


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