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Theoretical Condition

The equilibrium position of the droplet is obtained by finding the minimum of the Gibbs free energy. In this case, the minimization of the Gibbs free energy is equivalent to the minimization of the liquid surface area. [Pg.6]

The second case—that of an SCF—is different the volume of liquid is not constant in the system (dV 0), and the system evolves in the direction of lower energy. Hence [Pg.7]

Let us first investigate the upstream conditions. The upstream condition is most of the time given by the pressure condition of a reservoir of liquid. If we suppose that the reservoir is sufficiently large, as did Bruus [23], then the upstream pressure is constant and approximately equal to the atmospheric pressure (zero pressure difference), and the mean curvature of its free surface is small and nearly constant. [Pg.7]

SCF occurs as long as the pressure at the flow front is smaller than that of the reservoir (p 0), i.e., recalling that pressure may be regarded as the rate of change of energy with respect to volume. [Pg.7]

Considering that any change in is made at the expense of and using Youngs equation cosff=ygg ysL (l- ) becomes [Pg.8]


Point group symmetry, notation and representations, and the group theoretical condition for when an integral is zero. [Pg.444]

It is helpful to understand the relationship of vacuum to the other pressure measurements. Vacuums can range from atmospheric pressure down to zero absolute pressure , representing a perfect vacuum (a theoretical condition involving the total removal of all gas molecules from a given volume). The amount of vacuum is measured with a device called a vacuum gage. [Pg.635]

Fig. 6.2 Theoretical conditions of corrosion, immunity and passivation of gold, at 25°C... Fig. 6.2 Theoretical conditions of corrosion, immunity and passivation of gold, at 25°C...
Fig. 3.11 Theoretical condition of corrosion, immunity, and passivation of CulnSe2, Cu Se, and Se phases in an aqueous solution. Concentrations of Cu, In, and Se species in the aqueous solution at 25 °C were assumed to be 10 M. (Reproduced from [179], Copyright 2009, with permission from Elsevier)... Fig. 3.11 Theoretical condition of corrosion, immunity, and passivation of CulnSe2, Cu Se, and Se phases in an aqueous solution. Concentrations of Cu, In, and Se species in the aqueous solution at 25 °C were assumed to be 10 M. (Reproduced from [179], Copyright 2009, with permission from Elsevier)...
In this paper, we have answered the fundamental question of determining how many independent experimental measurements (or theoretical conditions) are needed to fix a projector. Conflicts which appear in the previous literature treating this question, and that we have simply noted earlier [15], have here been resolved. In particular, we have explained how to properly interpret the K-formulae in [1-3]. [Pg.152]

Neppiras EA, Noltingk BE (1951) Cavitation produced by ultrasonics theoretical conditions of the onset of cavitation. Proc Phys Soc B 64 1032-1038... [Pg.377]

Diffusion operates along well-defined physical principles first described in 1855 by Adolf Fick and now widely known as Fick s Laws of Diffusion. Philbert5 provides a detailed explanation of the laws and a historical account of Fick. While they were designed to describe the behavior of gas molecules under ideal theoretical conditions, Fick s Laws serve reasonably well to describe a wide variety of real diffusion events. Fick wrote the laws as a set of equations in the language of calculus but these can be rephrased in plain English. [Pg.197]

The orbital and vibrational matrix elements may now be examined for symmetry requirements other than g and u. The requirement may best be expressed as the group-theoretical condition... [Pg.244]

In the introduction to this chapter, we mentioned a representation theoretic condition which implies S i(L) = 1. Let us now, at the end of this section, look at this condition. [Pg.234]

Considering the literature review above, it is necessary to develop a comprehensive view that may apply to any system, whatever the luminescent probe is, each system being considered as one specific case of a more general theory. In this section, we first discuss the general scheme of (photo)chemical equations needed to describe a TRES experiment as well as a simplified scheme without photophysical reactions. The theoretical conditions to derive equilibrium constants from TRES data are discussed for the R(III), U(VI), and Cm(III) cases and are related to the experimental data presented above. [Pg.501]

For areas A and B, theoretical conditions show that the TI13P4 phase cannot form. [Pg.191]

The term dry saturated steam is sometimes used. It should be made clear that dryness is a theoretical condition of steam and that in practice, moist saturated steam is used. This also provides assurance that the steam really is saturated and is not superheated. The use of superheated steam may in fact cause problems in process management. [Pg.3531]

Formate can then, under the appropriate conditions, be further metabolized to C02 and H2 by a formate hydrogen lyase complex (enteric bacteria). The acetyl-CoA can be used to produce ATP and acetate. Therefore under ideal (theoretical) conditions ... [Pg.177]

In principle, electrolytic methods offer a reasonably selective means of separating and determining a number of ions. The feasibility of and theoretical conditions for accompli.shing a given separation can be derived from the standard electrode potentials of the species of interest, a.s illustrated in Example 22-2. [Pg.641]

Figure 11.4 Approximate position of some natural environments in terms of Eh and pH. The dashed line represents the limits of measurements in natural environments, as reported by Baas-Becking et al. (1960) and shown in Fig. 11.3. The crosshatched area defines theoretical conditions under which waters are calculated to contain dissolved oxygen at or above a detection limit of 5 /tg/L. Modified after R. M. Garrels and C. L. Christ (1965). Solutions, minerals and equilibria. Copyright 1965 by Freeman, Cooper and Company. Used by permission. Figure 11.4 Approximate position of some natural environments in terms of Eh and pH. The dashed line represents the limits of measurements in natural environments, as reported by Baas-Becking et al. (1960) and shown in Fig. 11.3. The crosshatched area defines theoretical conditions under which waters are calculated to contain dissolved oxygen at or above a detection limit of 5 /tg/L. Modified after R. M. Garrels and C. L. Christ (1965). Solutions, minerals and equilibria. Copyright 1965 by Freeman, Cooper and Company. Used by permission.
These qualitative observations go, in part, back to Fromherz (3) but they were connected with the ligand field treatment of internal transition of the partly filled d-shell and with the group-theoretical conditions for the symmetry types of the energy levels in a study [4—6)... [Pg.23]

Equation (5.132) states that when the particle velocity increases (or when the particle size increases) the theoretical conditions under which the deposition rate coefficient was derived are no longer valid and the actual deposition rate is smaller than the theoretical one (i.e. 7d c 1). Moreover, because particles have a finite size d, the deposition rate coefficient (derived assuming point particles) must be corrected. This correction is introduced through the interception efficiency ... [Pg.194]


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