Overview
Hess's Law states that the enthalpy change for a reaction is the same whether it occurs in one step or multiple steps. This allows us to calculate ΔH for reactions that are difficult to measure directly.
Statement of Hess's Law
ΔHtotal=ΔH1+ΔH2+ΔH3+⋯
Enthalpy is a state function - it depends only on initial and final states, not the path taken.
Using Hess's Law
Method: Algebraic Manipulation
- Write the target equation
- Manipulate given equations to match
- Apply the same operations to ΔH values
- Add the adjusted ΔH values
Rules for Manipulating Equations
| Operation | Effect on ΔH |
|---|
| Reverse reaction | Change sign of ΔH |
| Multiply by coefficient | Multiply ΔH by same factor |
| Divide by coefficient | Divide ΔH by same factor |
Example 1: Basic Application
Target: C(s)+21O2(g)→CO(g) , ΔH=?
Given:
(1)C(s)+O2(g)→CO2(g)ΔH1=−393.5 kJ
(2)CO(g)+21O2(g)→CO2(g)ΔH2=−283.0 kJ
Solution:
Keep equation (1):
C(s)+O2(g)→CO2(g)ΔH=−393.5 kJ
Reverse equation (2):
CO2(g)→CO(g)+21O2(g)ΔH=+283.0 kJ
Add and cancel CO₂ and simplify:
C(s)+21O2(g)→CO(g)ΔH=−110.5 kJ
Example 2: Three Equations
Target: 2C(s)+H2(g)→C2H2(g) , ΔH=?
Given:
(1)C2H2(g)+25O2(g)→2CO2(g)+H2O(l)ΔH1=−1299.6 kJ
(2)C(s)+O2(g)→CO2(g)ΔH2=−393.5 kJ
(3)H2(g)+21O2(g)→H2O(l)ΔH3=−285.8 kJ
Solution:
Reverse equation (1):
2CO2(g)+H2O(l)→C2H2(g)+25O2(g)ΔH=+1299.6 kJ
Multiply equation (2) by 2:
2C(s)+2O2(g)→2CO2(g)ΔH=−787.0 kJ
Keep equation (3):
H2(g)+21O2(g)→H2O(l)ΔH=−285.8 kJ
Add and simplify:
2C(s)+H2(g)→C2H2(g)ΔH=+226.8 kJ
Using Standard Enthalpies of Formation
A direct application of Hess's Law:
ΔHrxn°=∑nΔHf°(products)−∑nΔHf°(reactants)
Example
Calculate ΔH° for: 2NH3(g)+3Cl2(g)→N2(g)+6HCl(g)
ΔHf° values (kJ/mol):
- NH3(g)=−46.1
- Cl2(g)=0
- N2(g)=0
- HCl(g)=−92.3
ΔH°=[0+6(−92.3)]−[2(−46.1)+3(0)]
ΔH°=[−553.8]−[−92.2]=−461.6 kJ
Born-Haber Cycle
A special application of Hess's Law for calculating lattice energy of ionic compounds.
Steps for NaCl
- Sublimation: Na(s)→Na(g) → ΔHsub
- Ionization: Na(g)→Na+(g)+e− → IE
- Dissociation: 21Cl2(g)→Cl(g) → 21D
- Electron affinity: Cl(g)+e−→Cl−(g) → EA
- Lattice formation: Na+(g)+Cl−(g)→NaCl(s) → −U
Overall: Na(s)+21Cl2(g)→NaCl(s) → ΔHf°
ΔHf°=ΔHsub+IE+21D+EA+(−U)
Solving for lattice energy (U):
U=ΔHsub+IE+21D+EA−ΔHf°
Energy Cycle Diagrams
Visual Representation
Elements
/ \
Direct / \ Step-wise
Path / \ Path
/ \
↓ ↓
Products ←———————→ (Intermediates)
ΔHtotal
Key Points
- Enthalpy is a state function - path independent
- Energy is conserved - total ΔH is same regardless of route
- Reactions can be added - like algebraic equations
- Signs and coefficients matter - be careful with manipulations
- All ΔH values must have consistent units - usually kJ or kJ/mol
Problem-Solving Strategy
- Write the target equation clearly
- Identify what species need to be products vs reactants
- Manipulate given equations (reverse/multiply as needed)
- Check that intermediate species cancel
- Sum the adjusted ΔH values
- Verify final equation matches target