The dissolution process is how a solute is incorporated into a solvent, leading to the formation of a solution. This process can be explained in a few simple steps:
- The solute particles are surrounded by solvent molecules.
- These solvent molecules interact with the solute particles, breaking them apart and distributing them uniformly throughout the solvent.
- The result is a homogeneous solution where the solute is evenly spread.
The rate of dissolution can depend on several variables, including temperature and agitation. Stirring the mixture can speed up dissolution by bringing more solvent particles into contact with the solute. Meanwhile, increasing temperature generally increases the solubility of the solute, as the added heat enhances particle movement, helping the solute disperse more swiftly.