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The Condensation Point of Water in Degrees Fahrenheit

What is the condensation point of water in degrees Fahrenheit under standard atmospheric pressure?

Subject: General Chemistry Chapter: Matter Its Properties and Measurement Topic: Temperature Conversion Answer included
the condensation point of water in degrees fahrenheit condensation point of water boiling point of water in fahrenheit 212 F water liquid vapor equilibrium vapor pressure equals external pressure phase change temperature temperature conversion C to F
Accepted answer Answer included

Condensation point at standard pressure

The condensation point of water in degrees Fahrenheit is 212 °F when the pressure is standard atmospheric pressure (\(1\,\text{atm}\)) and the substance is pure water. The same temperature is also described as the normal boiling point, because liquid–vapor equilibrium is shared by boiling and condensation.

Equilibrium definition. The condensation (or boiling) temperature at a specified pressure satisfies \( P_{\text{vap}}(T) = P_{\text{ext}} \), where \(P_{\text{vap}}\) is the saturation vapor pressure of water and \(P_{\text{ext}}\) is the external pressure.

Temperature conversion to degrees Fahrenheit

The Fahrenheit–Celsius relationship is:

\[ T_F = \frac{9}{5}\,T_C + 32. \]

Under \(1\,\text{atm}\), the condensation temperature for water is \(T_C = 100\,^\circ\text{C}\). Substitution gives:

\[ T_F = \frac{9}{5}\cdot 100 + 32 = 180 + 32 = 212\,^\circ\text{F}. \]

Physical meaning in general chemistry

Condensation converts water vapor to liquid water. At the condensation point, vapor and liquid coexist in equilibrium, so the net rate of condensation equals the net rate of evaporation. The equilibrium temperature depends on pressure because vapor pressure is a strong function of temperature.

Pressure dependence and common interpretations

The value \(212\,^\circ\text{F}\) corresponds specifically to \(1\,\text{atm}\). At lower external pressure (high altitude or vacuum), the condensation/boiling temperature is lower; at higher pressure (pressure cooker), it is higher. Dissolved solutes also shift the phase-change temperature by changing the chemical potential of the liquid, producing boiling-point elevation and freezing-point depression in solution chemistry.

Condensation point and dew point

“Condensation point” for pure water in a phase-equilibrium sense is the liquid–vapor transition temperature at a specified pressure. “Dew point” refers to condensation of water vapor from air and is controlled by the partial pressure of water vapor (humidity), not by total pressure alone. The dew point is commonly far below \(212\,^\circ\text{F}\) because atmospheric water vapor is typically well below saturation at \(100\,^\circ\text{C}\).

Reference temperatures for water

Process Temperature in °C (at 1 atm) Temperature in °F Phase equilibrium
Freezing / melting \(0\,^\circ\text{C}\) \(32\,^\circ\text{F}\) Solid ⇌ liquid
Condensation / boiling \(100\,^\circ\text{C}\) \(212\,^\circ\text{F}\) Liquid ⇌ vapor

Visualization: vapor-pressure curve and the 1 atm condensation point

Saturation vapor pressure of water and the condensation point at 1 atm A rising curve shows water’s saturation vapor pressure increasing with temperature. A horizontal line at 1 atm intersects the curve at 100 °C, labeled as 212 °F. 1 atm Liquid Vapor Intersection at 100 °C Condensing at 212 °F Temperature (schematic, °C) Saturation Vapor Pressure (schematic) 0 100 higher
The condensation point corresponds to the temperature where water’s saturation vapor pressure equals the external pressure. At \(1\,\text{atm}\), this occurs at \(100\,^\circ\text{C}\), which converts to \(212\,^\circ\text{F}\).
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