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Differential vapor-pressure, degree

Numerous mathematical formulas relating the temperature and pressure of the gas phase in equilibrium with the condensed phase have been proposed. The Antoine equation (Eq. 1) gives good correlation with experimental values. Equation 2 is simpler and is often suitable over restricted temperature ranges. In these equations, and the derived differential coefficients for use in the Hag-genmacher and Clausius-Clapeyron equations, the p term is the vapor pressure of the compound in pounds per square inch (psi), the t term is the temperature in degrees Celsius, and the T term is the absolute temperature in kelvins (r°C -I- 273.15). [Pg.389]

The samples prepared by this chlorosilane route are characterized by high degrees of molecular and compositional homogeneities, as was confirmed by the exhaustive characterization data provided by SEC, membrane osmometry, low angle laser light scattering, differential refractometry, vapor pressure osmometry, UV-SEC, and NMR. The most important feature of the method is that every step of the reaction is monitored by taking small aliquots from the reaction mixture. [Pg.82]


See other pages where Differential vapor-pressure, degree is mentioned: [Pg.355]    [Pg.223]    [Pg.171]    [Pg.6]    [Pg.223]    [Pg.1733]    [Pg.4112]    [Pg.278]    [Pg.95]    [Pg.223]    [Pg.401]    [Pg.155]    [Pg.453]    [Pg.415]    [Pg.180]    [Pg.415]    [Pg.286]    [Pg.180]    [Pg.1043]    [Pg.984]    [Pg.286]    [Pg.620]    [Pg.122]    [Pg.872]    [Pg.57]   


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Differential vapor pressure

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