Clausius - clapeyron equation in particle formation
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The Clausius-Clapeyron equation allows us to estimate the vapor pressure at another temperature, if the vapor pressure is known at some temperature, and if the enthalpy of vaporization is known.
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- The rate at which water vapor is made available for the formation of cloud droplets by a known rate of cooling can be calculated from the Clausius–Clapeyron equation, which relates the saturation vapor pressure to the temperature in degrees Kelvin.
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