Boiling-point elevation



Boiling-point elevation describes the phenomenon that the solution has a higher boiling point than a pure solvent. This happens whenever a solute is added to a pure solvent, such as water.


Explanation

 

The boiling point elevation is a chemical potential of the solvent. In both cases, the explanation depends on the fact that many solutes are only present in the liquid phase and do not enter into the gas phase (except at extremely high temperatures).

Put in vapor pressure terms, a liquid boils at the temperature when its vapor pressure equals the surrounding pressure. For the solvent, the presence of the solute decreases its vapor pressure by dilution. A non-volatile solute has a vapor pressure of zero, so the vapor pressure of the solution is the same as the vapor pressure of the solvent. Thus, a higher temperature is needed for the vapor pressure to reach the surrounding pressure, and the boiling point is elevated.

Put in chemical potential terms, at the boiling point, the liquid phase and the gas (or vapor) phase have the same chemical potential (or vapor pressure) meaning that they are energetically equivalent. The chemical potential is dependent on the temperature, and at other temperatures either the liquid or the gas phase has a lower chemical potential and is more energetically favourable than the other phase. This means that when a non-volatile solute is added, the chemical potential of the solvent in the liquid phase is decreased by dilution, but the chemical potential of the solvent in the gas phase is not affected. This means in turn that the equilibrium between the liquid and gas phase is established at another temperature for a solution than a pure liquid, i.e., the boiling point is elevated.[1]

The phenomenon of freezing-point depression is analgous to boiling point elevation. However, the magnitude of the freezing point depression is larger than the boiling point elevation for the same solvent and the same concentration of a solute. Because of these two phenomena, the liquid range of a solvent is increased in the presence of a solute.

Calculations

The extent of boiling-point elevation can be calculated by applying molal concentration of the solution according to the equation:[1]

ΔTb = Kb · mB

where

  • ΔTb, the boiling point elevation, is defined as Tb (solution) - Tb (pure solvent).
  • Kb, the ebullioscopic constant, which is dependent on the properties of the solvent. It depends on can be calculated as Kb = RTb2M/ΔHv, where R is the heat of vaporization per mole of the solvent.
  • mB is the molality of the solution, calculated by taking dissociation into account since the boiling point elevation is a colligative property, dependent on the number of particles in solution. This is most easily done by using the van 't Hoff factor i as mB = msolute · i. The factor i accounts for the number of individual particles (typically ions) formed by a compound in solution. Examples:
    • i = 1 for sugar in water
    • i = 2 for sodium chloride in water, due to the full dissociation of NaCl into Na+ and Cl-
    • i = 3 for calcium chloride in water, due to dissociation of CaCl2 into Ca2+ and Cl-

At high concentrations, the above formula is less precise due to phase diagram of the mixture.

Ebullioscopic constants

Values of the ebullioscopic constants KB for selected solvents:[2]

Compound Boiling point in °C Ebullioscopic constant KB in units of (K · kg) / mol
Acetic acid 118.1 3.07
Benzene 80.1 2.53
Carbon disulfide 46.2 2.37
Carbon tetrachloride 76.8 4.95
Naphthalene 217.9 5.8
Phenol 181.75 3.04
Water 100 0.51

Uses

Together with the formula above, the boiling-point elevation can in principle be used to measure the degree of dissociation or the cryoscopy.

A common mis-attribution of the use of boiling-point elevation is adding salt when cooking foods to elevate the temperature of the water before it boils. However, the temperature increase caused by the amounts of salt added when cooking is generally not enough to raise the temperature by a single degree, as a comparison, seawater has a boiling point of 100.6°C. The salt is added simply to season the food and prevent pasta from sticking.[citation needed]

See also

References

  1. ^ a b c P. W. Atkins, Physical Chemistry, 4th Ed., Oxford University Press, Oxford, 1994, ISBN 0-19-269042-6, p. 222-225
  2. ^ P. W. Atkins, Physical Chemistry, 4th Ed., p. C17 (Table 7.2)
 
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