Vapor pressure (also known as equilibrium vapor pressure), is the pressure of a vapor in equilibrium with its liquid or solid phase. At any given temperature, for a specific substance, there is a pressure at which the gas of that specific substance is in equilibrium with its liquid or solid forms — i.e., when the rates at which molecules escape from and return into the vaporizing liquid or solid are equal. This is the vapor pressure of the specific substance at that temperature.
The vapor pressure of a substance increases with increasing temperature.
Volatility of liquids
The vapor pressure is an indication of a liquid's evaporation rate. It relates to the tendency of molecules and atoms to escape from a liquid or a solid. A substance with a high vapor pressure at normal temperatures is often referred to as volatile.
Relative volatility is a measure that compares the vapor pressures of the components in a liquid mixture of chemicals. This measure is widely used in designing large industrial distillation, absorption and other separation processes that involve the contacting of vapor and liquid phases in a series of equilibrium stages. In effect, it indicates the ease or difficulty of separating the more volatile components from the less volatile components in a liquid mixture.
Calculating vapor pressures with Antoine equation
and it can be transformed into this temperature-explicit form:
where: is the absolute vapor pressure of a substance
- is the temperature of the substance
- , and are substance-specific coefficients (i.e., constants or parameters)
- is typically either or
A simpler form of the equation with only two coefficients is sometimes used:
which can be transformed to:
Sublimations and vaporizations of the same substance have separate sets of Antoine coefficients, as do components in mixtures. The Antoine equation is accurate to a few percent for most volatile substances (with vapor pressures over 10 Torr).
Vapor pressures and normal boiling points of liquids
The atmospheric pressure boiling point of a liquid (also known as the normal boiling point) is the temperature where the vapor pressure equals the ambient atmospheric pressure. With any incremental increase in that temperature, the vapor pressure becomes sufficient to overcome atmospheric pressure and lift the liquid to form bubbles inside the bulk of the substance. Bubble formation deeper in the liquid requires a higher pressure, and therefore higher temperature, because the fluid pressure becomes higher than atmospheric pressure as the depth increases.
The higher the vapor pressure of a liquid at a given temperature, the lower the normal boiling point (i.e., the boiling point at atmospheric pressure) of the liquid.
The vapor pressure chart to the right has graphs of the vapor pressures versus temperatures for a variety of liquids. As can be seen in the chart, the liquids with the highest vapor pressures have the lowest normal boiling points.
For example, at any given temperature, methyl chloride has the highest vapor pressure of any of the liquids in the chart. It also has the lowest normal boiling point (– 26 °C), which is where the vapor pressure curve of methyl chloride (the blue line) intersects the horizontal pressure line of one atmosphere (atm) of absolute vapor pressure.
As another example, butane has a vapor pressure of 1 atmosphere at about 0 degrees Celsius. As a result, at sea level the temperature must be higher than this in order for a butane lighter to function, since the pressure of the butane vapor must be above 1 atmosphere in order for the vapor to escape from its container into the surrounding air.
Although the relation between vapor pressure and temperature is non-linear, the chart uses a logarithmic vertical axis in order to obtain slightly curved lines so that one chart can graph many liquids.
Units of vapor pressure
per square inch
per square centimeter
|1 Pa||≡ 1 N/m2||10−5||9.8692×10−6||7.5006×10−3||145.04×10−6||1.01972×10−5|
|1 bar||100,000||≡ 106 dyn/cm2||0.98692||750.06||14.504||1.01972|
|1 atm||101,325||1.01325||≡ 1 atm||760||14.696||1.03323|
|1 torr||133.322||1.3332×10−3||1.3158×10−3||≡ 1 torr
≈ 1 mmHg
|1 psi||6,894.76||68.948×10−3||68.046×10−3||51.715||≡ 1 lbf/in2||7.03059×10−2|
|1 kgf/cm2||98,066.5||0.980665||0.967838||735.5576||14.22357||≡ 1 kgf/cm2|
Example reading: 1 Pa = 1 N/m2 = 10−5 bar = 9.8692×10−6 atm = 7.5006×10−3 torr, etc.
Note: mmHg is an abbreviation for millimetre of mercury
About the torr: There is no consensus in the technical literature about whether the name of the torr should be "Torr" or "torr". Nor is there any consensus about whether the symbol for that unit of pressure should be "Torr" or "torr". Both the United Kingdom's National Physical Laboratory (see Pressure Units) and New Zealand's Measurement Standards Laboratory (see Barometric Pressure Units) use "torr" as the name and as the symbol. An extensive search of the website of the U.S. National Institute of Standards and Technology found no such clear-cut definitions. Therefore, this table uses "torr" as both the name and the symbol.
Vapor pressure of liquid mixtures
Raoult's law gives an approximation to the vapor pressure of mixtures of liquids. It states that the vapor pressure of a liquid mixture is equal to the mole-fraction-weighted sum of the vapor pressures of the mixture's pure components:
where p tot is the mixture's vapor pressure, i is one of the components of the mixture and Χi is the mole fraction of that component in the liquid mixture. The term piΧi is the partial pressure of component i in the mixture.
Systems that have vapor pressures higher than indicated by the above equation are said to have positive deviations. Such a deviation suggests weaker intermolecular attraction than in the pure components, so that the molecules can be thought of as being "held in" the liquid phase less strongly than in the pure liquid. An example is the azeotrope of approximately 95% ethanol and water. Because the azeotrope's vapor pressure is higher than predicted by Raoult's law, it boils at a temperature below that of either pure component.
There are also systems with negative deviations that have vapor pressures that are lower than expected. Such a deviation is evidence for stronger intermolecular attraction between the constituents of the mixture than exists in the pure components. Thus, the molecules are "held in" the liquid more strongly when a second molecule is present. An example is a mixture of trichloromethane (chloroform) and 2-propanone (acetone), which boils above the boiling point of either pure component.
Vapor pressure of solids
All solid materials have a vapor pressure which, for most solids, is very low. Some notable exceptions are naphthalene, ice and dry ice (carbon dioxide). The vapor pressure of dry ice is 5.73 MPa (56.5 atm) at 20 °C which would cause most sealed containers to rupture.
Due to their often extremely low values, measurement of the vapor pressure of solids can be rather difficult. Typical techniques for such measurements include the use of thermogravimetry and gas transpiration.
The vapor pressure of a solid can be defined as the pressure at which the rate of sublimation of a solid matches the rate of deposition of its vapor phase.
There are a number of methods for calculating the sublimation pressure (i.e., the vapor pressure) of a solid. One method is to estimate the sublimation pressure from extrapolated liquid vapor pressures (of the supercooled liquid), if the heat of fusion is known, by using this particular form of the Clausius–Clapeyron relation:
where: = Sublimation pressure of the solid component at the temperature = Extrapolated vapor pressure of the liquid component at the temperature = Heat of fusion = Universal gas constant = Sublimation temperature = Melting point temperature
This method assumes that the heat of fusion is temperature-independent, ignores additional transition temperatures between different solid phases, and it gives a fair estimation for temperatures not too far from the melting point. It also shows that the sublimation pressure is lower than the extrapolated liquid vapor pressure (ΔHm is positive) and the difference grows with increased distance from the melting point.
The ratio, often expressed as a percentage, of the partial pressure of water in the atmosphere at some observed temperature, to the vapor pressure of pure water at this temperature. It may be expressed as:
|= percent relative humidity of the atmospheric air-water mixture|
|= partial pressure of water in the atmospheric air-water mixture|
|= vapor pressure of pure water at the temperature of the atmospheric air-water mixture|
At 100 percent relative humidity, the atmospheric air is said to be saturated with water. That occurs when the partial pressure of the water in the air, , is equal to the vapor pressure of pure water at the air temperature, .
Given the wet-bulb temperature and the dry-bulb temperature of the atmosphere, which are readily measured by using a sling psychrometer, the relative humidity can be obtained from a psychrometric chart.
Vapor pressure terminology in meteorology
The terminology defined and discussed in this article is the terminology used extensively by chemists, chemical engineers and others.
The terminology used by workers in the field of meteorology is unique to that field of science and it defines vapor pressure and similar terms quite a bit differently than is done in this article. For example, the American Meteorological Society (AMS) uses the following definitions:
- Vapor pressure: The portion of the total air pressure exerted by the water vapor component of air. (That would be the partial pressure of the water vapor in the air using the terminology defined in this article.)
- Saturation vapor pressure: The maximum vapor pressure in a sample of air at a specific temperature. (That is not the meaning of "saturation vapor pressure" as defined in this article. In the terminology defined in this article, it can be said that air at a specific temperature is saturated when the partial pressure of the water in the air is equal to the vapor pressure of pure water at that specific temperature. In other words, when relative humidity is 100%.)
To avoid any confusion, this article makes no attempt to go into any further detail concerning the terminology used in meteorology.
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