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Identity models

Fully developed nonisothermal flow may also be similar at different Reynolds numbers, Prandtl numbers, and Schmidt numbers. The Archimedes number will, on the other hand, always be an important parameter. Figure 12.30 shows a number of model experiments performed in three geometrically identical models with the heights 0.53 m, 1.60 m, and 4.75 m." Sixteen experiments carried out in the rotxms at different Archimedes numbers and Reynolds numbers show that the general flow pattern (jet trajectory of a cold jet from a circular opening in the wall) is a function of the Archimedes number but independent of the Reynolds number. The characteristic length and velocity in Fig. 12.30 are defined as = 4WH/ 2W + IH) and u = where W is... [Pg.1184]

If we had given out uncoloured models of this molecule with this book, and asked each reader to paint one H green and one H black, we would have no way at all of giving instructions about which to paint what colour. But it wouldn t matter because, even without these instructions, every reader would produce an identical model, whichever way they painted their Hs. [Pg.836]

In practice, diere are an infinite, or at least very large, number of statistically identical models diat can be obtained from a system. If I know that a chromatographic peak consists of two components, I can come up widi any number of ways of fitting the chromatogram all with identical least squares fits to die data. In the absence of further information, a smoother solution is preferable and most definitions of entropy will pick such an answer. [Pg.172]

Figure 9. Molecular model for the primary events in rhodopsin. An essentially identical model (with the exception of the HYPSO route) is also proposed for all-trans bacteriorho-dopsin (BR-t), with anci Kfilo replacing PBAT and BAT, respectively, and the C13-C14 rotation replacing the Cn-Ci2 rotation (Adapted from ref. 307.)... Figure 9. Molecular model for the primary events in rhodopsin. An essentially identical model (with the exception of the HYPSO route) is also proposed for all-trans bacteriorho-dopsin (BR-t), with anci Kfilo replacing PBAT and BAT, respectively, and the C13-C14 rotation replacing the Cn-Ci2 rotation (Adapted from ref. 307.)...
Several CMK inactivators have been examined in vivo. The relatively weak CMK (5-3) was tested in an elastase-induced emphysema model in the hamster. It was effective when administered i.p. at a total dose of 19 mg/hamster both before and after elastase exposme [113]. CMK (5-5) was effective i.t. at a dose of 0.5 mg/hamster when administered either 1 h before or 1 h after HLE exposure, in an identical model [114]. The most effective compound (5-6) worked following p.o. administration in a similar model in mice [115], or after i.t. administration in the elastase-induced acute haemorrhage model in hamsters [116]. Although peptide CMKs were the first low-molecular-weight inhibitors shown to be effective in vivo against elastase, they have consistently demonstrated toxic side-effects which have precluded their development [117, 118]. [Pg.80]

How do we know that each of these arrangements could give rise to only one substance of formula CH3Y As always for problems like this, the answer lies in the use of molecular models. (Gumdrops and toothpicks can be used to make structures like 1 and II, for which the bond angles of ordinary molecular models are not suited.) For example, we make two identical models of 1. In one model we... [Pg.116]

Fig. 6. Global surface temperature and PCO2 histories for two otherwise identical models with high and low heat flows. The models assume a current mid-ocean ridge flux Fridge = 2 x 10 moles a". The low heat-flow models feature relatively little secular change in the oceanic crustal creation rate and the continental metamorphic recycling rate. Fig. 6. Global surface temperature and PCO2 histories for two otherwise identical models with high and low heat flows. The models assume a current mid-ocean ridge flux Fridge = 2 x 10 moles a". The low heat-flow models feature relatively little secular change in the oceanic crustal creation rate and the continental metamorphic recycling rate.
Practise this ring inversion of chair cyclohexane with the aid of models. Adopt the protocol described in Section 1.8 for formation of a boat conformation of cyclohexane, Then hold carbons C(6), C(5) and C l) clamped in the hand, and rotate the right-hand three carbons downward to complete the inversion. It is helpful to make two identical models with H1 and H2 marked by, for example, different coloured tape or similar. Keep one model for reference, and perform the inversion on the other. [Pg.15]

The above conclusions are also valid for specific adsorption of cations whose valence is different from two, and for specific adsorption of anions. Figure 5.133 shows the calculated uptake curves of trivalent Gd on alumina. Identical model as in Fig. 5.120 was used 1-pK-diftuse layer model (Sprycha) for primary surface charging, and one proton released per one adsorbed Gd, except the logarithm of the stability constant of Gd-alumina complex equals 3.76 (from the condition pHso S at 10 g alumina/dm and lO " mol dm inert electrolyte). The uptake curves in Fig. 5.133 are steeper than corresponding curves in Fig. 5.120. This result is not surprising in view of higher valence of Gd (cf. Eq. (5.1)), and indeed, the experimental uptake curves are usually steeper for trivalent than for divalent cations. [Pg.695]

The entries in Tables 4.1 and 4.2 with multiple formulae of surface species and logarithms of their stability constants usually indicate that the adsorption model assumed simultaneous formation of these surface species. Interpretation of such results requires carefulness. First, each surface species requires an additional adjustable parameter (its stability constant), and it is well known that simultaneous fitting of many adjustable parameters usually does not produce unequivocal results. Thus the reported set of values of stability constants should be rather considered as one of many sets (producing nearly identical model curves). This aspect of models with multiple surface species was discussed in more detail elsewhere [104]. [Pg.699]

If we assume that the reaction mentioned in Section 10.3.2 is a fundamental description of the processes controlling the concentration of DOC in groundwater, then this reaction would also control the concentration of iron in groundwater at the same time. An easy way to check this was to run two model calculations, both with identical model parameters. However, one of these calculations was run without considering the reduction of DOC. In this case the distribution of DOC is only controlled by the input from the river Oder and the physical transport with advection and dispersion along the flow through the aquifer. The difference between calculated distribution of concentration with reaction and distribution calculated at same conditions but without reduction of DOC will show the reduced quantity of DOC for each point of the flow field. Now this quantity can be converted stoichiometricly into the equivalent quantity of dissolved iron. Thus one mol of CO2 from oxidised DOC corresponds with four times the amount of used iron(III)oxide and the resulting Fe + in solution. [Pg.186]

Models created in accordance with a consistent conceptual framework and modeling methods are comparable if the objects have been named in conformity with established conventions and if identical modeling objects as well as equivalent degrees of deteiiling have been used. In models created with different modeling methods, it is important to make sure that their metamodels can be compared. [Pg.284]

Gallegos, P. V., Sc Ferdman, B. M. (2012). Latina and Latino ethnoracial identity orientations A dynamic and developmental perspective. In G. L. Wijeyesinghe Sc B. W. Jackson III (Eds.), New perspectives on racial identity development Integrating emerging paradigms into racial identity models (pp. 51-80). New York New York University Press. [Pg.152]

The slopes and the intercepts are similar to those of the fish baseline models (about 0.8-1 and -2 on the mmol/1 scale respectively), indicating a similar sensitivity of fish and daphnids towards non-specific toxicants. The derivation of almost identical models by different investigators with different sets of chemicals supports the reliability of these baseline QSARs for estimating the toxicity of non-polar non-reactive chemicals to Daphnia. Any compound is expected to be at least as toxic as predicted from these models. [Pg.167]

What comes out from this comparison is that not all transfers are identically modeled and that two categories of transfer processes must be distinguished ... [Pg.480]

As in PCA, PLS will generate as many latent variables (q) as the smaller of N (dimensions) or P (samples). Thus far, PLS appears to generate identical models to PCR so what is the difference (other than terminology) The answer is that the PLS procedure calculates the latent variables and the regression coefficients in eqn (7.9) all at the same time. The algorithm is actually an iterative procedure (Wold 1978) but the effect is to combine the... [Pg.153]

A practically identical model has been proposed independently by Weinstein and his CO workers the interaction field modified Hamiltonian (IFMH) model [141]. These authors discussed in details the case of the HF. .. HCOF complex and compared the IFMH results with perturbational calculations. It is interesting to note that in the course of the IFMH calculation the first iteration and the fully converged results yield practically identical interaction energy at least for the actual case. On the other hand, individual components of the interaction energy differ considerably in the two calculations, which shows the importance of charge reorganizations. [Pg.23]


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See also in sourсe #XX -- [ Pg.58 ]




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