The dissolution process involves a solid substance dissolving in a solvent, leading to the formation of ions in solution. It is the key event that sets the stage for establishing an equilibrium between the dissolved ions and undissolved solid.
This process depends on various factors including temperature, pressure, and the nature of the solvent.
Solubility increases when more of the solid is capable of dissolving, contributing to a higher concentration of ions.
- In the dissolution of
AgCl, the solid silver chloride dissociates into silver ions (Ag⁺) and chloride ions (Cl⁻).
- Similarly, dissolving
Mg(OH)₂ will produce magnesium ions (Mg²⁺) and hydroxide ions (OH⁻).
A balance is sought where the rate of dissolution equals the rate of precipitation, yielding a dynamic equilibrium. Understanding this process facilitates the calculation of Ksp values, allowing prediction of solubility under various conditions.