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S1.1 - Introduction to the particulate nature of matter S1.2 - The nuclear atom S1.3 - Electron configurations S1.4 - Counting particles by mass - The mole S1.5 - Ideal gases S2.1 - The ionic model S2.2 - The covalent model S2.3 - The metallic model S2.4 - From models to materials S3.1 - The periodic table - Classification of elements S3.2 - Functional groups - Classification of organic compounds R1.1 - Measuring enthalpy changes R1.2 - Energy cycles in reactions R1.3 - Energy from fuels R1.4 - Entropy and spontaneity AHL R2.1 - How much? The amount of chemical change R2.2 - How fast? The rate of chemical change R2.3 - How far? The extent of chemical change R3.1 - Proton transfer reactions R3.2 - Electron transfer reactions R3.3 - Electron sharing reactions R3.4 - Electron-pair sharing reactions

R1.1 - Measuring enthalpy changes

1.1.1 Energy Transfer 1.1.2 Endothermic and Exothermic 1.1.3 Energy Profile 1.1.4 Enthalpy Change

Standard Enthalpy Change (ΔH⦵) and Calorimetry

Specification Reference R1.1.4

Quick Notes:

  • ΔH⦵ is the standard enthalpy change: heat transferred under standard conditions (298 K, 100 kPa, 1 mol dm⁻³, substances in their standard states).
  • Units: kJ mol⁻¹
  • Use two key equations:
    • Q = mcΔT
      to find heat energy (Q) transferred
    • ΔH = −Q/n
      to calculate enthalpy change per mole of substance reacted
  • Specific heat capacity of water, c = 4.18 J g⁻¹ K⁻¹ (given in data booklet).

Full Notes:

Note – Enthalpy (H) is the total heat energy of a chemical system at constant pressure. ΔH is the change in enthalpy when a chemical reaction occurs.

What Is ΔH⦵?

The standard enthalpy change of reaction, ΔH⦵, is the heat energy transferred during a reaction under standard conditions, with all substances in their standard states.

Standard conditions:

Calorimetry and the Equation Q = mcΔT

Calorimetry is an experimental technique used to measure enthalpy changes.

The key equation used is:

Q = mcΔT

This gives the total heat change in the experiment.

From Heat to Enthalpy: ΔH = −Q/n

Once you’ve calculated Q, we can find ΔH using:

ΔH = −Q / n

The negative sign indicates whether the reaction is exothermic (−ΔH) or endothermic (+ΔH).

Worked Example

A student mixes 50.0 g of water with a salt, and the temperature rises by 6.0 °C. Calculate ΔH⦵ if 0.020 mol of salt reacted.

  1. Step 1: Calculate Q
    Q = mcΔT = 50.0 × 4.18 × 6.0 = 1254 J = 1.254 kJ
  2. Step 2: Calculate ΔH
    ΔH = −Q / n = −1.254 / 0.020 = −62.7 kJ mol⁻¹

Summary Table

Equation Use Units Notes
Q = mcΔT Find heat energy transferred Q in joules (J) Use c = 4.18 J g⁻¹ K⁻¹ for water
ΔH = −Q / n Find enthalpy change per mole ΔH in kJ mol⁻¹ Convert Q to kJ; use limiting reagent

Tool 1, Inquiry 1, 2, 3 – Linked Course Question

How can the enthalpy change for combustion reactions, such as for alcohols or food, be investigated experimentally?

IB Chemistry calorimetry experiment setup for measuring enthalpy of combustion using a spirit burner and water calorimeter.

The enthalpy of combustion is the energy change when one mole of a substance burns completely in oxygen.

Method:

  • Measure a known volume of water in a calorimeter (beaker or copper can).
  • Record the starting temperature of the water.
  • Weigh the spirit burner containing the fuel.
  • Light the burner and allow it to heat the water.
  • Stir and measure the final temperature of the water.
  • Reweigh the burner to determine mass of fuel burned.
  • Calculate q using Q = mcΔT, then use ΔH = q / n.

Sources of Error:

  • Heat loss to surroundings (e.g., air, beaker).
  • Incomplete combustion (producing CO instead of CO2).
  • Evaporation of fuel from the wick.


Tool 1, Inquiry 3 – Linked Course Question

Why do calorimetry experiments typically measure a smaller temperature change than expected?

Calorimetry often gives lower temperature changes than theoretical values because of heat losses to the surroundings, incomplete combustion, or absorption of heat by the apparatus. These experimental limitations mean not all the energy released is transferred to the water or measured system.

Summary