This MCQ module is based on: First Law Internal Energy
First Law Internal Energy
This assessment will be based on: First Law Internal Energy
Upload images, PDFs, or Word documents to include their content in assessment generation.
First Law of Thermodynamics, Internal Energy and Enthalpy
5.6 The First Law of Thermodynamics
The First Law of Thermodynamics is the law of conservation of energy applied to thermodynamic processes:
Consequence: for an isolated system q = 0 and w = 0, so ΔU = 0 — the energy of an isolated system is constant.
5.7 Work in Expansion / Compression of Gases
Consider a gas confined in a cylinder by a piston of cross-sectional area A. If the gas pushes the piston outward by distance dx against external pressure P_ext, the work done by the gas is P_ext · A · dx = P_ext · dV. By IUPAC convention (work done on the system positive):
\[w = -P_\text{ext}\,\Delta V\]5.7.1 Free Expansion (against vacuum)
If P_ext = 0 (expansion into vacuum), w = 0. No work is done by or on the system.
5.7.2 Reversible Isothermal Expansion of an Ideal Gas
For a reversible expansion at constant T, P_ext = P_gas at every instant. Integrating:
\[w_\text{rev} = -\int_{V_1}^{V_2} P\,dV = -nRT\ln\frac{V_2}{V_1} = -2.303\,nRT\log\frac{V_2}{V_1}\]For an isothermal ideal gas, ΔU = 0 (U depends only on T). Therefore q = −w = +nRT ln(V₂/V₁).
5.7.3 Isobaric Process
If P_ext = P (constant), w = −P·ΔV.
5.7.4 Isochoric Process
ΔV = 0 → w = 0 → ΔU = q_v (the entire heat raises U).
5.8 Enthalpy (H) — A Useful State Function
Most laboratory chemistry happens in open vessels at constant atmospheric pressure, not constant volume. For such conditions, internal energy isn't directly the most useful quantity. We define a new state function called enthalpy:
Derivation (constant P): ΔU = q_p + w = q_p − PΔV ⇒ q_p = ΔU + PΔV. But ΔH = Δ(U + PV) = ΔU + Δ(PV) = ΔU + PΔV (since P is constant). Therefore q_p = ΔH. ✓
5.8.1 Relationship between ΔH and ΔU
For reactions involving gases, the change in moles of gaseous species (Δn_g) matters:
\[\Delta H = \Delta U + \Delta n_g RT\]where Δn_g = (moles of gaseous products) − (moles of gaseous reactants), and R = 8.314 J K⁻¹ mol⁻¹.
| Reaction type | Δn_g | Relation |
|---|---|---|
| No gas, only solids/liquids | 0 | ΔH = ΔU |
| Same number of gas moles on both sides | 0 | ΔH = ΔU |
| More gas moles produced (e.g., CaCO₃ → CaO + CO₂) | +ve | ΔH > ΔU |
| Fewer gas moles produced (e.g., 2H₂ + O₂ → 2H₂O(l)) | −ve | ΔH < ΔU |
5.8.2 Exothermic vs Endothermic Reactions
An exothermic reaction releases heat: ΔH < 0. An endothermic reaction absorbs heat: ΔH > 0.
5.9 Extensive vs Intensive Properties
| Type | Depends on amount? | Examples |
|---|---|---|
| Extensive | Yes (proportional to size) | U, H, V, mass, n, heat capacity (C) |
| Intensive | No (independent of size) | P, T, density, molar volume, specific heat (c) |
🎯 Interactive: ΔH ↔ ΔU Converter
Convert between ΔU and ΔH using ΔH = ΔU + Δn_g RT. Adjust the temperature and Δn_g to see the conversion live.
ΔH = ΔU + Δn_g RT = −100.00 kJ
No change in moles of gas → ΔH = ΔU.
Setup: Place 10 g of solid Ba(OH)₂·8H₂O and 5 g of solid NH₄SCN in a small plastic bag. Seal it and shake. Place it on a wet wooden block.
The reaction Ba(OH)₂·8H₂O + 2NH₄SCN → Ba(SCN)₂ + 2NH₃ + 10 H₂O is strongly endothermic (ΔH ≈ +60 kJ/mol).
The bag becomes ICY COLD (~−20 °C). Water on the wooden block freezes solid, gluing the block to the bag — you can lift the block by the bag!
Why? Heat needed for reaction is drawn from surroundings, lowering their temperature. This proves that endothermic reactions absorb heat from the environment.
Worked Example 5.3: Reversible Isothermal Expansion
2 moles of an ideal gas expand isothermally and reversibly at 300 K from 5 L to 50 L. Calculate q, w, ΔU and ΔH. (R = 8.314 J K⁻¹ mol⁻¹)
w_rev = −2.303 × nRT × log(V₂/V₁) = −2.303 × 2 × 8.314 × 300 × log(50/5) = −2.303 × 4988.4 × 1 = −11489 J ≈ −11.49 kJ.
q = ΔU − w = 0 − (−11489) = +11489 J ≈ +11.49 kJ.
The gas absorbs 11.49 kJ from the surroundings and uses it entirely to do 11.49 kJ of expansion work.
Worked Example 5.4: ΔH from ΔU
For the reaction C(graphite) + ½ O₂(g) → CO(g), ΔU = −110.5 kJ at 300 K. Calculate ΔH. (R = 8.314 × 10⁻³ kJ K⁻¹ mol⁻¹)
ΔH = ΔU + Δn_g RT = (−110.5) + (0.5)(8.314 × 10⁻³)(300)
= −110.5 + 1.247 = −109.25 kJ.
Slightly less negative than ΔU because more moles of gas means PV-work is done on the surroundings.
🎯 Competency-Based Questions
Q1. The mathematical statement of the first law of thermodynamics for a closed system is: L1 Remember
Q2. For which of the following processes is q_p = ΔH valid? L2 Understand
Q3. For the reaction 2H₂(g) + O₂(g) → 2H₂O(l), what is Δn_g and how does ΔH compare with ΔU? L3 Apply
ΔH = ΔU + Δn_g RT = ΔU − 3RT, so ΔH is MORE NEGATIVE than ΔU. The system loses extra energy to the atmosphere as the surroundings push in (compression work received reduces |ΔU| but heat released exceeds it).
Q4. Fill in the blank: For free expansion of an ideal gas into vacuum, w = ____ and q = ____. L3 Apply
Q5. HOT (Analyse): The combustion of glucose in a bomb calorimeter gives q_v = −2802 kJ/mol at 298 K. Calculate ΔH for the reaction C₆H₁₂O₆(s) + 6O₂(g) → 6CO₂(g) + 6H₂O(l). L4 Analyse
Δn_g = 6 (CO₂ products) − 6 (O₂ reactants) = 0.
So ΔH = ΔU + 0 = −2802 kJ/mol.
This is the energy your body extracts per mole of glucose (~180 g) you metabolise — the basis of calorie counting in nutrition.
🧠 Assertion–Reason Questions
Choose: (A) Both true, R explains A. (B) Both true, R doesn't explain A. (C) A true, R false. (D) A false, R true.
A: For an isothermal expansion of an ideal gas, q = −w.
R: Internal energy of an ideal gas depends only on temperature.
A: Enthalpy is more useful than internal energy for chemists working at atmospheric pressure.
R: The change in enthalpy at constant pressure equals the heat exchanged.
A: ΔH = ΔU + Δn_g RT applies to all reactions.
R: Only gaseous species contribute appreciably to PΔV at moderate temperatures.