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Timescales reduction based

Figure 6. Reservoir sizes, residence times, and 5 Fe values for aqueous Fe(II), as calculated for DIR assuming first-order rate laws. Timescale arbitrarily set to 100 days. Calculations based on rate constant determined for a 23 day DIR experiment involving hydrous ferric oxide (HFO) by S. algae (Beard et al. 1999). The percent total reduction at 100 days is shown in the grey box on the lower right side of the lower diagrams, based on the value of k. Parts A-C assume a 2/ 1 ratio of 10, whereas parts D-F assume Bikjki ratio of 1000. As constrained by first-order rate laws, the proportion of the intermediate products Fe(III)-L, followed by Fe(II)-L, increase before substantial accumulation of the final Fe(II)aq product (Parts A and D). Tlie fraction of Fe(III)-L in the exchangeable pool of Fe (Fe(III)-L + Fe(II)-L + Fe(II)aq) decreases with time, primarily due to accumulation of the Fe(II)aq end product, where the rate of change is a function of the kjk ratio. Figure 6. Reservoir sizes, residence times, and 5 Fe values for aqueous Fe(II), as calculated for DIR assuming first-order rate laws. Timescale arbitrarily set to 100 days. Calculations based on rate constant determined for a 23 day DIR experiment involving hydrous ferric oxide (HFO) by S. algae (Beard et al. 1999). The percent total reduction at 100 days is shown in the grey box on the lower right side of the lower diagrams, based on the value of k. Parts A-C assume a 2/ 1 ratio of 10, whereas parts D-F assume Bikjki ratio of 1000. As constrained by first-order rate laws, the proportion of the intermediate products Fe(III)-L, followed by Fe(II)-L, increase before substantial accumulation of the final Fe(II)aq product (Parts A and D). Tlie fraction of Fe(III)-L in the exchangeable pool of Fe (Fe(III)-L + Fe(II)-L + Fe(II)aq) decreases with time, primarily due to accumulation of the Fe(II)aq end product, where the rate of change is a function of the kjk ratio.
Another kind of cell, made by Graham and Curran, was based on an internal reflection crystal [80]. A gold minigrid was mounted directly on a prism (9 x 9 x 45 mm) and on top of this was a zinc selenide prism. The distance (observation) between the minigrid and the prism is typically 13-15 pm, which results in a very short response time. For a potential-step experiment, maximum absorbance is achieved within a couple of seconds. The cell is especially well-suited for potential-scan experiments because the intermediate generated at the electrode will rapidly fill out most of the observation distance even when moderately fast sweep rates (50 mV s ) are applied. Some memory effect is, however, present, because the diffusion layer will not be completely evolved on this timescale. At smaller sweep rates (2 mV s ) all of the observation layer behaves like a thin layer, where the concentrations are in equilibrium with the electrode surface concentrations. The cell has been used to study the reduction process of Fe(CO)s by CV, where it was pos-... [Pg.564]

The one-electron oxidation of hydroxy(tetramesitylporphyrinato)iron(III) in CH2C12 is reversible on the cyclic voltametric timescale and its spectrum, obtained by double potential step chrono-absorptometry, indicates ring-based oxidation. However, at longer times, loss of hydroxide ion occurs, followed by reduction of the dication in an ECE process.61 Loss of axial ligand also was shown to occur for indium porphyrin during both oxidation and reduction.62... [Pg.781]

Rabitz s use of a multiple-time-scale representation of the collision dynamics is somewhat different. The separation of timescales in this theory is based on the rate of phase accumulation, since in the semiclassical limit this is related to the time needed for transfer of a quantum of ener r. When the interactions are such as to generate rapid-phase accumulation, as in the description of deflected translational motion, classical mechanics is appropriate, and when the interactions generate slow-phase accumulation, as in vibrational depopulation, quantum mechanics must be used. The effect of interactions on rotational motion spans the range of behavior between these two limits. The stochastic assumption introduced by Rabitz asserts that large and rapidly varying phases permit use of a random phase approximation. Reduction of the equations of motion to a useful form requires further approximations the reader is referred to the original paper for full discussion of these. The theory described has some very interest-... [Pg.243]

The two-phase motion problem is very stiff, with a wide separation of timescales and a transport matrix which becomes singular as the solution relaxes to its quasi-steady state. The asymptotic analysis presented eliminates the stiffness that is the bane of numerical simulations, affording computational speed-up of 3-4 orders of magnitude over the full system. Building this model into a unit cell simulation code promises huge reductions in computational cost and admits the possibility of performing either full stack-based calculations or doing extensive inverse calculations and parameter estimation. [Pg.274]

An interesting example is the oxidation of the bases of single strand DNA, in which an oxidation scan followed by a reduction differential pulse scan clearly show the adsorption and blocking of the electrode surface [15] the relatively slow timescale of the DP scan is appropriate for this purpose. [Pg.115]

One result of the reaction lumping above is the removal of the highly reactive species D. This means that a fast timescale was removed from the system, and the stiffness of the corresponding ODE system was decreased. The calculation of lifetimes of species is discussed in Sect. 6.2. Reaction lumping based on timescales may remove species and decrease stiffness, and thus may lead to increases in simulation speed. For example, its application was successful for the further reduction of a skeletal scheme describing n-heptane oxidation in Peters et al. (2002). This will be discussed more fully in connection with the application of the QSSA in Sect. 7.8.6. [Pg.35]

The implication of distinguishing between fast and slow variables is that a short time after the perturbation, the values of the fast variables are determined by the values of the slow ones. Appropriate algebraic expressions to determine the values of the fast variables as functions of the values of the slow ones can therefore be developed. This is the starting point of model reduction methods based on timescale analysis. One such method was introduced in Sect. 2.3 where the quasi-steady-state approximation (QSSA) was demonstrated for the reduction in the number of variables of a simple example. In this case, the system timescales were directly associated with chemical species. We shah see in the later discussion that this need not always be the case. [Pg.152]

Sikalo et al. (2014) compared several options for the application of genetic algorithms to mechanism reduction, exploring the trade-off between the size and accuracy of the resulting mechanisms. Information on the speed of solution was also taken into account, so that, for example, the least stiff system (Sect. 6.7) could be selected. An automatic method for the reduction of chemical kinetic mechanisms was suggested and tested for the performance of reduced mechanisms used within homogeneous constant pressure reactor and burner-stabilised flame simulations. The flexibility of this type of approach has clear utility when restrictions are placed on the number of variables that can be tolerated within a scheme in the computational sense. However, the development of skeletal mechanisms is rarely the end point of any reductiOTi procedure since the application of lumping or timescale-based methods can be applied subsequently. These methods will be discussed in later sections. [Pg.208]

Kalachev and Field (2001) reduced a simplified reaction model of tropospheric chemistry. Using non-dimensionalisation and timescale-based variable reduction, a simple 4-variable model was obtained. The features of this model were investigated and compared with other small skeleton tropospheric chemical models. [Pg.242]


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