Dove's LibraryDove's Library

9.6 - Free Energy of Dissolution

Overview

Why does table salt dissolve in water while chalk (CaCO3\mathrm{CaCO_3}) barely does? Dissolving is a process like any other, so it has a ΔH∘\Delta H^\circ, a ΔS∘\Delta S^\circ, and a ΔG∘\Delta G^\circ. This topic breaks dissolving into three particle-level changes, estimates the sign of ΔH\Delta H and ΔS\Delta S for each, and shows why the total ΔG∘\Delta G^\circ is hard to predict: large contributions mostly cancel.

Dissolving is an equilibrium

When an ionic solid dissolves, its ions separate and spread through the water:
AgCl(s)⇌Ag+(aq)+Cl−(aq)\mathrm{AgCl(s) \rightleftharpoons Ag^{+}(aq) + Cl^{-}(aq)}
The equilibrium constant for dissolving is the solubility product, KspK_{sp} (Topic 7.11), so everything from Topic 9.5 applies. If ΔGsoln∘<0\Delta G^\circ_\mathrm{soln} < 0, then K>1K > 1 and the salt is very soluble. If ΔGsoln∘>0\Delta G^\circ_\mathrm{soln} > 0, then K<1K < 1 and the salt has low solubility. The more positive ΔGsoln∘\Delta G^\circ_\mathrm{soln} is, the smaller KspK_{sp} is. For NaCl, ΔGsoln∘=−9.0 kJ/molrxn\Delta G^\circ_\mathrm{soln} = -9.0\ \mathrm{kJ/mol_{rxn}}, which gives K≈38K \approx 38, the value quoted in Topic 7.11.

Three things happen when a salt dissolves

The free energy change for dissolving reflects three factors. For each one, you can estimate the sign of ΔH\Delta H and ΔS\Delta S from what the particles are doing.

1. Breaking apart the solid

The attractions that hold the solid together have to be overcome: ion-ion attractions in an ionic solid, or intermolecular forces in a molecular solid. That takes energy, so ΔH>0\Delta H > 0. It's large for ionic solids, and largest for small, highly charged ions, which attract each other most strongly (Coulomb's law). The particles also go from fixed positions in a lattice to moving freely through the whole solution, so ΔS>0\Delta S > 0.

2. Reorganizing the solvent

Water molecules have to move apart to make room, which breaks some hydrogen bonds between them (ΔH>0\Delta H > 0). Then they line up around each dissolved particle in a hydration shell: the oxygen ends (partial negative) face cations, and the hydrogen ends (partial positive) face anions (Topic 3.10). Water molecules locked in a shell can't move or turn as freely as they could in pure water, so this reorganization lowers the entropy (ΔS<0\Delta S < 0). The effect is biggest for small or highly charged ions, like Li+\mathrm{Li^{+}}, Ca2+\mathrm{Ca^{2+}}, F−\mathrm{F^{-}}, and CO32−\mathrm{CO_3^{2-}}, which hold their shells tightly.

3. Attractions between the dissolved particles and the solvent

New ion-dipole attractions form between the ions and water (for a molecular solute, hydrogen bonds or dipole attractions). Forming attractions releases energy, so ΔH<0\Delta H < 0. Like the attractions in the solid, these are strongest for small, highly charged ions. They're also what holds the hydration shell in place, so they go along with the entropy loss in factor 2.
Factor
What the particles do
ΔH\Delta H
ΔS\Delta S
1. Breaking apart the solid
ions leave their fixed positions and spread out
++ (energy in)
++ (more freedom)
2. Reorganizing the solvent
water molecules move apart, then line up in hydration shells
++ (some hydrogen bonds broken)
−- (water held in place)
3. Solute-solvent attractions
ion-dipole attractions form
−- (energy out)
goes with the ordering in factor 2
9.6 - Free Energy of Dissolution
In this particle model, the two entropy effects pull in opposite directions. The ions gain freedom, but the water molecules around them lose it. For ions with a charge of 1 and a fairly large size, like K+\mathrm{K^{+}} and Cl−\mathrm{Cl^{-}}, the freed ions win and ΔSsoln∘>0\Delta S^\circ_\mathrm{soln} > 0. For small or highly charged ions, the ordering of water can win, and ΔSsoln∘<0\Delta S^\circ_\mathrm{soln} < 0.

Why the total is hard to predict

Each factor can be large, and their signs are opposite, so the total is a small difference between big numbers. Here is the enthalpy side for sodium chloride, drawn to scale:
9.6 - Free Energy of Dissolution
Pulling one mole of NaCl apart into separate gaseous ions takes about 787 kJ. Surrounding those ions with water (factors 2 and 3 together) releases about 783 kJ. The net ΔHsoln∘\Delta H^\circ_\mathrm{soln} is only +3.9 kJ/molrxn+3.9\ \mathrm{kJ/mol_{rxn}}, less than 1% of either step. A small error in either big number would flip the sign of the answer. Entropy works the same way. That's why you can estimate the sign and rough size of each factor, but the total ΔGsoln∘\Delta G^\circ_\mathrm{soln} has to come from measured data.

Enthalpy vs. entropy in real salts

The table gives values for six salts at 25 °C, rounded from standard thermodynamic tables. ΔGsoln∘\Delta G^\circ_\mathrm{soln} is calculated as ΔHsoln∘−TΔSsoln∘\Delta H^\circ_\mathrm{soln} - T\Delta S^\circ_\mathrm{soln} at 298 K, and each KspK_{sp} comes from ΔG∘\Delta G^\circ, so it can differ a little from a measured value (Topic 7.11 lists 1.8×10−101.8 \times 10^{-10} for AgCl).
Salt
ΔHsoln∘\Delta H^\circ_\mathrm{soln} (kJ/molrxn\mathrm{kJ/mol_{rxn}})
ΔSsoln∘\Delta S^\circ_\mathrm{soln} (J/(K⋅molrxn)\mathrm{J/(K{\cdot}mol_{rxn})})
ΔGsoln∘\Delta G^\circ_\mathrm{soln} (kJ/molrxn\mathrm{kJ/mol_{rxn}})
In water
KCl\mathrm{KCl}
+17.2+17.2
+76.4+76.4
−5.6-5.6
dissolves well; the solution gets colder
NaCl\mathrm{NaCl}
+3.9+3.9
+43.4+43.4
−9.0-9.0
dissolves well; the temperature barely changes
CaCl2\mathrm{CaCl_2}
−81.3-81.3
−44.7-44.7
−68.0-68.0
dissolves well; the solution gets hot
LiF\mathrm{LiF}
+4.9+4.9
−36.1-36.1
+15.7+15.7
slightly soluble (Ksp≈1.8×10−3K_{sp} \approx 1.8 \times 10^{-3})
AgCl\mathrm{AgCl}
+65.5+65.5
+33.0+33.0
+55.7+55.7
insoluble (Ksp≈1.7×10−10K_{sp} \approx 1.7 \times 10^{-10})
CaCO3\mathrm{CaCO_3}
−13.1-13.1
−202.9-202.9
+47.4+47.4
insoluble (Ksp≈4.9×10−9K_{sp} \approx 4.9 \times 10^{-9})
9.6 - Free Energy of Dissolution
Each red dot is the sum of the two bars next to it, since ΔG∘=ΔH∘+(−TΔS∘)\Delta G^\circ = \Delta H^\circ + (-T\Delta S^\circ). What the graph shows:
  • KCl dissolves even though dissolving is endothermic, because the entropy term is bigger. This is entropy-driven, and the solution gets colder. The cold-pack salt from Topic 6.1, NH4NO3\mathrm{NH_4NO_3}, works the same way: its ΔHsoln∘\Delta H^\circ_\mathrm{soln} is +25.7 kJ/molrxn+25.7\ \mathrm{kJ/mol_{rxn}}, but TΔSsoln∘T\Delta S^\circ_\mathrm{soln} is larger at room temperature.
  • CaCl2\mathrm{CaCl_2} has a negative ΔSsoln∘\Delta S^\circ_\mathrm{soln}, but dissolving is so exothermic that ΔG∘\Delta G^\circ is strongly negative anyway. This is enthalpy-driven, and the solution gets hot (it's used in hot packs).
  • AgCl gains entropy when it dissolves, but the enthalpy cost is much larger, so ΔG∘>0\Delta G^\circ > 0.
  • LiF and CaCO3\mathrm{CaCO_3} have negative ΔSsoln∘\Delta S^\circ_\mathrm{soln}: their small or doubly charged ions order so much water that entropy works against dissolving. Calcium carbonate is the striking case. Dissolving it releases heat, yet it's insoluble.
The takeaway: neither ΔH\Delta H nor ΔS\Delta S alone tells you whether a salt dissolves. A salt can dissolve while absorbing heat (KCl), and a salt can stay put even though dissolving would release heat (CaCO3\mathrm{CaCO_3}).
Temperature matters too. From Topic 9.5, KK grows with temperature when the process is endothermic, so KCl is more soluble in hot water than in cold. Dissolving CaCO3\mathrm{CaCO_3} is exothermic, and it really is less soluble in hot water.

Example 1: An entropy-driven salt

Use the table for KCl. (a) Calculate ΔGsoln∘\Delta G^\circ_\mathrm{soln} at 25 °C. (b) Which term drives the dissolving? (c) Explain the sign of ΔSsoln∘\Delta S^\circ_\mathrm{soln} at the particle level.
(a) Convert ΔS∘\Delta S^\circ to kJ (+0.0764 kJ/(K⋅molrxn)+0.0764\ \mathrm{kJ/(K{\cdot}mol_{rxn})}):
ΔG∘=17.2−(298)(0.0764)=17.2−22.8=−5.6 kJ/molrxn\Delta G^\circ = 17.2 - (298)(0.0764) = 17.2 - 22.8 = -5.6\ \mathrm{kJ/mol_{rxn}}
(b) The enthalpy term (+17.2 kJ/molrxn+17.2\ \mathrm{kJ/mol_{rxn}}) works against dissolving. The entropy term (−TΔS∘=−22.8 kJ/molrxn-T\Delta S^\circ = -22.8\ \mathrm{kJ/mol_{rxn}}) favors it and is larger. Entropy drives it.
(c) K+\mathrm{K^{+}} and Cl−\mathrm{Cl^{-}} leave the ordered crystal and spread through the whole solution, a big entropy gain. Both ions have a charge of only 1 and fairly large radii, so they hold their hydration shells loosely, and the entropy lost by ordering water is smaller. The net ΔS∘\Delta S^\circ is positive.

Example 2: Calcium carbonate (AP-style)

Calcium carbonate dissolves only slightly:
CaCO3(s)⇌Ca2+(aq)+CO32−(aq)\mathrm{CaCO_3(s) \rightleftharpoons Ca^{2+}(aq) + CO_3^{2-}(aq)}
ΔHsoln∘=−13.1 kJ/molrxn\Delta H^\circ_\mathrm{soln} = -13.1\ \mathrm{kJ/mol_{rxn}} and ΔSsoln∘=−202.9 J/(K⋅molrxn)\Delta S^\circ_\mathrm{soln} = -202.9\ \mathrm{J/(K{\cdot}mol_{rxn})}.
(a) A student claims that because dissolving CaCO3\mathrm{CaCO_3} is exothermic, CaCO3\mathrm{CaCO_3} must be soluble. Use ΔG∘\Delta G^\circ to evaluate the claim. (b) Calculate KspK_{sp} at 25 °C. (c) Explain, in terms of particles, why ΔSsoln∘\Delta S^\circ_\mathrm{soln} is negative for CaCO3\mathrm{CaCO_3} but positive for KCl.
(a)
ΔG∘=−13.1−(298)(−0.2029)=−13.1+60.5=+47.4 kJ/molrxn\Delta G^\circ = -13.1 - (298)(-0.2029) = -13.1 + 60.5 = +47.4\ \mathrm{kJ/mol_{rxn}}
ΔGsoln∘>0\Delta G^\circ_\mathrm{soln} > 0, so the claim is wrong. The favorable enthalpy change is outweighed by the large, unfavorable entropy term (−TΔS∘=+60.5 kJ/molrxn-T\Delta S^\circ = +60.5\ \mathrm{kJ/mol_{rxn}}).
(b)
Ksp=e−ΔG∘/RT=e−(47,400)/[(8.314)(298)]=e−19.13=4.9×10−9K_{sp} = e^{-\Delta G^\circ/RT} = e^{-(47{,}400)/[(8.314)(298)]} = e^{-19.13} = 4.9 \times 10^{-9}
That's close to measured values for calcium carbonate (a few times 10−910^{-9}), so it's insoluble.
(c) Ca2+\mathrm{Ca^{2+}} and CO32−\mathrm{CO_3^{2-}} each carry a charge of 2. Their strong ion-dipole attractions lock many water molecules into tight hydration shells, and the entropy those molecules lose is larger than the entropy the ions gain by leaving the solid. K+\mathrm{K^{+}} and Cl−\mathrm{Cl^{-}} carry charges of only 1, so their shells are looser, and the freed ions win.

Common mistakes

  • Assuming an endothermic process can't happen on its own. KCl and NH4NO3\mathrm{NH_4NO_3} dissolve while absorbing heat because the entropy term wins.
  • Assuming dissolving always increases entropy. The ions spread out, but water ordered in hydration shells can make ΔSsoln∘\Delta S^\circ_\mathrm{soln} negative (LiF, CaCO3\mathrm{CaCO_3}).
  • Predicting solubility from one factor. The factors nearly cancel, so you need the total ΔH∘\Delta H^\circ and ΔS∘\Delta S^\circ (or ΔG∘\Delta G^\circ).
  • Mixing up which steps release energy. Breaking apart the solid and pushing water molecules apart absorb energy. Forming solute-water attractions releases it.
  • Forgetting to convert ΔS∘\Delta S^\circ to kJ before using ΔG∘=ΔH∘−TΔS∘\Delta G^\circ = \Delta H^\circ - T\Delta S^\circ.

AP® is a registered trademark of the College Board, which is not affiliated with Dove's Library and was not involved in the production of, and does not endorse, this website.

Providing free, high-quality AP notes to help students succeed, earn college credit, and reach their educational goals, ensuring everyone has access to the resources they need.

© 2026 Standard Learning Group, Inc., which operates Dove's Library. All rights reserved.