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Distinguish homogeneous and heterogeneous equilibria and write equilibrium constants for both types of reactions from a balanced equation.
Definitions
A homogeneous equilibrium has all reactants and products in the same phase, such as all gases or all dissolved in one solution.
Example: N2(g)+3H2(g)⇌2NH3(g).
A heterogeneous equilibrium involves more than one phase, such as a solid in contact with a gas or a solution.
Example: CaCO3(s)⇌CaO(s)+CO2(g).
Why the distinction matters: activities
The rigorous equilibrium constant is built from activities, ai, which are dimensionless:
K=∏iaiνi, with νi>0 for products and νi<0 for reactants.
Activity of an ideal gas: a=p/p∘.
Activity of a dilute solute: a=c/c∘.
Activity of a pure solid or pure liquid: a=1.
Its molar free energy is essentially fixed, because the molecular environment does not change as more or less of it is present.
Activity of a solvent in a dilute solution: a≈1, so water is omitted.
Because K is a product of dimensionless activities, K is dimensionless. In practice we write concentrations or pressures and implicitly divide by c∘ or p∘.
Writing the expression
Products go in the numerator and reactants in the denominator, with each activity raised to its stoichiometric coefficient.
Omit pure solids and liquids.
Pressure form: Kp (gases). Concentration form: Kc. Mixed systems use whichever variable applies to each species.
Reaction | Expression |
|---|---|
N2+3H2⇌2NH3 (all gas) | K=pN2pH23pNH32 |
CaCO3(s)⇌CaO(s)+CO2(g) | K=pCO2 |
PbCl2(s)⇌Pb2+(aq)+2Cl−(aq) | K=[Pb2+][Cl−]2 |
CH3COOH+H2O(l)⇌H3O++CH3COO− | K=[CH3COOH][H3O+][CH3COO−] |
21H2(g)+21I2(s)⇌HI(g) (your slide) | K=pH21/2pHI |
Common pitfalls
A solid does not appear in K, but it must be present for equilibrium to exist. If all the CaCO3 decomposes, the system is not at equilibrium and pCO2 is no longer fixed.
For CaCO3(s), pCO2 depends only on temperature, not on how much solid is present.
Do not leave out coefficients. Writing [Pb2+][Cl−] instead of [Pb2+][Cl−]2 is the most common error.
Water is omitted only when it is the solvent in dilute solution. If water is a gaseous reactant or product, such as H2O(g), it must be included.
Worked example
Write K for 2NaHCO3(s)⇌Na2CO3(s)+H2O(g)+CO2(g).
The phases are two solids and two gases, so the system is heterogeneous.
Both solids have a=1 and drop out.
The gases appear in the numerator with coefficient 1:
K=pH2O⋅pCO2, which is dimensionless after dividing each pressure by p∘.
Relate the Gibbs free energy of reaction to the composition of the reaction mixture.
Core relationship
ΔG=ΔG∘+RTlnQ
ΔG (J mol⁻¹) is the Gibbs free energy change per mole of reaction at the current composition.
ΔG∘ (J mol⁻¹) is the standard value, with every species in its standard state.
R=8.314 J mol−1K−1.
T is in kelvin.
Q is the reaction quotient, with the same form as K but using current activities.
Where it comes from
Each species has a chemical potential μi=μi∘+RTlnai.
The RTlnai term reflects the entropy of mixing: a more dilute species has more available microstates, so it has lower free energy per mole.
The reaction free energy is ΔG=∑iνiμi.
Substituting gives ΔG=∑νiμi∘+RT∑νilnai=ΔG∘+RTlnQ.
ΔG is the slope of the Gibbs energy versus extent of reaction at constant T and p.
If ΔG<0, G falls as the reaction moves forward, so the forward reaction is spontaneous.
If ΔG>0, the reverse reaction is spontaneous.
At the minimum of G, the slope is zero: ΔG=0, which is equilibrium.
Connection to the second law (from your slides)
At constant T and p with a large heat bath, ΔGsys=−TΔSuniv.
ΔSsurr=−ΔHsys/T, so −ΔGsys/T=ΔSsys+ΔSsurr.
A negative ΔG is therefore the same statement as ΔSuniv>0.
Interpreting the sign of ΔG
Q<K gives lnQ<lnK and ΔG<0, so the reaction goes forward.
Q=K gives ΔG=0, so the system is at equilibrium.
Q>K gives ΔG>0, so the reaction goes in reverse.
Pitfalls
ΔG∘ and ΔG are different things. ΔG∘ is a fixed number at a given T. ΔG changes as the reaction proceeds and reaches zero at equilibrium.
ΔG∘>0 does not mean no reaction occurs. If Q is small enough, ΔG can still be negative.
ΔG gives the direction and driving force, not the rate. Kinetics decides how fast.
Use ΔG in J if R is in J. Mixing kJ and J is the classic error.
Q uses p/p∘ and c/c∘, and pure solids and liquids are omitted, as for K.
Worked example (your slide’s NH₃ case)
N2+3H2⇌2NH3 at 298 K, with pN2=1.0, pH2=3.0, pNH3=4.0 atm and ΔG∘=−33.32 kJ mol−1.
Q=(3.0)3(1.0)4.02=2716=0.593.
RT=(8.314 J mol−1K−1)(298 K)=2478 J mol−1=2.478 kJ mol−1.
RTlnQ=(2.478)(ln0.593)=(2.478)(−0.523)=−1.30 kJ mol−1.
ΔG=−33.32+(−1.30)=−34.6 kJ mol−1, or about −35 kJ mol⁻¹ to 2 sig. figs.
Your slide shows −1.43 for the correction term, but the arithmetic gives −1.30. The final answer to 2 sig. figs. is unchanged.
ΔG<0, so the mixture shifts forward toward NH₃.
Calculate an equilibrium constant from a standard Gibbs free energy.
Derivation
Start with ΔG=ΔG∘+RTlnQ.
At equilibrium, ΔG=0 and Q=K:
0=ΔG∘+RTlnK.
Therefore ΔG∘=−RTlnK, or lnK=−RTΔG∘, or K=e−ΔG∘/RT.
Variables and units
ΔG∘ is in J mol⁻¹ (convert kJ to J).
R=8.314 J mol−1K−1.
T is in K.
K is dimensionless.
ΔG∘ is per mole of reaction as written, so it is tied to the specific balanced equation.
Obtaining ΔG∘
From formation values: ΔGrxn∘=∑nΔGf∘(products)−∑mΔGf∘(reactants).
Elements in their standard states have ΔGf∘=0.
From enthalpy and entropy: ΔG∘=ΔH∘−TΔS∘.
From Hess’s law: combine reactions and add their ΔG∘ values.
Physical interpretation
ΔG∘ measures the free-energy gap between pure standard-state reactants and pure standard-state products.
A large negative value makes products much more stable, so K≫1.
A large positive value gives K≪1.
ΔG∘=0 gives K=1.
At 298 K, every change of 2.303RT=5.71 kJ mol−1 in ΔG∘ changes K by a factor of 10.
Pitfalls
K depends exponentially on ΔG∘, so small errors in ΔG∘ give large errors in K.
Your slide says “the higher the ΔGrxn∘, the more likely the reaction.” This is backwards. More negative ΔG∘ means larger K and a more product-favored reaction.
K>1 does not mean a fast reaction.
ΔG∘ is evaluated at the specific temperature of interest.
The sign of ΔG∘ tells you which side is favored at standard conditions, not whether the reaction proceeds under non-standard conditions. That is the job of ΔG.
Worked example (your slide)
21H2(g)+21I2(s)→HI(g), ΔG∘=+1.70 kJ mol−1 at 25.00 °C.
Convert: ΔG∘=1700 J mol−1 and T=298.15 K.
lnK=−(8.3145 J mol−1K−1)(298.15 K)1700 J mol−1=−0.686. The mol and K units cancel, leaving a dimensionless number.
K=e−0.686=0.50.
Because ΔG∘ is positive, K<1, which is consistent.
For scale, the slide’s 2H2+O2→2H2O(g) has ΔG∘=−457.14 kJ. Then lnK=457140/2478=184.5 and K=1.4×1080.
Calculate an equilibrium concentration.
Strategy
Step 1: Write the balanced equation and the correct K expression, omitting pure solids and liquids (Card 1).
Step 2: Make sure K matches the equation as written and the temperature of interest (Card 7).
Step 3: Decide which quantities are known at equilibrium and which are unknown.
Step 4: Solve algebraically for the unknown.
If only one concentration is unknown, rearrange K directly.
If initial amounts are given instead, use an equilibrium table (Card 8).
Step 5: Substitute back to verify that Q=K.
Useful relationships
Gases: pi=ciRT, which links Kp and Kc (Card 6).
Mole fraction and partial pressure: pA=xAPtotal, where xA=nA/ntotal (as in your slide).
Dalton’s law: Ptotal=∑pi.
Pitfalls
Equilibrium values are not the initial values.
Concentrations must be in mol L⁻¹, not moles, unless Δngas=0 so that volume cancels.
If you are solving for a pressure, use Kp and pressures. If you are solving for a concentration, use Kc.
Roots must be physically meaningful, meaning positive and not exceeding the available material.
Taking a square root when the stoichiometric power is 2 is valid only for a single unknown with exponent 2.
Worked example
For N2O4(g)⇌2NO2(g), Kc=4.6×10−3 at 298 K. At equilibrium [N2O4]=0.100 M. Find [NO2].
Kc=[N2O4][NO2]2.
Rearrange: [NO2]2=Kc[N2O4]=(4.6×10−3)(0.100 M). Since Kc is dimensionless, the units are M².
[NO2]2=4.6×10−4 M2.
[NO2]=4.6×10−4=0.0214 M.
Check: (0.0214)2/0.100=4.6×10−3. ✓
Predict the direction of a reaction, given K and the concentration of reactants and products.
Rule
Compute Q, using the current concentrations or pressures in the same form as K, and compare it with K.
Q<K: too many reactants, so the reaction proceeds forward (toward products).
Q=K: the system is at equilibrium and there is no net change.
Q>K: too many products, so the reaction proceeds in reverse (toward reactants).
Why it works
ΔG=RTln(Q/K), which follows from ΔG=ΔG∘+RTlnQ and ΔG∘=−RTlnK.
Q<K gives a negative ΔG (forward spontaneous).
Q>K gives a positive ΔG (reverse spontaneous).
Molecularly, the forward and reverse rates are unequal away from equilibrium. The net flow continues until the rates match and Q=K.
Pitfalls
Q is not an equilibrium quantity. It can be evaluated for any composition, including the very start of a reaction.
Do not compare raw concentrations. Always compare Q with K.
K must be for the same equation, temperature, and form (Kc versus Kp) as Q.
Pure solids and liquids are omitted from Q just as from K.
If K is huge, nearly every mixture has Q<K. If K is tiny, nearly every mixture has Q>K.
The direction tells you nothing about speed.
Worked example (continuing the slide’s NH₃ system)
N2+3H2⇌2NH3 at 298 K, ΔG∘=−33.32 kJ mol−1, with Q=16/27=0.593.
lnK=(8.314)(298)33320=13.45, so K=6.9×105.
Compare: Q=0.593≪K=6.9×105.
Since Q<K, the reaction proceeds forward, making more NH₃. This agrees with the negative ΔG from Card 2.
Convert between K and Kc.
Setup
Kc is built from molar concentrations. K (the thermodynamic constant, also called Kp when only gases are involved) is built from partial pressures.
Both are dimensionless in their rigorous form.
Derivation
For an ideal gas, pi=ciRT.
Substitute into K=∏(pi/p∘)νi:
K=∏(p∘ciRT)νi=∏(c∘ci)νi(p∘c∘RT)Δn.
With numerical values in bar and mol L⁻¹, this simplifies to:
K=Kc(RT)Δn, or equivalently Kc=K(RT)−Δn.
Δn = (moles of gaseous products) − (moles of gaseous reactants).
R=0.083145 L bar mol−1K−1 when pressures are in bar.
T is in K.
Pitfalls
Count only gases in Δn. Solids, liquids, and dissolved species do not contribute.
The value of R must match the pressure unit. Using 8.314 J mol⁻¹K⁻¹ here is wrong. Use L·bar (0.08314) or L·atm (0.08206).
If Δn=0, then K=Kc.
Using atm instead of bar changes K slightly, because 1 atm = 1.01325 bar. The standard convention is bar.
The conversion assumes ideal-gas behavior.
Worked example
N2O4(g)⇌2NO2(g) has Kp=0.113 at 298.15 K. Find Kc.
Δn=2−1=+1.
RT=(0.083145 L bar mol−1K−1)(298.15 K)=24.79 L bar mol−1.
Kc=Kp(RT)−Δn=24.790.113=4.6×10−3.
This matches the Kc used in Card 4.
Calculate the effect on K of reversing a reaction or multiplying the chemical equation by a factor.
Rules
Reversing the reaction: Krev=1/K.
Multiplying the equation by a factor n: Knew=Kn.
Halving the equation (n=21) gives a square root.
Adding reactions: Ktotal=K1⋅K2⋯.
Why: the connection to ΔG∘ (which obeys Hess’s law)
ΔG∘=−RTlnK.
Reversing the equation flips the sign of ΔG∘, so lnK→−lnK and K→1/K.
Multiplying by n multiplies ΔG∘ by n, so lnK→nlnK and K→Kn.
Adding reactions adds their ΔG∘ values, so the lnK values add and the K values multiply.
Pitfalls
K is meaningless without its equation. Always state the balanced reaction it refers to.
Multiplying the equation by 2 squares K. It does not double it.
Q transforms the same way. If K is changed, Q must be written for the same new equation.
Do not add K values when adding reactions. Multiply them.
K changes by these rules at fixed temperature. Temperature changes are a separate matter (Card 10).
Worked example (using the HI reaction from Card 3)
Given 21H2+21I2(s)→HI(g), K=0.50.
Reverse: HI→21H2+21I2(s), K=1/0.50=2.0.
Double: H2+I2(s)→2HI, K=(0.50)2=0.25.
Combining with Hess’s law (your slide’s CO example)
ΔG∘ for 2CO+O2→2CO2 equals +1088+2(−801)=−514 kJ.
In K language, K=(1/Ka)(Kb)2, where Ka is for the first given reaction and Kb for the second.
Use an equilibrium table to carry out equilibrium calculations.
The ICE method (Initial, Change, Equilibrium)
Step 1: Write the balanced equation and the K expression.
Step 2: Initial row. Enter starting concentrations (or pressures). Use 0 for species not yet present.
Step 3: Change row. Let the extent of reaction be x.
Each species changes by its coefficient times x, positive for products formed and negative for reactants consumed.
The direction is set by comparing Q with K (Card 5).
Step 4: Equilibrium row. Add Initial and Change.
Step 5: Substitute the equilibrium row into K and solve for x.
Step 6: Discard impossible roots (negative concentrations) and check by recomputing K.
Simplification (small-x approximation)
If K is very small compared with the initial concentration, assume x≪ initial amount and drop x from sums such as (0.50−x)≈0.50.
Check: x should be less than about 5% of the initial value. If not, solve the quadratic exactly.
Pitfalls
The coefficients in the Change row must match the stoichiometry. For a 2HI product, the change is +2x, and in K it is squared as (2x)2.
Work in concentrations (mol L⁻¹), not moles, unless Δngas=0.
If the volume changes, recompute the initial concentrations first.
Solids and pure liquids do not get entries in K.
With pressures, use Kp and a pressure table. Do not mix the two.
Worked example
H2(g)+I2(g)⇌2HI(g), Kc=50.0. Start with 1.00 M H₂ and 1.00 M I₂ and no HI.
H₂ | I₂ | 2HI | |
|---|---|---|---|
I | 1.00 | 1.00 | 0 |
C | −x | −x | +2x |
E | 1.00−x | 1.00−x | 2x |
Kc=(1.00−x)2(2x)2=50.0.
The expression is a perfect square, so take the root: 1.00−x2x=50.0=7.071.
Solve: 2x=7.071−7.071x, so 9.071x=7.071 and x=0.780.
[HI]=2x=1.56 M and [H2]=[I2]=1.00−0.780=0.220 M.
Check: (1.56)2/(0.220)2=50.3, which is within rounding of 50.0. ✓
Use Le Chatelier’s principle to predict how the equilibrium composition of a reaction mixture is affected by adding or removing reagents, compressing or expanding the mixture, or changing the temperature.
Principle
When a system at equilibrium is disturbed, it shifts to partially counteract the disturbance and re-establish equilibrium.
It is a qualitative shortcut for the more fundamental test: compare Q with K after the disturbance.
1. Adding or removing a species (at constant T)
K does not change, but Q does.
Adding a reactant lowers Q below K, so the system shifts forward.
Adding a product raises Q above K, so the system shifts in reverse.
Removing a species shifts the system toward replacing it.
Adding or removing a pure solid or liquid has no effect, because its activity is 1.
2. Compressing or expanding (gases)
Compression increases pressure, and the system shifts toward the side with fewer moles of gas.
Expansion shifts it toward the side with more moles of gas.
If Δngas=0, there is no shift.
K does not change.
Molecular reason: concentrations of all gases scale together, but species raised to higher total powers in Q respond more strongly.
Adding an inert gas at constant volume changes no partial pressures, so there is no shift. Adding an inert gas at constant pressure increases the volume, which acts like expansion.
3. Changing temperature
This is the only disturbance that changes K.
Treat heat as a reagent:
Endothermic (ΔH∘>0): raising T shifts the system forward and increases K.
Exothermic (ΔH∘<0): raising T shifts the system in reverse and decreases K.
The quantitative form is the van’t Hoff equation (Card 10).
4. Catalysts
A catalyst speeds forward and reverse reactions equally. It changes neither K nor the equilibrium composition, only the time to reach it.
Pitfalls
Adding a reagent does not change K. It changes Q.
Pressure changes caused by compression do not change K.
Le Chatelier’s principle can mislead for complex combined disturbances. When in doubt, compute Q.
“Shifts toward products” does not mean products exceed reactants. It means the equilibrium position moves in that direction.
Worked example
N2O4(g)⇌2NO2(g) at equilibrium. The volume is suddenly halved at constant T. Which way does it shift?
K=pN2O4/p∘(pNO2/p∘)2.
Halving the volume doubles every partial pressure:
Q=2pN2O4(2pNO2)2=2pN2O4pNO22=2K.
Q=2K>K, so the reaction shifts in reverse, toward N2O4.
This agrees with the rule: the reactant side has fewer gas moles (1 versus 2).
Predict the value of K at a different temperature.
The van’t Hoff equation
From ΔG∘=ΔH∘−TΔS∘ and ΔG∘=−RTlnK:
lnK=−RTΔH∘+RΔS∘.
Writing this at two temperatures and subtracting gives lnK1K2=−RΔH∘(T21−T11).
ΔH∘ is in J mol⁻¹.
R=8.314 J mol−1K−1.
T1,T2 are in K.
Assumptions
ΔH∘ and ΔS∘ are approximately independent of temperature over the range considered. This is a good approximation for modest temperature ranges.
The plot of lnK versus 1/T is a straight line with slope −ΔH∘/R.
Interpretation
Endothermic (ΔH∘>0): the slope is negative, so K increases as T rises.
Exothermic (ΔH∘<0): the slope is positive, so K decreases as T rises.
Physically, the entropy term TΔS∘ grows in importance as T rises, so entropy-driven processes become more favorable at high T.
Pitfalls
Use kelvin and convert ΔH∘ from kJ to J.
The sign in front of ΔH∘/R is negative. Check your answer against the Le Chatelier direction in Card 9.
Use ΔH∘ for the equation as written.
Your slide states that for a phase change ΔG∘=0. Strictly, ΔG=0 at equilibrium, and ΔG∘=0 only when K=1, which for a vaporization means the normal boiling point at 1 bar.
Worked example (the slide’s Br₂ system)
Br2(l)⇌Br2(g) has ΔH∘=31 kJ mol−1 and ΔS∘=93 J K−1mol−1. At T1=333 K, K1=1 (because ΔG∘=0 there). Find K at T2=298.15 K.
RΔH∘=8.314 J mol−1K−131000 J mol−1=3729 K.
T21−T11=298.151−3331=0.003354−0.003003=3.51×10−4 K−1.
lnK1K2=−(3729)(3.51×10−4)=−1.31.
K2=e−1.31=0.27, since K1=1.
Since K=pBr2/p∘, this predicts a vapor pressure of about 0.27 bar at 25 °C, lower than at 333 K, as expected for an endothermic process.
Cross-check: ΔG298∘=31000−(298.15)(93)=3272 J mol−1, so K=e−3272/2479=0.27. ✓