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When an ionic solid dissolves in water, two things happen:
Whether the overall process is exothermic or endothermic depends on the balance between these two contributions. The overall enthalpy change is called the enthalpy of solution.
Definition (OCR): The enthalpy of hydration is the enthalpy change when one mole of gaseous ions dissolves in water to form one mole of aqueous ions under standard conditions.
Examples:
Na+(g) + aq -> Na+(aq) ΔH°_hyd = -406 kJ mol^-1
Cl-(g) + aq -> Cl-(aq) ΔH°_hyd = -364 kJ mol^-1
Hydration is always exothermic because the partial charges on water molecules are attracted to the ion. Water behaves as a dipolar molecule: the slightly negative oxygen attracts cations, and the slightly positive hydrogens attract anions.
graph TD
A[Gaseous ion Na+] -->|water shell forms<br/>exothermic hydration| B[Aqueous ion Na+ aq]
Hydration enthalpy follows the same kind of electrostatic logic as lattice enthalpy: the stronger the interaction between the ion and the surrounding water dipoles, the more exothermic the hydration enthalpy.
| Ion | Charge | Radius / pm | ΔH°_hyd / kJ mol^-1 |
|---|---|---|---|
| Li+ | +1 | 76 | -519 |
| Na+ | +1 | 102 | -406 |
| K+ | +1 | 138 | -322 |
| Rb+ | +1 | 152 | -301 |
| Cs+ | +1 | 167 | -276 |
| Mg^2+ | +2 | 72 | -1920 |
| Ca^2+ | +2 | 100 | -1650 |
| F- | -1 | 133 | -506 |
| Cl- | -1 | 181 | -364 |
| Br- | -1 | 196 | -335 |
| I- | -1 | 220 | -293 |
Definition (OCR): The enthalpy of solution is the enthalpy change when one mole of an ionic compound dissolves in a given amount of water (usually enough to produce an "infinitely dilute" solution) under standard conditions.
Example: NaCl(s) + aq -> Na+(aq) + Cl-(aq) ΔH°_sol = +3.9 kJ mol^-1
Note the small, positive value: dissolving NaCl is slightly endothermic, which is why a cold pack containing solid NH4NO3 (much more endothermic) gets cold when crushed.
To relate everything we construct a Hess-law cycle with three routes or arrows:
Route 1: Solid ionic compound -> aqueous ions directly (ΔH°_sol)
Route 2: Solid -> gaseous ions (minus lattice enthalpy) -> aqueous ions (sum of hydration enthalpies)
graph TD
A[NaCl s] -->|enthalpy of solution<br/>direct route| B[Na+ aq plus Cl- aq]
A -->|minus lattice enthalpy<br/>break lattice| C[Na+ g plus Cl- g]
C -->|hydration of Na+<br/>plus hydration of Cl-| B
Hess's law gives:
ΔH°_sol = -ΔH°_LE + ΔH°_hyd(cation) + ΔH°_hyd(anion)
Remember the minus sign in front of ΔH°_LE: the lattice step in the cycle goes in the reverse direction to lattice enthalpy (breaking the lattice instead of forming it).
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