Topic 12: Entropy and Energetics
- Syllabus
- 2017
- Topic
- —
- Level
- A2
A negative enthalpy change can favour a change, but enthalpy alone does not decide whether it occurs. Some endothermic processes happen spontaneously at room temperature because the increase in total entropy outweighs the unfavourable energy transfer.
| Process | Enthalpy observation | Missing decision factor |
|---|---|---|
| ammonium nitrate dissolves in water | solution cools: endothermic | dispersal of ions/energy can make total entropy increase |
| hydrated barium hydroxide reacts with ammonium chloride | strongly endothermic | products and energy can be dispersed in more ways |
The complete criterion combines the reacting system with its surroundings. A change is thermodynamically feasible in the forward direction when ΔStotal is positive at the stated temperature.
‘Endothermic’ does not mean impossible, and ‘exothermic’ does not guarantee feasibility. Enthalpy controls the surroundings contribution, not the whole entropy balance.
Entropy describes disorder through the random dispersal of particles and of energy quanta. A state has higher entropy when the particles or energy can be arranged among more possible distributions.
| Four energy quanta shared by two molecules | Possible allocations |
|---|---|
| all concentrated | (4,0) or (0,4) |
| unevenly shared | (3,1) or (1,3) |
| evenly shared | (2,2) |
With many molecules and quanta, dispersed arrangements vastly outnumber concentrated ones. Natural change therefore tends towards macrostates compatible with more microscopic arrangements.
Entropy is not simply ‘movement’ or visible mess. It concerns the number and dispersal of particle and energy arrangements available to the system.
| Change | Entropy effect | Particle/energy reason |
|---|---|---|
| temperature rises within one state | increases gradually | more energy quanta and distributions become accessible |
| solid → liquid | increases sharply | particles leave fixed lattice positions |
| liquid → gas | increases sharply again | particles occupy a much larger volume with far more arrangements |
On an entropy–temperature graph, entropy rises within each phase and jumps upward at melting and boiling. For water at standard pressure these transitions occur near 273 K and 373 K.
A perfect crystal at 0 K has one perfectly ordered arrangement and is assigned zero entropy. Imperfections or temperatures above 0 K introduce additional arrangements.
During a phase change temperature may remain constant while entropy increases: absorbed energy changes the distribution and state rather than raising temperature.
\Delta S_{total}>0\quad\text{for a thermodynamically feasible forward change}
When a partition is removed, gas molecules spread into the available volume. The dispersed state corresponds to vastly more arrangements than all molecules confined to one side, so entropy increases and spontaneous remixing is overwhelmingly favoured.
| ΔStotal | Thermodynamic interpretation |
|---|---|
| positive | forward direction is feasible |
| zero | boundary/equilibrium condition |
| negative | reverse direction is favoured |
Feasible describes thermodynamic direction, not speed. A positive total entropy change can still correspond to a reaction that is imperceptibly slow because of a high activation energy.
| Process | Main dispersal change | Usual direction |
|---|---|---|
| solid → liquid → gas | particles become less positionally constrained | entropy increases |
| gas → liquid → solid | particles occupy fewer arrangements | entropy decreases |
| ionic solid dissolves | lattice ions disperse through solution, while hydration may order nearby water | direction depends on the balance |
| more moles of gas formed | more independently moving gas particles/distributions | often increases |
| fewer moles of gas formed | fewer gas-particle arrangements | often decreases |
For sodium chloride, ions fixed in a lattice become mobile and dispersed in water; rearrangement/disruption of water structure also contributes, so ΔSsystem is positive. Other salts must be judged from evidence because strong hydration can order water.
Count changes in gas moles before relying on total stoichiometric moles: a solid-to-solid reaction can change particle count without the large dispersal change associated with gases.
\Delta S_{total}=\Delta S_{system}+\Delta S_{surroundings}
| Part | What it includes |
|---|---|
| system | reactants and products specified by the chemical equation |
| surroundings | everything receiving or supplying heat to the system at the stated temperature |
Add the signed values after converting them to the same units. For example, ΔStotal=−78.7 and ΔSsurroundings=+157.4 J K−1 mol−1 give ΔSsystem=−236.1 J K−1 mol−1.
A negative system entropy change does not decide the direction alone; a larger positive surroundings change can make the total positive.
\Delta S_{system}^{\circ}=\sum \nu S^{\circ}(\text{products})-\sum \nu S^{\circ}(\text{reactants})
Multiply each standard molar entropy by its balanced-equation coefficient, total the products, total the reactants, then subtract reactants from products. Preserve state symbols because the same substance has different entropy in different states.
If product entropies total 738.2 and reactant entropies total 401.9 J K−1 mol−1, then ΔSsystem∘=+336.3 J K−1 mol−1. The positive sign means the products have greater entropy.
Do not subtract individual entries before applying stoichiometric coefficients. Standard molar entropy values are usually positive; it is their products-minus-reactants difference that may be negative.
\Delta S_{surroundings}=-\frac{\Delta H}{T}
| Reaction enthalpy | Heat flow | ΔSsurroundings |
|---|---|---|
| exothermic, ΔH<0 | system releases heat | positive |
| endothermic, ΔH>0 | system absorbs heat | negative |
Use temperature in kelvin and make units consistent: convert ΔH from kJ mol−1 to J mol−1 when combining with entropy in J K−1 mol−1. Then add the signed surroundings and system values.
For ΔH=−67.2 kJ mol−1 at 298 K, ΔSsurroundings=+225.5 J K−1 mol−1. The minus sign in the equation reverses the sign of the exothermic enthalpy.
Do not add 0.2255 kJ K−1 mol−1 directly to an entropy in J K−1 mol−1; convert first.
\Delta S_{total}=\Delta S_{system}-\frac{\Delta H}{T}
| ΔH | ΔSsystem | Temperature effect |
|---|---|---|
| negative | positive | feasible at all temperatures |
| positive | negative | not feasible at any temperature |
| positive | positive | high temperature can make the positive system term dominate |
| negative | negative | low temperature can make the positive surroundings term dominate |
\Delta S_{total}=0\Rightarrow T=\frac{\Delta H}{\Delta S_{system}}
At the threshold use kelvin and identical energy units. Decide which side of the threshold is feasible from the signs, not from the algebra alone. The equivalent ΔG=ΔH−TΔSsystem approach is permitted but not required.
Increasing temperature always reduces the magnitude of ΔSsurroundings=−ΔH/T; whether that helps feasibility depends on the sign of ΔH.
| ΔSsystem | ΔSsurroundings | Result |
|---|---|---|
| positive | positive | total necessarily positive |
| positive | negative | feasible if system increase is larger |
| negative | positive | feasible if surroundings increase is larger |
| negative | negative | total necessarily negative |
If ΔSsystem=−120 and ΔSsurroundings=+180 J K−1 mol−1, then ΔStotal=+60 J K−1 mol−1 and the forward reaction is feasible despite the system becoming more ordered.
A negative component is not a veto. Always compare signed magnitudes and state the sign of the total.
| Concept | Deciding evidence | Meaning |
|---|---|---|
| thermodynamic stability/feasibility | sign of ΔStotal (or ΔG) | whether products or reactants are favoured energetically/entropically |
| kinetic stability | activation energy and rate | whether conversion occurs fast enough to observe |
A reaction can be thermodynamically feasible (ΔStotal>0) but extremely slow because a large activation barrier makes the reactant kinetically stable. Heating or a catalyst can increase rate without changing the thermodynamic balance.
‘Does not react’ is ambiguous: it may be thermodynamically unfavourable or merely too slow. Entropy data diagnose the first; kinetic evidence and activation energy diagnose the second.
| Quantity | Definition for one mole | Typical sign |
|---|---|---|
| standard atomisation enthalpy, ΔatH∘ | element in its standard state forms gaseous atoms | positive |
| first electron affinity | gaseous atoms each gain one electron to form gaseous 1− ions | usually negative |
| subsequent electron affinity | a gaseous negative ion gains another electron | may be positive because of repulsion |
| lattice energy, ΔlattH∘ | gaseous ions form one mole of ionic solid | negative with this formation convention |
\ce{X(g) + e^- -> X^-(g)}
This course defines lattice energy for formation, so it is exothermic. Reversing the arrow to separate the solid into gaseous ions changes the sign.
| Stage from elements to ionic solid | Enthalpy term |
|---|---|
| elements in standard states → gaseous atoms | atomisation enthalpies with stoichiometric factors |
| gaseous metal atoms → gaseous cations + electrons | successive ionisation energies |
| gaseous non-metal atoms + electrons → gaseous anions | electron affinities, including successive values |
| gaseous ions → ionic solid | lattice energy of formation |
\Delta_fH^{\circ}=\sum\Delta_{at}H^{\circ}+\sum IE+\sum EA+\Delta_{latt}H^{\circ}
For MgCl2, include atomisation of one Mg and two Cl atoms, first and second ionisation energies of Mg, twice the first electron affinity of Cl, then lattice energy. Every line needs correct formulae, charges, electrons, coefficients and state symbols.
Apply Hess’s law around the closed cycle and rearrange only after all arrows have signs. A step used in reverse contributes the negative of its stated value.
Do not use Cl2(g) where gaseous Cl atoms are required, or omit the second ionisation energy for Mg2+.
| Comparison | Interpretation |
|---|---|
| experimental Born–Haber value close to theoretical value | electrostatic ionic model fits; bonding is predominantly ionic |
| experimental value appreciably more exothermic than theoretical | real lattice has extra stabilisation from covalent character |
The theoretical value treats ions as spherical charges interacting electrostatically. Its magnitude becomes larger for higher ionic charges and smaller ionic radii because attraction is stronger at shorter distance.
NaF shows close experimental/theoretical values, while MgCl2 shows a larger discrepancy. The higher-charge Mg2+ distorts the larger Cl− electron cloud more strongly, adding covalent character beyond the simple ionic model.
Compare both the overall magnitude and the experimental–theoretical gap. A more negative lattice energy can arise from stronger ionic attraction even when the percentage covalent character is small.
| Ion feature | Effect |
|---|---|
| small, highly charged cation | high charge density; strong polarising power |
| large anion | diffuse electron cloud; high polarisability |
| strong cation–anion combination | anion cloud is distorted toward cation, creating shared electron density |
A fluoride ion is small and difficult to polarise, so calcium fluoride is close to the ionic model. Iodide is larger and readily polarised by Ca2+, so calcium iodide has more covalent character and a larger experimental–theoretical lattice-energy difference.
Polarisation does not mean the compound ceases to be ionic. It describes a continuum: an ionic lattice can contain a measurable degree of covalent character.
| Quantity | Defined change for one mole |
|---|---|
| ΔsolH∘ | one mole of ionic solid dissolves in enough water to form an infinitely dilute solution |
| ΔhydH∘ of an ion | one mole of gaseous ions becomes completely hydrated as aqueous ions at infinite dilution |
\ce{M^{z+}(g) -> M^{z+}(aq)}
Hydration is normally exothermic because ion–dipole attractions form between ions and water. Enthalpy of solution may be positive or negative because separating the lattice costs energy while hydrating the ions releases energy.
Hydration enthalpy does not mean dissolving one mole of ions in one mole of water or making a 1 mol dm−3 solution; the definition is complete hydration at infinite dilution.
\Delta_{sol}H^{\circ}=-\Delta_{latt}H^{\circ}+\sum\Delta_{hyd}H^{\circ}(\text{ions})
| Route | Enthalpy direction with formation-convention lattice energy |
|---|---|
| ionic solid → gaseous ions | reverse lattice energy, −ΔlattH∘, positive |
| gaseous ions → aqueous ions | sum of ion hydration enthalpies, negative |
| ionic solid → aqueous ions | enthalpy of solution, their algebraic sum |
For MX2, include one cation hydration term and twice the anion hydration term. If a missing anion value is required, subtract the known lattice/solution/cation terms, then divide by two.
Label every energy level with formulae, charges and state symbols. Arrow direction controls sign: the course lattice energy arrow points from gaseous ions down to solid.
Do not add the negative lattice energy directly when dissolving the solid; dissolution uses the reverse, endothermic lattice-separation step.
| Change | Lattice energy of formation | Hydration enthalpy |
|---|---|---|
| higher ionic charge | more negative: stronger ion–ion attraction | more negative: stronger ion–dipole attraction |
| smaller ionic radius | more negative: ions approach more closely | more negative: water approaches charge more closely |
| larger ionic radius | less negative | less negative |
Lattice energy depends on both ions’ charges and their separation; hydration enthalpy is quoted for one ion and follows its charge density. Down a group, anions become larger, so both their hydration enthalpy and the corresponding lattice energy generally become less exothermic.
For NH4Cl versus NH4Br, Br− is larger: its hydration is less exothermic, but the NH4Br lattice energy is also less exothermic. Because both effects weaken, their difference—and hence ΔsolH—may remain similar.
Do not predict enthalpy of solution from hydration or lattice energy alone; it is the difference between both large contributions.
\Delta S_{total}=\Delta S_{system}-\frac{\Delta_{sol}H}{T}
| Supplied value | Role in solubility prediction |
|---|---|
| ΔSsystem for dissolving | measures dispersal/order change of solute and water |
| ΔsolH | sets the surroundings entropy term |
| temperature | changes the magnitude of −ΔsolH/T |
| resulting ΔStotal | positive value supports thermodynamically feasible dissolving |
KCl has an endothermic ΔsolH of about +17 kJ mol−1 yet is soluble because its positive system entropy change is large enough to make ΔStotal positive at 298 K.
Use supplied entropy and enthalpy data to explain the Unit 2 trends: Group 2 hydroxides become more soluble down the group, whereas Group 2 sulfates become less soluble. Compare the total entropy balance for each salt rather than relying on lattice energy alone.
Positive ΔStotal predicts thermodynamic feasibility, not an exact solubility or a fast dissolving rate. Equilibrium position and kinetics remain distinct.