Chemical Thermodynamics
Systems, First Law, PV Work, Enthalpy, Calorimetry, Hess's Law, Born-Haber Cycle, Entropy & Gibbs Energy
Topic 5.1 & 5.2.2(b): Thermodynamic Systems, State vs Path Functions, Extensive vs Intensive & Internal Energy (U)
Picture three cups of hot Sulaimani tea on your study table. Pour one into an open cup: steam escapes into the air and it cools down—both matter and heat leave (an open system). Seal the second inside a steel water bottle: no steam escapes, yet the steel warms your hand—only energy crosses the wall (a closed system). Pour the third into a vacuum thermos flask: neither steam nor heat escapes—that is an isolated system!
Thermodynamics studies energy transformations in macroscopic systems at equilibrium. We divide the universe into two parts: Universe = System + Surroundings, separated by a real or imaginary boundary.
1. Three Types of Thermodynamic Systems
| System Type | Matter Exchange | Energy Exchange | NCERT Example |
|---|---|---|---|
| Open System | Yes ✓ | Yes ✓ | Reactants in an open beaker |
| Closed System | No ✗ | Yes ✓ | Reactants in a closed conducting steel/copper vessel |
| Isolated System | No ✗ | No ✗ | Reactants in a thermos flask or closed insulated vessel |
2. State Functions vs Path Functions
- State Variables / State Functions: Depend ONLY on initial and final states, NOT on the path taken (e.g., Pressure p, Volume V, Temperature T, Internal Energy U, Enthalpy H, Entropy S, Gibbs Energy G). Like the height of water in a pond—it doesn't matter whether rain or a tube-well filled it!
- Path Functions: Depend on how the change is carried out—Heat (q) and Work (w). Yet remarkably, their sum q + w = ΔU IS a state function!
3. Extensive vs Intensive Properties
- Extensive Properties: Depend on the quantity/size of matter (Mass, Volume V, Internal Energy U, Enthalpy H, Heat Capacity C, Entropy S, Gibbs Energy G). Partition a box in half and each half has V/2!
- Intensive Properties: Independent of sample size (Temperature T, Pressure p, Density, Molar volume Vm, Molar heat capacity Cm, Concentration).
4. Internal Energy (U) as a State Function
The sum of all chemical, electrical, kinetic, and mechanical energies inside a system is its Internal Energy (U). J. P. Joule (1840–50) proved using an insulated (adiabatic) vessel that doing 1 kJ of mechanical paddle work or 1 kJ of electrical work produces the exact same temperature rise: ΔU = U2 − U1 = wad.
• q > 0: Heat absorbed BY system (endothermic) | q < 0: Heat evolved BY system
• w > 0: Work done ON system (compression) | w < 0: Work done BY system (expansion)
Topic 5.1.4 – 5.2.2(a): First Law (ΔU = q + w), Reversible/Irreversible PV Work & Enthalpy (H = U + pV)
Imagine lifting a heavy weight on a gas piston. If you yank away one big brick suddenly, the gas bursts outward in one rapid jump (irreversible)—doing modest work. Instead, if you remove tiny grains of sand one at a time, the gas pushes gently in near-equilibrium at every step (reversible)—and extracts the maximum possible work!
1. First Law of Thermodynamics
We cannot measure the absolute value of U, only its change ΔU. For adiabatic walls (q = 0), ΔU = wad. At constant volume (ΔV = 0), w = 0 so ΔU = qV.
2. Pressure-Volume (PV) Work: Irreversible vs Reversible
- Irreversible Constant External Pressure: w = −pex ΔV = −pex(Vf − Vi).
- Free Expansion (pex = 0, vacuum): w = 0 always! For isothermal free expansion of an ideal gas, Joule showed q = 0 and ΔU = 0.
- Reversible Process: Proceeds infinitely slowly through equilibrium states (pex = pin ± dp) so it can be reversed at any instant by an infinitesimal change.
wrev = −nRT ln(Vf / Vi) = −2.303 nRT log(Vf / Vi) = −2.303 nRT log(pi / pf)
• Into vacuum (pex = 0): w = 0, q = 0.
• Against constant 1 atm: q = −w = pex(10 − 2) = 8 L·atm (w = −8 L·atm).
• 1 mol reversibly: q = −w = 2.303 × 1 × 0.08206 × 298 × log(10/2) = 39.37 L·atm (Maximum work!).
3. Enthalpy (H) & Relation Between ΔH and ΔU
Most lab reactions occur in open flasks at constant atmospheric pressure, where expansion work occurs. Defining Enthalpy: H = U + pV (state function, extensive) gives ΔH = ΔU + pΔV = qp (heat at constant pressure). ΔH < 0 for exothermic reactions; ΔH > 0 for endothermic reactions.
where Δng = (moles of gaseous products) − (moles of gaseous reactants)
Here Δng = 1 − 0 = 1. Thus ΔU = ΔH − ΔngRT = 41.00 − (1)(8.3 × 10-3)(373) = 41.00 − 3.096 = 37.90 kJ mol-1.
Topic 5.2.2(c)–(d) & 5.3: Heat Capacity (C_p − C_V = R) & Calorimetry (Bomb & Constant-Pressure)
Why does coastal Kerala stay pleasantly breezy while desert sand turns scorching hot by noon? Water has an unusually huge heat capacity—it absorbs vast heat with only a tiny temperature rise! Meanwhile, food scientists burn cashews inside a sealed steel Bomb Calorimeter submerged in water to measure exact food energy (ΔU) without losing a single joule.
1. Heat Capacity, Specific Heat & Molar Heat Capacity
- Heat Capacity (C): Heat needed to raise a system's temperature by 1 K (or 1 °C): q = C ΔT (extensive).
- Molar Heat Capacity (Cm = C / n): Heat needed for 1 mole per kelvin rise (intensive, J mol-1 K-1).
- Specific Heat Capacity (c): Heat needed for 1 unit mass (1 g or 1 kg) per kelvin rise: q = m × c × ΔT.
2. Relationship Between Cp and CV for an Ideal Gas
At constant volume, qV = CVΔT = ΔU. At constant pressure, qp = CpΔT = ΔH. For 1 mole of an ideal gas:
CpΔT = CVΔT + RΔT ⇒ Cp − CV = R (for n moles: Cp − CV = nR)
Why is Cp > CV? At constant pressure, part of the supplied heat does expansion work pushing back the atmosphere, so extra heat (R per mole per kelvin) is needed for the same 1 K temperature rise!
3. Calorimetry: Measuring ΔU and ΔH Experimentally
- Bomb Calorimeter (Constant Volume → ΔU): Sample burns in pure O2 inside a sealed steel bomb immersed in a known water bath. Since ΔV = 0, w = 0 and qV = ΔU!
- Constant-Pressure Calorimeter (Atmospheric → ΔH): Reaction occurs in an open insulated vessel; heat measured equals qp = ΔH.
• Heat released by 1 g graphite: q = −CV × ΔT = −20.7 × (299 − 298) = −20.7 kJ.
• For 1 mole (12 g) graphite: ΔU = −20.7 × 12 = −248.4 kJ mol-1 ≈ −2.48 × 102 kJ mol-1.
• Reaction: C(graphite) + O2(g) → CO2(g) has Δng = 1 − 1 = 0 ⇒ ΔH = ΔU = −2.48 × 102 kJ mol-1.
Topic 5.4 & 5.5(a)–(c): Reaction Enthalpies: Phase Changes, Formation (Δ_fH°), Combustion, Atomization & Bond Enthalpy
Step out of a swimming pool with a thin 18 g film of water on your skin and you instantly shiver—because vaporising 1 mole of water steals 44.01 kJ of heat directly from your body! Every physical transition and chemical reaction carries a characteristic enthalpy price tag measured against standard conditions (1 bar, 298 K).
Reaction Enthalpy: ΔrH = Σ ai Hm(Products) − Σ bi Hm(Reactants). Under standard state (pure substance at 1 bar and specified T, usually 298 K), it is written ΔrH°.
1. Phase Transformation Enthalpies (Always Endothermic, +)
- Standard Enthalpy of Fusion (ΔfusH°): 1 mol solid → liquid at melting point (H2O: +6.00 kJ mol-1 at 273 K).
- Standard Enthalpy of Vaporisation (ΔvapH°): 1 mol liquid → vapour at boiling point (H2O: +40.79 kJ mol-1 at 373 K; +44.01 kJ mol-1 at 298 K).
- Standard Enthalpy of Sublimation (ΔsubH°): 1 mol solid → vapour directly (Dry ice CO2: 25.2 kJ mol-1; Naphthalene: 73.0 kJ mol-1). Note: ΔsubH° = ΔfusH° + ΔvapH°.
2. Standard Enthalpy of Formation (ΔfH°)
Enthalpy change when 1 mole of a compound is formed from its elements in their most stable reference states at 1 bar & T (e.g., H2(g), O2(g), C(graphite), S(rhombic), Br2(l)). By convention, ΔfH° = 0 for every element in its reference state!
NCERT Example: CaCO3(s) → CaO(s) + CO2(g) ⇒ ΔrH° = (−635.1) + (−393.5) − (−1206.9) = +178.3 kJ mol-1.
3. Combustion, Atomization & Bond Enthalpies
- Enthalpy of Combustion (ΔcH°): Complete combustion of 1 mole of substance in excess O2 (always exothermic: butane C4H10 = −2658 kJ mol-1; glucose = −2802 kJ mol-1).
- Enthalpy of Atomization (ΔaH°): Breaking 1 mole of bonds completely to yield gaseous atoms (H2(g) → 2H(g): +435.0 kJ mol-1; Na(s) → Na(g): +108.4 kJ mol-1).
- Bond Enthalpy (ΔbondH°): In polyatomic molecules like CH4, successive C–H bonds differ (427, 439, 452, 347 kJ mol-1), so we use Mean Bond Enthalpy = 1665 / 4 = 416 kJ mol-1.
ΔrH° ≈ Σ Bond Enthalpies(Reactants) − Σ Bond Enthalpies(Products)
• Using Enthalpies of Formation: Products MINUS Reactants.
• Using Bond Enthalpies: Reactants MINUS Products!
Also check stoichiometry:
H₂ + Br₂ → 2 HBr gives 2 × ΔfH°(HBr), and CaO + CO₂ → CaCO₃ is NOT ΔfH° because CaO and CO₂ are compounds, not elements!Topic 5.4(e): Hess's Law of Constant Heat Summation & Thermochemical Algebra
Imagine climbing from Kochi (sea level) to Munnar (1,600 m). Whether you helicopter straight to the top or stop for tea at Neriamangalam and Adimali along the winding ghat road, your net gain in altitude is identical! Because Enthalpy H is a state function, Germain Hess realized chemical reactions obey the exact same altitude rule.
Hess's Law of Constant Heat Summation
Statement: If a reaction takes place in several steps, then its standard reaction enthalpy is the algebraic sum of the standard enthalpies of the intermediate reactions into which the overall reaction may be divided at the same temperature.
Why Do Chemists Need Hess's Law?
Many reactions cannot be measured directly in a calorimeter—for example, burning graphite in limited O2 always forms some CO2 alongside CO, making direct measurement of ΔfH°(CO) impossible!
Given: (i) C(graphite) + O2(g) → CO2(g); ΔrH° = −393.5 kJ mol-1
(ii) CO(g) + ½O2(g) → CO2(g); ΔrH° = −283.0 kJ mol-1
Reverse (ii) to place CO(g) on the right: CO2(g) → CO(g) + ½O2(g); ΔrH° = +283.0 kJ mol-1.
Add (i) + reversed (ii) so CO2 cancels: ΔfH°(CO) = −393.5 + 283.0 = −110.5 kJ mol-1!
• 6 × [C + O2 → CO2] = 6 × (−393.5) = −2361.0 kJ
• 3 × [H2 + ½O2 → H2O(l)] = 3 × (−285.83) = −857.49 kJ
• Reverse C6H6 combustion: 6CO2 + 3H2O → C6H6 + 15/2O2 = +3267.0 kJ
• Add all three: ΔfH°(C6H6, l) = −3218.49 + 3267.0 = +48.51 kJ mol-1.
Topic 5.5(d)–(f): Lattice Enthalpy, Born-Haber Cycle (NaCl), Enthalpy of Solution & Dilution
How much energy holds table salt crystals together? Nobody can pull one mole of solid NaCl cleanly apart into isolated gaseous Na+ and Cl− ions in a calorimeter! Instead, Max Born and Fritz Haber applied Hess's Law as a 5-step vertical energy ladder—unlocking Lattice Enthalpy and explaining why table salt barely changes temperature when stirred into water.
1. Lattice Enthalpy (ΔlatticeH°)
The enthalpy change when 1 mole of an ionic compound dissociates into its ions in the gaseous state:
2. Born-Haber Cycle for NaCl(s)
Equating the direct formation of NaCl(s) (ΔfH° = −411.2 kJ mol-1) to a 5-step Hess pathway:
| Step | Process | Enthalpy Term | Value (kJ mol-1) |
|---|---|---|---|
| 1 | Sublimation: Na(s) → Na(g) | ΔsubH° | +108.4 |
| 2 | Ionization: Na(g) → Na+(g) + e− | ΔiH° | +496.0 |
| 3 | Dissociation: ½Cl2(g) → Cl(g) | ½ ΔbondH° | +121.0 |
| 4 | Electron Gain: Cl(g) + e− → Cl−(g) | ΔegH° | −348.6 |
| 5 | Lattice Formation: Na+(g) + Cl−(g) → NaCl(s) | −ΔlatticeH° | −U |
⇒ ΔlatticeH° = 108.4 + 496 + 121 − 348.6 − (−411.2) = +788 kJ mol-1
3. Enthalpy of Solution (ΔsolH°) & Hydration (ΔhydH°)
Dissolving an ionic salt happens in two conceptual steps: breaking the crystal lattice (+ΔlatticeH°) and hydrating the gaseous ions in water (−exothermic ΔhydH°):
Enthalpy of Dilution: Heat change when extra solvent is added to a solution (e.g., HCl·25 aq + 15 aq → HCl·40 aq, ΔH = −0.76 kJ mol-1). As solvent → ∞, ΔsolH approaches the limiting value at infinite dilution.
Topic 5.6(a)–(e): Spontaneity, Entropy (S), Second Law (ΔS_total > 0) & Third Law of Thermodynamics
Drop a spoon of ink into still water—it swirls outward until the whole glass turns tinted, never gathering back into one neat droplet on its own! Why do gases mix across a removed partition even when ΔH = 0, and why does ice melt spontaneously on a warm table despite being endothermic? Because nature is driven by Entropy (S)—the unstoppable spread of disorder!
1. What is a Spontaneous Process?
A process having the potential to proceed on its own without external assistance (irreversible; reversed only by external agency). Caution: Spontaneity tells us direction, NOT speed—H2 and O2 react spontaneously yet imperceptibly slowly at room temperature!
Why ΔH < 0 alone fails: Some endothermic processes (ΔH > 0, like ½N2 + O2 → NO2 or ice melting) and zero-enthalpy processes (ΔH = 0, gas diffusion) are spontaneous!
2. Entropy (S) & Second Law of Thermodynamics
- Entropy (S): A thermodynamic state function and extensive property measuring the degree of randomness or disorder. Order of entropy: Sgas >> Sliquid > Ssolid.
- Quantitative Definition: ΔS = qrev / T (Unit: J K-1 mol-1). Heat added at lower T creates greater disorder than the same heat at higher T.
- Second Law: For any spontaneous process, total entropy of the universe increases: ΔStotal = ΔSsystem + ΔSsurroundings > 0. At equilibrium, entropy is maximum and ΔStotal = 0.
(i) Liquid crystallises → solid: more ordered → ΔS < 0.
(ii) Crystalline solid heated from 0 K to 115 K: particles vibrate → ΔS > 0.
(iii) 2 NaHCO3(s) → Na2CO3(s) + CO2(g) + H2O(g): gases formed → ΔS > 0.
(iv) H2(g) → 2 H(g): moles of gas double → ΔS > 0.
4 Fe(s) + 3 O2(g) → 2 Fe2O3(s) has ΔSsys = −549.4 J K-1 mol-1, yet ΔrH° = −1648 × 103 J mol-1 at 298 K.
ΔSsurr = −ΔrH° / T = +1648000 / 298 = +5530 J K-1 mol-1.
⇒ ΔStotal = 5530 + (−549.4) = +4980.6 J K-1 mol-1 > 0 → Spontaneous!
3. Third Law of Thermodynamics
Statement: The entropy of any pure crystalline substance approaches zero as temperature approaches absolute zero (T → 0 K, S → 0). Note: Does NOT hold for solutions or supercooled liquids/glasses. Enables measurement of absolute entropies!
Topic 5.6(c) & 5.7: Gibbs Energy (ΔG = ΔH − TΔS), Four Temperature Cases & Equilibrium (ΔG° = −RT ln K)
Checking surroundings entropy for every reaction in the universe is exhausting! Josiah Willard Gibbs invented one brilliant system-only referee—Gibbs Free Energy (G)—that pits energy release (ΔH) against disorder gain (TΔS) in a tug-of-war controlled by temperature T, and even tells us the exact equilibrium yield K!
1. Gibbs Energy & Spontaneity at Constant T and P
Define G = H − TS (state function, extensive). Since ΔStotal = ΔSsys − ΔHsys/T, multiplying by −T yields the legendary Gibbs Equation:
Physical Meaning: −ΔG represents the maximum useful (non-PV) work available from a reaction—hence called Free Energy.
2. Effect of Temperature on Spontaneity (NCERT Table 5.4)
| ΔrH° | ΔrS° | ΔrG° = ΔH° − TΔS° | Spontaneity Verdict |
|---|---|---|---|
| − (Exo) | + (More disorder) | Always − | Spontaneous at ALL temperatures |
| − (Exo) | − (Less disorder) | − at low T; + at high T | Spontaneous at LOW temperature (|ΔH| > |TΔS|) |
| + (Endo) | + (More disorder) | + at low T; − at high T | Spontaneous at HIGH temperature (TΔS > ΔH) |
| + (Endo) | − (Less disorder) | Always + | Non-spontaneous at ALL temperatures |
3. Standard Gibbs Energy & Equilibrium Constant (K)
At dynamic equilibrium, free energy reaches its minimum so ΔrG = 0. Relating standard Gibbs energy change (ΔrG°) to equilibrium constant K:
• 5.12: 3/2 O2(g) → O3(g) at 298 K has Kp = 2.47 × 10-29 ⇒ ΔrG° = −2.303(8.314)(298) log(2.47 × 10-29) = +163 kJ mol-1.
• 5.13: If ΔrG° = −13.6 kJ mol-1 at 298 K ⇒ log K = 13600 / (2.303 × 8.314 × 298) = 2.38 ⇒ K = 2.4 × 102.
ΔG = ΔH − TΔS! ΔH is usually given in kJ mol-1 while ΔS is given in J K-1 mol-1! Always divide ΔS by 1000 (or multiply ΔH by 1000) before subtracting! Similarly, in ΔG° = −2.303 RT log K, if R = 8.314 J K-1 mol-1, your ΔG° comes out in Joules—divide by 1000 for kJ!Solved Previous Year Questions (Kerala DHSE & NCERT)
Q1 (Kerala HSE March (Repeated Favorite) • 1 Marks): Classify the following properties into extensive and intensive: Enthalpy, Temperature, Heat capacity, Density.
Extensive Properties (depend on quantity of matter): Enthalpy, Heat capacity.
Intensive Properties (independent of quantity of matter): Temperature, Density.
Q2 (Kerala HSE SAY • 1 Marks): What is the standard enthalpy of formation of an element in its reference state? Mention the reference states of Carbon and Sulphur.
By convention, ΔfH° of an element in its reference state is zero (0).
Reference state of Carbon: C (graphite); Reference state of Sulphur: S (rhombic).
Q3 (Kerala HSE Model • 1 Marks): Write the mathematical statement of the First Law of Thermodynamics. What is ΔU for an isolated system?
Mathematical statement: ΔU = q + w.
For an isolated system (q = 0, w = 0), ΔU = 0 (energy remains constant).
Q4 (Kerala HSE March (Most Asked) • 2 Marks): Derive the relationship between heat capacities Cp and CV for one mole of an ideal gas.
At constant volume: qV = ΔU = CVΔT.
At constant pressure: qp = ΔH = CpΔT.
For 1 mole of an ideal gas (pV = RT): ΔH = ΔU + Δ(pV) = ΔU + RΔT.
Substituting ΔH and ΔU: CpΔT = CVΔT + RΔT ⇒ Cp − CV = R.
Q5 (Kerala HSE SAY (High Yield) • 2 Marks): State Hess's Law of Constant Heat Summation. Illustrate how it helps find ΔfH° of CO(g).
Statement: If a reaction takes place in several steps, its standard reaction enthalpy is the sum of the standard enthalpies of the intermediate reactions at the same temperature (ΔrH = ΔrH1 + ΔrH2 + ...).
Illustration: From C(s) + O2(g) → CO2(g) (ΔH1 = −393.5 kJ) and reversing CO(g) + ½O2(g) → CO2(g) (ΔH2 = −283.0 kJ), we get ΔfH°(CO) = −393.5 + 283.0 = −110.5 kJ mol-1.
Q6 (Kerala HSE March • 2 Marks): Write the Gibbs equation. Predict the signs of ΔH and ΔS for a reaction that is: (i) spontaneous at all temperatures, (ii) spontaneous only at high temperatures.
Gibbs equation: ΔG = ΔH − TΔS.
(i) Spontaneous at ALL temperatures: ΔH < 0 (−) and ΔS > 0 (+).
(ii) Spontaneous only at HIGH temperatures: ΔH > 0 (+) and ΔS > 0 (+) (so TΔS > ΔH at high T).
Q7 (Kerala HSE Improvement • 2 Marks): State the Second and Third Laws of Thermodynamics. Predict the entropy change when a crystalline solid is heated from 0 K to 115 K.
Second Law: For any spontaneous process in an isolated system, entropy increases (ΔStotal = ΔSsys + ΔSsurr > 0).
Third Law: The entropy of any pure crystalline substance approaches zero as temperature approaches absolute zero (0 K).
When heated from 0 K to 115 K, particles oscillate about lattice sites and disorder increases, so ΔS increases (> 0).
Q8 (Kerala HSE March (Standard Numerical) • 2 Marks): For the reaction 2 A + B → C, ΔH = 400 kJ mol-1 and ΔS = 0.2 kJ K-1 mol-1. At what temperature will the reaction become spontaneous?
At equilibrium, ΔG = ΔH − TΔS = 0 ⇒ T = ΔH / ΔS = 400 / 0.2 = 2000 K.
Since both ΔH > 0 and ΔS > 0, ΔG becomes negative above 2000 K. Hence the reaction is spontaneous at T > 2000 K (NCERT Exercise 5.17).
Q9 (Kerala HSE March (Repeated Numerical) • 3 Marks): The enthalpies of combustion of methane, graphite, and dihydrogen at 298 K are −890.3 kJ mol-1, −393.5 kJ mol-1, and −285.8 kJ mol-1 respectively. Calculate the standard enthalpy of formation of CH4(g).
Target: C(graphite) + 2H2(g) → CH4(g).
(i) C(s) + O2(g) → CO2(g); ΔH1 = −393.5 kJ
(ii) 2H2(g) + O2(g) → 2H2O(l); ΔH2 = 2(−285.8) = −571.6 kJ
(iii) Reverse combustion of CH4: CO2(g) + 2H2O(l) → CH4(g) + 2O2(g); ΔH3 = +890.3 kJ
Adding (i) + (ii) + (iii): ΔfH°(CH4) = −393.5 − 571.6 + 890.3 = −74.8 kJ mol-1.
Q10 (Kerala HSE Model / NCERT 5.6 • 3 Marks): 1 g of graphite is burnt in a bomb calorimeter in excess O2 at 298 K and 1 atm: C(graphite) + O2(g) → CO2(g). Temperature rises from 298 K to 299 K. If the heat capacity of the bomb calorimeter is 20.7 kJ K-1, find ΔU and ΔH per mole of graphite.
Heat from 1 g graphite: q = −CV ΔT = −20.7 × (299 − 298) = −20.7 kJ.
For 1 mole (12 g) graphite: ΔU = −20.7 × 12 = −248.4 kJ mol-1 (−2.48 × 102 kJ mol-1).
For C(s) + O2(g) → CO2(g), Δng = 1 − 1 = 0, so ΔH = ΔU = −2.48 × 102 kJ mol-1.
Q11 (Kerala HSE March / NCERT 5.19 • 3 Marks): For the reaction 2 A(g) + B(g) → 2 D(g), ΔU° = −10.5 kJ and ΔS° = −44.1 J K-1 at 298 K. Calculate ΔG° and predict whether the reaction may occur spontaneously.
Δng = 2 − (2 + 1) = −1.
ΔH° = ΔU° + ΔngRT = −10.5 + (−1)(8.314 × 10-3)(298) = −10.5 − 2.478 = −12.98 kJ.
ΔG° = ΔH° − TΔS° = −12.98 − 298(−44.1 × 10-3) = −12.98 + 13.14 = +0.16 kJ.
Since ΔG° > 0, the reaction is non-spontaneous at 298 K.
Q12 (Kerala HSE March (Essay / Cycle) • 4 Marks): What is Lattice Enthalpy? Explain the Born-Haber Cycle to calculate the lattice enthalpy of NaCl(s) given: ΔfH° = −411.2, ΔsubH° = +108.4, ΔiH° = +496, ½ΔbondH° = +121, ΔegH° = −348.6 kJ mol-1.
Lattice Enthalpy (ΔlatticeH°): The enthalpy change when 1 mole of an ionic crystal dissociates completely into gaseous ions: NaCl(s) → Na+(g) + Cl−(g).
5 Steps of the Born-Haber Cycle:
1. Na(s) → Na(g) [ΔsubH° = +108.4 kJ]
2. Na(g) → Na+(g) + e− [ΔiH° = +496 kJ]
3. ½Cl2(g) → Cl(g) [½ΔbondH° = +121 kJ]
4. Cl(g) + e− → Cl−(g) [ΔegH° = −348.6 kJ]
5. Na+(g) + Cl−(g) → NaCl(s) [−ΔlatticeH°]
By Hess's Law: ΔfH° = ΔsubH° + ΔiH° + ½ΔbondH° + ΔegH° − ΔlatticeH°
⇒ ΔlatticeH° = 108.4 + 496 + 121 − 348.6 − (−411.2) = +788 kJ mol-1.