The condensation point of water in Kelvin is 373.15 K. This is the temperature at which water vapor condenses into liquid water at standard atmospheric pressure.
Condensation occurs when water vapor cools down and changes from a gaseous state to a liquid state. The condensation point is the same as the boiling point of water, which is 100°C or 373.15 K. This is because both processes involve the phase change between liquid and gas at the same temperature and pressure conditions.
Understanding the condensation point is important in various scientific and engineering applications, such as meteorology, HVAC systems, and industrial processes where controlling the phase change of water is crucial.