In colligative property measurements, the freezing point changes by approximately how many degrees Celsius per osmole increase of solute?

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Multiple Choice

In colligative property measurements, the freezing point changes by approximately how many degrees Celsius per osmole increase of solute?

Explanation:
In colligative properties, how much the freezing point changes depends on how many dissolved particles are present, not on their identity. The freezing point depression is given by ΔTf = i Kf m. For water, Kf is about 1.86 °C·kg/mol. So, for one osmole of solute in 1 kg of solvent (m ≈ 1) and with an ideal solute (i ≈ 1), the freezing point decreases by roughly 1.86 °C. If the solute dissociates, the effective number of particles (i) increases, making the depression larger accordingly. The other options refer to different colligative properties: vapor pressure changes, boiling point elevation (≈0.52 °C per osmole), or osmotic pressure, none of which describe the freezing-point change per osmole.

In colligative properties, how much the freezing point changes depends on how many dissolved particles are present, not on their identity. The freezing point depression is given by ΔTf = i Kf m. For water, Kf is about 1.86 °C·kg/mol. So, for one osmole of solute in 1 kg of solvent (m ≈ 1) and with an ideal solute (i ≈ 1), the freezing point decreases by roughly 1.86 °C. If the solute dissociates, the effective number of particles (i) increases, making the depression larger accordingly. The other options refer to different colligative properties: vapor pressure changes, boiling point elevation (≈0.52 °C per osmole), or osmotic pressure, none of which describe the freezing-point change per osmole.

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