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Interfacial surface, description

Christoffersen J, Christoffersen MR, Kibalczyc W, Andersen FA (1989) A contribution to the understanding of the formation of calcium phosphates. J Ciyst Growth 94 767-777 Christoffersen J, Landis WJ (1991) A contribution with review to the description of mineralization of bone and other calcified tissues in vivo. Anatom Rec 230 435-450 Christoffersen J, Rostmp E, Christoffersen MR (1991) Relation between interfacial surface-tension of electrolyte ciystals in aqueous suspension and their solubility—A simple derivation based on surface nucleation. J Cryst Growth 113 599-605... [Pg.82]

By calculating the time constant of each resistance, the largest resistance for mass transfer can be determined. For this purpose, the partition coefficients rrii and m2, the mass transfer coefficients kpon and kcOj- well as the interfacial surface areas Apopw and ATjyco2 have been determined in various ways as discussed below. For a more detailed description we refer to eleven [48]. [Pg.324]

The choice of one of the above conventions for the treatment of adsorption systems is a matter of convenience, although the thermodynamics of excesses is the most rigorous mode of interfacial phenomena description. It should be stressed at this point that the Gibbs method does not require any distinct model of the surface phase and its popularity in the chemistry of interfaces is due to its great utility in experimental studies [36-37]. [Pg.5]

In recognizing that arguments based on the rate of spontaneous fluctuations fail to describe the out-of-equilibrium dynamics and in view of recent activity on the influence of adsorption on the glassy dynamics in confinement, we identify the free interfacial surface as the main parameter determining the magnitude of negative deviations from bulk behaviour. In doing so, we emphasize how a suitable model for the description of the out-of-equilibrium dynamics in confinement must account for the presence of dominant bulk linear dynamics and the amount of free interface. We show how there exists solid indications that the FVHD model nicely fits in the idea that the free interface is the key parameter to describe the out-of-equilibrium dynamics in confinement. [Pg.288]

Flow Past Deformable Bodies. The flow of fluids past deformable surfaces is often important, eg, contact of Hquids with gas bubbles or with drops of another Hquid. Proper description of the flow must allow for both the deformation of these bodies from their shapes in the absence of flow and for the internal circulations that may be set up within the drops or bubbles in response to the external flow. DeformabiUty is related to the interfacial tension and density difference between the phases internal circulation is related to the drop viscosity. A proper description of the flow involves not only the Reynolds number, dFp/p., but also other dimensionless groups, eg, the viscosity ratio, 1 /p En tvos number (En ), Api5 /o and the Morton number (Mo),giJ.iAp/plG (6). [Pg.92]

Second-Order Integral Equations for Associating Fluids As mentioned above in Sec. II A, the second-order theory consists of simultaneous evaluation of the one-particle (density profile) and two-particle distribution functions. Consequently, the theory yields a much more detailed description of the interfacial phenomena. In the case of confined simple fluids, the PY2 and HNC2 approaches are able to describe surface phase transitions, such as wetting and layering transitions, in particular see, e.g.. Ref. 84. [Pg.186]

Similar surface terms are commonly used in the description of interfacial systems. They correspond to the idea of a localized interaction with the wall. This has been used in the description of adsorption (see, e.g., [29]), wetting phenomena [30] and interfacial criticality [31],... [Pg.812]

The description of the sorption of charged molecules at a charged interface includes an electrostatic term, which is dependent upon the interfacial potential difference, Ai//(V). This term is in turn related to the surface charge density, electric double layer model. The surface charge density is calculated from the concentrations of charged molecules at the interface under the assumption that the membrane itself has a net zero charge, as is the case, for example, for membranes constructed from the zwitterionic lecithin. Moreover,... [Pg.224]

The surface complexation models used are only qualitatively correct at the molecular level, even though good quantitative description of titration data and adsorption isotherms and surface charge can be obtained by curve fitting techniques. Titration and adsorption experiments are not sensitive to the detailed structure of the interfacial region (Sposito, 1984) but the equilibrium constants given reflect - in a mean field statistical sense - quantitatively the extent of interaction. [Pg.74]

It is important to establish the origin and magnitude of the acidity (and hence, the charge) of mineral surfaces, because the reactivity of the surface is directly related to its acidity. Several microscopic-mechanistic models have been proposed to describe the acidity of hydroxyl groups on oxide surfaces most describe the surface in terms of amphoteric weak acid groups (14-17), but recently a monoprotic weak acid model for the surface was proposed (U3). The models differ primarily in their description of the EDL and the assumptions used to describe interfacial structure. "Intrinsic" acidity constants that are derived from these models can have substantially different values because of the different assumptions employed in each model for the structure of the EDL (5). Westall (Chapter 4) reviews several different amphoteric models which describe the acidity of oxide surfaces and compares the applicability of these models with the monoprotic weak acid model. The assumptions employed by each of the models to estimate values of thermodynamic constants are critically examined. [Pg.5]

Experimental studies of the thermodynamic, spectroscopic and transport properties of mineral/water interfaces have been extensive, albeit conflicting at times (4-10). Ambiguous terms such as "hydration forces", "hydrophobic interactions", and "structured water" have arisen to describe interfacial properties which have been difficult to quantify and explain. A detailed statistical-mechanical description of the forces, energies and properties of water at mineral surfaces is clearly desirable. [Pg.21]

An understanding of much of aqueous geochemistry requires an accurate description of the water-mineral interface. Water molecules in contact with> or close to, the silicate surface are in a different environment than molecules in bulk water, and it is generally agreed that these adsorbed water molecules have different properties than bulk water. Because this interfacial contact is so important, the adsorbed water has been extensively studied. Specifically, two major questions have been examined 1) how do the properties of surface adsorbed water differ from bulk water, and 2) to what distance is water perturbed by the silicate surface These are difficult questions to answer because the interfacial region normally is a very small portion of the water-mineral system. To increase the proportion of surface to bulk, the expanding clay minerals, with their large specific surface areas, have proved to be useful experimental materials. [Pg.51]

These ten interfacial parameters give a very complete description of the energetics of a detergency system. Further surface tension variables for a fluid-air or solid-air interface will also be used to evaluate these ten interfacial parameters. The remainder of this section will explore their evaluation. [Pg.253]

Unfortunately, little direct information is available on the physicochemical properties of the interface, since real interfacial properties (dielectric constant, viscosity, density, charge distribution) are difficult to measure, and the interpretation of the limited results so far available on systems relevant to solvent extraction are open to discussion. Interfacial tension measurements are, in this respect, an exception and can be easily performed by several standard physicochemical techniques. Specialized treatises on surface chemistry provide an exhaustive description of the interfacial phenomena [10,11]. The interfacial tension, y, is defined as that force per unit length that is required to increase the contact surface of two immiscible liquids by 1 cm. Its units, in the CGS system, are dyne per centimeter (dyne cm" ). Adsorption of extractant molecules at the interface lowers the interfacial tension and makes it easier to disperse one phase into the other. [Pg.224]

In the sections that follow, we first outline and summarize, in the context of contemporary ET theory, the experimental behavior of systems involving only weak, electrostatic interactions between dye molecules and the semiconductor surface. This is followed by (1) a description of the behavior of covalently linked dye-semiconductor combinations, which is remarkably different from that seen with weakly interacting systems, (2) a discussion of the fundamental energetics for the reactions—which again appears to differ significantly for the two reaction subclasses—and (3) a comparative discussion of possible interfacial reaction mechanisms. [Pg.91]

Beside the theoretically derived Gibbs adsorption isotherm, a large number of models have been developed that empirically describe a relationship between the interfacial coverage, the surface tension, and the surfactant concentration in the bulk phase. These adsorption isotherms are known under the names of the authors that first described them—i.e., the Fangmuir, Frumkin, or Volmer isotherms. A complete mathematical description of these isotherms is beyond the scope of this unit and the reader is encouraged to consult the appropriate literature instead (e.g., Dukhin et al., 1995). [Pg.619]

Young s equation is the basis for a quantitative description of wetting phenomena. If a drop of a liquid is placed on a solid surface there are two possibilities the liquid spreads on the surface completely (contact angle 0 = 0°) or a finite contact angle is established.1 In the second case a three-phase contact line — also called wetting line — is formed. At this line three phases are in contact the solid, the liquid, and the vapor (Fig. 7.1). Young s equation relates the contact angle to the interfacial tensions 75, 7l, and 7sl [222,223] ... [Pg.118]


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