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Equilibrium of water

Often, H+ or OH ions are involved in the electrode reactions, and the electrode potential then depends on the concentration of these ions (or solution pH). Because of the dissociation equilibrium of water, the activities of these ions are interrelated as fle+floH = = 1-27 X 10 moH/L. For this reason these reactions can be for-... [Pg.48]

The discharge of Offi ions disturbs the ionic equilibrium of water, and so more water ionizes to restore it ... [Pg.691]

To run adsorption storage systems efficiently the appropriate adsorbent has to be used. The right choice is possible on the basis of the measured adsorption equilibrium. The adsorption equilibrium of water vapor and different adsorbents (zeolites and silica gels) was experimentally found [3,4], The differential heat of adsorption (AHd) was calculated from the equilibrium data. [Pg.400]

In the next section, you will focus on the equilibrium of water. You will discover how the pH scale is related to the concentrations of the ions that form when water dissociates. As well, you will learn how to calculate the pH values of solutions of weak acids and bases. [Pg.387]

Under steady-state operation with a constant water flux through the membrane, mechanical equilibrium of water will prevail locally at external membrane faces and inside fhe membrane that involves the balance of local liquid, gas, capillary, and elastic pressures. This condition corresponds to a stationary distribution of wafer in the membrane. However, the condition of chemical equilibrium, Equafion (6.5), will be violafed due to the chemical flux of species. [Pg.379]

Many different types of reversible reactions exist in chemistry, and for each of these an equilibrium constant can be defined. The basic principles of this chapter apply to all equilibrium constants. The different types of equilibrium are generally denoted using an appropriate subscript. The equilibrium constant for general solution reactions is signified as or K, where the c indicates equilibrium concentrations are used in the law of mass action. When reactions involve gases, partial pressures are often used instead of concentrations, and the equilibrium constant is reported as (p indicates that the constant is based on partial pressures). and are used for equilibria associated with acids and bases, respectively. The equilibrium of water with the hydrogen and hydroxide ions is expressed as K. The equilibrium constant used with the solubility of ionic compounds is K p. Several of these different K expres-... [Pg.152]

Most biological processes in the cell take place in a water-based environment. Water is an amphoteric substance that is, it may serve as a proton donor (acid) or a proton acceptor (base). Equation 2.1 shows the ionic equilibrium of water. [Pg.36]

Mixtures with excess combustible (hydrogen) were exploded the oxygen concentration in the explosion products of such mixtures was determined from the dissociation equilibrium of water vapor. All the experiments were carried out in glass flasks at an initial pressure of 200 mm the nitric oxide was absorbed by water in the presence of air over a period of 24 hours. The... [Pg.398]

Fig. 3.1. Three equations for the equilibrium of water ice and liquid water for temperatures ranging from 180 to 273 K. Reprinted from Marion (2002) with permission... Fig. 3.1. Three equations for the equilibrium of water ice and liquid water for temperatures ranging from 180 to 273 K. Reprinted from Marion (2002) with permission...
Note that considering H+ and OH- from the ionization of water introduces two additional components, but also two addition constraints the ionization equilibrium of water and the requirement that [H+] = [OH-], so that cind and/ are unchanged. [Pg.212]

J. Vorholz et al., Vapor + liquid equilibrium of water, carbon dioxide, and the binary system, water + carbon dioxide, from molecular simulation. Fluid Phase Equilib. 170, 203 (2000)... [Pg.357]

These data are represented5 m the pressure-temperature diagram (fig. 42) by the fusion curve AB, which is steep, but curved towards the abscissa,6 as the results in the last column of the above table clearly demand. This curve represents the equilibrium between ordinary ice or ice I and water, the triple point A representing the condition of equilibrium of water-vapour, liquid water, and ice I. Under a pressure of 2200 kilograms, corresponding to the point B in the figure, there is a break in the fusion curve, a new form of ice appearing, known as ice III,... [Pg.250]

I. Salts of strong acids and strong bases, when dissolved in water, show a neutral reaction, as neither the anion nor the cation combines with hydrogen or hydroxyl ions respectively to form sparingly dissociated products. The dissociation equilibrium of water... [Pg.39]

In Chapter 2 we used classical thermodynamics to derive the condition for incipient plasmolysis (n°lasmolysis = rTplasmolysis, Eq. 2.20 also see Fig. 2-13), which occurs when the hydrostatic pressure inside a plant cell P1 just becomes zero. The derivation assumed equilibrium of water (i.e., equal water potentials) across a membrane impermeable to solutes. However, the assumptions of water equilibrium and solute impermeability are often not valid. We can remedy this situation using an approach based on irreversible thermodynamics. [Pg.165]

Now, if in this period, both evaporation from the granules and the internal equilibrium of water vapor in the bed are rapid compared to the transfer of moisture over the bed-stream interface, then the diffusion equation can be solved (23). Using the dimensionless parameter... [Pg.217]

Infer the effect of heat on the solubility equilibrium of water and cornstarch. [Pg.960]

Investigations of the state of carbonate equilibrium of water which is transiting the vadose zone have not been numerous. The equilibrium COj (carbon dioxide partial pressure) and state of saturation with respect to calcite was studied by Holland et al. (1964) in Indian Echo Cave, Pennsylvania, and Luray Caverns, Virginia, and by Thrailkill (1971) in Carlsbad Caverns, New Mexico. These investigations showed that seepage water entering the cave was in equilibrium with a f cO2 much higher than that of the normal atmosphere and was often supersaturated with respect to calcite. [Pg.196]

TABLE 4.1. Solution for Equilibrium of Water-Gas Shift Reaction... [Pg.43]

TABLE 4.4. Equilibrium of Water-Gas Shift Reaction at 500 K and 1 atm (a) Eeed with Reactants Only, (b) Eeed with Reactants and Products... [Pg.51]

Thus the change of the concentration of free base of one order of magnitude will produce an increase of potential of 59 millivolts at 25°, i.e., the increase of base concentration from 1CH to 10 mol per liter will produce the same effect on the potential as the change from 10-3 to lO2 mol per liter. A plot of E against the volume of added base will be very closely of the form given in Fig. 2 (o). A more adequate discussion of the theory of the acid-base titration, including the ionization equilibrium of water, is given later in this chapter. [Pg.303]

Figure 7.6 (A) An illustration of the dynamic equilibrium of water molecules at the hydration layer of a protein, with bound (1), quasi-free (2) and free water molecules (3). Figure 7.6 (A) An illustration of the dynamic equilibrium of water molecules at the hydration layer of a protein, with bound (1), quasi-free (2) and free water molecules (3).
The cover picture is derived artistically from the potential-energy profile for the dynamic equilibrium of water molecules in the hydration layer of a protein see A. Douhal s chapter in volume 1) and the three-dimensional vibrational wavefunctions for reactants, transition state, and products in a hydride-transfer reaction (see the chapter by S.J. Benkovic and S. Hammes-Schiffer in volume 4). [Pg.1568]

The dissociation equilibrium of water is characterized by the dissociation constant ... [Pg.24]

Heats of chemisorption of oxygen have been measured on palladium black and on palladium-silver alloys, in the temperature range 500-700° K, and fraction of surface coverages, 0, 1 X 10" to 0.7. Heat of chemisorption data were obtained by means of measurements of reaction equilibrium of water decomposition on palladium and palladium-silver alloys. For palladium blaek, a value of the adsorption heat of —24 kcal. /mole oxide was obtained. This value is not much different from the value corresponding to the formation of bulk palladium oxide (PdO). [Pg.424]

The pH of solid dosage form and API is measured directly in administered solutions or after material is dissolved. The pH of an API is measured after the compound is dissolved completely in a portion of water, and the sample is allowed to come to the same temperature as that of the calibration buffers. If API does not dissolve in water, the compound cannot react with the water molecules creating a new equilibrium of water and hydronium ions. Even small amounts of polar organic solvents alter the true pH measurement. [Pg.213]

Figure 13 Phase equilibrium of water and COj at 50 °C (from compilation of [42 and references therein). Figure 13 Phase equilibrium of water and COj at 50 °C (from compilation of [42 and references therein).
The reviewed ion equilibrium of water solutions are a model, which allows deriving most close to reality idea of atom interaction in the composition of ground water. The presented data, as a rule, are based on not exactly reliable data both of analytical composition and of equilibrium constants. [Pg.130]


See other pages where Equilibrium of water is mentioned: [Pg.450]    [Pg.1297]    [Pg.688]    [Pg.396]    [Pg.395]    [Pg.231]    [Pg.419]    [Pg.91]    [Pg.20]    [Pg.31]    [Pg.59]    [Pg.1432]    [Pg.170]    [Pg.30]    [Pg.425]    [Pg.298]    [Pg.91]    [Pg.105]    [Pg.182]   
See also in sourсe #XX -- [ Pg.513 , Pg.514 ]




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Equilibrium water

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