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Saturation matrix modeling

The parameterization of the remaining reactions is less complicated. For simplicity, the rate v2(TP,ADP) is assumed to follow mass-action kinetics, giving rise to saturation parameters equal to one. Finally, the ATPase represents the overall ATP consumption within the cell and is modeled with a simple Michaelis Menten equation, corresponding to a saturation parameter 6 e [0,1], The saturation matrix is thus specified by four nonzero entries ... [Pg.199]

From the modelling results for bilayers composed of unsaturated lipids one can begin to speculate about the various roles unsaturated lipids play in biomembranes. One very well-known effect is that unsaturated bonds suppress the gel-to-liquid phase transition temperature. Unsaturated lipids also modulate the lateral mobility of molecules in the membrane matrix. The results discussed above suggest that in biomembranes the average interpenetration depth of lipid tails into opposite monolayers can be tuned by using unsaturated lipids. Rabinovich and co-workers have shown that the end-to-end distance of multiple unsaturated acyl chains was significantly less sensitive to the temperature than that of saturated acyls. They suggested from this that unsaturated... [Pg.73]

To specify the matrix 0we take into account the minimal model discussed in Section VII.A.4 The first reaction vj (ATP), including the lumped PFK reaction, depends on ATP only (with glucose assumed to constant). The cofactor ATP may activate, as well as inhibit, the rate (substrate inhibition). To specify the interval of the corresponding saturation parameter, we use Eq. (79) as a proxy and obtain... [Pg.199]

As the second step, the matrix of saturation parameters has to be specified. For simplicity, and following the model of Wolf et al. [126], all reactions are assumed to be irreversible and dependent on their substrates only. The matrix is then specified by 12 free parameters ... [Pg.204]

The dependence (1 TP of v, on ATP is modeled as in the previous section, using an interval C [—00,1] that reflects the dual role of the cofactor ATP as substrate and as inhibitor of the reaction. All other reactions are assumed to follow Michaelis Menten kinetics with ()rs E [0, 1], No further assumption about the detailed functional form of the rate equations is necessary. Given the stoichiometry, the metabolic state and the matrix of saturation parameter, the structural kinetic model is fully defined. An explicit implementation of the model is provided in Ref. [84],... [Pg.204]

The construction of the structural kinetic model proceeds as described in Section VIII.E. Note that in contrast to previous work [84], no simplifying assumptions were used the model is a full implementation of the model described in Refs. [113, 331]. The model consists of m = 18 metabolites and r = 20 reactions. The rank of the stoichiometric matrix is rank (N) = 16, owing to the conservation of ATP and total inorganic phosphate. The steady-state flux distribution is fully characterized by four parameters, chosen to be triosephosphate export reactions and starch synthesis. Following the models of Petterson and Ryde-Petterson [113] and Poolman et al. [124, 125, 331], 11 of the 20 reactions were modeled as rapid equilibrium reactions assuming bilinear mass-action kinetics (see Table VIII) and saturation parameters O1 1. [Pg.217]

Saturated complex polyesters, particularly, poly (butylene terephthalate) (PBT) are used as engineering thermoplastics possesing good thermo - and wearstability, excellent moulding. These properties also allow to use them as matrix material for polymer composites [1], One of the perspective ways of search of effective catalysts for such systems is kinetic study of the reesterification model reaction, performed in the presence of various catalysts and comparison it with the results of the similar reaction without catalyst. Clarification on the example of model system of the most effective catalysts list allows to use them for obtaining both filled and nonfilled PBT and compare catalytic activity of various catalysts. The purpose of the... [Pg.233]

The released U(VI) from the U()2 matrix will continue to be dissolved until saturation with secondary U(VI) solid phases is reached. The observations from both laboratory and natural systems would indicate that the kinetically preferred phase is hydrated schoepite. This will be denoted as U02(0H)2(s) for the sake of description of the model, although the correct notation would be U03-xH20, with x oscillating between 0 and 2. Depending on the presence of carbonates in the contacting solution, the reactions can be described as ... [Pg.523]

It would lie far beyond the aim of this chapter to introduce the state-of-the art concepts that have been developed to quantify the influence of colloids on transport and reaction of chemicals in an aquifer. Instead, a few effects will be discussed on a purely qualitative level. In general, the presence of colloidal particles, like dissolved organic matter (DOM), enhances the transport of chemicals in groundwater. Figure 25.8 gives a conceptual view of the relevant interaction mechanisms of colloids in saturated porous media. A simple model consists of just three phases, the dissolved (aqueous) phase, the colloid (carrier) phase, and the solid matrix (stationary) phase. The distribution of a chemical between the phases can be, as first step, described by an equilibrium relation as introduced in Section 23.2 to discuss the effect of colloids on the fate of polychlorinated biphenyls (PCBs) in Lake Superior (see Table 23.5). [Pg.1174]

Eq (A-l)], but at the same time makes it easier for the penetrant to move through the matrix [Eq (A-2)]. The dual mode model offers the physical interpretation that concavity in the isotherm arises from a site saturation mechanism related to filling of unrelaxed gaps—a phenomenon which is not only easily visualized and understood, but also has been tested explicitly with independently obtained dilatometric data (See Figure 5). [Pg.74]

In this paper a static linear elastic deformation problem for a fluid saturated solid is formulated in which the behavior of the solid matrix is described by a second gradient model. The non-deformed configuration, chosen as a reference configuration, for the considered mixture can not be stress-free indeed the saturating fluid must exhibit internal stresses acting both on the solid constituent and on its sub-bodies. [Pg.230]

Abstract A simplified quintuple model for the description of freezing and thawing processes in gas and liquid saturated porous materials is investigated by using a continuum mechanical approach based on the Theory of Porous Media (TPM). The porous solid consists of two phases, namely a granular or structured porous matrix and an ice phase. The liquid phase is divided in bulk water in the macro pores and gel water in the micro pores. In contrast to the bulk water the gel water is substantially affected by the surface of the solid. This phenomenon is already apparent by the fact that this water is frozen by homogeneous nucleation. [Pg.329]

Taking into account the aforementioned effects of ice formation in porous materials, a macroscopic quintuple model within the framework of the Theory of Porous Media (TPM) for the numerical simulation of initial and boundary value problems of freezing and thawing processes in saturated porous materials will be investigated. The porous solid is made up of a granular or structured porous matrix (a = S) and ice (a = I), where it will be assumed that both phases have the same motion. Due to the different freezing points of water in the macro and micro pores, the liquid will be distinguished into bulk water ( a = L) in the macro pores and gel water (a = P, pore solution) in the micro pores. With exception of the gas phase (a = G), all constituents will be considered as incompressible. [Pg.330]

To reduce the number of unknown parameters of the model, it was assumed [203] that the dependence (Jmm( h) can be determined from existing experimental data [200,212]. Fig. 8.13 compares the shear modulus for two limiting states of the membrane matrix equilibrium (rj) and nonequilibrium (77 ). The model proposed qualitatively agrees with few reliable experimental data on the effect of dissolved hydrogen on the mechanical modules. It correctly predicts the decrease in both Young s modulus and sheer modulus during the saturation of the metal with hydrogen in a wide... [Pg.424]

A two-dimensional numerical model was developed to describe the transport of dissolved organics originating from nonaqueous phase liquid pool dissolution in saturated porous media in the presence of dissolved humic substances. The model assumes that the dissolved contaminant (NAPL dissolved in the aqueous phase) may sorb onto the solid matrix as well as onto humic substances suspended in the aqueous phase, contaminant-humic particles and humic substances may sorb onto the solid matrix, the dissolved contaminant may undergo first-order decay, and humic substances are introduced into the aquifer from a line source. [Pg.113]

Fig. 8 Schematic diagram of the conceptual model showing the unidirectional velocity Ux, the DNAPL pool with aqueous saturation concentration Cs, the humic substance line source of height Lh> and the modes of interaction between dissolved contaminant, dissolved humic substances, and the solid matrix (adopted from Tatalovich et al. [57])... Fig. 8 Schematic diagram of the conceptual model showing the unidirectional velocity Ux, the DNAPL pool with aqueous saturation concentration Cs, the humic substance line source of height Lh> and the modes of interaction between dissolved contaminant, dissolved humic substances, and the solid matrix (adopted from Tatalovich et al. [57])...
Current multimedia models are inadequate in many respects. Description of intermedia transport across the soil-air and unsaturated soil-saturated soil zones suffers from the absence of a suitable theory for multiphase transport through the multiphase soil matrix. These phenomena are crucial in describing pollutant migration associated with hazardous chemical waste sites. Existing unsaturated-zone soil transport models fail to include mass transfer limitations associated with adsorption and desorption and with absorption and volatilization processes. Rather, most models assume equilibrium among the soil-air, soil-solid, solid-water, and soil-contaminant phases. [Pg.273]


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See also in sourсe #XX -- [ Pg.192 , Pg.194 ]




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