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Capillaiy constant

Equation 1 can be used to determine the pore diameter of an MCM-41 sample which exhibits capillary condensation at a certain relative pressure, or to determine the capillary condensation pressure for an MCM-41 sample of a certain pore diameter. To construct model adsorption isotherms for MCM-41, one also needs a description of the monolayer-multilayer formation on the pore walls. This description can be based on the experimental finding that the statistical film thickness in MCM-41 pores of different sizes (especially above 3 nm) is relatively constant for pressures sufficiently lower from those of the capillaiy condensation and can be adequately approximated by the t-curve for a suitable reference silica [29-31], for instance that reported in Ref. 35. In these studies [29-31], the statistical film thickness in MCM-41 pores, tMcM-4i, was calculated according to the following equation [29] ... [Pg.579]

We proceed with illustrative examples for application of the proposed up-scaling scheme to seven soil types with properties listed in Table 1-2. The closed-form solution for degree of saturation (Eq. [23]) was fitted to measured data by optimizing parameters p, go, X, and the chemical potential pd at air entry point (that defines Lmax). Note that the Hamaker constant was estimated beforehand, as described in Estimation of the Effective Hamaker Constant for Solid-Vapor Interactions for Different Soils above. The estimated parameters were then used to calculate the liquid-vapor interfacial area for each soil (Eq. [28]). We used square shaped central pores for all soil types except the artificial sand mixture, where triangular pores were applied to emphasize capillaiy processes over adsorption in sand. I lowcver, the closed-form solutions for retention and interfacial area were derived lo accommodate any regular polygon-shaped central pore. Constants for various shapes are described in Table I-1. The values of primary physical constants employed in (he calculations and (heir units are shown in Table 1-3. [Pg.23]

Taylor, by considering a static balance between capillary and electric stresses, showed the existence of a conical meniscus with a half angle of 49.3° at equilibrium for a perfectly conducting liquid. In this Umit, the meniscus behaves as a constant potential body, and hence, the field is external to the drop the field lines intersect the interface orthogonally. The normal gas phase electric field then scales as / /R, and hence, the normal electric stress pe scales as HR. At every point R along the interface, the normal electric stress exactly balances the azimuthal capillaiy pressure pc ylR- This exact balance and absence of a specific length scale, is responsible for the formation of a static Taylor cone [6]. [Pg.2505]

Solution viscosities of linear polymers relate empirically to their molecular weights. This is used in various ways in industry to designate the size of polymers. The values are obtained by measuring the efflux time t of a polymer solution through a capillaiy. It is then related to the efflux time of pure solvent. Typical viscometers, like those designed by Ubbelohde, Cannon-Fenske, (shown in Fig. 1.3), and other similar ones are utilized and measurements are carried out in constant temperature baths. The viscosity is expressed in following ways ... [Pg.53]

When the steady state mode is estabhshed, a reactant or a product is assayed, generally through spectroscopy at various distances from the mixer along the capillaiy. Under constant flow rate, each distance corresponds to a reaction time and the experimenter can measure these. This method also enables ns to measure extremely fast reactions. [Pg.85]


See other pages where Capillaiy constant is mentioned: [Pg.1183]    [Pg.129]    [Pg.57]    [Pg.627]    [Pg.177]    [Pg.497]    [Pg.389]    [Pg.334]   
See also in sourсe #XX -- [ Pg.493 ]




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