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In chemistry and biochemistry, the acidity constant or acid dissocation constant (<math>K_a<math>) is a specific type of dissociation constant that indicates the extent of dissociation of hydrogen ions from an acid. An acid with an acidity constant near 1 is almost completely dissociated when dissolved in water; conversely, an acid with an acidity constant near 0 remains almost completely undissociated. In lay terms, the higher the <math>K_a<math>, the stronger the acid in question.
Because this number varies over many degrees of magnitude, the acidity constant is often represented by the inverse of its common logarithm, represented by <math>pK_a<math>. (cf. pH).
Given a weak acid HA, its dissolution into water is subject to the following equilibrium:
This is often written as:
The species A– is referred to as the conjugate base of the acid. The acidity constant for the acid HA is the dissociation constant for this equilibrium. Thus:
where [X] denotes the molar concentration of X in the solution.
By analogy, one can define the basicity constant (<math>K_b<math>, and similarly <math>pK_b<math>) of the conjugate base A–:
For the equilibrium:
Analogously to <math>K_a<math>, the magnitude of <math>K_b<math> indicates the relative strength of the base, with <math>K_b<math> closer to 1 indicating a much stronger base.
The relation between Ka and Kb is:
where Kw is the dissociation constant of water, which is 1.0x10-14 mol2 dm-6at 20 °C.
As the product of Ka and Kb must remain a constant, it follows that stronger acids will have weaker conjugate bases, and vice versa.