11.1-11.2 - Kc And Kp Calculations

11.1-11.2 - Kc And Kp Calculations

Use equilibrium amounts, concentrations and partial pressures to calculate equilibrium constants. Build amount tables, handle heterogeneous systems and derive the units from the powers in the expression.

Why An Equilibrium Constant Is Useful

Imagine sealing nitrogen dioxide and dinitrogen tetroxide in a flask:

NX2OX4(g)⇌2 NOX2(g)\ce{N2O4(g) <=> 2NO2(g)}

The mixture is dynamic: molecules keep reacting in both directions. At equilibrium the forward and reverse rates are equal, but the amounts of each gas do not have to be equal. The useful question is not "has the reaction stopped?" but "what ratio of products to reactants is fixed at this temperature?"

For this equation, the pressure ratio

p(NOX2)2p(NX2OX4)\frac{p(\ce{NO2})^{2}}{p(\ce{N2O4})}

has a constant value at a fixed temperature once equilibrium has been reached. A different starting mixture can reach the same equilibrium constant because the constant describes the final equilibrium ratio for the equation, not the route taken to get there.

There are two common forms in this specification:

  • KcK_{\mathrm c} uses equilibrium concentrations, usually in mol dm−3\mathrm{mol\,dm^{-3}}.
  • KpK_{\mathrm p} uses equilibrium partial pressures of gases, in atm.

For the same defined equation and unit convention, a larger equilibrium constant means a larger product-to-reactant concentration or partial-pressure ratio, with the stoichiometric powers included. Actual product fractions also depend on the total concentration or pressure and the starting mixture; a dimensional constant alone is not a universal percentage yield. Do not treat this as a rate statement: KcK_{\mathrm c} and KpK_{\mathrm p} describe position at equilibrium, not how quickly equilibrium is reached.

Writing Kc And Kp Expressions

Start with the balanced equation. Products go on the top, reactants go on the bottom, and the powers come from the coefficients in that exact equation.

For a general homogeneous equilibrium:

\(K_{\mathrm c}\) and \(K_{\mathrm p}\) expressions

aA+bB⇌cC+dDa\mathrm{A} + b\mathrm{B} \rightleftharpoons c\mathrm{C} + d\mathrm{D} Kc=[C]c[D]d[A]a[B]bKp=p(C)c p(D)dp(A)a p(B)bK_{\mathrm c} = \frac{[\mathrm{C}]^{c}[\mathrm{D}]^{d}}{[\mathrm{A}]^{a}[\mathrm{B}]^{b}} \qquad K_{\mathrm p} = \frac{p(\mathrm{C})^{c}\,p(\mathrm{D})^{d}}{p(\mathrm{A})^{a}\,p(\mathrm{B})^{b}}

[ ][\,] = equilibrium concentration in mol dm−3\mathrm{mol\,dm^{-3}}; p(X)p(\mathrm{X}) = equilibrium partial pressure of gas X in atm. KpK_{\mathrm p} includes gases only; pure solids and pure liquids are omitted from both. Units follow from the expression.

Homogeneous examples

All species are in the same phase:

FeX3X+(aq)+SCNX−(aq)⇌[FeSCN]X2+(aq)\ce{Fe3+(aq) + SCN-(aq) <=> [FeSCN]^2+(aq)} Kc=[[FeSCN]X2+]/([FeX3X+][SCNX−])K_{\mathrm c} = [\ce{[FeSCN]^2+}] / ([\ce{Fe3+}][\ce{SCN-}])

For the gas equilibrium

NX2(g)+3 HX2(g)⇌2 NHX3(g)\ce{N2(g) + 3H2(g) <=> 2NH3(g)} Kp=p(NHX3)2/(p(NX2)p(HX2)3)K_{\mathrm p} = p(\ce{NH3})^{2} / (p(\ce{N2})p(\ce{H2})^{3})

A gas equilibrium can also be treated with KcK_{\mathrm c} if the data is given as concentrations:

Kc=[NHX3]2/([NX2][HX2]3)K_{\mathrm c} = [\ce{NH3}]^{2} / ([\ce{N2}][\ce{H2}]^{3})

Heterogeneous examples

A heterogeneous equilibrium contains more than one phase. In A level equilibrium expressions, pure solids and pure liquids are omitted because their effective concentration is treated as constant.

C(s)+HX2O(g)⇌CO(g)+HX2(g)\ce{C(s) + H2O(g) <=> CO(g) + H2(g)}

The solid carbon is not included:

Kp=p(CO)p(HX2)/p(HX2O)K_{\mathrm p} = p(\ce{CO})p(\ce{H2}) / p(\ce{H2O})

If the same idea is expressed as a concentration constant for a heterogeneous reaction, pure solids are still omitted:

NHX4Cl(s)⇌NHX3(g)+HCl(g)Kc=[NHX3][HCl]\ce{NH4Cl(s) <=> NH3(g) + HCl(g)}\qquad K_{\mathrm c} = [\ce{NH3}][\ce{HCl}]

For thermal decomposition:

CaCOX3(s)⇌CaO(s)+COX2(g)\ce{CaCO3(s) <=> CaO(s) + CO2(g)}

both solids are omitted:

Kp=p(COX2)K_{\mathrm p} = p(\ce{CO2})

Common-error contrast

Wrong:

Kp=p(CaO)p(COX2)/p(CaCOX3)K_{\mathrm p} = p(\ce{CaO})p(\ce{CO2}) / p(\ce{CaCO3})

This treats solids as if they had partial pressures. The correct expression is only p(COX2)p(\ce{CO2}).

Calculating Kc From Experimental Data

KcK_{\mathrm c} calculations need equilibrium concentrations. If the data gives amounts in moles and a volume, convert each equilibrium amount using:

c=n/Vc = n/V, with nn in mol and VV in dm3\mathrm{dm^{3}}.

Worked example: an equilibrium amount table

Hydrogen and iodine react in a sealed 2.00dm32.00 \mathrm{dm^{3}} container:

HX2(g)+IX2(g)⇌2 HI(g)\ce{H2(g) + I2(g) <=> 2HI(g)}

Initially there are 0.300 mol0.300\,\mathrm{mol} of HX2\ce{H2} and 0.300 mol0.300\,\mathrm{mol} of IX2\ce{I2}, with no HI\ce{HI}. At equilibrium, 0.400 mol0.400\,\mathrm{mol} of HI\ce{HI} is present. Calculate KcK_{\mathrm c}.

Step 1: use the mole ratio.

For every 2 mol2\,\mathrm{mol} of HI\ce{HI} formed, 1 mol1\,\mathrm{mol} of HX2\ce{H2} and 1 mol1\,\mathrm{mol} of IX2\ce{I2} are used.

HI\ce{HI} formed =0.400 mol= 0.400\,\mathrm{mol}, so HX2\ce{H2} used =0.200 mol= 0.200\,\mathrm{mol} and IX2\ce{I2} used =0.200 mol= 0.200\,\mathrm{mol}.

Step 2: find equilibrium amounts.

SpeciesInitial / molChange / molEquilibrium / mol
HX2\ce{H2}0.300-0.2000.100
IX2\ce{I2}0.300-0.2000.100
HI\ce{HI}0.000+0.4000.400

Step 3: convert to equilibrium concentrations.

[HX2]=0.100/2.00=0.0500mol dm−3[\ce{H2}] = 0.100 / 2.00 = 0.0500 \mathrm{mol\,dm^{-3}} [IX2]=0.100/2.00=0.0500mol dm−3[\ce{I2}] = 0.100 / 2.00 = 0.0500 \mathrm{mol\,dm^{-3}} [HI]=0.400/2.00=0.200mol dm−3[\ce{HI}] = 0.400 / 2.00 = 0.200 \mathrm{mol\,dm^{-3}}

Step 4: substitute into the expression.

Kc=[HI]2/([HX2][IX2])K_{\mathrm c} = [\ce{HI}]^{2} / ([\ce{H2}][\ce{I2}]) Kc=(0.200)2/(0.0500×0.0500)K_{\mathrm c} = (0.200)^{2} / (0.0500\times 0.0500)

Kc=16.0K_{\mathrm c} = 16.0

Step 5: check units.

(mol dm−3)2(mol dm−3)(mol dm−3)=1\frac{(\mathrm{mol\,dm^{-3}})^{2}}{(\mathrm{mol\,dm^{-3}})(\mathrm{mol\,dm^{-3}})}=1

The units cancel, so this KcK_{\mathrm c} has no units.

Chemical interpretation: for this fixed temperature and the equation as written, the equilibrium concentration ratio favours HI\ce{HI} compared with the remaining HX2\ce{H2} and IX2\ce{I2}.

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