Why Internal Energy Alone Is Not Enough

The first law gives a clean result at constant volume. With ΔV=0\Delta V = 0 there is no expansion work, so w=0w = 0 and

ΔU=qV\Delta U = q_V

The heat measured in a rigid sealed vessel is exactly the change in internal energy. That is a genuinely useful result, and it is how a bomb calorimeter works.

The trouble is that almost no chemistry is done that way. A reaction in a test tube, a beaker, a round-bottom flask or a conical flask is open to the room. Gas evolved during the reaction does not stay put — it pushes the atmosphere back and escapes. The volume of the system changes freely while the pressure stays pinned at whatever the atmosphere happens to be, roughly 1bar1\,\mathrm{bar}.

Rigid sealed vessel at constant volume beside an open flask at constant atmospheric pressure

So a laboratory reaction runs at constant pressure, not constant volume. Under that condition part of the energy released by the reaction is spent pushing the atmosphere out of the way, and only the rest shows up as heat in the thermometer. The heat measured is no longer ΔU\Delta U.

Start from the first law at constant pressure. The only work is expansion work, w=pΔVw = -p\,\Delta V, so

ΔU=qppΔV\Delta U = q_p - p\,\Delta V

The measured heat qpq_p is therefore ΔU+pΔV\Delta U + p\Delta V, and that quantity — not ΔU\Delta U by itself — is what a chemist actually measures in a flask. Chemistry needs a state function whose change equals qpq_p, in the same way that ΔU\Delta U equals qVq_V. That function is enthalpy.

How much energy is lost to the atmosphere

The size of the effect is easy to estimate. Suppose a reaction releases one mole of gas at 298K298\,\mathrm{K} against an atmospheric pressure of 1bar1\,\mathrm{bar}. The gas produced occupies about 24.8L24.8\,\mathrm{L}, so the system pushes the atmosphere back through that volume:

pΔV=nRT=1×8.314×298=2478J2.5kJp\,\Delta V = nRT = 1 \times 8.314 \times 298 = 2478\,\mathrm{J} \approx 2.5\,\mathrm{kJ}

Two and a half kilojoules per mole of gas released never reaches the thermometer. Against a combustion enthalpy of several hundred kilojoules that is a small slice, but it is not zero, and it is exactly the gap between the two quantities this section is about.

Key Point: At constant volume the heat exchanged is ΔU\Delta U. At constant pressure it is not, because some energy goes into pushing the surroundings. A second state function is defined to handle the constant-pressure case.

Enthalpy, H = U + pV

Rearrange the constant-pressure first law with initial state 1 and final state 2:

U2U1=qpp(V2V1)U_2 - U_1 = q_p - p(V_2 - V_1)

Collecting the state-2 terms on one side and the state-1 terms on the other,

qp=(U2+pV2)(U1+pV1)q_p = (U_2 + pV_2) - (U_1 + pV_1)

Both brackets have the same form, U+pVU + pV. That combination is given a name.

Key Point (Definition): Enthalpy is defined as H=U+pVH = U + pV. Its SI unit is the joule; chemists usually quote it in kJmol1\mathrm{kJ\,mol^{-1}}.

With that definition the two brackets are H2H_2 and H1H_1, so

qp=H2H1=ΔHq_p = H_2 - H_1 = \Delta H

Key Point: At constant pressure, ΔH=qp\Delta H = q_p. The heat absorbed by a system at constant pressure is its enthalpy change.

Why H is a state function

UU is a state function, pp is a state variable and VV is a state variable. HH is built only from these three, so its value depends only on the present state of the system and not on how the system got there. ΔH\Delta H between two given states is fixed, whatever the route.

This has a consequence worth pausing on. Heat is a path function — the heat exchanged between two states depends on the route taken. But once the pressure is held constant, qpq_p is forced to equal ΔH\Delta H, and ΔH\Delta H is route-independent. Pinning the pressure removes the freedom that made qq path-dependent. The same thing happened at constant volume, where qVq_V was forced to equal ΔU\Delta U.

The finite-change form

Written for a finite change,

ΔH=ΔU+Δ(pV)\Delta H = \Delta U + \Delta(pV)

When the pressure is constant this collapses to

ΔH=ΔU+pΔV\Delta H = \Delta U + p\,\Delta V

Read the three terms physically. ΔU\Delta U is the energy actually stored inside the system. pΔVp\Delta V is the energy the system spent shoving the atmosphere aside to make room for itself. ΔH\Delta H is the sum, and it is the quantity a thermometer in an open flask reports.

Only changes in enthalpy can be measured

The absolute enthalpy of a substance is unknown, because the absolute internal energy UU is unknown — nobody can count the total kinetic and potential energy of every particle in a mole of a substance. What can be measured is the difference between two states, and that is all chemistry ever needs:

ΔH=HfinalHinitial\Delta H = H_{final} - H_{initial}

For a reaction, "final" means the products and "initial" means the reactants, so

ΔrH=HproductsHreactants\Delta_r H = \sum H_{products} - \sum H_{reactants}

The old name "heat content" for enthalpy survives in some books and is misleading. A system does not contain a stock of heat that it hands out; heat is energy in transit across the boundary. Enthalpy is a property of the state, and it happens to change by exactly the amount of heat transferred when, and only when, the pressure is held constant.

[Board] State the condition with the result. ΔH=qp\Delta H = q_p is true at constant pressure only, and ΔH=ΔU+pΔV\Delta H = \Delta U + p\Delta V needs constant pressure as well. A bare "ΔH=q\Delta H = q" loses the mark.

The Sign of Delta H

An exothermic change gives out heat. Heat leaves the system, so qpq_p is negative, and

ΔH<0for an exothermic change\Delta H < 0 \quad \text{for an exothermic change}

An endothermic change takes in heat. Heat enters the system, qpq_p is positive, and

ΔH>0for an endothermic change\Delta H > 0 \quad \text{for an endothermic change}

Enthalpy level diagrams for an exothermic reaction and an endothermic reaction

An enthalpy level diagram makes this visual. Enthalpy is plotted upward. For an exothermic reaction the products sit lower than the reactants: the system has shed enthalpy into the surroundings and ΔH=HproductsHreactants\Delta H = H_{products} - H_{reactants} comes out negative. Combustion of methane, neutralisation of an acid by an alkali and the setting of cement are all of this kind, and all warm their surroundings.

For an endothermic reaction the products sit higher. The system has drawn enthalpy in from the surroundings, so ΔH\Delta H is positive and the flask feels cold. Dissolving ammonium chloride in water and decomposing limestone both behave this way.

Change Heat flow Sign of qpq_p Sign of ΔH\Delta H Flask feels
Exothermic out of the system negative negative warm
Endothermic into the system positive positive cold

One caution about the word "system". The flask feels warm in an exothermic reaction because the heat has gone into the surroundings — your hand is part of the surroundings, not part of the system. The system itself has lost enthalpy. Students who reason from the temperature they feel often get the sign backwards.

Key Point: ΔH\Delta H negative means heat released, products lower in enthalpy. ΔH\Delta H positive means heat absorbed, products higher in enthalpy.

Writing the value with the equation

A balanced equation carrying its enthalpy change is a thermochemical equation:

CH4(g)+2O2(g)CO2(g)+2H2O(l)ΔH=890.3kJmol1\mathrm{CH_4(g) + 2O_2(g) \rightarrow CO_2(g) + 2H_2O(l)} \qquad \Delta H = -890.3\,\mathrm{kJ\,mol^{-1}}

Two conventions travel with it. Every species carries its physical state, because the value depends on it. And the value belongs to the equation exactly as written — for the amounts shown by the coefficients, not per mole of any one species picked at random.

Reversing the equation reverses the sign. Condensation of water gives out the same 40.79kJmol140.79\,\mathrm{kJ\,mol^{-1}} that vaporisation at 373K373\,\mathrm{K} absorbed:

H2O(l)H2O(g)ΔH=+40.79kJmol1\mathrm{H_2O(l) \rightarrow H_2O(g)} \qquad \Delta H = +40.79\,\mathrm{kJ\,mol^{-1}}

H2O(g)H2O(l)ΔH=40.79kJmol1\mathrm{H_2O(g) \rightarrow H_2O(l)} \qquad \Delta H = -40.79\,\mathrm{kJ\,mol^{-1}}

This follows from HH being a state function: swapping the initial and final states can only flip the sign of the difference.

Relating Delta H to Delta U for Reactions Involving Gases

ΔH=ΔU+pΔV\Delta H = \Delta U + p\Delta V is correct but awkward, because ΔV\Delta V for a reaction is not something anyone measures. For gases the ideal gas equation converts it into something countable.

Take a reaction run at constant temperature TT and constant pressure pp. Let nAn_A be the total moles of gaseous reactants occupying total volume VAV_A, and nBn_B the total moles of gaseous products occupying VBV_B. Applying pV=nRTpV = nRT to each side,

pVA=nARTpVB=nBRTpV_A = n_A RT \qquad pV_B = n_B RT

Subtracting,

pVBpVA=(nBnA)RTpV_B - pV_A = (n_B - n_A)RT

p(VBVA)=(nBnA)RTp(V_B - V_A) = (n_B - n_A)RT

The volume difference VBVAV_B - V_A is the volume change of the reaction, and nBnAn_B - n_A is given the symbol Δng\Delta n_g:

pΔV=ΔngRTp\,\Delta V = \Delta n_g RT

Counting gaseous moles on each side of three reactions to get delta n gas

Substituting into ΔH=ΔU+pΔV\Delta H = \Delta U + p\Delta V gives the working relation of this section.

Key Point: ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT, where Δng\Delta n_g is the number of moles of gaseous products minus the number of moles of gaseous reactants.

Rearranged the other way, ΔU=ΔHΔngRT\Delta U = \Delta H - \Delta n_g RT. Bomb calorimetry delivers ΔU\Delta U and the relation converts it to ΔH\Delta H; an open-flask measurement delivers ΔH\Delta H and the relation converts it back. Both directions appear in exams.

Counting Delta n_g

Only species labelled (g)(g) are counted. Solids, liquids and aqueous species contribute nothing, because their volumes are thousands of times smaller than the volume of a gas and are treated as negligible.

Δng=(moles of gaseous products)(moles of gaseous reactants)\Delta n_g = (\text{moles of gaseous products}) - (\text{moles of gaseous reactants})

The moles are the stoichiometric coefficients of the balanced equation as it is written, so Δng\Delta n_g belongs to that equation, not to the reaction in the abstract. Doubling every coefficient doubles Δng\Delta n_g, and it doubles ΔH\Delta H and ΔU\Delta U with it.

Fractional coefficients give fractional values, and that is fine. CO(g)+12O2(g)CO2(g)\mathrm{CO(g) + \tfrac{1}{2}O_2(g) \rightarrow CO_2(g)} has Δng=11.5=0.5\Delta n_g = 1 - 1.5 = -0.5.

What the derivation assumed

Three assumptions went into ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT, and each one is worth knowing.

The gases were treated as ideal, so that pV=nRTpV = nRT could be applied to both sides. Real gases at ordinary pressures are close enough for the correction term, which is small anyway.

The temperature was the same before and after. If a reaction heats itself up, the relation applies to the reactants and products compared at the same temperature.

The volumes of solids, liquids and solutions were taken as negligible against the volumes of gases. At 298K298\,\mathrm{K} a mole of gas occupies about 24.8L24.8\,\mathrm{L} and a mole of water about 18mL18\,\mathrm{mL}, a ratio of roughly 14001400 to 11, so the approximation is a safe one.

Working Through Delta n_g, and When the Two Are Equal

Three reactions, one of each kind.

Positive Δng\Delta n_g. Limestone decomposing:

CaCO3(s)CaO(s)+CO2(g)\mathrm{CaCO_3(s) \rightarrow CaO(s) + CO_2(g)}

Gaseous products: 11. Gaseous reactants: 00 — the solids are not counted. So Δng=10=+1\Delta n_g = 1 - 0 = +1. Gas is created, the system expands, it spends energy pushing the atmosphere back, and ΔH\Delta H is larger than ΔU\Delta U.

Negative Δng\Delta n_g. Ammonia synthesis:

N2(g)+3H2(g)2NH3(g)\mathrm{N_2(g) + 3H_2(g) \rightarrow 2NH_3(g)}

Δng=24=2\Delta n_g = 2 - 4 = -2. Gas is consumed, the system shrinks, the atmosphere does work on it, and ΔH\Delta H is smaller than ΔU\Delta U — more negative, in this exothermic case.

Zero Δng\Delta n_g. Burning graphite:

C(s)+O2(g)CO2(g)\mathrm{C(s) + O_2(g) \rightarrow CO_2(g)}

One mole of gas in, one mole of gas out. The solid carbon is not counted at all, so Δng=11=0\Delta n_g = 1 - 1 = 0, and ΔH=ΔU\Delta H = \Delta U exactly.

The two cases where Delta H equals Delta U

The first is Δng=0\Delta n_g = 0, as above. The gas volume created equals the gas volume destroyed, no net expansion work is done, and the two quantities coincide.

The second is a reaction involving only solids and liquids. Condensed phases barely change volume on reacting or on heating, so pΔVp\Delta V is tiny compared with the energies of chemical change, and

ΔHΔUfor solids and liquids only\Delta H \approx \Delta U \quad \text{for solids and liquids only}

A number makes the size of the neglect clear. One mole of a gas at 298K298\,\mathrm{K} and 1bar1\,\mathrm{bar} occupies about 25L25\,\mathrm{L}; one mole of a liquid or solid occupies tens of millilitres. Expanding by one mole of gas costs RT=2.48kJRT = 2.48\,\mathrm{kJ}, while the volume changes of condensed phases cost a few joules at most.

Key Point: ΔH=ΔU\Delta H = \Delta U when Δng=0\Delta n_g = 0, and ΔHΔU\Delta H \approx \Delta U when no gases take part at all.

The mistakes that cost marks

  • Counting a solid or a liquid in Δng\Delta n_g. H2(g)+I2(s)2HI(g)\mathrm{H_2(g) + I_2(s) \rightarrow 2HI(g)} has Δng=21=+1\Delta n_g = 2 - 1 = +1, not 22=02 - 2 = 0.
  • Counting an aqueous species. Zn(s)+2HCl(aq)ZnCl2(aq)+H2(g)\mathrm{Zn(s) + 2HCl(aq) \rightarrow ZnCl_2(aq) + H_2(g)} has Δng=10=+1\Delta n_g = 1 - 0 = +1.
  • Missing the phase label on water. 2H2(g)+O2(g)2H2O(l)\mathrm{2H_2(g)+O_2(g) \rightarrow 2H_2O(l)} has Δng=3\Delta n_g = -3, but writing 2H2O(g)\mathrm{2H_2O(g)} instead makes it 1-1. The phase in the equation decides it.
  • Reversing the subtraction. It is products minus reactants, in that order.

[JEE/NEET] When a question offers "ΔH=ΔU\Delta H = \Delta U" as an option, count Δng\Delta n_g before dismissing it. Combustion of graphite, H2(g)+Cl2(g)2HCl(g)\mathrm{H_2(g)+Cl_2(g) \rightarrow 2HCl(g)} and the esterification of ethanoic acid by ethanol all qualify.

Using the Relation Without Slipping on Units

Three habits keep ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT from going wrong.

Match the energy units. R=8.314JK1mol1R = 8.314\,\mathrm{J\,K^{-1}\,mol^{-1}} produces ΔngRT\Delta n_g RT in joules, while ΔH\Delta H and ΔU\Delta U are almost always quoted in kJmol1\mathrm{kJ\,mol^{-1}}. Divide the correction by 10001000 before adding it. At 298K298\,\mathrm{K},

RT=8.314×298=2478Jmol1=2.48kJmol1RT = 8.314 \times 298 = 2478\,\mathrm{J\,mol^{-1}} = 2.48\,\mathrm{kJ\,mol^{-1}}

That single number handles most room-temperature problems: the correction is 2.48Δng2.48\,\Delta n_g kilojoules.

Use kelvin. TT in the relation is absolute temperature. A question quoting 25C25\,{}^\circ\mathrm{C} means 298K298\,\mathrm{K}, and 100C100\,{}^\circ\mathrm{C} means 373K373\,\mathrm{K}.

Fix the direction of the conversion. Going from ΔU\Delta U to ΔH\Delta H, add ΔngRT\Delta n_g RT. Going from ΔH\Delta H to ΔU\Delta U, subtract it. Writing the equation down before substituting prevents the sign flip.

A physical check catches most sign errors without any arithmetic. If gas is created, Δng\Delta n_g is positive, the system had to spend energy pushing the atmosphere back, and ΔH\Delta H comes out greater than ΔU\Delta U. If gas is consumed, the atmosphere pushed inward and did work on the system, so ΔH\Delta H is less than ΔU\Delta U. An answer that violates that pattern has a sign error somewhere.

The other RR value, 0.08206LatmK1mol10.08206\,\mathrm{L\,atm\,K^{-1}\,mol^{-1}}, is for work in litre-atmospheres and has no business in this relation unless the enthalpies themselves are quoted in litre-atmospheres.

A size check

For most reactions the correction is small. Combustion of methane has ΔH=890.3kJmol1\Delta H = -890.3\,\mathrm{kJ\,mol^{-1}} and a correction of about 5kJmol15\,\mathrm{kJ\,mol^{-1}} — under one per cent. This is why the difference between ΔH\Delta H and ΔU\Delta U can be ignored in rough work but never in an exam answer that asks for both.

The correction matters most for phase changes and for reactions with a large Δng\Delta n_g. Vaporising water at 373K373\,\mathrm{K} has ΔH=40.79kJmol1\Delta H = 40.79\,\mathrm{kJ\,mol^{-1}} and a correction of 3.10kJmol13.10\,\mathrm{kJ\,mol^{-1}}, which is nearly eight per cent of the answer.

Reaction Δng\Delta n_g Correction at 298K298\,\mathrm{K}
C(s)+O2(g)CO2(g)\mathrm{C(s)+O_2(g) \rightarrow CO_2(g)} 00 00
CaCO3(s)CaO(s)+CO2(g)\mathrm{CaCO_3(s) \rightarrow CaO(s)+CO_2(g)} +1+1 +2.48kJ+2.48\,\mathrm{kJ}
N2(g)+3H2(g)2NH3(g)\mathrm{N_2(g)+3H_2(g) \rightarrow 2NH_3(g)} 2-2 4.96kJ-4.96\,\mathrm{kJ}
2H2(g)+O2(g)2H2O(l)\mathrm{2H_2(g)+O_2(g) \rightarrow 2H_2O(l)} 3-3 7.43kJ-7.43\,\mathrm{kJ}
2KClO3(s)2KCl(s)+3O2(g)\mathrm{2KClO_3(s) \rightarrow 2KCl(s)+3O_2(g)} +3+3 +7.43kJ+7.43\,\mathrm{kJ}

Key Point: The correction term ΔngRT\Delta n_g RT is 2.48Δng2.48\,\Delta n_g kilojoules at 298K298\,\mathrm{K}. Its sign follows the sign of Δng\Delta n_g.

Solved Examples

Question 1: Vaporising one mole of water

Treating water vapour as an ideal gas, the molar enthalpy change for vaporisation of 1mol1\,\mathrm{mol} of water at 1bar1\,\mathrm{bar} and 100C100\,{}^\circ\mathrm{C} (373K373\,\mathrm{K}) is 40.79kJmol140.79\,\mathrm{kJ\,mol^{-1}}. Calculate the internal energy change for the same process.

Answer:

The change is H2O(l)H2O(g)\mathrm{H_2O(l) \rightarrow H_2O(g)}. Liquid water is not counted, so the gaseous moles go from 00 to 11:

Δng=10=+1\Delta n_g = 1 - 0 = +1

The temperature is 100C=373K100\,{}^\circ\mathrm{C} = 373\,\mathrm{K}. I want ΔU\Delta U, so I subtract the correction:

ΔU=ΔHΔngRT\Delta U = \Delta H - \Delta n_g RT

ΔngRT=1×8.314×373=3101Jmol1=3.10kJmol1\Delta n_g RT = 1 \times 8.314 \times 373 = 3101\,\mathrm{J\,mol^{-1}} = 3.10\,\mathrm{kJ\,mol^{-1}}

ΔU=40.793.10=37.69kJmol1\Delta U = 40.79 - 3.10 = 37.69\,\mathrm{kJ\,mol^{-1}}

ΔU\Delta U is smaller because part of the 40.79kJ40.79\,\mathrm{kJ} supplied was spent making room for the vapour, not on separating the molecules.

Ans: ΔU=37.69kJmol1\Delta U = 37.69\,\mathrm{kJ\,mol^{-1}}

Watch out: 373K373\,\mathrm{K}, not 373C373\,{}^\circ\mathrm{C} and not 100100. Using 100100 in place of 373373 gives a correction of 0.83kJ0.83\,\mathrm{kJ} and a wrong answer.

Question 2: Counting the gaseous moles

Find Δng\Delta n_g for each reaction.

(a) 2H2(g)+O2(g)2H2O(l)\mathrm{2H_2(g) + O_2(g) \rightarrow 2H_2O(l)} (b) NH4NO3(s)N2O(g)+2H2O(g)\mathrm{NH_4NO_3(s) \rightarrow N_2O(g) + 2H_2O(g)} (c) H2(g)+I2(s)2HI(g)\mathrm{H_2(g) + I_2(s) \rightarrow 2HI(g)} (d) Fe2O3(s)+3CO(g)2Fe(s)+3CO2(g)\mathrm{Fe_2O_3(s) + 3CO(g) \rightarrow 2Fe(s) + 3CO_2(g)}

Answer:

Each time I list only the species carrying a (g)(g) label and subtract reactants from products.

(a) Products: liquid water, so 00 moles of gas. Reactants: 2+1=32 + 1 = 3. Δng=03=3\Delta n_g = 0 - 3 = -3.

(b) Products: 1+2=31 + 2 = 3. Reactants: the solid contributes nothing, so 00. Δng=+3\Delta n_g = +3.

(c) Products: 22. Reactants: hydrogen only, since iodine is a solid here, so 11. Δng=21=+1\Delta n_g = 2 - 1 = +1.

(d) Products: 33. Reactants: 33. The two solids drop out. Δng=0\Delta n_g = 0.

Ans: (a) 3-3 (b) +3+3 (c) +1+1 (d) 00

Watch out: In (c) the temptation is to write Δng=0\Delta n_g = 0 by counting I2\mathrm{I_2}. It is a solid, and solids never enter Δng\Delta n_g.

Question 3: Combustion of graphite

For the combustion of 1mol1\,\mathrm{mol} of graphite at 298K298\,\mathrm{K}, ΔU=393.5kJmol1\Delta U = -393.5\,\mathrm{kJ\,mol^{-1}}. Find ΔH\Delta H.

Answer:

The equation is C(s)+O2(g)CO2(g)\mathrm{C(s) + O_2(g) \rightarrow CO_2(g)}.

Gaseous products =1= 1, gaseous reactants =1= 1, and graphite is not counted.

Δng=11=0\Delta n_g = 1 - 1 = 0

ΔH=ΔU+(0)RT=ΔU=393.5kJmol1\Delta H = \Delta U + (0)RT = \Delta U = -393.5\,\mathrm{kJ\,mol^{-1}}

Ans: ΔH=393.5kJmol1\Delta H = -393.5\,\mathrm{kJ\,mol^{-1}}

Question 4: Ammonia synthesis

For N2(g)+3H2(g)2NH3(g)\mathrm{N_2(g) + 3H_2(g) \rightarrow 2NH_3(g)}, ΔH=92.4kJ\Delta H = -92.4\,\mathrm{kJ} at 298K298\,\mathrm{K}. Calculate ΔU\Delta U.

Answer:

Gaseous products =2= 2; gaseous reactants =1+3=4= 1 + 3 = 4.

Δng=24=2\Delta n_g = 2 - 4 = -2

ΔU=ΔHΔngRT=92.4(2)(8.314)(298)/1000\Delta U = \Delta H - \Delta n_g RT = -92.4 - (-2)(8.314)(298)/1000

ΔngRT=2×2.478=4.96kJ\Delta n_g RT = -2 \times 2.478 = -4.96\,\mathrm{kJ}

ΔU=92.4+4.96=87.4kJ\Delta U = -92.4 + 4.96 = -87.4\,\mathrm{kJ}

The system contracted, so the surroundings did 4.96kJ4.96\,\mathrm{kJ} of work on it. That energy stayed inside, which is why ΔU\Delta U is less negative than ΔH\Delta H.

Ans: ΔU=87.4kJ\Delta U = -87.4\,\mathrm{kJ}

Watch out: Subtracting a negative correction adds. Writing 92.44.96=97.4kJ-92.4 - 4.96 = -97.4\,\mathrm{kJ} is the commonest slip in this question.

Question 5: Cyanamide burnt in a bomb

The reaction

NH2CN(s)+32O2(g)N2(g)+CO2(g)+H2O(l)\mathrm{NH_2CN(s) + \tfrac{3}{2}O_2(g) \rightarrow N_2(g) + CO_2(g) + H_2O(l)}

has ΔU=742.7kJmol1\Delta U = -742.7\,\mathrm{kJ\,mol^{-1}} at 298K298\,\mathrm{K}. Calculate ΔH\Delta H.

Answer:

Gaseous products: nitrogen and carbon dioxide, 1+1=21 + 1 = 2. Liquid water is not counted. Gaseous reactants: oxygen only, 1.51.5; the solid cyanamide is not counted.

Δng=21.5=+0.5\Delta n_g = 2 - 1.5 = +0.5

ΔngRT=0.5×8.314×298=1239J=1.24kJ\Delta n_g RT = 0.5 \times 8.314 \times 298 = 1239\,\mathrm{J} = 1.24\,\mathrm{kJ}

ΔH=ΔU+ΔngRT=742.7+1.24=741.5kJmol1\Delta H = \Delta U + \Delta n_g RT = -742.7 + 1.24 = -741.5\,\mathrm{kJ\,mol^{-1}}

Ans: ΔH=741.5kJmol1\Delta H = -741.5\,\mathrm{kJ\,mol^{-1}}

Watch out: A fractional Δng\Delta n_g is perfectly legal. The half comes from the 32\tfrac{3}{2} in front of oxygen and must not be rounded to 11 or 22.

Question 6: Combustion of benzene

Liquid benzene burns according to

C6H6(l)+152O2(g)6CO2(g)+3H2O(l)\mathrm{C_6H_6(l) + \tfrac{15}{2}O_2(g) \rightarrow 6CO_2(g) + 3H_2O(l)}

with ΔU=3263.9kJmol1\Delta U = -3263.9\,\mathrm{kJ\,mol^{-1}} at 298K298\,\mathrm{K}. Find ΔH\Delta H.

Answer:

Gaseous products =6= 6. Gaseous reactants =7.5= 7.5. Both benzene and water are liquids and are ignored.

Δng=67.5=1.5\Delta n_g = 6 - 7.5 = -1.5

ΔngRT=1.5×2.478=3.72kJ\Delta n_g RT = -1.5 \times 2.478 = -3.72\,\mathrm{kJ}

ΔH=3263.9+(3.72)=3267.6kJmol1\Delta H = -3263.9 + (-3.72) = -3267.6\,\mathrm{kJ\,mol^{-1}}

Ans: ΔH=3267.6kJmol1\Delta H = -3267.6\,\mathrm{kJ\,mol^{-1}}

Question 7: Decomposing limestone

CaCO3(s)CaO(s)+CO2(g)\mathrm{CaCO_3(s) \rightarrow CaO(s) + CO_2(g)} has ΔH=+178.3kJmol1\Delta H = +178.3\,\mathrm{kJ\,mol^{-1}} at 298K298\,\mathrm{K}. Calculate ΔU\Delta U and say whether the reaction is exothermic or endothermic.

Answer:

Only carbon dioxide is a gas, and there are no gaseous reactants.

Δng=10=+1\Delta n_g = 1 - 0 = +1

ΔU=ΔHΔngRT=178.32.48=175.8kJmol1\Delta U = \Delta H - \Delta n_g RT = 178.3 - 2.48 = 175.8\,\mathrm{kJ\,mol^{-1}}

ΔH\Delta H is positive, so the reaction absorbs heat and is endothermic.

Ans: ΔU=175.8kJmol1\Delta U = 175.8\,\mathrm{kJ\,mol^{-1}}; the reaction is endothermic.

Question 8: The phase of the water changes the answer

Methane burns as

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

with ΔH=890.3kJmol1\Delta H = -890.3\,\mathrm{kJ\,mol^{-1}} at 298K298\,\mathrm{K}.

(a) Find ΔU\Delta U. (b) What would Δng\Delta n_g have been if the water had been produced as vapour?

Answer:

(a) Gaseous products: carbon dioxide only, 11, because the water is liquid. Gaseous reactants: 1+2=31 + 2 = 3.

Δng=13=2\Delta n_g = 1 - 3 = -2

ΔU=ΔHΔngRT=890.3(2)(2.478)=890.3+4.96=885.3kJmol1\Delta U = \Delta H - \Delta n_g RT = -890.3 - (-2)(2.478) = -890.3 + 4.96 = -885.3\,\mathrm{kJ\,mol^{-1}}

(b) With 2H2O(g)\mathrm{2H_2O(g)} the gaseous products become 1+2=31 + 2 = 3, and

Δng=33=0\Delta n_g = 3 - 3 = 0

so ΔH\Delta H and ΔU\Delta U would have been equal.

Ans: (a) ΔU=885.3kJmol1\Delta U = -885.3\,\mathrm{kJ\,mol^{-1}} (b) Δng=0\Delta n_g = 0

Watch out: The same reaction gives two different Δng\Delta n_g values depending on the state of the water. Read the phase labels before counting anything.

Question 9: Heat measured in an open beaker

Burning 0.500mol0.500\,\mathrm{mol} of a compound in an open vessel at 1bar1\,\mathrm{bar} releases 24.6kJ24.6\,\mathrm{kJ} of heat. What is ΔH\Delta H per mole of the compound?

Answer:

The vessel is open, so the pressure is constant and the heat measured is qp=ΔHq_p = \Delta H.

Heat is released, so qpq_p is negative: qp=24.6kJq_p = -24.6\,\mathrm{kJ} for 0.500mol0.500\,\mathrm{mol}.

ΔH=24.60.500=49.2kJmol1\Delta H = \frac{-24.6}{0.500} = -49.2\,\mathrm{kJ\,mol^{-1}}

Ans: ΔH=49.2kJmol1\Delta H = -49.2\,\mathrm{kJ\,mol^{-1}}

Watch out: Had the same reaction been run in a sealed rigid bomb, the measured heat would have been qV=ΔUq_V = \Delta U instead, and the two answers would differ by ΔngRT\Delta n_g RT.

Question 10: Working backwards to Delta n_g

For a certain reaction at 298K298\,\mathrm{K}, ΔHΔU=4.95kJ\Delta H - \Delta U = -4.95\,\mathrm{kJ}. Find Δng\Delta n_g and suggest a reaction that fits.

Answer:

From the working relation, ΔHΔU=ΔngRT\Delta H - \Delta U = \Delta n_g RT.

Δng=ΔHΔURT=49508.314×298=49502478=2.0\Delta n_g = \frac{\Delta H - \Delta U}{RT} = \frac{-4950}{8.314 \times 298} = \frac{-4950}{2478} = -2.0

Two moles of gas disappear. Ammonia synthesis, N2(g)+3H2(g)2NH3(g)\mathrm{N_2(g) + 3H_2(g) \rightarrow 2NH_3(g)}, has exactly this Δng\Delta n_g.

Ans: Δng=2\Delta n_g = -2

Watch out: Convert 4.95kJ-4.95\,\mathrm{kJ} to 4950J-4950\,\mathrm{J} before dividing, because RR carries joules.

Question 11: Zinc dissolving in acid

Zn(s)+2HCl(aq)ZnCl2(aq)+H2(g)\mathrm{Zn(s) + 2HCl(aq) \rightarrow ZnCl_2(aq) + H_2(g)} releases 154.0kJ154.0\,\mathrm{kJ} per mole of zinc when carried out in an open flask at 298K298\,\mathrm{K}. Find ΔH\Delta H and ΔU\Delta U.

Answer:

Open flask means constant pressure, so the measured heat is ΔH\Delta H, and it is released:

ΔH=154.0kJmol1\Delta H = -154.0\,\mathrm{kJ\,mol^{-1}}

For Δng\Delta n_g, the only gas anywhere in the equation is hydrogen. Zinc is a solid; the acid and the zinc chloride are aqueous.

Δng=10=+1\Delta n_g = 1 - 0 = +1

ΔU=ΔHΔngRT=154.02.48=156.5kJmol1\Delta U = \Delta H - \Delta n_g RT = -154.0 - 2.48 = -156.5\,\mathrm{kJ\,mol^{-1}}

Ans: ΔH=154.0kJmol1\Delta H = -154.0\,\mathrm{kJ\,mol^{-1}}, ΔU=156.5kJmol1\Delta U = -156.5\,\mathrm{kJ\,mol^{-1}}

Watch out: Aqueous species carry no entry in Δng\Delta n_g. Counting 2HCl(aq)\mathrm{2HCl(aq)} as gas would give Δng=1\Delta n_g = -1 and reverse the sign of the correction.

Question 12: A reaction with no gases at all

The neutralisation HCl(aq)+NaOH(aq)NaCl(aq)+H2O(l)\mathrm{HCl(aq) + NaOH(aq) \rightarrow NaCl(aq) + H_2O(l)} has ΔH=57.1kJmol1\Delta H = -57.1\,\mathrm{kJ\,mol^{-1}}. What is ΔU\Delta U, and why?

Answer:

No species in the equation carries a (g)(g) label, so Δng=0\Delta n_g = 0 and the correction term vanishes:

ΔH=ΔU+(0)RT\Delta H = \Delta U + (0)RT

Beyond that, everything present is a liquid or a solution, and condensed phases change volume by only a few millilitres during a reaction. The pΔVp\Delta V term is a few joules against an enthalpy change of 57100J57100\,\mathrm{J}, which is negligible.

ΔU=57.1kJmol1\Delta U = -57.1\,\mathrm{kJ\,mol^{-1}}

Ans: ΔU=57.1kJmol1\Delta U = -57.1\,\mathrm{kJ\,mol^{-1}}; with no gases involved, ΔH\Delta H and ΔU\Delta U are equal to the accuracy quoted.