Heat Chemistry Equation- Thermochemistry Formulas
What Is a Heat Chemistry Equation?
A heat chemistry equation is a balanced chemical equation that includes thermal energy changes. It shows whether a reaction absorbs or releases heat.
Standard equations show mass and moles. Heat equations go further—they tell you exactly how much energy flows in or out.
The Basic Heat Chemistry Equation
The fundamental relationship:
Q = mcΔT
Where:
- Q = heat energy (usually in Joules)
- m = mass of the substance (in grams)
- c = specific heat capacity (J/g·°C)
- ΔT = temperature change (T_final - T_initial)
This is the workhorse of thermochemistry. Memorize it.
Understanding Enthalpy (ΔH)
Enthalpy is the total heat content of a system. The change in enthalpy—ΔH—tells you if a reaction is endothermic or exothermic.
Endothermic Reactions
Heat is absorbed. ΔH is positive.
Example: Photosynthesis
6CO₂ + 6H₂O → C₆H₁₂O₆ + 6O₂ ΔH = +2803 kJ/mol
Exothermic Reactions
Heat is released. ΔH is negative.
Example: Combustion of methane
CH₄ + 2O₂ → CO₂ + 2H₂O ΔH = -890 kJ/mol
Key Thermochemistry Formulas
| Formula | Use Case | Units |
|---|---|---|
| Q = mcΔT | Calculate heat from temperature change | Joules (J) |
| ΔH = ΣH_products - ΣH_reactants | Calculate reaction enthalpy | kJ/mol |
| ΔH = ΔU + ΔnRT | Enthalpy from internal energy | kJ/mol |
| n = Q/ΔH | Moles of substance from heat | moles |
Hess's Law
Heat total stays the same regardless of the reaction path. This lets you calculate ΔH for reactions you can't measure directly.
Rules:
- Reverse a reaction → change the sign of ΔH
- Multiply a reaction → multiply ΔH by the same factor
- Add reactions together → add their ΔH values
Example:
N₂ + O₂ → 2NO ΔH = +180 kJ
2NO + O₂ → 2NO₂ ΔH = -112 kJ
Combined: N₂ + 2O₂ → 2NO₂ ΔH = +68 kJ
Calorimetry and Heat Capacity
A calorimeter measures heat directly. The heat lost by the system equals the heat gained by the surroundings.
q_system + q_surroundings = 0
For coffee cup calorimeters (constant pressure):
q_reaction = -mcΔT
The negative sign accounts for heat flow direction. If the water heats up, the reaction released heat.
Specific Heat Capacities (common values)
| Substance | c (J/g·°C) |
|---|---|
| Water | 4.18 |
| Ice | 2.09 |
| Steam | 2.01 |
| Aluminum | 0.897 |
| Iron | 0.449 |
Bond Energy Calculations
You can estimate ΔH using bond dissociation energies:
ΔH ≈ Σ(bonds broken) - Σ(bonds formed)
Bonds broken absorbs energy (+). Bonds formed releases energy (-).
How To Solve Heat Chemistry Problems
Step 1: Identify what you're solving for
Is it heat (Q), enthalpy change (ΔH), or temperature change (ΔT)?
Step 2: List your known variables
Write down mass, specific heat, initial/final temperatures.
Step 3: Choose the right formula
Q = mcΔT for calorimetry. ΔH = products - reactants for reactions.
Step 4: Plug in the numbers
Watch your units. Convert grams to kg if needed. Use Kelvin for temperature calculations.
Step 5: Check your sign
Positive = heat absorbed (endothermic). Negative = heat released (exothermic).
Example Problem
Question: 50g of water at 25°C absorbs 4200J of heat. What's the final temperature?
Solution:
ΔT = Q/(mc)
ΔT = 4200 J / (50g × 4.18 J/g·°C)
ΔT = 4200 / 209
ΔT = 20.1°C
T_final = 25 + 20.1 = 45.1°C
Common Mistakes to Avoid
- Confusing mass with moles—check your units
- Forgetting the negative sign in q = -mcΔT
- Using Celsius instead of Kelvin for gas calculations
- Mixing up specific heat of water with other substances
- Skipping the sign convention when reversing reactions
Quick Reference Cheat Sheet
- Exothermic = heat leaves = negative ΔH
- Endothermic = heat enters = positive ΔH
- Calorimeter = closed system heat measurement
- Hess's Law = path independence of ΔH
- Bond energy = breaking costs, forming pays