The amount of solute that dissolves in a solvent is determined by the solute's solubility, which is influenced by factors like temperature, pressure, and the nature of the solute and solvent. You can determine how much solute dissolves by conducting experiments to reach saturation, where no more solute can dissolve. Observing changes, such as the clarity of the solution or the presence of undissolved solute at the bottom, will indicate saturation. Additionally, solubility is often expressed in grams per liter or molarity for specific temperature and pressure conditions.
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