When a solute is introduced to a system containing two immiscible liquids, it distributes itself between the two solvents. This distribution reaches a dynamic equilibrium, where the rate at which the solute moves from the first solvent to the second equals the rate at which it moves from the second to the first.
Consider two immiscible liquids, such as ether (less dense, forms the upper layer) and water. If a solute that dissolves in both liquids is added to this system and shaken vigorously, the solute will distribute itself between the two phases. At equilibrium, the concentration of solute in each layer becomes constant.
The distribution of solute between water and ether can be represented by the following equilibrium:
The equilibrium constant for this distribution is known as the partition coefficient and is denoted by or . It is defined as the ratio of the concentration of the solute in the organic (ether) layer to its concentration in the aqueous (water) layer.
The concept governing the distribution of a solute between two immiscible solvents is known as the distribution law or Nernst distribution law. This law states that at a constant temperature, a solute distributes itself between two immiscible solvents in contact with each other in such a way that the ratio of its concentrations in the two solvents is constant, provided the solute is in the same molecular state in both solvents.
The partition coefficient () is therefore defined as: The ratio of the concentrations of a solute in two different immiscible solvents in contact with each other when equilibrium has been established at a particular temperature.
Since the partition coefficient is a ratio of two concentrations (e.g., ), it is a dimensionless quantity and thus has no units. Its value is constant at a constant temperature.
The partition coefficient can be calculated using the equilibrium expression when the solute exists in the same physical state in both solvents. This principle is widely used in solvent extraction, a technique often used to separate organic products from aqueous reaction mixtures.
Procedure:
Calculations:
of a solution of aqueous methylamine () is shaken with of an organic solvent. After equilibrium, of the aqueous layer is run off and titrated against . of was used.
Data for calculations:
Goal: Calculate the partition coefficient of methylamine in the organic solvent and water.
Solution:
Step 1: Write down the equilibrium equation.
Step 2: Write down the expression.
Step 3: Determine the total moles of methylamine in the original solution.
Given Values:
Apply Formula: Moles () = Concentration () Volume ()
Calculation:
Step 4: Determine the number of moles of methylamine in the aqueous layer after equilibrium.
The reaction during titration is: The stoichiometry is of reacts with of .
Step 5: Determine the number of moles of present in the organic layer.
Step 6: Change the number of moles into concentrations.
Step 7: Substitute the values into the expression.
Since the value of is larger than 1, methylamine is more soluble in the organic solvent than in water.
The partition coefficient () quantifies how a solute distributes between two immiscible phases. Several factors can influence its numerical value:
The Polarity of the Solute:
The Solvent Polarity:
Temperature:
Molecular Structure and Size:
Partition coefficients are crucial in various chemical and biological processes, including: