Evaporation and boiling
In Leadville, Colorado, about 3,100 m up, air pressure is about 68 kPa and water boils at about 90 °C.
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A puddle dries on a cool day without ever getting near 100 °C. A pot of water on the stove, on the other hand, sits quietly until it starts to bubble at about 100 °C. Both are vaporization, the change from liquid to gas, but they are not the same process. Evaporation happens only at the surface and at any temperature. Boiling happens all through the liquid, at one particular temperature that depends on the pressure above it.
Evaporation and vapour pressure
In any liquid the molecules have a range of speeds. A few at the surface are moving fast enough to break away from their neighbours and escape into the air. That is evaporation. Because the fastest molecules leave first, the ones left behind have a lower average energy, so the liquid cools. Sweat works this way. OpenStax estimates that evaporating 1.5 L of sweat in a hot climate removes about 3,600 kJ of heat from the body.
In a closed bottle, escaping molecules collect above the liquid, and some of them bump back into it. Eventually as many return as leave each second. The pressure of the vapour at that point is the vapour pressure of the liquid. It depends on the substance and the temperature, not on the size of the bottle. Liquids whose molecules attract weakly have high vapour pressures: at 20 °C methanol's is 11.9 kPa and ethanol's is 5.95 kPa. Heat a liquid and more molecules have enough energy to escape, so its vapour pressure rises.
Boiling depends on the air above
A liquid boils when its vapour pressure equals the pressure of the surroundings. Then bubbles of vapour can form inside the liquid without being crushed. The normal boiling point is the boiling point at 1 atm, which is 101.3 kPa. For water that is 100 °C. High in the mountains the air pressure is lower, so water boils at a lower temperature: in Leadville, where the pressure is about 68 kPa, it boils at about 90 °C. A pressure cooker does the opposite. It traps steam, raises the pressure and lets the water get hotter than 100 °C before it boils.
Vaporizing takes a lot of energy, more than melting, because every attraction to neighbouring molecules has to be broken, not only loosened. For water the enthalpy of vaporization is 44.01 kJ/mol at 25 °C and 40.67 kJ/mol at the boiling point. Compare that with 6.01 kJ/mol to melt ice: boiling a mole of water takes almost seven times as much energy as melting it. Condensation, gas to liquid, gives that energy back, which is why a scald from steam is worse than one from water at the same temperature.
Skipping the liquid
Some solids turn straight into gas. This is sublimation. Dry ice, solid carbon dioxide, slowly vanishes at room temperature without leaving a puddle. NIST data show why: carbon dioxide can only be liquid above 5.185 bar, about five times normal air pressure, so at 1 atm it goes straight from solid to gas at about −78 °C. Its enthalpy of sublimation is 26.1 kJ/mol. The reverse change, gas straight to solid, is deposition. Frost on a car window on a cold, clear night grows this way.
- What is the difference between evaporation and boiling?
- Evaporation happens at the surface at any temperature; boiling happens throughout at one temperature
- Evaporation makes a gas, boiling makes a liquid
- There is no difference
- Why does evaporation cool a liquid?
- The fastest molecules leave, lowering the average energy of the rest
- Air is always colder than liquid
- Evaporation releases heat
- A liquid boils when its vapour pressure…
- equals the pressure of the surroundings
- reaches zero
- equals 1 kPa
- Why does water boil below 100 °C high in the mountains?
- The air pressure is lower
- The water is purer
- The Sun is closer
- Which liquid has the higher vapour pressure at 20 °C?
- Methanol (11.9 kPa)
- Ethanol (5.95 kPa)
- They are equal
- How much heat, in kJ, boils away 2.00 mol of water at 100 °C (40.67 kJ/mol)? 2 decimal places.
- Boiling one mole of water at 100 °C takes 40.67 kJ; melting one mole of ice takes 6.01 kJ. How many times more is boiling (1 decimal place)?
- Dry ice disappears without melting. That is…
- sublimation
- deposition
- condensation
- Why is a steam burn worse than a burn from water at the same temperature?
- Steam gives out its heat of vaporization as it condenses on the skin
- Steam is always hotter than 100 °C
- Steam is a plasma
- How does a pressure cooker cook faster?
- Higher pressure raises the boiling point above 100 °C
- It removes all the air so water boils at 0 °C
- It uses less water
- Evaporation: surface, any temperature, cools the liquid.
- Boiling: vapour pressure = outside pressure; 100 °C for water at 101.3 kPa.
- Water: ΔH vaporization 40.67 kJ/mol at 100 °C, about 6.8 times the 6.01 kJ/mol to melt.
- Sublimation: solid to gas (dry ice). Deposition: gas to solid (frost).
Sources for this course (8)
- OpenStax Chemistry 2e (openstax.org/books/chemistry-2e): 1.2 Phases and Classification of Matter (matter, three states, plasma, mass and weight, Moon 1/6, conservation of matter, sand and clouds)
- 9.2 gas laws (Boyle's law P1V1 = P2V2, syringe 15.0 mL 13.0 psi to 7.5 mL 26 psi, breathing, divers: every 33 ft of sea water adds 1 atm and halves the air volume at 33 ft, Amontons ~1700, Gay-Lussac ~1800, Charles, STP 273.15 K and 101.325 kPa, -273 °C absolute zero)
- 9.5 kinetic-molecular theory (average kinetic energy proportional to kelvin temperature, KEavg = 3/2 RT, urms = sqrt(3RT/M), N2 at 30 °C 519 m/s, O2 at -23 °C 441 m/s)
- 10.3 phase transitions (vapor pressure, normal boiling point at 1 atm = 101.3 kPa, Leadville 68 kPa about 90 °C, ΔHvap 44.01 kJ/mol at 25 °C and 40.67 kJ/mol at 100 °C, 1.5 L sweat 3600 kJ, ΔHfus 6.01 kJ/mol, ice at -12 °C staying at 0 °C while melting, CO2 sublimation 26.1 kJ/mol, frost is deposition, heating curve example 135 g ice -15 °C to steam 120 °C = 416 kJ with c ice 2.09, water 4.18, steam 1.86 J/g °C, burner turned up does not raise boiling temperature)
- NIST Chemistry WebBook phase change data (webbook.nist.gov: ethanol Tfus 159 K, Tboil 351.5 K; nitrogen Tfus 63.3 K, Tboil 77.34 K; oxygen Tfus 54.8 K, Tboil 90.2 K; mercury Tfus 234.31 K, Tboil 629.81 K; CO2 triple point 216.58 K at 5.185 bar, solid vapour-pressure equation Giauque and Egan 1937 giving 194.7 K at 1 atm)
- USGS Water Science School, Water Density (0.99987 g/cm³ at 0 °C, 1.00000 at 4 °C, 0.95865 at 100 °C; ice about 9% less dense)
- Britannica, Boyle's law (Robert Boyle 1662, air compressed by mercury; Edme Mariotte 1676)
- Boyle's 1662 table (48 spaces at 29 2/16 in, 12 spaces at 117 9/16 in of mercury) as reprinted in J. Appl. Physiol. 87 (1999) 1543.
Checked: 2026-10-17