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Gas constant and

Here G is the free energy and AG the change in free energy during the reaction. R the gas constant and T the absolute temperature. [Pg.66]

Activation Parameters. Thermal processes are commonly used to break labile initiator bonds in order to form radicals. The amount of thermal energy necessary varies with the environment, but absolute temperature, T, is usually the dominant factor. The energy barrier, the minimum amount of energy that must be suppHed, is called the activation energy, E. A third important factor, known as the frequency factor, is a measure of bond motion freedom (translational, rotational, and vibrational) in the activated complex or transition state. The relationships of yi, E and T to the initiator decomposition rate (kJ) are expressed by the Arrhenius first-order rate equation (eq. 16) where R is the gas constant, and and E are known as the activation parameters. [Pg.221]

The permeability varies with temperature according to equation 12 where is a constant, E is the activation energy for permeation, E. is the gas constant, and Tis the absolute temperature. [Pg.493]

The Tempered activation energy , is the activation energy divided by R, the gas constant, and is dimensionless. It will be shown here with a superscript T, e.g. 10 000. ... [Pg.46]

Here p is the density, a is the particle size, C and n are constants, Q is the activation energy for sintering, R is the gas constant and T is the absolute temperature, n is typically about 3, and Q is usually equal to the activation energy for grain boundary diffusion. [Pg.196]

For example, in the case of dilute solutions, the van t Hoff s equation may be used to piedict the osmotic pressure (jr = CRT) where n is the osmotic pressure of the solution, C is the molar concentration of the solute, ft is the universal gas constant and T is the absolute temperature, Fm dissociating solutes, the concentration is that of the total ions. For example, NaCI dissociates in water into two ions Na" " and Cl . Therefore, the total molar concentration of ions is hvice the molar concentration of NaCI. A useful rule of thumb for predicting osmotic pressure of aqueous solutions is 0,01 psi/ppm of solute (Weber, 1972). [Pg.265]

This is the state equation of an ideal gas, where p is pressure, v is specific volume, p is density, R is the gas constant, and T is absolute temperature. In an airflow there is a transfer of heat from one layer to another. This change of... [Pg.49]

Here 17 is the apparent viscosity at temperature T, R is the universal gas constant, and A is an empirical constant, called frequency factor for melt flow. The activation energy values for different systems and at different shear rates are summarized in Table 8. It is evident that activation energy for flow increases with filler loading, but it decreases with an increase in shear rate. [Pg.449]

The constant R is called the gas constant and has the same value for all gases because R is independent of the identity of the gas, we say that it is a universal constant. The value of the gas constant can be found by measuring P, V, n, and T and substituting their values into R = PV/nT. When we use SI units (pressure in pascals, volume in meters cubed, temperature in kelvins, and amount in moles),... [Pg.269]

V = equivalent volume of a spherically rotating molecule, R = the gas constant, and T = temperature in Kelvins. [Pg.184]


See other pages where Gas constant and is mentioned: [Pg.78]    [Pg.291]    [Pg.177]    [Pg.8]    [Pg.121]    [Pg.529]    [Pg.530]    [Pg.171]    [Pg.339]    [Pg.47]    [Pg.213]    [Pg.374]    [Pg.445]    [Pg.245]    [Pg.235]    [Pg.331]    [Pg.2292]    [Pg.45]    [Pg.286]    [Pg.286]    [Pg.287]    [Pg.67]    [Pg.158]    [Pg.80]    [Pg.47]    [Pg.504]    [Pg.148]    [Pg.1284]    [Pg.14]    [Pg.14]    [Pg.213]    [Pg.129]    [Pg.966]    [Pg.926]    [Pg.299]    [Pg.31]    [Pg.145]    [Pg.456]    [Pg.388]    [Pg.133]    [Pg.296]   
See also in sourсe #XX -- [ Pg.10 , Pg.98 , Pg.237 , Pg.238 ]




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AS for the Mixing of Ideal Gases at Constant T and

Gas constant

Heat Capacity at Constant Pressure of Inorganic and Organic Compounds in the Ideal Gas State Fit to Hyperbolic Functions Cp

Heat Capacity at Constant Pressure of Inorganic and Organic Compounds in the Ideal Gas State Fit to a Polynomial Cp

IDEAL GAS CONSTANT AND CONVERSION FACTORS

Isotherms of Real Gases and Critical Constants

Solubility as a Function of Temperature and Henrys Constant at 25C for Gases in Water

The Universal Gas Constant and Molecular Weights

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