Clausius-Clapeyron equation oor Spaans
Clausius-Clapeyron equation
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The Clausius–Clapeyron Equation 39.
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Now we can follow the procedure used in Appendix A-4 to derive the Clausius–Clapeyron equation.
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The isosteric heat of sorption (Qst) was determined by the Clausius-Clapeyron equation.
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Now we need to solve the Clausius–Clapeyron equation for the saturation vapor pressure P 0.
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The temperature dependence of the vapour pressure is described by the Clausius-Clapeyron equation
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Equation (7.19) is called the Clausius–Clapeyron equation in most physical chemistry texts.
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Use the Clausius–Clapeyron equation to find the saturation vapor pressure for temperatures in this range.
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Develop a Hand Example The Clausius–Clapeyron equation requires that all the variables have consistent units.
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The isosteric heat of adsorption (Qst) was determined using the Clausius-Clapeyron equation.
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The isosteric heat of adsorption (Qst) was determined by the Clausius-Clapeyron equation.
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From this consideration we were able to derive the Clausius-Clapeyron equation.
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The sorption isosteric heat (Qst) was determined with Clausius-Clapeyron equation.
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At 25°C, it is 44.02 kJ/mol—very close to what is predicted by the Clausius-Clapeyron equation.
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(e) Improved data for determining phase transition, including Henry’s law constants for reactive gaseous mercury species and their temperature dependence using the Clausius-Clapeyron equation;
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If the boiling temperature is not measured at normal atmospheric pressure, the temperature dependence of the vapour pressure can be described by the Clausius-Clapeyron equation
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The isosteric heat of sorption of water was determined using the Clausius-Clapeyron equation from the equilibrium data; isosteric heats of sorption were found to increase with increasing temperature and could be adjusted by an exponential relationship.
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The isosteric heat of sorptionwas computed using the Clausius-Clapeyron equation by means of the GAB model.A decrease in the isosteric heat of sorption was observed when the equilibrium moisture content increase, with a strong moisture effect at values lower than 0.8 kg kg-1 (d.b.).
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In a limited temperature range, the logarithm of the vapour pressure of a pure substance is a linear function of the inverse of the thermodynamic temperature according to the simplified Clapeyron-Clausius equation:
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In a limited temperature range, the logarithm of the vapour pressure of a pure substance is a linear function of the inverse of the thermodynamic temperature according to the simplified Clapeyron-Clausius equation
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The heat of adsorption at a specific degree of surface coverage (loading) can be calculated using the Clausius- Clapeyron equation.
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According to the Clausius-Clapeyron Equation, every 0.5 degrees Celsius of warming means an extra 3% or so of moisture in the air.
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The main scientific proof is a well-established law of physics: the Clausius-Clapeyron equation, which states that a warmer atmosphere contains more moisture.
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Using the Clausius-Clapeyron equation, it is shown that for every half degree Celsius that increases the temperature of the atmosphere, humidity increases by approximately 3%.
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