The single idea: more spread-out matter/energy = more microstates = higher S. Gases have far more microstates than liquids, liquids more than solids.
(a) Vapour → liquid: gas becomes liquid, molecules lose freedom → ΔSsys<0.
(b) Solid → gas: huge jump in freedom → ΔSsys>0.
(c) Count gas moles: left =1+3=4 mol gas; right =2 mol gas. Fewer gas moles → ΔSsys<0.
(d) A cold object gaining heat: its molecules jiggle over more energy levels → ΔSsys>0.
Rule of thumb used:Δngas>0⇒ΔS>0; heating something ⇒ΔS>0.
WHAT: the surroundings receive the heat the system dumps. WHY this formula: at constant P, qP=ΔH, and heat into surroundings is −ΔHsys, so
ΔSsurr=T−ΔHsys=310K−(−145000J)=+468J K−1.
Positive: exothermic reaction warms the surroundings, spreading energy → more microstates for them.
Recall Solution L2.2
At the boiling point liquid and vapour coexist reversibly, so the phase change is isothermal and reversible: qrev=ΔHvap.
ΔSsys=Tqrev=37340700=+109J K−1mol−1.
Positive because liquid → gas is a big jump in microstates. (This value near +109 is Trouton's rule — most liquids sit near 85–110J K−1mol−1.)
Recall Solution L2.3
WHY this formula: for an ideal gas at constant T, ΔU=0, so all the reversible heat becomes expansion work and ΔS=nRlnV1V2. Here V2/V1=3.
ΔS=nRlnV1V2=2.0×8.314×ln3=16.628×1.0986=+18.3J K−1.
Positive: bigger box = more positions per molecule = more microstates.
WHAT: we need the total entropy change, because the second law tests the universe, not the system.
First the surroundings:
ΔSsurr=T−ΔHsys=29855000=+184.6J K−1.
Then the total:
ΔSuniv=ΔSsys+ΔSsurr=−110+184.6=+74.6J K−1>0.Spontaneous. The system got more ordered (ΔSsys<0), but the large heat released disordered the surroundings even more — the sum still climbs. This is exactly the energy-bookkeeping point: the system can order itself if it pays the surroundings enough heat.
Recall Solution L3.2
Spontaneity fails when ΔSuniv falls to zero:
ΔSuniv=ΔSsys−TΔHsys=0⇒T=ΔSsysΔHsys.T=−110−55000=500K.Below 500K: the surroundings term (which grows as T shrinks) wins → spontaneous. Above 500K: the TΔH term shrinks, the system's own order (ΔSsys<0) dominates → non-spontaneous. See the figure — the two contributions cross exactly at 500K.
Step 1 — surroundings at 298 K. Melting absorbs heat, so heat leaves the surroundings: ΔHsys=+6010J (endothermic), thus
ΔSsurr=T−ΔHsys=298−6010=−20.17J K−1.Step 2 — total at 298 K.ΔSuniv=+22.0+(−20.17)=+1.83J K−1>0⇒spontaneous.Step 3 — why 273 K is different. Redo the surroundings at the melting point:
ΔSsurr(273)=273−6010=−22.0J K−1,
so ΔSuniv=22.0−22.0=0 → equilibrium, ice and water coexist.
The deep point:ΔSsys (a property of the substances) barely changes with T, but ΔSsurr=−ΔHsys/T shrinks in size as T grows. At the melting point they cancel; heat the system a little and the surroundings term weakens, tipping ΔSuniv positive — melting wins. This is a reversible vs irreversible boundary crossing.
Recall Solution L4.2
WHY an integral, not q/T? Here T is changing, so we cannot pull it out of ∫dqrev/T. At constant volume dqrev=CVdT, so
ΔS=∫T1T2TCVdT=CVlnT1T2.WHAT the ln does: summing up T1 across every tiny heating step gives a logarithm — each degree added near a cold start raises entropy more than the same degree near a hot end.
ΔS=12.47×ln300600=12.47×0.6931=+8.64J K−1.
Positive: hotter gas accesses more energy microstates (a Boltzmann spreading).
(a) Free expansion: gas pushes against nothing, so w=0; insulated, so q=0. Indeed ΔU=0 too (ideal gas, T unchanged).
(b) Entropy is a state function — it depends only on the start and end states, not the path taken. So to compute ΔS we imagine a reversible path between the same endpoints and use it:
ΔSsys=nRlnV1V2=1×8.314×ln2=+5.76J K−1.(c) No contradiction. The definition uses qrev, not the actual q. The real path had q=0, but the reversible replacement path would exchange qrev=nRTln2>0. The gas ends up more spread out either way, so ΔSsys>0.
Second-law check: surroundings unchanged (qsurr=0⇒ΔSsurr=0), so ΔSuniv=+5.76>0 — irreversible and spontaneous, exactly as expected.
Recall Solution L5.2
(a)S=kBln1=kB×0=0. This is the Third Law: a perfect crystal at absolute zero has zero entropy — the one degenerate, perfectly-ordered case that anchors the entropy scale.
(b) Take the log of a product: ln(4NA)=NAln4. So
S=kBNAln4=Rln4=8.314×1.3863=+11.5J K−1mol−1.
(We used kBNA=R.) Real disordered solids like CO ice do have a small residual S — an experimental fingerprint that S=kBlnW is literally counting arrangements.
Recall Self-test summary (reveal after attempting all)