Part of PC-04 — Chemical Thermodynamics

Reasoning Chain: Deriving $\Delta H = \Delta U + \Delta n_g RT$

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Premise 1: Definition of Enthalpy

H=U+PVH = U + PV This is the definition. Enthalpy is defined to be convenient for constant-pressure processes.

Premise 2: Change in Enthalpy

For a process at any conditions: ΔH=ΔU+Δ(PV)\Delta H = \Delta U + \Delta(PV) This follows directly from differentiating the definition.

Premise 3: Ideal Gas Law

For ideal gases: PV=nRTPV = nRT

Therefore: Δ(PV)=Δ(nRT)=RTΔng\Delta(PV) = \Delta(nRT) = RT\,\Delta n_g (at constant temperature TT)

Here Δng\Delta n_g represents the CHANGE in the number of moles of gas.

Premise 4: Substitution

ΔH=ΔU+Δ(PV)=ΔU+ΔngRT\Delta H = \Delta U + \Delta(PV) = \Delta U + \Delta n_g RT

Conclusion

ΔH=ΔU+ΔngRT\boxed{\Delta H = \Delta U + \Delta n_g RT}

Why Only Gaseous Moles?

Solids and liquids have negligible PV compared to gases:

  • 1 mol gas at 298 K, 1 atm: PV=RT=2479 JPV = RT = 2479\ \text{J}
  • 1 mol liquid water: PV=18 cm3×105 Pa=1.8 JPV = 18\ \text{cm}^3 \times 10^5\ \text{Pa} = 1.8\ \text{J} (1000× smaller)

Therefore, only gaseous moles contribute significantly to Δ(PV)\Delta(PV).

Practical Check

For CaCO3CaCO_{3}(s) → CaO(s) + CO2CO_{2}(g): Δng=1\Delta n_g = 1 ΔH=ΔU+1×8.314×103 kJ/(mol⋅K)×T\Delta H = \Delta U + 1 \times 8.314 \times 10^{-3}\ \text{kJ/(mol·K)} \times T

At 298 K: ΔHΔU=2.48\Delta H - \Delta U = 2.48 kJ/mol (small but measurable). At 500 K: ΔHΔU=4.16\Delta H - \Delta U = 4.16 kJ/mol.

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