What This Chapter Is Asked To Do

Thermodynamics sits in the physical-chemistry part of the paper, and in a typical paper it supplies one or two questions. Those questions are short by design. They are meant to be finished in under a minute each, which fixes what they can contain: no calculus, no three-stage reversible-adiabatic chains, no algebra that runs past four lines. What they contain instead is a definition, a sign, one substitution into a single formula, or a comparison of two signs.

The table below is the shape of the demand.

Theme How heavily it is drawn on The usual form What you must have ready
Sign conventions and vocabulary Very heavy "which statement is correct" qq and ww are positive when energy enters the system; ΔU=q+w\Delta U = q + w
State function against path function Very heavy pick the odd one out of four quantities the two lists, memorised
Simple first-law numericals Heavy one substitution, answer in J or kJ ΔU=q+w\Delta U = q + w, w=pexΔVw = -p_{ex}\Delta V, 1 Lbar=100 J1\ \mathrm{L\,bar} = 100\ \mathrm{J}
ΔH\Delta H against ΔU\Delta U Heavy given one, find the other; or "for which reaction are they equal" ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT and how to count Δng\Delta n_g
Hess's law and formation enthalpies Heavy three equations to combine, or a ΔfH\Delta_f H^{\circ} sum reverse changes the sign, multiply scales the value
Entropy and the second law Moderate sign of ΔS\Delta S for a stated change gas count rises means ΔS\Delta S positive; ΔS=qrev/T\Delta S = q_{rev}/T
Spontaneity from the signs of ΔH\Delta H and ΔS\Delta S Heavy four sign pairs, one temperature statement the spontaneity grid
Gibbs energy and equilibrium Moderate ΔG=0\Delta G = 0 at equilibrium, or KK from ΔrG\Delta_r G^{\circ} ΔrG=2.303RTlogK\Delta_r G^{\circ} = -2.303\,RT\log K
Heat capacity and calorimetry Lighter one q=mcΔTq = mc\Delta T substitution cc of water =4.18 Jg1K1= 4.18\ \mathrm{J\,g^{-1}\,K^{-1}}
Bond, lattice and solution enthalpies Lighter a definition, or one bond-enthalpy sum bond enthalpies: reactant bonds minus product bonds

Two of those rows carry more marks than their size suggests. The sign-convention row and the state-function row are pure recall; a student who has the lists is never going to lose those marks, and a student who has not cannot reason them out in the time available.

The rows that look like calculation are not really calculation either. A ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT question is decided by whether you counted Δng\Delta n_g correctly, and the arithmetic after that is one multiplication. A Hess's law question is decided by whether you flipped the right equation. The number-crunching is deliberately small.

What the paper does not do here

It does not ask you to derive w=2.303nRTlog(Vf/Vi)w = -2.303\,nRT\log(V_f/V_i). It does not set adiabatic pVγpV^{\gamma} problems, Kirchhoff's equation, or Born-Haber cycles with six unknown steps. It does not ask for the Carnot efficiency. Those live in the harder engineering-entrance syllabus. What it does do is take a small idea and test whether you hold it exactly: not roughly, exactly.

That word "exactly" is the difference between this chapter and most of organic chemistry. In organic you can often reason your way to an answer you half-remember. Here a half-remembered sign convention gives you a confident wrong answer, and a confident wrong answer costs you the negative mark as well as the mark you missed.

Key Point: The whole chapter runs on one convention. qq is positive when heat flows into the system, ww is positive when work is done on the system, and ΔU=q+w\Delta U = q + w. Some physics texts write the first law as ΔU=qw\Delta U = q - w with ww meaning work done by the gas. Both are self-consistent; mixing them is what produces wrong signs. Use the convention above and nothing else.

The formats it comes in

Four wrappings account for nearly everything set from this chapter. A plain single-correct question with four numerical or symbolic options. A "which of the following statements is correct" list, where three statements carry a planted error and one is exact. An assertion-reason pair, where the assertion and the reason are each true or false and you must also judge whether the reason explains the assertion. And a match-the-column, usually pairing four processes with four sign patterns or four formulae. The chemistry is identical across all four; only the reading changes, and the statement and assertion-reason formats reward the precise wording of a definition far more than the numerical ones do.

How to spend the minute

Read the quantity being asked for and its unit before reading the data. If the options are in JK1mol1\mathrm{J\,K^{-1}\,mol^{-1}} the question wants an entropy, and any option quoted in kJmol1\mathrm{kJ\,mol^{-1}} is dead on arrival. If the options split two positive and two negative, the sign alone removes half the paper before you have touched a calculator.

[NEET] A large share of the questions from this chapter are settled by a sign, a unit or a definition rather than by arithmetic. Train the sign check as a reflex: decide whether the answer must be positive or negative first, then compute only if two options survive.

The Definitions You Must Have Word-Perfect

Recall questions are free marks or lost marks; there is no middle ground. The tables below are the ones worth committing exactly.

Systems and their boundaries

Type of system Exchanges matter? Exchanges energy? Everyday example
Open Yes Yes hot tea in an open cup; a reaction in an open beaker
Closed No Yes tea in a sealed steel flask that still feels warm outside
Isolated No No tea in a stoppered vacuum flask (an idealisation)

The system is the part of the universe under study; the surroundings are everything else that can exchange energy or matter with it; the boundary is the real or imagined surface separating them. A boundary that allows heat through is diathermic; one that does not is adiabatic.

Key Point (Definition): A system is isolated only if it exchanges neither matter nor energy. A thermos flask is the standard example, and it is only an approximation, because no real wall is perfectly adiabatic.

State functions and path functions

A state function is a property whose value depends only on the present state of the system, fixed by the state variables pp, VV, TT and nn, and not at all on how the system reached that state. A path function depends on the route taken between the same two end states.

Key Point (Definition): Internal energy UU, enthalpy HH, entropy SS and Gibbs energy GG are state functions. Heat qq and work ww are path functions. The sum q+wq + w is a state function change even though neither term separately is.

Extensive and intensive

An extensive property depends on the amount of substance present; an intensive property does not.

Extensive Intensive
mass, volume, number of moles temperature, pressure, density
internal energy UU, enthalpy HH molar internal energy, molar enthalpy
entropy SS, Gibbs energy GG molar entropy, molar Gibbs energy
heat capacity CC of an object specific heat cc, molar heat capacity CmC_m

Dividing one extensive property by another gives an intensive one: mass over volume is density, enthalpy over moles is molar enthalpy. That single trick answers most questions in this row.

The named enthalpies

Name Symbol Definition (per mole, in the standard state) Sign
Standard enthalpy of formation ΔfH\Delta_f H^{\circ} for forming 1 mol of the compound from its elements in their reference states either
Standard enthalpy of combustion ΔcH\Delta_c H^{\circ} for the complete combustion of 1 mol of a substance in excess oxygen always negative
Enthalpy of fusion ΔfusH\Delta_{fus} H^{\circ} for melting 1 mol of a solid at its melting point positive
Enthalpy of vaporisation ΔvapH\Delta_{vap} H^{\circ} for vaporising 1 mol of a liquid at its boiling point positive
Enthalpy of sublimation ΔsubH\Delta_{sub} H^{\circ} solid straight to vapour; equals ΔfusH+ΔvapH\Delta_{fus}H^{\circ} + \Delta_{vap}H^{\circ} positive
Bond dissociation enthalpy ΔbondH\Delta_{bond} H^{\circ} to break 1 mol of a particular bond in the gas phase positive
Lattice enthalpy ΔlatticeH\Delta_{lattice} H^{\circ} to separate 1 mol of an ionic solid into gaseous ions positive
Enthalpy of solution ΔsolH\Delta_{sol} H^{\circ} for dissolving 1 mol of solute in a very large amount of solvent either
Ionization enthalpy ΔiH\Delta_i H^{\circ} to remove an electron from 1 mol of gaseous atoms positive
Electron gain enthalpy ΔegH\Delta_{eg} H^{\circ} for 1 mol of gaseous atoms gaining an electron usually negative

Key Point: An element in its most stable form at 1 bar and the stated temperature is its reference state, and ΔfH\Delta_f H^{\circ} for that form is exactly zero. Graphite has ΔfH=0\Delta_f H^{\circ} = 0 and diamond does not. O2(g)\mathrm{O_2(g)} has zero and O3(g)\mathrm{O_3(g)} does not. Br2(l)\mathrm{Br_2(l)} has zero and Br2(g)\mathrm{Br_2(g)} does not.

The processes, by what is held fixed

Process What stays constant The immediate consequence
Isothermal temperature ΔU=0\Delta U = 0 and ΔH=0\Delta H = 0 for an ideal gas, so q=wq = -w
Isobaric pressure qp=ΔHq_p = \Delta H, and w=pΔVw = -p\Delta V
Isochoric volume w=0w = 0, so qv=ΔUq_v = \Delta U
Adiabatic no heat exchanged, q=0q = 0 ΔU=w\Delta U = w, so a gas cools as it expands
Cyclic system returns to its starting state every state function change is zero, so ΔU=0\Delta U = 0 and q=wq = -w
Reversible driven by an infinitesimal imbalance, at equilibrium throughout the slowest route, and the one that delivers the most work
Irreversible a finite imbalance, everything real less work delivered than the reversible route between the same states

The isothermal and adiabatic rows are the two most often confused. Isothermal fixes the temperature and lets heat flow in or out to keep it fixed; adiabatic forbids the heat flow and lets the temperature move. Both cannot hold at once for a change of volume in an ideal gas.

Entropy and Gibbs energy

Entropy SS is a state function that measures the degree of dispersal or randomness of a system. For a reversible change at temperature TT,

ΔS=qrevT\Delta S = \frac{q_{rev}}{T}

with units JK1mol1\mathrm{J\,K^{-1}\,mol^{-1}}. Gibbs energy is defined as G=HTSG = H - TS, and at constant temperature its change is

ΔG=ΔHTΔS\Delta G = \Delta H - T\Delta S

with units kJmol1\mathrm{kJ\,mol^{-1}}. ΔG-\Delta G equals the maximum non-expansion work the change can deliver.

One Formula Card for the Whole Chapter

Everything the paper can ask of you from this chapter is on this card. The third column is the one students skip and then lose marks on: a formula used outside its conditions gives a wrong answer that looks right.

Formula Reads as Valid when The trap
ΔU=q+w\Delta U = q + w first law always ww is work done on the system
ΔU=qv\Delta U = q_v heat at constant volume rigid container, no other work a bomb calorimeter measures ΔU\Delta U, not ΔH\Delta H
ΔH=qp\Delta H = q_p heat at constant pressure open vessel or fixed external pressure a coffee-cup calorimeter measures ΔH\Delta H
ΔU=0\Delta U = 0 no change in internal energy isothermal change of an ideal gas needs the gas to be ideal
q=0q = 0 adiabatic insulated walls ΔU=w\Delta U = w here, so the gas cools on expanding
H=U+pVH = U + pV definition of enthalpy always not U+pΔVU + p\Delta V
w=pexΔVw = -p_{ex}\Delta V expansion work external pressure constant ΔV=VfVi\Delta V = V_f - V_i; expansion gives negative ww
w=0w = 0 free expansion expansion into a vacuum, pex=0p_{ex} = 0 volume changes but no work is done
w=2.303nRTlogVfViw = -2.303\,nRT\log\dfrac{V_f}{V_i} isothermal reversible work ideal gas, temperature constant use log\log with the 2.3032.303, or ln\ln without it, never both
ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT linking the two constant temperature, gases ideal Δng\Delta n_g counts gaseous moles only
CpCv=RC_p - C_v = R molar heat capacities 1 mol of an ideal gas per mole; for nn mol the difference is nRnR
q=mcΔTq = mc\Delta T heat from a temperature rise no phase change during the rise mm in g when cc is in Jg1K1\mathrm{J\,g^{-1}\,K^{-1}}
q=CΔTq = C\Delta T same, with a heat capacity CC is for the whole object C=mcC = mc
ΔrH=aΔfH(products)bΔfH(reactants)\Delta_r H^{\circ} = \sum a\,\Delta_f H^{\circ}(\text{products}) - \sum b\,\Delta_f H^{\circ}(\text{reactants}) reaction enthalpy from formation data all species in standard states multiply each by its stoichiometric coefficient
ΔrH=ΔbondH(reactants)ΔbondH(products)\Delta_r H^{\circ} = \sum \Delta_{bond}H^{\circ}(\text{reactants}) - \sum \Delta_{bond}H^{\circ}(\text{products}) reaction enthalpy from bond enthalpies all species gaseous this one is reactants minus products, the opposite way round
ΔS=qrevT\Delta S = \dfrac{q_{rev}}{T} entropy change reversible path, constant TT at a phase change TT is the transition temperature in kelvin
ΔStotal=ΔSsys+ΔSsurr>0\Delta S_{total} = \Delta S_{sys} + \Delta S_{surr} > 0 second law spontaneous change the universe, not the system, must gain entropy
ΔSsurr=ΔHsysT\Delta S_{surr} = -\dfrac{\Delta H_{sys}}{T} surroundings' share constant pp and TT the minus sign is the whole content of it
ΔG=ΔHTΔS\Delta G = \Delta H - T\Delta S Gibbs energy change constant TT and pp ΔH\Delta H in kJ, ΔS\Delta S in J: convert one of them
ΔrG=2.303RTlogK\Delta_r G^{\circ} = -2.303\,RT\log K equilibrium constant standard states, equilibrium ΔG\Delta G^{\circ}, not ΔG\Delta G

The constants and conversions

R=8.314 JK1mol1=0.08206 LatmK1mol1=0.0831 LbarK1mol1R = 8.314\ \mathrm{J\,K^{-1}\,mol^{-1}} = 0.08206\ \mathrm{L\,atm\,K^{-1}\,mol^{-1}} = 0.0831\ \mathrm{L\,bar\,K^{-1}\,mol^{-1}}

1 Lbar=100 J1 Latm=101.3 J1 cal=4.184 J1\ \mathrm{L\,bar} = 100\ \mathrm{J} \qquad 1\ \mathrm{L\,atm} = 101.3\ \mathrm{J} \qquad 1\ \mathrm{cal} = 4.184\ \mathrm{J}

Two derived numbers save real time. At any temperature 2.303R=19.15 JK1mol12.303\,R = 19.15\ \mathrm{J\,K^{-1}\,mol^{-1}}. At 298 K,

2.303RT=5705 Jmol1=5.705 kJmol12.303\,RT = 5705\ \mathrm{J\,mol^{-1}} = 5.705\ \mathrm{kJ\,mol^{-1}}

so at room temperature ΔrG=5.705logK\Delta_r G^{\circ} = -5.705\log K in kJmol1\mathrm{kJ\,mol^{-1}}. A ΔG\Delta G^{\circ} of 5.705 kJmol1-5.705\ \mathrm{kJ\,mol^{-1}} means K=10K = 10; 11.41-11.41 means K=100K = 100; +5.705+5.705 means K=0.1K = 0.1. Recognising those three pairs converts a calculation question into a recall question.

Decision tree matching question wording to the correct thermodynamics formula

Counting Δng\Delta n_g

Δng\Delta n_g is the number of moles of gaseous products minus the number of moles of gaseous reactants, read straight off the balanced equation. Solids, liquids and species in solution contribute nothing.

N2(g)+3H2(g)2NH3(g)Δng=24=2\mathrm{N_2(g) + 3H_2(g) \rightarrow 2NH_3(g)} \qquad \Delta n_g = 2 - 4 = -2

C(s)+O2(g)CO2(g)Δng=11=0\mathrm{C(s) + O_2(g) \rightarrow CO_2(g)} \qquad \Delta n_g = 1 - 1 = 0

CH4(g)+2O2(g)CO2(g)+2H2O(l)Δng=13=2\mathrm{CH_4(g) + 2O_2(g) \rightarrow CO_2(g) + 2H_2O(l)} \qquad \Delta n_g = 1 - 3 = -2

The third line is the one that catches people: the water is liquid, so it is not counted, and Δng\Delta n_g is 2-2 rather than +1+1.

[NEET] When Δng=0\Delta n_g = 0, ΔH=ΔU\Delta H = \Delta U exactly. Scanning four reactions for the one with equal gas moles on both sides is a five-second job and it is a whole question.

The Spontaneity Grid

A spontaneous process is one that can take place on its own, without continuous outside help. The test is the sign of the Gibbs energy change at constant temperature and pressure:

ΔG=ΔHTΔS\Delta G = \Delta H - T\Delta S

with the change spontaneous when ΔG<0\Delta G < 0, at equilibrium when ΔG=0\Delta G = 0, and non-spontaneous in the direction written when ΔG>0\Delta G > 0.

Because TT is always positive on the kelvin scale, the signs of ΔH\Delta H and ΔS\Delta S decide almost everything, and temperature settles the two cases where they disagree.

ΔH\Delta H ΔS\Delta S TΔS-T\Delta S ΔG\Delta G Spontaneous Typical case
Negative Positive negative negative at every TT Yes, at all temperatures 2H2O2(l)2H2O(l)+O2(g)\mathrm{2H_2O_2(l) \rightarrow 2H_2O(l) + O_2(g)}
Negative Negative positive negative only while TT is small Yes at low TT, no at high TT N2(g)+3H2(g)2NH3(g)\mathrm{N_2(g) + 3H_2(g) \rightarrow 2NH_3(g)}; water freezing below 273 K
Positive Positive negative negative only once TT is large No at low TT, yes at high TT CaCO3(s)CaO(s)+CO2(g)\mathrm{CaCO_3(s) \rightarrow CaO(s) + CO_2(g)}; ice melting above 273 K
Positive Negative positive positive at every TT Never 3O2(g)2O3(g)\mathrm{3O_2(g) \rightarrow 2O_3(g)}

Reading the grid takes one habit: look at TΔS-T\Delta S, not at ΔS\Delta S. A positive ΔS\Delta S makes TΔS-T\Delta S negative, which pushes ΔG\Delta G down, which favours the change.

The crossover temperature

In the two middle rows the two terms fight, and the winner changes at the temperature where they balance. Setting ΔG=0\Delta G = 0,

T=ΔHΔST = \frac{\Delta H}{\Delta S}

Above that temperature the TΔST\Delta S term is the bigger of the two; below it the ΔH\Delta H term is. For the endothermic, entropy-increasing row (row three) the reaction turns spontaneous above T=ΔH/ΔST = \Delta H/\Delta S. For the exothermic, entropy-decreasing row (row two) it turns non-spontaneous above that temperature. Which way round it goes is not worth memorising separately, because substituting one large TT and one small TT into ΔHTΔS\Delta H - T\Delta S settles it in ten seconds.

Four quadrant grid of enthalpy and entropy signs against spontaneity and temperature

The hedges that questions are built on

Three statements sound right and are wrong, and each of them has been the whole content of a question.

Spontaneous does not mean fast. Thermodynamics says nothing about rate. The conversion of diamond to graphite has ΔG\Delta G negative at room temperature and takes geological time. A mixture of hydrogen and oxygen has an enormously negative ΔG\Delta G for forming water and will sit unchanged in a flask for years until a spark arrives. Spontaneity is about direction, and rate belongs to kinetics.

A negative ΔH\Delta H does not by itself mean spontaneous. Exothermic changes are usually spontaneous, which is why the idea is tempting, but the counter-examples are common. Water freezing at 283 K is exothermic and does not happen; the entropy loss beats the enthalpy release. A reaction with ΔH=10 kJmol1\Delta H = -10\ \mathrm{kJ\,mol^{-1}} and ΔS=100 JK1mol1\Delta S = -100\ \mathrm{J\,K^{-1}\,mol^{-1}} has ΔG=10+29.8=+19.8 kJmol1\Delta G = -10 + 29.8 = +19.8\ \mathrm{kJ\,mol^{-1}} at 298 K, and does not go.

A positive ΔSsys\Delta S_{sys} does not by itself mean spontaneous either. The second law is about the total. What must increase is

ΔStotal=ΔSsys+ΔSsurr>0\Delta S_{total} = \Delta S_{sys} + \Delta S_{surr} > 0

An exothermic reaction dumps heat into the surroundings and raises ΔSsurr\Delta S_{surr} by ΔHsys/T-\Delta H_{sys}/T, and that term is often what makes the total positive even when the system itself becomes more ordered. The ΔG\Delta G criterion is the same statement rearranged for the system alone: dividing ΔG=ΔHTΔS\Delta G = \Delta H - T\Delta S by T-T gives exactly ΔStotal\Delta S_{total}.

Key Point: ΔG<0\Delta G < 0 and ΔStotal>0\Delta S_{total} > 0 are the same criterion written two ways. ΔG\Delta G is more convenient because it uses only quantities belonging to the system, but it is valid only at constant temperature and pressure.

Sign of ΔS\Delta S without any data

Most entropy questions give no numbers at all and ask only for a sign. Count the gas molecules.

Change ΔS\Delta S Why
Solid to liquid to gas Positive particles gain freedom at each step
Gaseous moles increase Positive more ways to arrange the same matter
Gaseous moles decrease Negative freedom is lost
Gaseous moles unchanged Small, sign from the details no dominant term
A solid dissolving in water Usually positive the ordered lattice breaks up
Two gases mixing Positive mixing always disperses
A gas being compressed Negative less volume, fewer arrangements

2NO(g)+O2(g)2NO2(g)\mathrm{2NO(g) + O_2(g) \rightarrow 2NO_2(g)} goes from 3 mol of gas to 2 mol, so ΔS\Delta S is negative without a single calculation.

Reading a spontaneity question in fifteen seconds

Take the ammonia synthesis, N2(g)+3H2(g)2NH3(g)\mathrm{N_2(g) + 3H_2(g) \rightarrow 2NH_3(g)}, with ΔH\Delta H negative, and a question asking about its spontaneity.

Gaseous moles fall from 4 to 2, so ΔS\Delta S is negative. ΔH\Delta H is negative because the reaction is exothermic. Negative with negative places it in row two: spontaneous at low temperature, non-spontaneous once the temperature is high enough. Any option saying "spontaneous at all temperatures" or "spontaneous only at high temperature" is gone, and no arithmetic was needed.

The industrial detail sits neatly on top of that reading. The process is run hot even though heat works against the equilibrium, because at low temperature the rate is hopeless. That is spontaneity and speed pulling in opposite directions in a single real example, and it is why the two ideas have to be kept apart.

[NEET] When a spontaneity question gives a reaction rather than numbers, get ΔS\Delta S from the change in gas moles and ΔH\Delta H from whether the reaction is a combustion, a decomposition or a synthesis. Two signs, then the grid.

State Functions and Path Functions, as a List

This is the one-mark question the paper returns to most reliably, and it is answered from memory or not at all. Learn the two columns.

State functions (depend only on the present state) Path functions (depend on the route)
Internal energy UU Heat qq
Enthalpy HH Work ww
Entropy SS
Gibbs energy GG
Pressure pp, volume VV, temperature TT
Number of moles nn, concentration
Density, molar mass, refractive index
Heat capacity, specific heat
Free energy change ΔG\Delta G of a stated reaction

The right-hand column has two entries and that is the whole of it. Heat and work are the only path functions the chapter defines, and every other quantity in it is a state function.

Why those two are different is worth one sentence, because the reason is what a well-set question probes. A system in a given state has a definite internal energy, but it does not "contain" heat or work; qq and ww are names for energy in transit, and how much of the transfer arrives as heat and how much as work depends entirely on the route.

Two paths between the same two states giving equal internal energy change

Same ends, different routes

Take one mole of an ideal gas from state 1 to state 2 by two routes: a single-step expansion against a constant external pressure, and a slow reversible expansion between the same two states. The reversible route does more work and absorbs more heat. Both routes give the same ΔU\Delta U, because the initial and final states are the same and UU is a state function.

ΔUroute 1=ΔUroute 2w1w2q1q2\Delta U_{\text{route 1}} = \Delta U_{\text{route 2}} \qquad w_1 \ne w_2 \qquad q_1 \ne q_2

The sum q+wq + w comes out the same on both routes even though each term separately does not. That is the first law being useful rather than merely true.

The exception that questions are built on

Under a constraint, a path function can become as good as a state function.

qv=ΔUqp=ΔHq_v = \Delta U \qquad q_p = \Delta H

At constant volume no expansion work is possible, so the whole of the energy transfer arrives as heat and qq has only one possible value. At constant pressure the same happens for enthalpy. Heat has not stopped being a path function; the constraint has removed the choice of path.

Key Point: qq and ww are path functions. qvq_v and qpq_p are still heats, but because they are pinned to a state-function change they take a single value for given end states. That is exactly why calorimetry works.

Round a closed cycle

Take a system through any sequence of changes that brings it back to its starting state. Every state function returns to its original value, so

ΔU=0ΔH=0ΔS=0ΔG=0\Delta U = 0 \qquad \Delta H = 0 \qquad \Delta S = 0 \qquad \Delta G = 0

for the cycle as a whole, whatever happened in between. The first law then gives q=wq = -w: the net heat absorbed over the cycle equals the net work done by the system. Heat and work are not zero round a cycle, and that is the sharpest demonstration available that they are path functions while UU is not. An engine is exactly this arrangement.

Two lookalikes worth separating

Heat capacity appears in the state-function column, which surprises people, since it is defined through qq. It belongs there because it is a property of the material at a given state, C=q/ΔTC = q/\Delta T measured under a stated condition, and quoting it as CpC_p or CvC_v already names the path. Specific heat and molar heat capacity are the same property expressed per gram and per mole.

Work is a path function, but the change in a state function is not made into a path function by being written with a Δ\Delta. ΔU\Delta U, ΔH\Delta H, ΔS\Delta S and ΔG\Delta G are all differences of state functions and are all route-independent. There is no such thing as Δq\Delta q or Δw\Delta w, and an option that writes one is wrong on the notation alone.

[NEET] The commonest form of this question lists four quantities and asks which is not a state function. Scan for qq or ww; if neither appears, look for a quantity written as heat absorbed or work done in disguise, such as "heat of a process carried out irreversibly".

Fast Elimination and the Traps That Cost Marks

Speed here is not fast arithmetic. It is knowing which questions do not need arithmetic.

Habit 1: decide the sign before you compute

Before touching the numbers, ask what sign the answer must carry. A gas expanding does work on its surroundings, so ww is negative. A combustion is exothermic, so ΔH\Delta H is negative. A reaction that consumes gas has ΔS\Delta S negative. Melting is endothermic, so ΔH\Delta H and ΔS\Delta S are both positive.

Options in this chapter are usually built as two signs times two magnitudes, so fixing the sign halves the paper immediately. If the surviving two differ only in magnitude, you now have a one-step calculation instead of a four-way comparison.

Habit 2: check Δng\Delta n_g before reaching for ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT

Count gaseous moles on both sides first. If they match, Δng=0\Delta n_g = 0, the correction term vanishes, and ΔH=ΔU\Delta H = \Delta U. Any option that makes them differ is wrong, and the question is over.

If they do not match, the correction at 298 K is Δng×2.478 kJmol1\Delta n_g \times 2.478\ \mathrm{kJ\,mol^{-1}}, a number small enough to do in your head. A Δng\Delta n_g of 2-2 shifts ΔH\Delta H about 5 kJ5\ \mathrm{kJ} below ΔU\Delta U; a Δng\Delta n_g of +1+1 lifts it about 2.5 kJ2.5\ \mathrm{kJ} above. Options separated by more than that are not testing this formula at all.

Habit 3: read the units on the options

Units eliminate faster than algebra.

If the options carry The quantity is So reject any option in
JK1mol1\mathrm{J\,K^{-1}\,mol^{-1}} entropy, or a molar heat capacity kJmol1\mathrm{kJ\,mol^{-1}}
kJmol1\mathrm{kJ\,mol^{-1}} an enthalpy or a Gibbs energy JK1mol1\mathrm{J\,K^{-1}\,mol^{-1}}
J\mathrm{J} or kJ\mathrm{kJ} with no "per mol" heat or work for a stated amount anything per mole
no unit at all an equilibrium constant or a ratio anything with a unit
Lbar\mathrm{L\,bar} or Latm\mathrm{L\,atm} expansion work not yet converted joule answers, unless you convert

Entropies of common processes sit in the tens to low hundreds of JK1mol1\mathrm{J\,K^{-1}\,mol^{-1}}; enthalpies of reaction sit in the tens to thousands of kJmol1\mathrm{kJ\,mol^{-1}}. An "entropy" option of 40 kJK1mol140\ \mathrm{kJ\,K^{-1}\,mol^{-1}} is off by a factor of a thousand and can be struck out on sight.

Habit 4: use "spontaneous means ΔG\Delta G negative" to kill two options

Any question that says a process is spontaneous, or asks you to find the temperature at which it becomes spontaneous, has already told you the sign of ΔG\Delta G. Options with the wrong sign go. Options that say the process is spontaneous because it is exothermic go too, since that reasoning is unsound even when the conclusion happens to be right.

The same trick works backwards. If K>1K > 1 then logK>0\log K > 0 and ΔrG\Delta_r G^{\circ} is negative; if K<1K < 1 then ΔrG\Delta_r G^{\circ} is positive; if K=1K = 1 then ΔrG=0\Delta_r G^{\circ} = 0. Any option pairing K=10K = 10 with a positive ΔG\Delta G^{\circ} is wrong before you compute anything.

Habit 5: sanity-check the magnitude

ΔvapH\Delta_{vap}H of water at 373 K373\ \mathrm{K} is 40.79 kJmol140.79\ \mathrm{kJ\,mol^{-1}} and ΔfusH\Delta_{fus}H of ice at 273 K273\ \mathrm{K} is 6.00 kJmol16.00\ \mathrm{kJ\,mol^{-1}}, so vaporisation costs several times more than melting. Bond enthalpies run from about 150150 to about 950 kJmol1950\ \mathrm{kJ\,mol^{-1}}. Lattice enthalpies run to several hundred and beyond. Combustion enthalpies of small organic molecules run into the thousands. An answer three orders of magnitude off one of these is an arithmetic slip, usually a J-for-kJ conversion.

The traps table

Trap What actually goes wrong The fix
Sign of ww using ΔU=qw\Delta U = q - w from a physics book alongside w=pexΔVw = -p_{ex}\Delta V one convention only: ww positive when work is done on the system
Counting Δng\Delta n_g including solids, liquids or aqueous species gases only, products minus reactants
ΔH\Delta H versus ΔU\Delta U assuming they are always equal equal only when Δng=0\Delta n_g = 0
Mixed units in ΔG\Delta G ΔH\Delta H in kJ and ΔS\Delta S in J, added directly convert ΔS\Delta S to kJK1mol1\mathrm{kJ\,K^{-1}\,mol^{-1}}, or ΔH\Delta H to J
Temperature in C^\circ\mathrm{C} using 25 instead of 298 in TΔST\Delta S or qrev/Tq_{rev}/T every TT in thermodynamics is in kelvin
ΔfH=0\Delta_f H^{\circ} = 0 applying it to diamond, O3\mathrm{O_3} or Br2(g)\mathrm{Br_2(g)} only the reference state of an element is zero
Hess's law forgetting to change the sign on a reversed equation reverse means change sign; double means double the value
Bond enthalpy direction using products minus reactants bond enthalpies go reactants minus products
log\log against ln\ln using 2.303RTlnK2.303\,RT\ln K or RTlogKRT\log K 2.3032.303 pairs with log\log; nothing pairs with ln\ln
ΔG\Delta G against ΔG\Delta G^{\circ} putting ΔG\Delta G into 2.303RTlogK-2.303\,RT\log K only the standard value fixes KK; ΔG=0\Delta G = 0 at equilibrium, ΔG\Delta G^{\circ} generally is not
"Exothermic so spontaneous" treating ΔH<0\Delta H < 0 as sufficient ΔS\Delta S and TT still get a vote
"Spontaneous so fast" reading a rate into a ΔG\Delta G thermodynamics fixes direction, not speed
qq in a bomb calorimeter calling it ΔH\Delta H constant volume gives ΔU\Delta U; convert with ΔngRT\Delta n_g RT
CpCv=RC_p - C_v = R applying it to nn moles as written it is per mole; for nn moles the difference is nRnR

The order to do things in

For a numerical question from this chapter, the sequence that wastes the least time is fixed.

Read the unit on the options and decide what quantity is wanted. Decide the sign the answer must carry, and strike out whatever contradicts it. Check whether any given temperature is in Celsius and convert it. Check whether ΔH\Delta H and ΔS\Delta S are in different energy units and fix that before adding them. Then, and only then, substitute into one formula. If two options survive and both look defensible, the difference between them is almost always a factor of 2.3032.303, a factor of 10001000, or a sign, and each of those points at a specific slip you can check in five seconds.

For a recall question the sequence is shorter still. Find the word that carries the condition, which is usually "reversible", "at constant volume", "in its reference state", "gaseous" or "standard". Options in this chapter are made wrong by removing or altering exactly that word, and an option that has dropped the condition is the planted error.

Key Point: Read ΔG=2.303RTlogK\Delta G^{\circ} = -2.303\,RT\log K as a statement about the position of equilibrium, not about whether a reaction is possible. A positive ΔG\Delta G^{\circ} means K<1K < 1, so the reaction favours reactants at equilibrium; it does not mean nothing happens.

Question 1: Work in one line

A gas expands from 2.0 L2.0\ \mathrm{L} to 5.0 L5.0\ \mathrm{L} against a constant external pressure of 1.0 bar1.0\ \mathrm{bar}. Find the work done on the gas.

Answer:

The external pressure is constant, so I use w=pexΔVw = -p_{ex}\Delta V.

The gas expanded, so I already know the answer is negative. That kills any positive option.

ΔV=5.02.0=3.0 L\Delta V = 5.0 - 2.0 = 3.0\ \mathrm{L}

w=(1.0 bar)(3.0 L)=3.0 Lbarw = -(1.0\ \mathrm{bar})(3.0\ \mathrm{L}) = -3.0\ \mathrm{L\,bar}

Now I convert, using 1 Lbar=100 J1\ \mathrm{L\,bar} = 100\ \mathrm{J}.

w=3.0×100=300 Jw = -3.0 \times 100 = -300\ \mathrm{J}

Ans: w=300 Jw = -300\ \mathrm{J} Watch out: Leaving the answer as 3.0 Lbar-3.0\ \mathrm{L\,bar} is the trap here, because 3-3 will usually be sitting there as an option. If the pressure had been given in atmospheres the factor would be 101.3101.3, not 100100.

Question 2: The first law, with the signs done properly

A system absorbs 250 J250\ \mathrm{J} of heat and does 100 J100\ \mathrm{J} of work on its surroundings. Calculate the change in internal energy.

Answer:

Heat flows into the system, so q=+250 Jq = +250\ \mathrm{J}.

The system does work on the surroundings, which means work is done by the system. In the convention where ww is the work done on the system, that makes ww negative.

w=100 Jw = -100\ \mathrm{J}

ΔU=q+w=250+(100)=+150 J\Delta U = q + w = 250 + (-100) = +150\ \mathrm{J}

Ans: ΔU=+150 J\Delta U = +150\ \mathrm{J} Watch out: +350 J+350\ \mathrm{J} is on the option list for everyone who adds the two magnitudes. The phrase to read carefully is "on the surroundings" against "on the system"; those two produce answers that differ by twice the work.

Question 3: Spotting Δng=0\Delta n_g = 0

For which of these reactions is ΔH\Delta H equal to ΔU\Delta U?

(i) N2(g)+3H2(g)2NH3(g)\mathrm{N_2(g) + 3H_2(g) \rightarrow 2NH_3(g)} (ii) H2(g)+Cl2(g)2HCl(g)\mathrm{H_2(g) + Cl_2(g) \rightarrow 2HCl(g)} (iii) PCl5(g)PCl3(g)+Cl2(g)\mathrm{PCl_5(g) \rightarrow PCl_3(g) + Cl_2(g)} (iv) 2SO2(g)+O2(g)2SO3(g)\mathrm{2SO_2(g) + O_2(g) \rightarrow 2SO_3(g)}

Answer:

ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT, so the two are equal exactly when Δng=0\Delta n_g = 0. I count gaseous moles on each side.

(i) 24=22 - 4 = -2. Not equal. (ii) 22=02 - 2 = 0. Equal. (iii) 21=+12 - 1 = +1. Not equal. (iv) 23=12 - 3 = -1. Not equal.

Ans: Only reaction (ii) Watch out: The counting is of moles of gas, not of molecules or atoms. Everything here happens to be gaseous; had any species been a liquid or a solid it would have contributed nothing to the count.

Question 4: ΔH\Delta H from ΔU\Delta U

For the combustion of ethene,

C2H4(g)+3O2(g)2CO2(g)+2H2O(l)\mathrm{C_2H_4(g) + 3O_2(g) \rightarrow 2CO_2(g) + 2H_2O(l)}

the internal energy change at 298 K298\ \mathrm{K} is 1406.0 kJmol1-1406.0\ \mathrm{kJ\,mol^{-1}}. Find ΔH\Delta H.

Answer:

First I count the gaseous moles. Products give 22 mol of CO2\mathrm{CO_2}; the water is liquid and is not counted. Reactants give 1+3=41 + 3 = 4 mol.

Δng=24=2\Delta n_g = 2 - 4 = -2

RT=8.314×103×298=2.478 kJmol1RT = 8.314 \times 10^{-3} \times 298 = 2.478\ \mathrm{kJ\,mol^{-1}}

ΔH=ΔU+ΔngRT=1406.0+(2)(2.478)=1406.04.96\Delta H = \Delta U + \Delta n_g RT = -1406.0 + (-2)(2.478) = -1406.0 - 4.96

Ans: ΔH=1411.0 kJmol1\Delta H = -1411.0\ \mathrm{kJ\,mol^{-1}} Watch out: Counting the liquid water as gas would put 44 mol of gas on each side, so Δng=0\Delta n_g = 0 and the answer would come out unchanged at 1406.0 kJmol1-1406.0\ \mathrm{kJ\,mol^{-1}}, which will be one of the options. The state symbols are part of the data.

Question 5: Reaction enthalpy from formation data

Given ΔfH\Delta_f H^{\circ} values of 74.8 kJmol1-74.8\ \mathrm{kJ\,mol^{-1}} for CH4(g)\mathrm{CH_4(g)}, 393.5 kJmol1-393.5\ \mathrm{kJ\,mol^{-1}} for CO2(g)\mathrm{CO_2(g)} and 285.8 kJmol1-285.8\ \mathrm{kJ\,mol^{-1}} for H2O(l)\mathrm{H_2O(l)}, find the standard enthalpy of combustion of methane.

CH4(g)+2O2(g)CO2(g)+2H2O(l)\mathrm{CH_4(g) + 2O_2(g) \rightarrow CO_2(g) + 2H_2O(l)}

Answer:

ΔrH=aΔfH(products)bΔfH(reactants)\Delta_r H^{\circ} = \sum a\,\Delta_f H^{\circ}(\text{products}) - \sum b\,\Delta_f H^{\circ}(\text{reactants})

Oxygen is an element in its reference state, so its ΔfH\Delta_f H^{\circ} is zero and it drops out.

ΔrH=[(393.5)+2(285.8)][(74.8)]\Delta_r H^{\circ} = \left[(-393.5) + 2(-285.8)\right] - \left[(-74.8)\right]

=(393.5571.6)+74.8=965.1+74.8= (-393.5 - 571.6) + 74.8 = -965.1 + 74.8

Ans: ΔcH=890.3 kJmol1\Delta_c H^{\circ} = -890.3\ \mathrm{kJ\,mol^{-1}} Watch out: The coefficient 22 multiplies the water term, and the reactant sum is subtracted, so the negative ΔfH\Delta_f H^{\circ} of methane comes back as +74.8+74.8. Dropping the coefficient gives 604.5-604.5 and dropping the +74.8+74.8 gives 965.1-965.1, and both of those appear as options.

Question 6: Hess's law, two equations

Given

C(s)+O2(g)CO2(g)ΔH=393.5 kJmol1\mathrm{C(s) + O_2(g) \rightarrow CO_2(g)} \qquad \Delta H = -393.5\ \mathrm{kJ\,mol^{-1}}

CO(g)+12O2(g)CO2(g)ΔH=283.0 kJmol1\mathrm{CO(g) + \tfrac{1}{2}O_2(g) \rightarrow CO_2(g)} \qquad \Delta H = -283.0\ \mathrm{kJ\,mol^{-1}}

find the standard enthalpy of formation of CO(g)\mathrm{CO(g)}.

Answer:

The target equation is the formation of one mole of CO\mathrm{CO} from its elements.

C(s)+12O2(g)CO(g)\mathrm{C(s) + \tfrac{1}{2}O_2(g) \rightarrow CO(g)}

I get there by keeping the first equation as written and reversing the second, which changes the sign of its enthalpy to +283.0+283.0. Adding them, CO2\mathrm{CO_2} cancels from both sides and half a mole of O2\mathrm{O_2} cancels from the left.

ΔfH(CO)=393.5+283.0\Delta_f H^{\circ}(\mathrm{CO}) = -393.5 + 283.0

Ans: ΔfH(CO)=110.5 kJmol1\Delta_f H^{\circ}(\mathrm{CO}) = -110.5\ \mathrm{kJ\,mol^{-1}} Watch out: Adding the two values instead of subtracting gives 676.5 kJmol1-676.5\ \mathrm{kJ\,mol^{-1}}. Reversing an equation always reverses the sign of its enthalpy change.

Question 7: A coffee-cup calorimeter

50.0 mL50.0\ \mathrm{mL} of 1.0 M1.0\ \mathrm{M} HCl\mathrm{HCl} is mixed with 50.0 mL50.0\ \mathrm{mL} of 1.0 M1.0\ \mathrm{M} NaOH\mathrm{NaOH}, both initially at 25.0 C25.0\ {}^\circ\mathrm{C}. The temperature rises to 31.7 C31.7\ {}^\circ\mathrm{C}. Take the density of the mixture as 1.0 gmL11.0\ \mathrm{g\,mL^{-1}} and its specific heat as 4.18 Jg1K14.18\ \mathrm{J\,g^{-1}\,K^{-1}}. Find the enthalpy of neutralisation per mole of water formed.

Answer:

The solution is what warms up, so its mass is the total volume times the density.

m=100.0 mL×1.0 gmL1=100.0 gm = 100.0\ \mathrm{mL} \times 1.0\ \mathrm{g\,mL^{-1}} = 100.0\ \mathrm{g}

ΔT=31.725.0=6.7 K\Delta T = 31.7 - 25.0 = 6.7\ \mathrm{K}

qsolution=mcΔT=100.0×4.18×6.7=2800.6 Jq_{\text{solution}} = mc\Delta T = 100.0 \times 4.18 \times 6.7 = 2800.6\ \mathrm{J}

The solution gained that heat, so the reaction released it, and the reaction enthalpy is negative.

Moles of water formed equal the moles of acid, since acid and base are present in equal amounts.

n=0.0500 L×1.0 molL1=0.0500 moln = 0.0500\ \mathrm{L} \times 1.0\ \mathrm{mol\,L^{-1}} = 0.0500\ \mathrm{mol}

ΔH=2800.60.0500=56012 Jmol1\Delta H = -\frac{2800.6}{0.0500} = -56012\ \mathrm{J\,mol^{-1}}

Ans: ΔH=56.0 kJmol1\Delta H = -56.0\ \mathrm{kJ\,mol^{-1}} Watch out: A temperature difference is the same number in C^\circ\mathrm{C} and in K, so 6.76.7 is correct here. That is not a licence to use Celsius anywhere a temperature itself appears, such as in qrev/Tq_{rev}/T. The vessel is open, so this heat is qpq_p and equals ΔH\Delta H, not ΔU\Delta U.

Question 8: Entropy of a phase change

The enthalpy of fusion of ice is 6.00 kJmol16.00\ \mathrm{kJ\,mol^{-1}} at its melting point. Calculate the entropy change of the system when one mole of ice melts at 0 C0\ {}^\circ\mathrm{C}, and state the total entropy change.

Answer:

Melting at the melting point is a reversible change, so ΔS=qrev/T\Delta S = q_{rev}/T with qrev=ΔfusHq_{rev} = \Delta_{fus}H at constant pressure.

The temperature must be in kelvin.

T=0+273=273 KT = 0 + 273 = 273\ \mathrm{K}

ΔSsys=6000 Jmol1273 K=+22.0 JK1mol1\Delta S_{sys} = \frac{6000\ \mathrm{J\,mol^{-1}}}{273\ \mathrm{K}} = +22.0\ \mathrm{J\,K^{-1}\,mol^{-1}}

The surroundings supplied that same heat at the same temperature, so

ΔSsurr=6000273=22.0 JK1mol1\Delta S_{surr} = -\frac{6000}{273} = -22.0\ \mathrm{J\,K^{-1}\,mol^{-1}}

ΔStotal=22.022.0=0\Delta S_{total} = 22.0 - 22.0 = 0

Ans: ΔSsys=+22.0 JK1mol1\Delta S_{sys} = +22.0\ \mathrm{J\,K^{-1}\,mol^{-1}}; ΔStotal=0\Delta S_{total} = 0 Watch out: A total entropy change of zero is the signature of equilibrium, and ice and water are indeed in equilibrium at 273 K273\ \mathrm{K}. Above that temperature the same melting has ΔStotal>0\Delta S_{total} > 0 and runs on its own. Using 6.006.00 instead of 60006000 gives 0.0220.022, which is the same number with the kilo lost.

Question 9: The temperature at which it turns spontaneous

For CaCO3(s)CaO(s)+CO2(g)\mathrm{CaCO_3(s) \rightarrow CaO(s) + CO_2(g)}, ΔH=+178.3 kJmol1\Delta H = +178.3\ \mathrm{kJ\,mol^{-1}} and ΔS=+160.6 JK1mol1\Delta S = +160.6\ \mathrm{J\,K^{-1}\,mol^{-1}}. Above what temperature is the decomposition spontaneous?

Answer:

ΔH\Delta H is positive and ΔS\Delta S is positive, so this is the third row of the grid: non-spontaneous when cold, spontaneous once TT is large enough. The changeover is where ΔG=0\Delta G = 0.

ΔG=ΔHTΔS=0T=ΔHΔS\Delta G = \Delta H - T\Delta S = 0 \quad \Rightarrow \quad T = \frac{\Delta H}{\Delta S}

The two quantities must be in the same energy unit, so I put ΔH\Delta H into joules.

T=178300 Jmol1160.6 JK1mol1=1110 KT = \frac{178300\ \mathrm{J\,mol^{-1}}}{160.6\ \mathrm{J\,K^{-1}\,mol^{-1}}} = 1110\ \mathrm{K}

Ans: Spontaneous above about 1110 K1110\ \mathrm{K}, roughly 837 C837\ {}^\circ\mathrm{C} Watch out: Forgetting to convert 178.3 kJ178.3\ \mathrm{kJ} to joules gives 1.11 K1.11\ \mathrm{K}, which is absurd and is always one of the options. The result also matches practice: limestone is calcined in a kiln at well over 1000 K1000\ \mathrm{K}, not at room temperature.

Question 10: From ΔH\Delta H and ΔS\Delta S to KK

A reaction has ΔH=20.0 kJmol1\Delta H = -20.0\ \mathrm{kJ\,mol^{-1}} and ΔS=50.0 JK1mol1\Delta S = -50.0\ \mathrm{J\,K^{-1}\,mol^{-1}} at 298 K298\ \mathrm{K}. Find ΔG\Delta G^{\circ}, say whether the reaction is spontaneous, and calculate KK.

Answer:

The two terms disagree in sign, so I cannot read the answer off the grid; this is row two, spontaneous only while the temperature is low enough.

I convert the entropy into kJ\mathrm{kJ} so both terms share a unit.

ΔS=50.0 JK1mol1=0.0500 kJK1mol1\Delta S = -50.0\ \mathrm{J\,K^{-1}\,mol^{-1}} = -0.0500\ \mathrm{kJ\,K^{-1}\,mol^{-1}}

ΔG=ΔHTΔS=20.0(298)(0.0500)=20.0+14.9=5.1 kJmol1\Delta G^{\circ} = \Delta H - T\Delta S = -20.0 - (298)(-0.0500) = -20.0 + 14.9 = -5.1\ \mathrm{kJ\,mol^{-1}}

Negative, so the reaction is spontaneous at 298 K298\ \mathrm{K}.

For the equilibrium constant I use ΔrG=2.303RTlogK\Delta_r G^{\circ} = -2.303\,RT\log K, with 2.303RT=5.705 kJmol12.303\,RT = 5.705\ \mathrm{kJ\,mol^{-1}} at this temperature.

logK=ΔrG5.705=5.15.705=0.894\log K = \frac{-\Delta_r G^{\circ}}{5.705} = \frac{5.1}{5.705} = 0.894

K=100.894=7.8K = 10^{0.894} = 7.8

Ans: ΔG=5.1 kJmol1\Delta G^{\circ} = -5.1\ \mathrm{kJ\,mol^{-1}}, spontaneous, K7.8K \approx 7.8 Watch out: Adding 20.0-20.0 and 14.9-14.9 without noticing the double negative gives 34.9 kJmol1-34.9\ \mathrm{kJ\,mol^{-1}} and a KK near 10610^{6}. A negative ΔG\Delta G^{\circ} must give K>1K > 1, and here the value is only modestly above 1, matching a ΔG\Delta G^{\circ} of a few kJmol1\mathrm{kJ\,mol^{-1}}. Spontaneous at 298 K298\ \mathrm{K} says nothing about how quickly the reaction reaches that equilibrium.