The van't Hoff factor, often represented as \( i \), is a measure used to account for the effect of solute particles on colligative properties such as osmotic pressure, boiling point elevation, and freezing point depression. It is particularly useful for solutions containing ionic compounds, which dissociate in water to produce multiple ions. Here are some key points about the van't Hoff factor:
- For a completely dissociated ionic compound like \( \text{CaCl}_2 \), which ideally dissociates into three ions (one \( \text{Ca}^{2+} \) and two \( \text{Cl}^- \) ions), the theoretical van't Hoff factor would be 3.
- In practice, the van't Hoff factor may differ from the theoretical value due to ion interactions and other real-world factors. For example, in this exercise, \( i \) is calculated to be 0.92, lower than the ideal value of 3.
- The experimental van't Hoff factor is determined by comparing the experimental osmotic pressure with the theoretical osmotic pressure calculated assuming ideal dissociation.
Understanding \( i \) helps explain discrepancies between expected and observed colligative properties.