Entropy and Gibbs Free Energy
Enthalpy alone is insufficient to predict whether a reaction will occur spontaneously. The
Dissolution of ammonium nitrate in water is endothermic yet proceeds spontaneously. The
Decomposition of calcium carbonate requires continuous heating. To resolve these cases, we need a
Second state function: entropy, and its combination with enthalpy in the Gibbs free energy.
Entropy (S)
Statistical Definition
Entropy is a measure of the number of microstates (W) accessible to a system — that is, the
Number of ways the energy of the system can be distributed among its particles:
S=kBlnW
Where kB=1.381×10−23J/K is the Boltzmann constant. A system with more
Accessible microstates has higher entropy. This is the Boltzmann equation, engraved on his
Tombstone.
Thermodynamic Definition
The entropy change is defined as:
ΔS=∫L◆B◆δqrev◆RB◆◆LB◆T◆RB◆
For an isothermal process:
ΔS=L◆B◆qrev◆RB◆◆LB◆T◆RB◆
This shows that entropy is heat divided by temperature. Transferring a given amount of heat at a
Lower temperature produces a larger entropy change than at a higher temperature.
Factors Affecting Entropy
| Factor | Effect on S | Rationale |
|---|
| More gas molecules produced | Increase | More ways to distribute energy among more particles |
| Change from solid to liquid to gas | Increase | Gases have the most microstates; solids the fewest |
| Higher temperature | Increase | More energy available to distribute; more accessible microstates |
| Dissolution of a solid ionic compound | Increase () | Ions dispersed in solution have more freedom than in the lattice |
| Fewer moles of gas | Decrease | Fewer particles, fewer microstates |
| Increased pressure of a gas | Decrease | Reduced volume constrains the available positions |
Standard Entropy Values (S∘)
Standard entropies are absolute values (not relative to a reference, unlike enthalpy). At
0KA perfect crystal has S=0 (third law of thermodynamics). Standard entropies are
Always positive.
Typical values (Jmol−1K−1):
| Substance | S∘ |
|---|
| C(diamond) | 2.4 |
| C(graphite) | 5.7 |
| Fe(s) | 27.3 |
| NaCl(s) | 72.1 |
| H2O(l) | 69.9 |
| H2O(g) | 188.8 |
| CO2(g) | 213.7 |
| N2(g) | 191.6 |
Gases have much higher standard entropies than liquids and solids. Diamond has a lower entropy than
Graphite due to its more rigid, ordered structure.
Standard Entropy Change
ΔS∘=∑S∘(products)−∑S∘(reactants)
Worked Example. Calculate ΔS∘ for the thermal decomposition of calcium carbonate:
CaCO3(s)→CaO(s)+CO2(g)
ΔS∘=S∘(CaO)+S∘(CO2)−S∘(CaCO3)=38.1+213.7−92.9=+158.9Jmol−1K−1
The entropy increases because a gas is produced from a solid, creating many more microstates.
The Second Law of Thermodynamics
The total entropy of the universe increases in any spontaneous process:
ΔSuniverse=ΔSsystem+ΔSsurroundings>0
At equilibrium: ΔSuniverse=0.
Entropy Change of the Surroundings
The surroundings gain or lose heat as a result of the reaction. The entropy change of the
Surroundings is:
ΔSsurroundings=−L◆B◆ΔHsystem◆RB◆◆LB◆T◆RB◆
The negative sign arises because when the system releases heat (exothermic, ΔH<0), the
Surroundings gain that heat and their entropy increases. When the system absorbs heat (endothermic,
ΔH>0), the surroundings lose heat and their entropy decreases.
Combining with the second law:
ΔSuniverse=ΔSsystem−L◆B◆ΔHsystem◆RB◆◆LB◆T◆RB◆>0
Multiplying through by T (which is always positive):
TΔSsystem−ΔHsystem>0
Rearranging:
ΔHsystem−TΔSsystem<0
Gibbs Free Energy (G)
Derivation
The inequality above defines the Gibbs free energy:
ΔG=ΔH−TΔS
This is the most important equation in chemical thermodynamics. It combines the enthalpy and entropy
Contributions into a single quantity that determines spontaneity.
Spontaneity Criterion
| ΔG | Process |
|---|
| ΔG<0 | Spontaneous (thermodynamically favourable) |
| ΔG=0 | At equilibrium |
| ΔG>0 | Non-spontaneous (thermodynamically unfavourable) |
A spontaneous process is one that proceeds without external intervention once initiated.
“Spontaneous” does not mean “fast” — kinetics determines the rate; thermodynamics determines the
Direction.
Standard Gibbs Free Energy Change
ΔG∘=ΔH∘−TΔS∘
This uses standard enthalpy and entropy data at 298K.
Relationship to the Equilibrium Constant
ΔG∘=−RTlnK
Where R=8.314Jmol−1K−1, T is in Kelvin, and K is the equilibrium
Constant (dimensionless, using activities).
This equation is one of the most powerful in chemistry because it connects thermodynamic data to
Measurable equilibrium constants.
| ΔG∘ | K | Equilibrium Position |
|---|
| ΔG∘<0 | K>1 | Products favoured |
| ΔG∘=0 | K=1 | Neither favoured |
| ΔG∘>0 | K<1 | Reactants favoured |
Worked Example. For the Haber process at 298K:
N2(g)+3H2(g)⇌2NH3(g)
ΔH∘=−92kJ/mol, ΔS∘=−199Jmol−1K−1.
ΔG∘=−92000−298×(−199)=−92000+59302=−32698J/mol=−32.7kJ/mol
Since ΔG∘<0The reaction is spontaneous at 298K (but kinetically
Extremely slow without a catalyst).
K=exp(L◆B◆−ΔG∘◆RB◆◆LB◆RT◆RB◆)=exp(L◆B◆32698◆RB◆◆LB◆8.314×298◆RB◆)=exp(13.19)=5.3×105
The equilibrium constant is very large, confirming that products are strongly favoured at
298K.
Temperature Dependence of Feasibility
The ΔG=ΔH−TΔS equation reveals that the spontaneity of a reaction can change
With temperature. The four cases:
| ΔH | ΔS | Low T | High T | Example |
|---|
| − | + | Spontaneous | Spontaneous | Combustion of hydrogen |
| − | − | Spontaneous | Non-spontaneous | Freezing of water |
| + | + | Non-spontaneous | Spontaneous | Thermal decomposition of CaCO3 |
| + | − | Non-spontaneous | Non-spontaneous | Decomposition of N2O |
The Temperature of Equilibrium
The temperature at which a reaction changes from spontaneous to non-spontaneous (or vice versa) is
The temperature at which ΔG=0:
T=L◆B◆ΔH∘◆RB◆◆LB◆ΔS∘◆RB◆
Worked Example. At what temperature does the thermal decomposition of calcium carbonate become
Spontaneous?
CaCO3(s)→CaO(s)+CO2(g)
ΔH∘=+178kJ/mol, ΔS∘=+160Jmol−1K−1.
T=L◆B◆178×103◆RB◆◆LB◆160◆RB◆=1113K=840∘C
Above 1113K, ΔG∘<0 and decomposition is spontaneous. In a lime kiln,
Temperatures of approximately 900—1000∘C are used to ensure thermodynamic
Feasibility while maintaining a practical rate.
Graphical Interpretation
A plot of ΔG∘ vs T is a straight line with slope =−ΔS∘ and y-intercept
=ΔH∘ (at T=0).
- When ΔS∘>0: the line slopes downward. The reaction becomes more spontaneous as
temperature increases.
- When ΔS∘<0: the line slopes upward. The reaction becomes less spontaneous as
temperature increases.
- The x-intercept (ΔG∘=0) gives the equilibrium temperature.
Important caveat: This linear extrapolation assumes that ΔH∘ and ΔS∘
Are independent of temperature (Kirchhoff’s approximation). This is a reasonable approximation over
Small temperature ranges but fails over large ranges where heat capacities change significantly.
Non-Standard Conditions: ΔG vs ΔG∘
The standard free energy change (ΔG∘) applies when all reactants and products are in
Their standard states (1 mol/dm3 for solutions, 1 bar for gases). Under non-standard conditions:
ΔG=ΔG∘+RTlnQ
Where Q is the reaction quotient (the same expression as K but with current, non-equilibrium
Concentrations or partial pressures).
At equilibrium, Q=K and ΔG=0Recovering ΔG∘=−RTlnK.
Industrial Applications
The Haber Process
N2(g)+3H2(g)⇌2NH3(g)ΔH∘=−92kJ/mol
ΔH∘<0 (exothermic), ΔS∘<0 (4 moles of gas to 2 moles). By Le
Chatelier’s principle and the Gibbs equation:
- Low temperature favours the forward reaction (exothermic). But low temperature gives a slow
rate.
- High pressure favours the forward reaction (fewer gas moles on the product side).
- Compromise: 450∘C, 200atmWith an iron catalyst.
2SO2(g)+O2(g)⇌2SO3(g)ΔH∘=−198kJ/mol
ΔH∘<0, ΔS∘<0 (3 moles to 2 moles). Low temperature favours the
Product but slows the rate. Industrial conditions: 450∘C, 1—2atm
V2O5 catalyst.
Fe2O3(s)+3CO(g)⇌2Fe(l)+3CO2(g)ΔH∘=−23kJ/mol
ΔH∘<0 but small. The entropy change is favourable (3 moles of gas reactants to 3
Moles of gas products, but the solid is consumed). At the blast furnace temperature
(≈1500∘C), the reaction is thermodynamically feasible.
Common Pitfalls
-
Unit mismatch in the Gibbs equation. ΔH is in kJ/molWhile ΔS is in
Jmol−1K−1. Always convert to consistent units before combining: either
convert ΔH to J/mol or ΔS to kJmol−1K−1.
-
Using ΔG<0 to predict rate. Thermodynamics says nothing about kinetics. A
reaction with ΔG≪0 may be immeasurably slow (e.g. Diamond conversion to graphite at
room temperature: ΔG∘≈−2.9kJ/molBut the half-life is effectively
infinite).
-
Forgetting that ΔS∘ values are absolute. Unlike ΔHf∘ (which is
relative to elements in standard states), S∘ values are absolute entropies. S∘ of
an element in its standard state is not zero (except at 0K).
-
Confusing ΔG with ΔG∘. ΔG∘ is the free energy change under
standard conditions. The actual free energy change ΔG depends on the specific
concentrations/pressures and is given by ΔG=ΔG∘+RTlnQ.
-
Assuming the linear ΔG vs T relationship holds indefinitely. The equation
ΔG=ΔH−TΔS assumes ΔH and ΔS are temperature-independent.
Over large temperature ranges, this approximation fails.
Practice Problems
Problem 1
For the reaction C(s)+H2O(g)→CO(g)+H2(g):
ΔH∘=+131kJ/mol, ΔS∘=+134Jmol−1K−1.
(a) Calculate ΔG∘ at 298K. Is the reaction spontaneous? (b) At what
Temperature does the reaction become spontaneous? (c) Calculate K at 1000K.
Solution:
(a)
ΔG∘=131000−298×134=131000−39932=+91068J/mol=+91.1kJ/mol
ΔG∘>0: not spontaneous at 298K.
(b)
T=L◆B◆ΔH∘◆RB◆◆LB◆ΔS∘◆RB◆=134131000=978K=705∘C
Above 978KThe reaction becomes spontaneous.
(c) At 1000K:
ΔG∘=131000−1000×134=131000−134000=−3000J/mol
K=exp(L◆B◆−ΔG∘◆RB◆◆LB◆RT◆RB◆)=exp(L◆B◆3000◆RB◆◆LB◆8.314×1000◆RB◆)=exp(0.361)=1.43
K=1.43So products are slightly favoured at 1000K.
Problem 2
The melting of ice: H2O(s)→H2O(l) has
ΔH∘=+6.01kJ/mol and
ΔS∘=+22.0Jmol−1K−1.
(a) Calculate the normal melting point of ice. (b) Explain why ice melts spontaneously at room
Temperature despite the process being endothermic.
Solution:
(a) At the melting point, ΔG=0:
T=L◆B◆ΔH∘◆RB◆◆LB◆ΔS∘◆RB◆=22.06010=273K=0∘C
(b) Although ΔH∘>0 (endothermic), ΔS∘>0 (entropy increases). At
Temperatures above 273KThe TΔS term exceeds ΔHMaking ΔG<0.
The entropy gain from the increased disorder of the liquid phase more than Compensates for the
enthalpy cost of breaking the hydrogen-bonded lattice.
Problem 3
For the reaction 2NO2(g)⇌N2O4(g) at
298K:
ΔH∘=−57.2kJ/mol, ΔS∘=−175.8Jmol−1K−1.
(a) Calculate ΔG∘ and Kp at 298K. (b) At what temperature does
Kp=1? (c) Explain qualitatively whether increasing temperature increases or decreases the yield
of N2O4.
Solution:
(a)
ΔG∘=−57200−298×(−175.8)=−57200+52388=−4812J/mol=−4.81kJ/mol
Kp=exp(L◆B◆4812◆RB◆◆LB◆8.314×298◆RB◆)=exp(1.943)=6.98
(b) Kp=1 when ΔG∘=0:
T=L◆B◆ΔH∘◆RB◆◆LB◆ΔS∘◆RB◆=−175.8−57200=325K
(c) The forward reaction is exothermic (ΔH∘<0) and decreases entropy
(ΔS∘<0). Increasing temperature makes ΔG∘ less negative (eventually
positive), so Kp decreases. The yield of N2O4 decreases with increasing
temperature. This is consistent with Le Chatelier’s principle.
Entropy in Chemical Processes
Entropy of Phase Changes
At a phase transition, ΔG=0So ΔS=ΔH/T.
For vaporisation: ΔSvap=ΔHvap/Tboil
Trouton’s rule: ΔSvap≈85Jmol−1K−1 for most non-polar
liquids. Deviations indicate hydrogen bonding (e.g. Water:
ΔSvap=109Jmol−1K−1Due to extra ordering in the liquid from
H-bonds).
Entropy of Mixing
When two ideal gases (or two ideal solutions) mix, the entropy always increases:
ΔSmix=−nR(x1lnx1+x2lnx2)
Where x1 and x2 are the mole fractions. For equal amounts (x1=x2=0.5):
ΔSmix=−nR(0.5ln0.5+0.5ln0.5)=−nR(−0.693)=5.76nJ/K
This is the thermodynamic basis for diffusion: gases spontaneously mix because the mixed state has
higher entropy.
The Third Law of Thermodynamics
The entropy of a perfect crystal at absolute zero is zero:
S(0K)=0
This provides the reference point for absolute entropies (S∘ values tabulated in data books).
Unlike enthalpy, entropy has an absolute scale.
Worked Example: Calculating ΔS∘ from Absolute Entropies
Calculate ΔS∘ for the combustion of methane:
CH4(g)+2O2(g)→CO2(g)+2H2O(l)
S∘ values:
\mathrm{CH}_4(g) = 186.3$$\mathrm{O}_2(g) = 205.1$$\mathrm{CO}_2(g) = 213.7$$\mathrm{H}_2\mathrm{O}(l) = 69.9\,\mathrm{J\,mol^{-1}\,K^{-1}}.
ΔS∘=[213.7+2(69.9)]−[186.3+2(205.1)]=353.5−596.5=−243.0Jmol−1K−1
The entropy decreases because 3 moles of gas produce 1 mole of gas + 2 moles of liquid. The decrease
in the number of gaseous molecules dominates.
Gibbs Free Energy in Biological Systems
ATP hydrolysis is the energy currency of cells:
ATP+H2O→ADP+PiΔG∘=−30.5kJ/mol
The large negative ΔG∘ makes this reaction thermodynamically favourable, and it is
coupled to endergonic (unfavourable) reactions in the cell. For example, the synthesis of
glucose-6-phosphate from glucose and phosphate (ΔG∘=+13.8kJ/mol) is driven
by coupling with ATP hydrolysis:
Glucose+Pi+ATP→Glucose-6-phosphate+ADP
ΔGoverall∘=13.8+(−30.5)=−16.7kJ/mol
The coupled reaction is spontaneous because the overall ΔG∘ is negative.
Thermodynamic Cycles
Born-Haber Cycles (Recap)
Born-Haber cycles apply Hess’s Law to ionic compound formation. They are covered in detail in
Born-Haber Cycles.
Enthalpy-Entropy Compensation
Some reactions show enthalpy-entropy compensation: a more exothermic ΔH is offset by a more
negative ΔSSo ΔG changes less than expected. This is common in:
- Solvent reorganisation around dissolved species.
- Protein folding (hydrophobic effect).
- Ligand binding.
Worked Examples: Comprehensive Gibbs Free Energy Problems
Problem: Predicting Spontaneity at Different Temperatures
For the reaction
C(graphite)+CO2(g)⇌2CO(g):
ΔH∘=+173kJ/mol,ΔS∘=+176Jmol−1K−1
(a) Calculate ΔG∘ at 298K and 1000K.
(b) At what temperature does the reaction become spontaneous?
(c) Calculate K at 1000K.
(a) At 298K:
ΔG∘=173×103−298×176=173000−52448=+120552J/mol=+120.6kJ/mol
Not spontaneous at room temperature.
At 1000K:
ΔG∘=173×103−1000×176=173000−176000=−3000J/mol=−3.0kJ/mol
Spontaneous at 1000K.
(b) ΔG∘=0 when:
T=L◆B◆ΔH∘◆RB◆◆LB◆ΔS∘◆RB◆=L◆B◆173×103◆RB◆◆LB◆176◆RB◆=983K
(c) At 1000K:
K=exp(L◆B◆−ΔG∘◆RB◆◆LB◆RT◆RB◆)=exp(L◆B◆3000◆RB◆◆LB◆8.314×1000◆RB◆)=exp(0.361)=1.43
K>1Confirming that products are favoured.
Problem: Using Gibbs Energy to Predict Decomposition
Will Ag2CO3(s) decompose at 500K?
Ag2CO3(s)→Ag2O(s)+CO2(g)
\Delta H^\circ = +82\,\mathrm{kJ/mol}$$\Delta S^\circ = +170\,\mathrm{J\,mol^{-1}\,K^{-1}}.
ΔG∘=82000−500×170=82000−85000=−3000J/mol
ΔG∘<0So the decomposition is spontaneous at 500K. (The threshold
temperature is T=82000/170=482K.)
Advanced Entropy and Gibbs Energy
Entropy Changes of Mixing
When two ideal gases mix, the entropy always increases because there are more ways to arrange the
molecules in the larger volume.
Worked Example: 1.0mol of He and 1.0mol of
NeBoth initially in separate 10.0dm3 containers at 298KAre
allowed to mix in a combined volume of 20.0dm3. Calculate ΔSmix.
ΔSmix=−nR(xHelnxHe+xNelnxNe)
Where xHe=xNe=0.5:
ΔSmix=−(1.0+1.0)×8.314×(0.5ln0.5+0.5ln0.5)
=−2.0×8.314×ln0.5=−16.63×(−0.693)=+11.5JK−1
Phase Transitions and Entropy
At a phase transition, the system is at equilibrium so ΔG=0Giving:
ΔStransition=L◆B◆ΔHtransition◆RB◆◆LB◆Ttransition◆RB◆
| Transition | ΔH | ΔS | ΔG |
|---|
| Melting (fusion) | Positive (endothermic) | Positive (disorder increases) | 0 (at Tm) |
| Boiling (vaporisation) | Positive (endothermic) | Positive (large increase in disorder) | 0 (at Tb) |
| Freezing | Negative (exothermic) | Negative (order increases) | 0 (at Tm) |
| Sublimation | Positive (endothermic) | Positive | 0 (at Tsub) |
Worked Example: Calculate the entropy of vaporisation of water at 373K given
ΔHvap=+40.7kJ/mol.
ΔSvap=37340700=+109Jmol−1K−1
This is close to Trouton’s rule (ΔSvap≈88Jmol−1K−1 for
non-hydrogen-bonding liquids). Water is higher because of extensive hydrogen bonding in the liquid
phase.
Born-Haber Cycles and Gibbs Energy
Gibbs energy of formation can be calculated from Born-Haber cycles by using
ΔG=ΔH−TΔS for each step.
Worked Example: Calculate ΔGf∘ for NaCl(s) at 298K.
Using the Born-Haber cycle values:
- ΔHf∘(NaCl)=−411kJ/mol
- ΔSf∘=−72.1Jmol−1K−1 (system becomes more ordered: solid from
gas atoms)
ΔGf∘=−411000−298×(−72.1)=−411000+21486=−389514J/mol=−389.5kJ/mol
Coupled Reactions in Biochemistry
A thermodynamically unfavourable reaction (ΔG>0) can be driven by coupling it to a
thermodynamically favourable one (ΔG<0), provided the overall ΔG<0.
Example: Hydrolysis of ATP:
ATP+H2O→ADP+PiΔG∘=−30.5kJ/mol
This strongly exergonic reaction drives many endergonic processes in cells. If a reaction requires
+20kJ/molCoupling with ATP hydrolysis gives:
ΔGoverall=+20.0+(−30.5)=−10.5kJ/mol
Gibbs Energy and Equilibrium: Quantitative Treatment
The relationship between ΔGThe reaction quotient QAnd the equilibrium constant K:
ΔG=ΔG∘+RTlnQ
At equilibrium, ΔG=0 and Q=KGiving:
ΔG∘=−RTlnK
Worked Example: For the reaction
N2O4(g)⇌2NO2(g) at 298K:
ΔG∘=+4.72kJ/mol. Calculate K.
K=exp(L◆B◆−ΔG∘◆RB◆◆LB◆RT◆RB◆)=exp(L◆B◆−4720◆RB◆◆LB◆8.314×298◆RB◆)=exp(−1.905)=0.149
If the initial pressure of N2O4 is 1.00atm and no NO2
is present:
Q=L◆B◆(pNO2)2◆RB◆◆LB◆pN2O4◆RB◆=10=0
ΔG=4720+8.314×298×ln0=4720+(−∞)→−∞
ΔG is very negative, so the forward reaction is strongly favoured initially (the reaction
proceeds to the right until equilibrium is reached).
Common Pitfalls
-
Sign errors in ΔG=ΔH−TΔS: Remember the minus sign. A positive
ΔH and positive ΔS means the reaction is spontaneous at high T (the
−TΔS term dominates). Students often incorrectly write ΔG=ΔH+TΔS.
-
Units of ΔS: Always use Jmol−1K−1 for entropy and
kJ/mol for enthalpy. You must convert one of them before combining. Forgetting to
convert ΔS from J to kJ (divide by 1000) is the single most common
arithmetic error.
-
Standard vs non-standard conditions: ΔG∘ applies only when all components are in
their standard states (1 mol/dm3 for solutions, 100kPa for gases, pure
solids/liquids). Under non-standard conditions, use ΔG=ΔG∘+RTlnQ.
-
Assuming ΔG∘<0 means the reaction happens quickly: Thermodynamic feasibility
does not imply kinetic feasibility. Diamond converting to graphite has ΔG∘<0 but
the rate is essentially zero at room temperature.
-
Entropy of a pure element: The absolute entropy of a pure element in its standard state at
298K is not zero (only S∘ at 0K is zero, by the third law).
Practical Applications: Gibbs Energy in Industry
| Industrial Process | Reaction | ΔH∘ (kJ/mol) | ΔS∘ (J/mol/K) | Tthreshold (K) |
|---|
| Haber process | N2+3H2→2NH3 | −92 | −199 | Not applicable (ΔH<0, ΔS<0: spontaneous at low T) |
| Contact process | 2SO2+O2→2SO3 | −198 | −190 | Not applicable |
| Thermal decomposition of CaCO3 | CaCO3→CaO+CO2 | +178 | +161 | 1106 |
| Roasting of ZnS | 2ZnS+3O2→2ZnO+2SO2 | −880 | +100 | Spontaneous at all T |
Exam-Style Questions with Full Mark Schemes
Q1 (5 marks)
For the reaction C(s)+H2O(g)→CO(g)+H2(g):
ΔH∘=+131kJ/mol, ΔS∘=+134Jmol−1K−1.
(a) Calculate ΔG∘ at 298K and state whether the reaction is feasible. (3
marks)
(b) Calculate the minimum temperature at which the reaction becomes feasible. (2 marks)
Mark Scheme:
(a)
ΔG∘=131000−298×134=131000−39932=+91068J/mol=+91.1kJ/mol
(2 marks for calculation).
ΔG∘>0So the reaction is not feasible at 298K (1 mark).
(b) ΔG∘=0 when T=ΔH∘/ΔS∘=131000/134=978K
(2 marks).
The reaction becomes feasible above 978K.
Q2 (6 marks)
Explain why the entropy change for the reaction
N2O4(g)⇌2NO2(g) is positive, and calculate
ΔS∘ given the following standard entropies:
S∘(N2O4)=304Jmol−1K−1,
S∘(NO2)=240Jmol−1K−1.
Mark Scheme:
The entropy change is positive because one mole of gas produces two moles of gas (1 mark). There are
more ways to arrange the molecules and more microstates when there are more gas particles (1 mark).
The products have greater positional disorder than the reactants (1 mark).
ΔS∘=2×240−304=480−304=+176Jmol−1K−1 (3 marks
for calculation with correct units).
Q3 (5 marks)
A student claims that because the combustion of methane is highly exothermic
(ΔHc∘=−890kJ/mol), it must be thermodynamically feasible at all
temperatures. Evaluate this claim.
Mark Scheme:
CH4(g)+2O2(g)→CO2(g)+2H2O(l)
ΔS∘=[213+2(70)]−[186+2(205)]=353−596=−243Jmol−1K−1
(2 marks).
Since ΔH<0 and ΔS<0The reaction is feasible only when
ΔG=ΔH−TΔS<0I.e. When
T<∣ΔH/ΔS∣=890000/243=3663K (2 marks).
The claim is correct in practice (combustion is feasible at all reasonable temperatures), but
incorrect in principle — at sufficiently high temperatures (above 3663K), the
reaction would not be thermodynamically feasible (1 mark).
Q4 (4 marks)
The melting point of sodium is 371K and ΔHfus=+2.60kJ/mol.
Calculate the entropy change of fusion and explain its sign.
Mark Scheme:
ΔSfus=L◆B◆ΔHfus◆RB◆◆LB◆Tm◆RB◆=3712600=+7.01Jmol−1K−1
(2 marks).
The entropy change is positive because the solid sodium becomes a liquid, which has greater disorder
and more ways to arrange the particles (1 mark). The ions in the liquid are no longer fixed in a
lattice and have greater freedom of movement (1 mark).
Summary
This topic covers the fundamental principles of entropy and gibbs free energy, including the key
equations, experimental methods, and applications relevant to the specification.
Key concepts include:
- fundamental principles and equations
- SI units and dimensional analysis
- mathematical modelling of physical phenomena
- experimental techniques and measurement
- applications to real-world problems
A strong understanding of these principles, combined with regular practice of quantitative problems
andpastpaperquestions,isessentialforsuccessinexaminations.