Calculate ionic crystal lattice energy and lattice enthalpy (\(\text{kJ/mol}\), \(\text{kcal/mol}\), \(\text{eV}\)) using the Born-Haber thermochemical cycle, the Born-Landé & Born-Mayer equations, and the Kapustinskii empirical formula.
| Thermodynamic Step | Chemical Reaction Equation | Enthalpy (\(\Delta H\)) | Type |
|---|---|---|---|
| 1. Metal Sublimation | \(M(s) \to M(g)\) | +107.3 kJ | Endothermic |
| 2. Metal Ionization | \(M(g) \to M^+(g) + e^-\) | +495.8 kJ | Endothermic |
| 3. Non-Metal Dissociation | \(\frac{1}{2}X_2(g) \to X(g)\) | +121.7 kJ | Endothermic |
| 4. Electron Affinity | \(X(g) + e^- \to X^-(g)\) | -349.0 kJ | Exothermic |
| 5. Lattice Formation (\(\Delta H_{\text{latt}}\)) | \(M^+(g) + X^-(g) \to MX(s)\) | -787.0 kJ | Lattice Energy |
| Net Standard Formation (\(\Delta H_f^\circ\)) | \(M(s) + \frac{1}{2}X_2(g) \to MX(s)\) | -411.2 kJ | Target Enthalpy |
| Crystal Structure | Prototype | Coordination (C:A) | Madelung Constant (M) | \(M / (\nu/2)\) |
|---|---|---|---|---|
| Rocksalt (Halite) | NaCl, MgO, CaO | 6 : 6 (Octahedral) | 1.7476 | 1.748 |
| Cesium Chloride | CsCl, CsBr, TlCl | 8 : 8 (Cubic) | 1.7627 | 1.763 |
| Zinc Blende (Sphalerite) | ZnS, CuCl, BeO | 4 : 4 (Tetrahedral) | 1.6381 | 1.638 |
| Wurtzite (Hexagonal) | ZnS, ZnO, SiC | 4 : 4 (Tetrahedral) | 1.6413 | 1.641 |
| Fluorite | CaF₂, UO₂, CeO₂ | 8 : 4 (Cubic/Tetra) | 2.5194 | 1.679 |
| Rutile | TiO₂, SnO₂, MgF₂ | 6 : 3 (Distorted Oct) | 2.4080 | 1.605 |
Lattice energy (\(\Delta H_{\text{lattice}}\)) is the quantitative thermodynamic metric that measures the electrostatic cohesive forces holding together an infinite three-dimensional crystal lattice of ions. Because it is impossible to assemble or isolate individual gaseous ions into an infinite crystal in a single direct laboratory calorimeter experiment, lattice energy is determined either thermochemically via the Born-Haber cycle or theoretically via electrostatic crystal field models.
Two primary sign conventions are standard across chemical literature:
The enthalpy change when 1 mole of an ionic crystalline solid is formed from its infinitely separated constituent gaseous ions at standard state (\(298.15\,\text{K}, 1\,\text{bar}\)):
The energy required to completely separate 1 mole of a solid ionic crystal into isolated, non-interacting gaseous ions:
Applying the First Law of Thermodynamics and Hess's Law of constant heat summation across the closed thermodynamic state function path:
Rearranging the cycle to isolate the lattice formation enthalpy: $$\Delta H_{\text{lattice (form)}} = \Delta H_f^\circ - \left( \Delta H_{\text{sub}} + \sum \text{IE} + \frac{1}{2} D(X_2) + \sum \text{EA} \right)$$
Max Born and Alfred Landé modeled the net potential energy of an ionic crystal by summing the long-range Coulomb attractive potential and the short-range Born electron-cloud overlap repulsion (\(E_{\text{rep}} = B/r^n\)):
Where \(N_A = 6.022 \times 10^{23}\,\text{mol}^{-1}\) is Avogadro's constant, \(M\) is the geometric Madelung constant, \(z_+, z_-\) are formal ionic charges, \(e = 1.6022 \times 10^{-19}\,\text{C}\), \(\varepsilon_0 = 8.854 \times 10^{-12}\,\text{F/m}\), \(r_0 = r_+ + r_-\) is the interionic equilibrium distance, and \(n\) is the Born exponent (typically \(5\text{--}12\)).
The refined Born-Mayer equation replaces the power-law repulsion term with a quantum mechanical exponential decay term: $$U_0 = -\frac{N_A \cdot M \cdot |z_+ z_-| \cdot e^2}{4\pi \varepsilon_0 r_0} \left( 1 - \frac{\rho}{r_0} \right) \quad (\text{where }\rho \approx 34.5\,\text{pm})$$
Anatoli Kapustinskii discovered that dividing the Madelung constant \(M\) by half the number of ions per formula unit (\(\nu/2\)) yields an approximately constant value of \(\approx 0.88\) across almost all crystal geometries. This eliminates the requirement of knowing the crystal lattice type:
Where \(K = 1.202 \times 10^5\,\text{kJ}\cdot\text{pm/mol}\) (or \(1.202 \times 10^{-4}\,\text{J}\cdot\text{m/mol}\)), \(\nu\) is the total number of ions in the stoichiometric formula, \(r_+, r_-\) are thermochemical radii in picometers (\(\text{pm}\)), and \(d = 34.5\,\text{pm}\).
To understand how thermodynamic energy terms balance in practice, review three definitive benchmark calculations:
For \(\text{NaCl}(s)\) with \(\Delta H_f^\circ = -411.2\,\text{kJ/mol}\):
For \(\text{MgO}(s)\) with \(\Delta H_f^\circ = -601.7\,\text{kJ/mol}\):
For \(\text{CaF}_2(s)\) with \(\Delta H_f^\circ = -1,228.0\,\text{kJ/mol}\):
Comparative analysis of experimental Born-Haber cycle lattice energies against theoretical Born-Landé and Kapustinskii predictions across representative ionic solids:
| Compound | Crystal Type | \(r_0\) (pm) | Melting Pt (°C) | Born-Haber (\(\text{kJ}\)) | Born-Landé (\(\text{kJ}\)) | Kapustinskii (\(\text{kJ}\)) | % Error |
|---|---|---|---|---|---|---|---|
| LiF | Rocksalt (6:6) | 201.0 | 845 | -1,036 | -1,008 | -1,012 | 2.7% |
| LiCl | Rocksalt (6:6) | 257.0 | 605 | -853 | -822 | -830 | 3.6% |
| NaCl | Rocksalt (6:6) | 282.0 | 801 | -787 | -756 | -746 | 3.9% |
| KCl | Rocksalt (6:6) | 315.0 | 770 | -715 | -688 | -675 | 3.8% |
| CsCl | CsCl Body-Ctr (8:8) | 357.0 | 645 | -657 | -634 | -621 | 3.5% |
| MgO | Rocksalt (6:6) | 212.0 | 2,852 | -3,791 | -3,760 | -3,800 | 0.8% |
| CaO | Rocksalt (6:6) | 240.0 | 2,572 | -3,401 | -3,350 | -3,380 | 1.5% |
| CaF₂ | Fluorite (8:4) | 236.0 | 1,418 | -2,630 | -2,580 | -2,570 | 1.9% |
| AgCl (Covalent) | Rocksalt (6:6) | 277.0 | 455 | -916 | -765 | -755 | 16.5% |
| AgI (Covalent) | Wurtzite/ZB | 280.0 | 558 | -889 | -710 | -695 | 20.1% |
When substantial discrepancies occur between experimental Born-Haber lattice enthalpies and theoretical electrostatic formulas (such as \(\text{AgCl}\) with \(16.5\%\) error), Fajans' Rules explain the onset of partial covalent bonding:
Whether an ionic solid dissolves spontaneously in water is determined by the competition between lattice dissociation energy and hydration enthalpy:
Authoritative answers to common questions about calculating lattice energy, Born-Haber cycles, Madelung constants, and ionic crystal thermodynamics.