One Phase, One Set of Rules

An equilibrium is homogeneous when every reactant and every product sits in the same phase. Nothing is a solid while something else is a gas; nothing is a liquid while something else is dissolved. One phase, throughout.

Key Point (Definition): In a homogeneous equilibrium all the reacting species — reactants and products alike — are present in a single phase, either all gaseous or all in the same solution.

Two families of homogeneous equilibria turn up again and again.

All species gaseous

The synthesis of ammonia is the standard example:

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

Nitrogen, hydrogen and ammonia are all gases at the temperature of the reaction, so the mixture is a single gas phase filling the vessel uniformly. The same is true of

H2(g)+I2(g)2HI(g)\mathrm{H_2}(g) + \mathrm{I_2}(g) \rightleftharpoons 2\mathrm{HI}(g)

2SO2(g)+O2(g)2SO3(g)2\mathrm{SO_2}(g) + \mathrm{O_2}(g) \rightleftharpoons 2\mathrm{SO_3}(g)

PCl5(g)PCl3(g)+Cl2(g)\mathrm{PCl_5}(g) \rightleftharpoons \mathrm{PCl_3}(g) + \mathrm{Cl_2}(g)

N2O4(g)2NO2(g)\mathrm{N_2O_4}(g) \rightleftharpoons 2\mathrm{NO_2}(g)

Each of these can be handled with concentrations, and each can equally well be handled with pressures. That second option is what this section is about.

Homogeneous gas phase and homogeneous solution equilibria compared with a two phase system

All species in one solution

Homogeneous does not mean gaseous. A reaction in which everything is dissolved in the same solvent is equally homogeneous. The hydrolysis of ethyl acetate is written

CH3COOC2H5(aq)+H2O(l)CH3COOH(aq)+C2H5OH(aq)\mathrm{CH_3COOC_2H_5}(aq) + \mathrm{H_2O}(l) \rightleftharpoons \mathrm{CH_3COOH}(aq) + \mathrm{C_2H_5OH}(aq)

and the formation of the blood-red thiocyanato complex of iron is

Fe3+(aq)+SCN(aq)[Fe(SCN)]2+(aq)\mathrm{Fe^{3+}}(aq) + \mathrm{SCN^-}(aq) \rightleftharpoons \mathrm{[Fe(SCN)]^{2+}}(aq)

Every species here is in the aqueous solution phase. For such equilibria only KcK_c makes sense, because dissolved species have concentrations but no partial pressures of their own. Nothing in this section about KpK_p applies to them.

What homogeneous buys you

The reason the distinction matters is a practical one. In a homogeneous equilibrium every species that appears in the balanced equation also appears in the equilibrium constant expression. Nothing gets left out. The moment a pure solid or a pure liquid enters the equation the system becomes heterogeneous, and those species drop out of the expression — a separate rule dealt with in the next section.

So for

aA+bBcC+dDa\mathrm{A} + b\mathrm{B} \rightleftharpoons c\mathrm{C} + d\mathrm{D}

with all four species in one phase,

Kc=[C]c[D]d[A]a[B]bK_c = \frac{[\mathrm{C}]^c[\mathrm{D}]^d}{[\mathrm{A}]^a[\mathrm{B}]^b}

and no term is missing.

[NEET] A one-line test for homogeneous: read the state symbols. If they are all (g)(g), or all (aq)(aq), the equilibrium is homogeneous. A single (s)(s), or an (l)(l) present as a separate pure phase, makes it heterogeneous — with one exception, the solvent. The H2O(l)\mathrm{H_2O}(l) written in the ethyl acetate hydrolysis above is the medium the reaction is run in and not a second phase, so that equilibrium is homogeneous even though an (l)(l) appears in the equation.

Why Gases Prefer Pressure

A gas mixture at equilibrium can be described in two equivalent ways. You can quote the molar concentration of each gas, [A]=nA/V[\mathrm{A}] = n_\mathrm{A}/V in mol L1\mathrm{mol\ L^{-1}}. Or you can quote the partial pressure of each gas.

Key Point (Definition): The partial pressure of a gas in a mixture is the pressure that gas alone would exert if it occupied the whole container at the same temperature. The total pressure is the sum of the partial pressures (Dalton's law), and pi=xiPtotalp_i = x_i P_{\text{total}} where xix_i is the mole fraction of that gas.

Pressure wins on convenience for three reasons.

It is what the instrument reads. A pressure gauge on a reaction vessel gives the total pressure directly. Getting concentrations instead would mean withdrawing a sample, analysing it and dividing by the volume — slower and less accurate.

Composition follows from pressure without extra measurement. If a gas mixture is 40% by volume of one component, that component's mole fraction is 0.40, and its partial pressure is 0.40×Ptotal0.40 \times P_{\text{total}}. Volume percentage, mole percentage and pressure percentage are the same number for ideal gases.

Standard states for gases are defined in pressure. The standard state of a gas is a pressure of exactly 1 bar. Thermodynamic quantities such as ΔG\Delta G^{\circ} are tabulated against that reference, so an equilibrium constant already written in pressures links straight to thermodynamics.

Writing KpK_p

The recipe is identical to the one for KcK_c; only the quantity substituted changes. Products over reactants, each raised to its stoichiometric coefficient, with partial pressures in place of concentrations.

For H2(g)+I2(g)2HI(g)\mathrm{H_2}(g) + \mathrm{I_2}(g) \rightleftharpoons 2\mathrm{HI}(g):

Kp=(pHI)2(pH2)(pI2)K_p = \frac{(p_{\mathrm{HI}})^2}{(p_{\mathrm{H_2}})(p_{\mathrm{I_2}})}

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

Kp=(pNH3)2(pN2)(pH2)3K_p = \frac{(p_{\mathrm{NH_3}})^2}{(p_{\mathrm{N_2}})(p_{\mathrm{H_2}})^3}

For 2SO2(g)+O2(g)2SO3(g)2\mathrm{SO_2}(g) + \mathrm{O_2}(g) \rightleftharpoons 2\mathrm{SO_3}(g):

Kp=(pSO3)2(pSO2)2(pO2)K_p = \frac{(p_{\mathrm{SO_3}})^2}{(p_{\mathrm{SO_2}})^2(p_{\mathrm{O_2}})}

Key Point: KpK_p is the equilibrium constant written with equilibrium partial pressures of the gaseous species, each raised to its stoichiometric coefficient, products in the numerator.

Both constants describe the same equilibrium at the same temperature, so they must be connected. The connection is the ideal gas equation.

Deriving Kp=Kc(RT)ΔnK_p = K_c(RT)^{\Delta n}

The whole derivation rests on one substitution. Start from the ideal gas equation for a single gas in the mixture:

pV=nRTpV = nRT

Divide both sides by VV:

p=nVRTp = \frac{n}{V}RT

The ratio n/Vn/V is moles per unit volume, which is exactly molar concentration. Writing cc for it,

p=cRTp = cRT

or, for a species A\mathrm{A} in the mixture,

pA=[A]RTp_{\mathrm{A}} = [\mathrm{A}]RT

At a fixed temperature RTRT is a constant, so the partial pressure of each gas is directly proportional to its molar concentration: p[gas]p \propto [\text{gas}].

Six step derivation chain from ideal gas equation to Kp and Kc relation

The general case, step by step

Take the general homogeneous gaseous equilibrium

aA(g)+bB(g)cC(g)+dD(g)a\mathrm{A}(g) + b\mathrm{B}(g) \rightleftharpoons c\mathrm{C}(g) + d\mathrm{D}(g)

Step 1. Write KpK_p from the definition:

Kp=(pC)c(pD)d(pA)a(pB)bK_p = \frac{(p_{\mathrm{C}})^c(p_{\mathrm{D}})^d}{(p_{\mathrm{A}})^a(p_{\mathrm{B}})^b}

Step 2. Replace every partial pressure by pi=[i]RTp_i = [i]RT:

Kp=([C]RT)c([D]RT)d([A]RT)a([B]RT)bK_p = \frac{([\mathrm{C}]RT)^c([\mathrm{D}]RT)^d}{([\mathrm{A}]RT)^a([\mathrm{B}]RT)^b}

Step 3. Expand each bracket. A product raised to a power is the product of the powers, so ([C]RT)c=[C]c(RT)c([\mathrm{C}]RT)^c = [\mathrm{C}]^c(RT)^c:

Kp=[C]c(RT)c[D]d(RT)d[A]a(RT)a[B]b(RT)bK_p = \frac{[\mathrm{C}]^c(RT)^c \cdot [\mathrm{D}]^d(RT)^d}{[\mathrm{A}]^a(RT)^a \cdot [\mathrm{B}]^b(RT)^b}

Step 4. Collect the concentration terms in one fraction and the RTRT terms in another:

Kp=[C]c[D]d[A]a[B]b×(RT)c+d(RT)a+bK_p = \frac{[\mathrm{C}]^c[\mathrm{D}]^d}{[\mathrm{A}]^a[\mathrm{B}]^b} \times \frac{(RT)^{c+d}}{(RT)^{a+b}}

Step 5. The first fraction is KcK_c. The second collapses by the law of indices, xm/xn=xmnx^m/x^n = x^{m-n}:

Kp=Kc×(RT)(c+d)(a+b)K_p = K_c \times (RT)^{(c+d)-(a+b)}

Step 6. Name the exponent. Writing Δn\Delta n for (c+d)(a+b)(c+d) - (a+b),

Kp=Kc(RT)Δn\boxed{\,K_p = K_c(RT)^{\Delta n}\,}

Key Point: Kp=Kc(RT)ΔnK_p = K_c(RT)^{\Delta n}, where Δn=\Delta n = (total number of moles of gaseous products) - (total number of moles of gaseous reactants), read off the balanced equation.

A worked check on the formula

Apply it to H2(g)+I2(g)2HI(g)\mathrm{H_2}(g) + \mathrm{I_2}(g) \rightleftharpoons 2\mathrm{HI}(g) from scratch instead of quoting the result:

Kp=(pHI)2(pH2)(pI2)=([HI]RT)2([H2]RT)([I2]RT)=[HI]2(RT)2[H2][I2](RT)2K_p = \frac{(p_{\mathrm{HI}})^2}{(p_{\mathrm{H_2}})(p_{\mathrm{I_2}})} = \frac{([\mathrm{HI}]RT)^2}{([\mathrm{H_2}]RT)([\mathrm{I_2}]RT)} = \frac{[\mathrm{HI}]^2(RT)^2}{[\mathrm{H_2}][\mathrm{I_2}](RT)^2}

The (RT)2(RT)^2 cancels top and bottom:

Kp=[HI]2[H2][I2]=KcK_p = \frac{[\mathrm{HI}]^2}{[\mathrm{H_2}][\mathrm{I_2}]} = K_c

Consistent with Δn=22=0\Delta n = 2 - 2 = 0 and (RT)0=1(RT)^0 = 1.

Now the ammonia synthesis, where the cancellation is incomplete:

Kp=(pNH3)2(pN2)(pH2)3=[NH3]2(RT)2[N2](RT)[H2]3(RT)3=[NH3]2[N2][H2]3(RT)24K_p = \frac{(p_{\mathrm{NH_3}})^2}{(p_{\mathrm{N_2}})(p_{\mathrm{H_2}})^3} = \frac{[\mathrm{NH_3}]^2(RT)^2}{[\mathrm{N_2}](RT) \cdot [\mathrm{H_2}]^3(RT)^3} = \frac{[\mathrm{NH_3}]^2}{[\mathrm{N_2}][\mathrm{H_2}]^3}(RT)^{2-4}

Kp=Kc(RT)2K_p = K_c(RT)^{-2}

which matches Δn=2(1+3)=2\Delta n = 2 - (1+3) = -2.

The Three Cases of Δn\Delta n

Everything the relation can do is decided by the sign of one small integer.

Three cases of delta n positive negative and zero with named example reactions

Case 1: Δn>0\Delta n > 0 — more gas moles on the right

PCl5(g)PCl3(g)+Cl2(g),Δn=21=+1\mathrm{PCl_5}(g) \rightleftharpoons \mathrm{PCl_3}(g) + \mathrm{Cl_2}(g), \qquad \Delta n = 2 - 1 = +1

Kp=Kc(RT)+1=Kc(RT)K_p = K_c(RT)^{+1} = K_c(RT)

At any ordinary temperature RTRT is a large number — at 500 K it is 0.0831×500=41.60.0831 \times 500 = 41.6 — so KpK_p comes out larger than KcK_c, here by a factor of about 42.

Another with Δn=+1\Delta n = +1:  N2O4(g)2NO2(g)\ \mathrm{N_2O_4}(g) \rightleftharpoons 2\mathrm{NO_2}(g), since 21=+12 - 1 = +1.

Case 2: Δn<0\Delta n < 0 — more gas moles on the left

2SO2(g)+O2(g)2SO3(g),Δn=23=12\mathrm{SO_2}(g) + \mathrm{O_2}(g) \rightleftharpoons 2\mathrm{SO_3}(g), \qquad \Delta n = 2 - 3 = -1

Kp=Kc(RT)1=KcRTK_p = K_c(RT)^{-1} = \frac{K_c}{RT}

Now KpK_p is smaller than KcK_c, divided by that same large factor.

The strongest common example is ammonia synthesis, N2(g)+3H2(g)2NH3(g)\mathrm{N_2}(g) + 3\mathrm{H_2}(g) \rightleftharpoons 2\mathrm{NH_3}(g), with Δn=24=2\Delta n = 2 - 4 = -2 and

Kp=Kc(RT)2K_p = \frac{K_c}{(RT)^2}

At 500 K that divides by 41.62173041.6^2 \approx 1730.

Case 3: Δn=0\Delta n = 0 — the numbers are equal

H2(g)+I2(g)2HI(g),Δn=22=0\mathrm{H_2}(g) + \mathrm{I_2}(g) \rightleftharpoons 2\mathrm{HI}(g), \qquad \Delta n = 2 - 2 = 0

Kp=Kc(RT)0=Kc×1=KcK_p = K_c(RT)^0 = K_c \times 1 = K_c

Key Point: Kp=KcK_p = K_c exactly when Δn=0\Delta n = 0, and only then. This holds at every temperature, because (RT)0=1(RT)^0 = 1 whatever TT may be.

Other equilibria with Δn=0\Delta n = 0:

CO(g)+H2O(g)CO2(g)+H2(g),Δn=22=0\mathrm{CO}(g) + \mathrm{H_2O}(g) \rightleftharpoons \mathrm{CO_2}(g) + \mathrm{H_2}(g), \qquad \Delta n = 2 - 2 = 0

N2(g)+O2(g)2NO(g),Δn=22=0\mathrm{N_2}(g) + \mathrm{O_2}(g) \rightleftharpoons 2\mathrm{NO}(g), \qquad \Delta n = 2 - 2 = 0

2HI(g)H2(g)+I2(g),Δn=22=02\mathrm{HI}(g) \rightleftharpoons \mathrm{H_2}(g) + \mathrm{I_2}(g), \qquad \Delta n = 2 - 2 = 0

The three cases side by side

Δn\Delta n Meaning Relation Size comparison Named example
+1+1 one extra mole of gas formed Kp=Kc(RT)K_p = K_c(RT) Kp>KcK_p > K_c PCl5PCl3+Cl2\mathrm{PCl_5} \rightleftharpoons \mathrm{PCl_3} + \mathrm{Cl_2}
+2+2 two extra moles of gas formed Kp=Kc(RT)2K_p = K_c(RT)^2 KpKcK_p \gg K_c NH4HS(s)NH3(g)+H2S(g)\mathrm{NH_4HS}(s) \rightleftharpoons \mathrm{NH_3}(g) + \mathrm{H_2S}(g)
00 gas moles unchanged Kp=KcK_p = K_c equal H2+I22HI\mathrm{H_2} + \mathrm{I_2} \rightleftharpoons 2\mathrm{HI}
1-1 one mole of gas consumed Kp=Kc/(RT)K_p = K_c/(RT) Kp<KcK_p < K_c 2SO2+O22SO32\mathrm{SO_2} + \mathrm{O_2} \rightleftharpoons 2\mathrm{SO_3}
2-2 two moles of gas consumed Kp=Kc/(RT)2K_p = K_c/(RT)^2 KpKcK_p \ll K_c N2+3H22NH3\mathrm{N_2} + 3\mathrm{H_2} \rightleftharpoons 2\mathrm{NH_3}

[JEE Main] A question that gives KcK_c and asks for KpK_p without giving TT is answerable only if Δn=0\Delta n = 0. Check Δn\Delta n before hunting for a missing temperature.

Δn\Delta n Counts Gases and Nothing Else

This is where the marks go.

Key Point: Δn\Delta n in Kp=Kc(RT)ΔnK_p = K_c(RT)^{\Delta n} is the change in the number of moles of gaseous species only. Solids, pure liquids and dissolved species contribute zero, on both sides.

The reason follows from the derivation. The factors of RTRT appeared because each gaseous partial pressure was replaced by [i]RT[i]RT. A solid or a pure liquid never entered the equilibrium expression at all, so it never contributed an RTRT, so it cannot contribute to the exponent.

The error to avoid

The commonest mistake is to count every species in the balanced equation — the total change in moles — instead of only the gaseous ones. Three reactions expose the difference immediately.

C(s)+CO2(g)2CO(g)\mathrm{C}(s) + \mathrm{CO_2}(g) \rightleftharpoons 2\mathrm{CO}(g)

Total moles: 22 on the right, 22 on the left, so a total change of 00. Gaseous moles: 22 on the right, 11 on the left, so Δn=21=+1\Delta n = 2 - 1 = +1. The correct relation is Kp=Kc(RT)K_p = K_c(RT), and a student who used the total change would have written Kp=KcK_p = K_c and lost the whole answer.

NH4HS(s)NH3(g)+H2S(g)\mathrm{NH_4HS}(s) \rightleftharpoons \mathrm{NH_3}(g) + \mathrm{H_2S}(g)

Total change: 21=+12 - 1 = +1. Gaseous change: 20=+22 - 0 = +2. So Kp=Kc(RT)2K_p = K_c(RT)^2, not Kc(RT)K_c(RT).

Fe2O3(s)+3CO(g)2Fe(s)+3CO2(g)\mathrm{Fe_2O_3}(s) + 3\mathrm{CO}(g) \rightleftharpoons 2\mathrm{Fe}(s) + 3\mathrm{CO_2}(g)

Total change: 54=+15 - 4 = +1. Gaseous change: 33=03 - 3 = 0. So Kp=KcK_p = K_c exactly, at every temperature, even though the equation looks lopsided.

The habit that prevents it

Before touching the formula, rewrite the equation with the non-gaseous species struck out of the count:

  1. List the coefficients of the (g)(g) species on the product side and add them.
  2. List the coefficients of the (g)(g) species on the reactant side and add them.
  3. Subtract: products minus reactants. That number, and only that number, is Δn\Delta n.

(aq)(aq) species are counted the same way as solids — that is, not at all. A species dissolved in water has no partial pressure, so it contributes no RTRT.

[JEE/NEET] In a heterogeneous equilibrium, the solid and liquid species are absent from the KpK_p expression and absent from Δn\Delta n. Both omissions are the same omission.

Units, RR and the Standard-State Convention

Choosing RR to match the pressure unit

The value of RR substituted into (RT)Δn(RT)^{\Delta n} must carry the same pressure unit that KpK_p is expressed in. Two combinations are in common use.

Pressure unit for KpK_p Value of RR to use Units of RR
bar 0.08310.0831 L bar K1 mol1\mathrm{L\ bar\ K^{-1}\ mol^{-1}}
atm 0.08210.0821 L atm K1 mol1\mathrm{L\ atm\ K^{-1}\ mol^{-1}}

Concentrations are in mol L1\mathrm{mol\ L^{-1}} in both cases, and TT is always in kelvin.

This section uses R=0.0831 L bar K1 mol1R = 0.0831\ \mathrm{L\ bar\ K^{-1}\ mol^{-1}} and expresses every KpK_p in bar, because the standard state for pressure is defined as exactly 1 bar. Where a problem quotes KpK_p in atm, R=0.0821 L atm K1 mol1R = 0.0821\ \mathrm{L\ atm\ K^{-1}\ mol^{-1}} is used instead so that the units agree. Mixing them — a KpK_p in atm with R=0.0831R = 0.0831 — produces a wrong number by a factor of about 1.2% per power of Δn\Delta n, which is enough to miss a printed option.

Useful conversions: 1 bar=105 Pa1\ \mathrm{bar} = 10^5\ \mathrm{Pa}, and 1 atm=1.013 bar=1.013×105 Pa1\ \mathrm{atm} = 1.013\ \mathrm{bar} = 1.013 \times 10^5\ \mathrm{Pa}.

Units of KcK_c and KpK_p

Substituting concentrations in mol L1\mathrm{mol\ L^{-1}} and pressures in bar leaves the constant with units unless the powers on top and bottom cancel:

  • units of KcK_c are (mol L1)Δn(\mathrm{mol\ L^{-1}})^{\Delta n}
  • units of KpK_p are (bar)Δn(\mathrm{bar})^{\Delta n}

Worked through for three reactions:

Reaction Δn\Delta n Units of KcK_c Units of KpK_p
H2+I22HI\mathrm{H_2} + \mathrm{I_2} \rightleftharpoons 2\mathrm{HI} 00 none none
N2O42NO2\mathrm{N_2O_4} \rightleftharpoons 2\mathrm{NO_2} +1+1 mol L1\mathrm{mol\ L^{-1}} bar\mathrm{bar}
N2+3H22NH3\mathrm{N_2} + 3\mathrm{H_2} \rightleftharpoons 2\mathrm{NH_3} 2-2 mol2 L2\mathrm{mol^{-2}\ L^{2}} bar2\mathrm{bar^{-2}}

The same Δn\Delta n that sets the power of RTRT sets the units — one fact doing two jobs.

Why the constants are strictly dimensionless

Each concentration is properly divided by the standard concentration c=1 mol L1c^{\circ} = 1\ \mathrm{mol\ L^{-1}}, and each pressure by the standard pressure p=1 barp^{\circ} = 1\ \mathrm{bar}. A pressure of 4 bar becomes 4 bar/1 bar=44\ \mathrm{bar}/1\ \mathrm{bar} = 4, a pure number. Every term entering the expression is then a ratio, and KpK_p and KcK_c come out dimensionless.

The numerical values are still different whenever Δn0\Delta n \neq 0, because the two standard states are different. Being dimensionless does not make them equal.

Key Point: Written against standard states, both KpK_p and KcK_c are dimensionless. In routine numerical work the units (bar)Δn(\mathrm{bar})^{\Delta n} and (mol L1)Δn(\mathrm{mol\ L^{-1}})^{\Delta n} are still quoted, and quoting them is accepted.

[Board] State the temperature and the pressure unit whenever a KpK_p value is written down. A bare number with neither is incomplete.

Worked Questions

Question 1: Reading Δn\Delta n off four equations

State Δn\Delta n for each: (i) 2NOCl(g)2NO(g)+Cl2(g)2\mathrm{NOCl}(g) \rightleftharpoons 2\mathrm{NO}(g) + \mathrm{Cl_2}(g), (ii) CaCO3(s)CaO(s)+CO2(g)\mathrm{CaCO_3}(s) \rightleftharpoons \mathrm{CaO}(s) + \mathrm{CO_2}(g), (iii) C(s)+CO2(g)2CO(g)\mathrm{C}(s) + \mathrm{CO_2}(g) \rightleftharpoons 2\mathrm{CO}(g), (iv) Fe2O3(s)+3CO(g)2Fe(s)+3CO2(g)\mathrm{Fe_2O_3}(s) + 3\mathrm{CO}(g) \rightleftharpoons 2\mathrm{Fe}(s) + 3\mathrm{CO_2}(g).

Answer:

I count only the species carrying (g)(g).

(i) Gaseous products 2+1=32 + 1 = 3; gaseous reactants 22. So Δn=32=+1\Delta n = 3 - 2 = +1.

(ii) Gaseous products 11 (the CO2\mathrm{CO_2}); gaseous reactants 00, since CaCO3\mathrm{CaCO_3} is a solid. So Δn=10=+1\Delta n = 1 - 0 = +1.

(iii) Gaseous products 22; gaseous reactants 11, because the graphite does not count. So Δn=21=+1\Delta n = 2 - 1 = +1.

(iv) Gaseous products 33; gaseous reactants 33. So Δn=33=0\Delta n = 3 - 3 = 0, and Kp=KcK_p = K_c for this one.

Ans: (i) +1+1, (ii) +1+1, (iii) +1+1, (iv) 00 Watch out: In (iii) the total number of moles does not change at all, and in (iv) the total goes up by one. Both totals are irrelevant.

Question 2: KcK_c to KpK_p for nitrosyl chloride

For 2NOCl(g)2NO(g)+Cl2(g)2\mathrm{NOCl}(g) \rightleftharpoons 2\mathrm{NO}(g) + \mathrm{Cl_2}(g), Kc=3.75×106K_c = 3.75 \times 10^{-6} at 1069 K. Calculate KpK_p.

Answer:

First I find Δn\Delta n. Gaseous products =2+1=3= 2 + 1 = 3, gaseous reactants =2= 2, so Δn=+1\Delta n = +1.

The relation is Kp=Kc(RT)Δn=Kc(RT)1K_p = K_c(RT)^{\Delta n} = K_c(RT)^1.

With R=0.0831 L bar K1 mol1R = 0.0831\ \mathrm{L\ bar\ K^{-1}\ mol^{-1}} and T=1069 KT = 1069\ \mathrm{K}:

RT=0.0831×1069=88.83RT = 0.0831 \times 1069 = 88.83

Kp=3.75×106×88.83=3.33×104K_p = 3.75 \times 10^{-6} \times 88.83 = 3.33 \times 10^{-4}

Ans: Kp=3.33×104 barK_p = 3.33 \times 10^{-4}\ \mathrm{bar} Watch out: Δn\Delta n is +1+1, so RTRT multiplies. Dividing by 88.83 instead gives 4.2×1084.2 \times 10^{-8}, which is the answer to the reverse conversion.

Question 3: KpK_p to KcK_c for the contact process

At 450 K, Kp=2.0×1010 bar1K_p = 2.0 \times 10^{10}\ \mathrm{bar^{-1}} for 2SO2(g)+O2(g)2SO3(g)2\mathrm{SO_2}(g) + \mathrm{O_2}(g) \rightleftharpoons 2\mathrm{SO_3}(g). Find KcK_c.

Answer:

Gaseous products =2= 2, gaseous reactants =2+1=3= 2 + 1 = 3, so Δn=23=1\Delta n = 2 - 3 = -1.

Kp=Kc(RT)1Kc=Kp×RTK_p = K_c(RT)^{-1} \quad \Rightarrow \quad K_c = K_p \times RT

RT=0.0831×450=37.40RT = 0.0831 \times 450 = 37.40

Kc=2.0×1010×37.40=7.48×1011K_c = 2.0 \times 10^{10} \times 37.40 = 7.48 \times 10^{11}

Ans: Kc=7.48×1011 L mol1K_c = 7.48 \times 10^{11}\ \mathrm{L\ mol^{-1}} Watch out: The unit bar1\mathrm{bar^{-1}} printed with KpK_p is itself a check: (bar)Δn(\mathrm{bar})^{\Delta n} with Δn=1\Delta n = -1. If your Δn\Delta n disagrees with the printed unit, one of them is wrong.

Question 4: A carbonate with a solid on each side

Kp=167 kPaK_p = 167\ \mathrm{kPa} at 1073 K for CaCO3(s)CaO(s)+CO2(g)\mathrm{CaCO_3}(s) \rightleftharpoons \mathrm{CaO}(s) + \mathrm{CO_2}(g). Calculate KcK_c.

Answer:

The unit on KpK_p decides everything here. Both solids drop out, so KpK_p is simply pCO2p_{\mathrm{CO_2}}, and the figure 167 is in kilopascals — that is 1.67 bar1.67\ \mathrm{bar}, sitting sensibly beside the 2.0×105 Pa2.0 \times 10^{5}\ \mathrm{Pa} measured for this equilibrium near 1100 K. Read as 167 bar it would be absurd. So I take RR in the matching unit, R=8.31 L kPa K1 mol1R = 8.31\ \mathrm{L\ kPa\ K^{-1}\ mol^{-1}}.

Only CO2\mathrm{CO_2} is a gas, so Δn=10=+1\Delta n = 1 - 0 = +1.

RT=8.31×1073=8916RT = 8.31 \times 1073 = 8916

Kc=Kp(RT)Δn=1678916=1.87×102K_c = \frac{K_p}{(RT)^{\Delta n}} = \frac{167}{8916} = 1.87 \times 10^{-2}

Ans: Kc=1.87×102 mol L1K_c = 1.87 \times 10^{-2}\ \mathrm{mol\ L^{-1}} Watch out: Both solids are absent from the KpK_p expression and absent from Δn\Delta n. The other trap is the unit: pairing a KpK_p of 167 kPa with R=0.0831 L bar K1 mol1R = 0.0831\ \mathrm{L\ bar\ K^{-1}\ mol^{-1}} gives 1.871.87, a hundred times too large, because RR and the pressure unit no longer agree.

Question 5: Phosphorus pentachloride, KcK_c to KpK_p

For PCl5(g)PCl3(g)+Cl2(g)\mathrm{PCl_5}(g) \rightleftharpoons \mathrm{PCl_3}(g) + \mathrm{Cl_2}(g), Kc=8.3×103K_c = 8.3 \times 10^{-3} at 473 K. Find KpK_p.

Answer:

Δn=21=+1\Delta n = 2 - 1 = +1.

RT=0.0831×473=39.31RT = 0.0831 \times 473 = 39.31

Kp=Kc(RT)=8.3×103×39.31=0.326K_p = K_c(RT) = 8.3 \times 10^{-3} \times 39.31 = 0.326

Ans: Kp=0.326 barK_p = 0.326\ \mathrm{bar}

Question 6: Iodine vapour partly dissociated

At a total pressure of 105 Pa10^5\ \mathrm{Pa}, iodine vapour at equilibrium contains 40% by volume of I atoms. Calculate KpK_p for I2(g)2I(g)\mathrm{I_2}(g) \rightleftharpoons 2\mathrm{I}(g).

Answer:

A total pressure of 105 Pa10^5\ \mathrm{Pa} is 1 bar1\ \mathrm{bar}.

For ideal gases, percentage by volume equals mole percentage, so the mole fraction of I atoms is 0.400.40 and that of I2\mathrm{I_2} is 0.600.60.

Using pi=xiPtotalp_i = x_i P_{\text{total}}:

pI=0.40×1=0.40 bar,pI2=0.60×1=0.60 barp_{\mathrm{I}} = 0.40 \times 1 = 0.40\ \mathrm{bar}, \qquad p_{\mathrm{I_2}} = 0.60 \times 1 = 0.60\ \mathrm{bar}

Kp=(pI)2pI2=(0.40)20.60=0.160.60=0.267K_p = \frac{(p_{\mathrm{I}})^2}{p_{\mathrm{I_2}}} = \frac{(0.40)^2}{0.60} = \frac{0.16}{0.60} = 0.267

Ans: Kp=0.267 barK_p = 0.267\ \mathrm{bar} Watch out: The coefficient 2 in 2I2\mathrm{I} becomes a square, not a multiplier. Writing 2×0.40/0.602 \times 0.40/0.60 gives 1.331.33, a wrong answer produced by a very common slip.

Question 7: Hydrogen iodide decomposing, and why RR never appears

A sample of HI(g)\mathrm{HI}(g) is placed in a flask at a pressure of 0.2 atm. At equilibrium the partial pressure of HI\mathrm{HI} is 0.04 atm. Find KpK_p for 2HI(g)H2(g)+I2(g)2\mathrm{HI}(g) \rightleftharpoons \mathrm{H_2}(g) + \mathrm{I_2}(g), and state KcK_c.

Answer:

The pressure of HI falls from 0.2 atm to 0.04 atm, so 0.16 atm of HI has reacted.

From the stoichiometry, 2 mol HI give 1 mol H2\mathrm{H_2} and 1 mol I2\mathrm{I_2}. So the pressure of each product formed is 0.16/2=0.08 atm0.16/2 = 0.08\ \mathrm{atm}.

Kp=pH2pI2(pHI)2=0.08×0.08(0.04)2=0.00640.0016=4.0K_p = \frac{p_{\mathrm{H_2}} \cdot p_{\mathrm{I_2}}}{(p_{\mathrm{HI}})^2} = \frac{0.08 \times 0.08}{(0.04)^2} = \frac{0.0064}{0.0016} = 4.0

Here Δn=22=0\Delta n = 2 - 2 = 0, so Kp=Kc(RT)0=KcK_p = K_c(RT)^0 = K_c. No value of RR and no temperature are needed.

Ans: Kp=4.0K_p = 4.0 and Kc=4.0K_c = 4.0, both dimensionless Watch out: The 0.16 atm consumed is halved to get each product pressure. Using 0.16 for H2\mathrm{H_2} and I2\mathrm{I_2} gives 1616, four times too large.

Question 8: Working in atmospheres

Kp=0.04 atmK_p = 0.04\ \mathrm{atm} at 899 K for C2H6(g)C2H4(g)+H2(g)\mathrm{C_2H_6}(g) \rightleftharpoons \mathrm{C_2H_4}(g) + \mathrm{H_2}(g). Calculate KcK_c at this temperature.

Answer:

KpK_p is quoted in atm, so I use R=0.0821 L atm K1 mol1R = 0.0821\ \mathrm{L\ atm\ K^{-1}\ mol^{-1}} to keep the units consistent.

Δn=21=+1\Delta n = 2 - 1 = +1.

Kc=KpRT=0.040.0821×899K_c = \frac{K_p}{RT} = \frac{0.04}{0.0821 \times 899}

RT=0.0821×899=73.81RT = 0.0821 \times 899 = 73.81

Kc=0.0473.81=5.42×104K_c = \frac{0.04}{73.81} = 5.42 \times 10^{-4}

Ans: Kc=5.42×104 mol L1K_c = 5.42 \times 10^{-4}\ \mathrm{mol\ L^{-1}} Watch out: Using R=0.0831R = 0.0831 with a KpK_p in atm gives 5.35×1045.35 \times 10^{-4} — close enough to look right and wrong enough to miss the printed option.

Question 9: The ratio Kp/KcK_p/K_c for ammonia synthesis

For N2(g)+3H2(g)2NH3(g)\mathrm{N_2}(g) + 3\mathrm{H_2}(g) \rightleftharpoons 2\mathrm{NH_3}(g) at 500 K, find the ratio Kp/KcK_p/K_c.

Answer:

Δn=24=2\Delta n = 2 - 4 = -2, so

KpKc=(RT)Δn=(RT)2=1(RT)2\frac{K_p}{K_c} = (RT)^{\Delta n} = (RT)^{-2} = \frac{1}{(RT)^2}

RT=0.0831×500=41.55RT = 0.0831 \times 500 = 41.55

(RT)2=1726.4(RT)^2 = 1726.4

KpKc=11726.4=5.79×104\frac{K_p}{K_c} = \frac{1}{1726.4} = 5.79 \times 10^{-4}

Ans: Kp/Kc=5.79×104K_p/K_c = 5.79 \times 10^{-4}, so KpK_p is about 1700 times smaller than KcK_c Watch out: Δn\Delta n is 2-2, not 1-1. Using 1-1 gives 2.41×1022.41 \times 10^{-2}.

Question 10: When the answer needs no temperature

For which of these can KpK_p be found from KcK_c without knowing TT? (i) CO(g)+H2O(g)CO2(g)+H2(g)\mathrm{CO}(g) + \mathrm{H_2O}(g) \rightleftharpoons \mathrm{CO_2}(g) + \mathrm{H_2}(g), (ii) 2NO2(g)N2O4(g)2\mathrm{NO_2}(g) \rightleftharpoons \mathrm{N_2O_4}(g), (iii) Fe2O3(s)+3CO(g)2Fe(s)+3CO2(g)\mathrm{Fe_2O_3}(s) + 3\mathrm{CO}(g) \rightleftharpoons 2\mathrm{Fe}(s) + 3\mathrm{CO_2}(g).

Answer:

I check Δn\Delta n in each case.

(i) 22=02 - 2 = 0, so Kp=KcK_p = K_c. No temperature needed.

(ii) 12=11 - 2 = -1, so Kp=Kc/(RT)K_p = K_c/(RT). Temperature needed.

(iii) Gaseous only: 33=03 - 3 = 0, so Kp=KcK_p = K_c. No temperature needed, even though solids appear in the equation.

Ans: (i) and (iii) Watch out: In (iii), counting all species gives a total change of +1+1 and the false conclusion that TT is required.

Question 11: Building KpK_p from a starting pressure

A vessel at 400 C400\ {}^{\circ}\mathrm{C} is charged with an equimolar mixture of CO and steam at pCO=pH2O=4.0 barp_{\mathrm{CO}} = p_{\mathrm{H_2O}} = 4.0\ \mathrm{bar}. For CO(g)+H2O(g)CO2(g)+H2(g)\mathrm{CO}(g) + \mathrm{H_2O}(g) \rightleftharpoons \mathrm{CO_2}(g) + \mathrm{H_2}(g), Kp=10.1K_p = 10.1. Find the equilibrium partial pressure of H2\mathrm{H_2}.

Answer:

Let xx bar of CO react. Then xx bar of steam also reacts, and xx bar each of CO2\mathrm{CO_2} and H2\mathrm{H_2} form.

At equilibrium: pCO=pH2O=(4.0x)p_{\mathrm{CO}} = p_{\mathrm{H_2O}} = (4.0 - x), and pCO2=pH2=xp_{\mathrm{CO_2}} = p_{\mathrm{H_2}} = x.

Kp=xx(4.0x)(4.0x)=x2(4.0x)2=10.1K_p = \frac{x \cdot x}{(4.0-x)(4.0-x)} = \frac{x^2}{(4.0-x)^2} = 10.1

Both sides are perfect squares, so I take the square root:

x4.0x=10.1=3.178\frac{x}{4.0-x} = \sqrt{10.1} = 3.178

x=3.178(4.0x)=12.713.178xx = 3.178(4.0 - x) = 12.71 - 3.178x

4.178x=12.71x=3.044.178x = 12.71 \quad \Rightarrow \quad x = 3.04

Ans: pH2=3.04 barp_{\mathrm{H_2}} = 3.04\ \mathrm{bar} Watch out: Δn=0\Delta n = 0 here, so no conversion between KpK_p and KcK_c is involved at any stage. Taking the square root turns a quadratic into one line.

Question 12: Same reaction, opposite direction

KpK_p for N2O4(g)2NO2(g)\mathrm{N_2O_4}(g) \rightleftharpoons 2\mathrm{NO_2}(g) is 0.115 bar0.115\ \mathrm{bar} at 298 K. Find KcK_c for this reaction, and then KcK_c for 2NO2(g)N2O4(g)2\mathrm{NO_2}(g) \rightleftharpoons \mathrm{N_2O_4}(g).

Answer:

For the forward equation as written, Δn=21=+1\Delta n = 2 - 1 = +1.

RT=0.0831×298=24.76RT = 0.0831 \times 298 = 24.76

Kc=KpRT=0.11524.76=4.64×103K_c = \frac{K_p}{RT} = \frac{0.115}{24.76} = 4.64 \times 10^{-3}

Reversing an equation inverts its equilibrium constant:

Kc=14.64×103=215K_c' = \frac{1}{4.64 \times 10^{-3}} = 215

Ans: Kc=4.64×103 mol L1K_c = 4.64 \times 10^{-3}\ \mathrm{mol\ L^{-1}} for the dissociation, the value quoted for this equilibrium at 298 K throughout the chapter; Kc=215 L mol1K_c' = 215\ \mathrm{L\ mol^{-1}} for the dimerisation Watch out: Convert first, invert second — or invert first and convert with Δn=1\Delta n = -1. Both routes agree; mixing the sign of Δn\Delta n with the inversion does not.

Fixing the Section in Place

The chain of reasoning in six lines

  1. All species in one phase \Rightarrow homogeneous equilibrium, nothing dropped from the expression.
  2. For gases, partial pressure is the natural variable: it is measured directly and defines the standard state.
  3. pV=nRTpV = nRT gives p=(n/V)RT=cRTp = (n/V)RT = cRT for each gas separately.
  4. Substituting pi=[i]RTp_i = [i]RT into KpK_p pulls out a factor (RT)(RT) for every mole of gas in the equation.
  5. The factors collect into (RT)Δn(RT)^{\Delta n}, giving Kp=Kc(RT)ΔnK_p = K_c(RT)^{\Delta n}.
  6. Δn\Delta n = gaseous products - gaseous reactants. Nothing else is counted.

Four errors that cost marks

Counting non-gaseous species in Δn\Delta n. C(s)+CO2(g)2CO(g)\mathrm{C}(s) + \mathrm{CO_2}(g) \rightleftharpoons 2\mathrm{CO}(g) has Δn=+1\Delta n = +1, not 0. Strike out the solids and liquids before counting.

Getting the sign backwards. Kp=Kc(RT)ΔnK_p = K_c(RT)^{\Delta n} means multiply by (RT)Δn(RT)^{\Delta n} when going from KcK_c to KpK_p, and divide by it when going the other way. A quick sanity check: for Δn>0\Delta n > 0, KpK_p must be the bigger number.

Mismatching RR with the pressure unit. Bar goes with 0.08310.0831, atm goes with 0.08210.0821. Choose RR after looking at the unit printed on KpK_p.

Forgetting the stoichiometric powers inside the pressure expression. KpK_p for I22I\mathrm{I_2} \rightleftharpoons 2\mathrm{I} is (pI)2/pI2(p_{\mathrm{I}})^2/p_{\mathrm{I_2}}, never 2pI/pI22p_{\mathrm{I}}/p_{\mathrm{I_2}}.

Formula card

pi=[i]RTpi=xiPtotalPtotal=pip_i = [i]RT \qquad p_i = x_i P_{\text{total}} \qquad P_{\text{total}} = \sum p_i

Kp=Kc(RT)Δn,Δn=(moles of gaseous products)(moles of gaseous reactants)K_p = K_c(RT)^{\Delta n}, \qquad \Delta n = (\text{moles of gaseous products}) - (\text{moles of gaseous reactants})

R=0.0831 L bar K1 mol1 with Kp in bar;R=0.0821 L atm K1 mol1 with Kp in atmR = 0.0831\ \mathrm{L\ bar\ K^{-1}\ mol^{-1}} \text{ with } K_p \text{ in bar}; \qquad R = 0.0821\ \mathrm{L\ atm\ K^{-1}\ mol^{-1}} \text{ with } K_p \text{ in atm}

Units: Kc in (mol L1)Δn,Kp in (bar)Δn\text{Units: } K_c \text{ in } (\mathrm{mol\ L^{-1}})^{\Delta n}, \quad K_p \text{ in } (\mathrm{bar})^{\Delta n}

Δn=0    Kp=Kc\Delta n = 0 \iff K_p = K_c