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ETAL COMPLEX EQUILIBRIA

We also found the saturation kinetics for alkaline hydrolyses of 44 (PNPA), 3-nitro-4-acetoxybenzoic acid 56 (NABA), and 3-nitro-4-acetoxybenzenearsonie acid 57 (NABAA) in the presence of QPVP1025. If ester-polymer complex formation occurs prior to the attack of OH-, Eq. (5) holds, according to Bunton etal. 103 where K is the equilibrium association constant of polyelectrolyte (PE) and ester (S), and kt the first-order rate coefficients1035, PE, S, and P indicate the poly-... [Pg.159]

AuCl2- or even a higher order complex. While it is possible that the enhanced capacity of Au1 for complexation with soft ligands may account for the disparate distributions of Ag and Au, fractionation of Au and Ag may also be caused by a significant Aum chemistry in seawater. The major species of Au111 in seawater are expected to be Au(OH)3 or Au(OH)3C1 (Baes and Mesmer, 1976). Although the analysis ofTumer etal. (1981) indicated that the field of Aum stability is somewhat outside the oxidation-reduction conditions encountered in seawater, a paucity of direct formation-constant observations for both Aum and Au1 creates substantial uncertainties. Furthermore, with respect to thermodynamic predictions of oxidation-reduction behaviour the ocean is not a system at equilibrium. [Pg.340]

Using coal-based sorbents, Sivasamy et al. [62] evaluated their ability to remove fluoride from water. On equilibrium basis, Langmuir and Freundlich models were used to describe the data points, while the kinetic data points were interpreted in terms of reaction and mass transfer processes. Kaolinite, adioctahedral two-layered (silica and alumina) silicate (1 2 type), has also been tested in drinking water defluoridation. Recently, Sugita etal. [58] and earlier Kau etal. [63] and Weerasooriya et al. [10] presented fluoride adsorption results of kaolinite. The fluoride-binding sites in kaolinite consist of aluminol and silinol sites. The authors explained that the fluoride-kaolinite interaction led to the formations of both the inner- and outer-sphere complexes. [Pg.20]

Another indication of the problems associated with modularization of complex systems is the small number of formal mathematical methods that allow one to simplify kinetic models. The existing methods are all based on time-scale separation in the system which allows for the decomposition of the system into a module composed of fast processes and one composed of slow processes. Then the fast processes can be considered in the absence of the slow processes. The slow processes are then considered with the fast processes either in steady state or thermodynamic equilibrium (Klonowski 1983 Segel and Slemrod 1989 Schuster and Schuster 1991 Kholodenko etal. 1998 Stiefenhofer 1998 Schneider and Wilhelm 2000). Two successful approaches to modularization of complex networks do not consider dynamics. One is purely stmctural while the other is applicable only to systems in steady state and concerns the analysis of control. [Pg.252]

Such an assembly of mixing and separating equipment is represented In Figure 14.4(a), and more schematically in Figure 14.4(b). In the laboratory, the performance of a continuous countercurrent extractor can be simulated with a series of batch operations in separatory funnels, as in Figure 14.4(c). As the number of operations increases horizontally, the terminal concentrations Ei and R3 approach asymptotically those obtained in continuous equipment. Various kinds of more sophisticated continuous equipment also are widely used in laboratories some are described by Lo etal. (1983, pp. 497-506). Laboratory work is of particular importance for complex mixtures whose equilibrium relations are not known and for which stage requirements cannot be calculated. [Pg.483]

So far, only the reactions with the solvent assumed to be water have been considered. However, in practical situations other components are usually simultaneously present in the solutions, including impurities, reaction products, and cosolvents. We thus need a simple method to present the equilibrium of interest. One approach to resolve this problem is the use of conditional constants originally introduced by Schwarzenbach as apparent constants and developed further by Ringbom and Kolthoff. For a simple reaction between an L(igand) and a M(etal) ion, the ML complex is formed ... [Pg.456]

The dynamic surface tension of a monolayer may be defined as the response of a film in an initial state of static quasi-equilibrium to a sudden change in surface area. If the area of the film-covered interface is altered at a rapid rate, the monolayer may not readjust to its original conformation quickly enough to maintain the quasi-equilibrium surface pressure. It is for this reason that properly reported 11/A isotherms for most monolayers are repeated at several compression/expansion rates. The reasons for this lag in equilibration time are complex combinations of shear and dilational viscosities, elasticity, and isothermal compressibility (Manheimer and Schechter, 1970 Margoni, 1871 Lucassen-Reynders etal., 1974). Furthermore, consideration of dynamic surface tension in insoluble monolayers assumes that the monolayer is indeed insoluble and stable throughout the perturbation if not, a myriad of contributions from monolayer collapse to monomer dissolution may complicate the situation further. Although theoretical models of dynamic surface tension effects have been presented, there have been very few attempts at experimental investigation of these time-dependent phenomena in spread monolayer films. [Pg.60]

The first quantitative measurements on copper(I)-ethylene and -actylene complexes were made by Temkin etal. The reaction was followed by observing changes in potential of a copper electrode with changes in the equilibrium due to the introduction of the unsaturated hydrocarbon. [Pg.101]

There are now hundreds of programs designed to compute chemical equilibrium in complex, multi-component systems. These are too numerous to summarize completely here, but thorough reviews are available in the literature (Van Zeggeren and Storey, 1970 Nordstrom etal., 1979b Wolery, 1979,1983 Smith and Missen, 1982 Reed, 1982 Nordstrom and Ball, 1984 Nordstrom and Munoz, 1985, Appendix E De Capitani and Brown, 1987). [Pg.510]

It should be noted that the model of Felmy et al. is neither consistent with the complexes and equilibrium constants selected in the present review nor with the speci-ation calculated with the SIT approach. Therefore the equilibrium constants selected in the present review must not be used in combination with the Pitzer parameters of Felmy etal. [1997FEL/RAI], [1999FEL/RAI]. [Pg.637]

In addition to the effects of temperature and ionic strength, rates are also affected by changing pressure. By analogy to the effect of pressure on equilibrium constants, the expected effect of pressure on rate constants (Asano andleNobel, 1978 Drljaca etal, 1988 Eckert, 1972) is related to the change in volume that results from the conversion of the reactants to the activated complex. This activation volume (A F ) is the difference between the partial molal volumes of the reactants and the transition state. [Pg.90]

Schomacker etal. (1988) labelled human blood serum with Yb in vitro and showed, by alcohol fractionation at low temperature, that 95% of the radioactivity was associated with the albumin. Equilibrium dialysis studies in vitro using HSA-ianthan-ide solutions or whole human serum yielded values for the association constant for the lanthanide-albumin complex ranging, with increasing atomic number and decreasing ionic radius, from log Kp, = 4.7 for Ce to log = 9.5 for Yb, table 9. [Pg.609]

The pronounced effects of aqueous chemistry on actinide sorption behavior suggest that sorption modeling should account for changing physicochemical conditions. A number of different modeling approaches of varying complexity can be used to incorporate the effects of chemistry on radionuclide sorption. A class of models that has been used with success in modeling pH-dependent sorption for actinides and other metals is the electrostatic surface complexation model (SCM). These models are equilibrium representations of sorption at the mineral-water interface and are discussed in detail elsewhere (Davis Kent, 1990 Dzombak Morel, 1990 Hayes etal., 1991 Seme etal., 1990 Turner, 1995), with only a brief overview presented here. [Pg.222]


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ETALS

Equilibria complex

Equilibrium complexation

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