To determine the total entropy change for the process of ice at \( -5^\circ C \) heating to vapor at \( 110^\circ C \) under atmospheric pressure, we must consider the phase changes and temperature changes involved. Here's a step-by-step breakdown:
- Heating Ice from \( -5^\circ C \) to \( 0^\circ C \):
The heat capacity (\(C_{p,m}\)) is used to calculate the entropy change during temperature changes.
\(\Delta S_1 = \int_{268 \, \text{K}}^{273 \, \text{K}} \frac{C_{p,m}}{T} \, dT\) - Melting of Ice at \( 0^\circ C \):
The change of phase from solid to liquid involves latent heat of fusion (\(\Delta H_m \, \text{fusion}\)).
\(\Delta S_2 = \frac{\Delta H_m \, \text{fusion}}{T_f}\) where \(T_f = 273 \, \text{K}\) - Heating Water from \( 0^\circ C \) to \( 100^\circ C \):
Entropy change for the water as it is heated to boiling point.
\(\Delta S_3 = \int_{273 \, \text{K}}^{373 \, \text{K}} \frac{C_{p,m}}{T} \, dT\) - Vaporization of Water at \( 100^\circ C \):
Latent heat of vaporization (\(\Delta H_m \, \text{vaporisation}\)) is involved for liquid changing to gas.
\(\Delta S_4 = \frac{\Delta H_m \, \text{vaporisation}}{T_b}\) where \(T_b = 373 \, \text{K}\) - Heating Vapor from \( 100^\circ C \) to \( 110^\circ C \):
Further heating after vaporization.
\(\Delta S_5 = \int_{373 \, \text{K}}^{383 \, \text{K}} \frac{C_{p,m}}{T} \, dT\)
The total entropy change (\(\Delta S_{\text{total}}\)) for the entire process is the sum of all individual changes:
\(\Delta S_{\text{total}} = \Delta S_1 + \Delta S_2 + \Delta S_3 + \Delta S_4 + \Delta S_5\)
Among the given options, the correct formulation for entropy change, considering phase transitions at their respective temperatures, is:
\(\Delta S_{\text{process}} = \int_{268 \, \text{K}}^{273 \, \text{K}} \frac{C_{p,m}}{T} \, dT + \frac{\Delta H_m \, \text{fusion}}{T_f} + \frac{\Delta H_m \, \text{vaporisation}}{T_b}\)