SECTION 1
Historical Context & Motivation
Humans have always been fascinated by heat—fire was arguably the first chemical reaction our ancestors deliberately controlled. Yet for thousands of years, no one could precisely measure the energy released when wood burns or when acids dissolve metals. The idea that chemical reactions involve measurable energy changes only took shape once scientists developed careful experimental methods and a clear concept of heat as a form of energy. The story of how we learned to measure enthalpy change is a story of better tools, better theories, and the determination to quantify the invisible.
1780 • Lavoisier & Laplace — The Ice Calorimeter
1840 • Hess's Law of Constant Heat Summation
1865 • Clausius Formalizes Enthalpy
1923 • Standard Enthalpy Definitions
The central question that drove all of this work remains relevant today: How much energy does a chemical reaction release or absorb, and how can we measure it accurately? In the IB Chemistry course, answering this question is your entry point into the broader topic of what drives chemical reactions. In this lesson, you will learn the experimental technique of calorimetry and the mathematics behind calculating enthalpy changes.
SECTION 2
Core Principles & Definitions
Before you can measure enthalpy change, you need to understand a handful of foundational ideas. These definitions form the vocabulary you will use throughout the IB Reactivity topic, so it is worth taking time to internalize each one.
Enthalpy (H)
Exothermic vs. Endothermic
System & Surroundings
Specific Heat Capacity (c)
Calorimetry
KEY TAKEAWAY
SECTION 3
Visual Explanation — The Coffee-Cup Calorimeter
The most common calorimeter you will encounter in IB Chemistry is the coffee-cup calorimeter. It is inexpensive, simple to set up, and effective enough for many solution-based reactions. The diagram below shows its key components and how heat flows during an exothermic reaction.
Notice that the polystyrene cup acts as an insulator, minimizing heat loss to the room. In a perfect experiment, every joule of energy released by the reaction would be absorbed by the water. In practice, some heat always escapes, which is one reason why experimental ΔH values are typically less accurate than literature values. The key assumption in calorimetry is that the heat gained (or lost) by the water equals the heat lost (or gained) by the reaction.
SECTION 4
Mathematical Framework
Two equations form the backbone of every calorimetry calculation in IB Chemistry. The first lets you calculate the heat absorbed or released by the water, and the second converts that heat value into a molar enthalpy change for the reaction.
HEAT TRANSFER EQUATION
q = heat energy transferred (J) · m = mass of the water (g) · c = specific heat capacity of water (4.18 J g⁻¹ °C⁻¹) · ΔT = change in temperature (°C), calculated as Tfinal − Tinitial
MOLAR ENTHALPY CHANGE
ΔH = enthalpy change per mole of limiting reagent (kJ mol⁻¹) · q = heat absorbed by the water (J) · n = moles of the limiting reagent. The negative sign accounts for the fact that if the water gains heat, the reaction lost it (and vice versa).
Why the negative sign?
CONVERTING UNITS
Remember to convert joules to kilojoules by dividing by 1000. IB enthalpy values are always reported in kJ mol⁻¹.
SECTION 5
Enthalpy Profile Diagrams
An enthalpy profile diagram (sometimes called an enthalpy level diagram) is a visual way to represent the energy changes during a reaction. The y-axis shows enthalpy and the x-axis shows the progress of the reaction. The diagram below compares exothermic and endothermic reactions side by side, which is a common way IB exam questions present this concept.
These diagrams are crucial for IB exams because they visually connect what you observe in the lab (temperature going up or down) with the underlying energy changes. In an exothermic reaction, the products have less enthalpy than the reactants—the difference is released as heat to the surroundings, so the thermometer reading rises. In an endothermic reaction, the products have more enthalpy—the difference is taken from the surroundings, so the thermometer reading falls. The vertical yellow arrow on each diagram represents the magnitude of ΔH.
IB Exam Tip
SECTION 6
Worked Example — Neutralization Reaction
Let us walk through a complete calorimetry calculation, the kind you would see on an IB exam or perform in a lab. We will determine the molar enthalpy change for the neutralization of hydrochloric acid with sodium hydroxide.
Problem Statement
Calculating ΔH for Neutralization
- 1
Step 1 — Identify Given Values
Volume of HCl = 50.0 cm³, Volume of NaOH = 50.0 cm³, so total volume = 100.0 cm³. Since the density is 1.00 g cm⁻³, the total mass of solution is m = 100.0 g. The specific heat capacity c = 4.18 J g⁻¹ °C⁻¹. The temperature change ΔT = 28.8 − 22.0 = 6.8 °C.m = 100.0 g, c = 4.18 J g⁻¹ °C⁻¹, ΔT = 6.8 °C - 2
Step 2 — Calculate Heat Absorbed by Water (q)
Substitute into q = m × c × ΔT: q = 100.0 × 4.18 × 6.8 = 2842.4 J. Since the temperature increased, the water gained this heat, meaning the reaction is exothermic.q = 2842.4 J - 3
Step 3 — Calculate Moles of Limiting Reagent (n)
The reaction is HCl + NaOH → NaCl + H₂O with a 1:1 molar ratio. Moles of HCl = concentration × volume = 1.00 × (50.0 ÷ 1000) = 0.0500 mol. The same applies to NaOH, so neither is in excess.n = 0.0500 mol - 4
Step 4 — Calculate ΔH
Apply ΔH = −q ÷ n. First, convert q to kJ: 2842.4 J ÷ 1000 = 2.8424 kJ. Then ΔH = −2.8424 ÷ 0.0500 = −56.8 kJ mol⁻¹. The negative sign confirms the reaction is exothermic, as expected for a neutralization.ΔH = −56.8 kJ mol⁻¹ - 5
Step 5 — Evaluate the Result
The literature value for the enthalpy of neutralization of a strong acid with a strong base is approximately −57.1 kJ mol⁻¹. Our experimental value of −56.8 kJ mol⁻¹ is very close, with a percentage error of only about 0.5%. The small difference is due to heat loss to the surroundings.Percentage error ≈ 0.5% — excellent agreement
SECTION 7
Strengths & Limitations of Calorimetry
The coffee-cup calorimeter is a useful tool, but like any experimental method it has both strengths and weaknesses. Understanding these helps you evaluate your lab results and explains why your calculated ΔH values may differ from textbook values.
| Aspect | Strengths | Limitations |
|---|---|---|
| Equipment | Simple, inexpensive, and available in most school labs. Easy to set up and repeat. | Polystyrene is not a perfect insulator; heat escapes to the environment, producing systematic error. |
| Accuracy | Provides a reasonable estimate of ΔH for solution reactions. Repeated trials can improve reliability. | Typically gives values lower than literature values (for exothermic reactions) because not all heat is captured. |
| Assumptions | The assumption that the solution behaves like water simplifies calculations significantly. | Dilute solutions only; concentrated solutions have different densities and specific heat capacities. |
| Scope | Works well for neutralizations, dissolutions, and displacement reactions in aqueous solution. | Cannot measure enthalpy changes for combustion reactions or gas-phase reactions (bomb calorimeter needed). |
Comparison of strengths and limitations of the coffee-cup calorimeter
KEY TAKEAWAY
SECTION 8
Connection to Advanced Concepts
The calorimetry techniques you have learned in this lesson are the experimental foundation for more advanced topics in IB Chemistry. Understanding where simple calorimetry fits in the broader thermodynamics landscape helps you see how the IB syllabus connects.
| This Lesson (Reactivity 1.1) | Advanced Topics (Later in IB) |
|---|---|
| Measure ΔH experimentally using a coffee-cup calorimeter. | Use Hess's Law to calculate ΔH for reactions that cannot be measured directly. |
| Report ΔH in kJ mol⁻¹ for a specific reaction. | Use standard enthalpies of formation (ΔH°f) to calculate ΔH for any reaction. |
| Classify reactions as exothermic or endothermic. | Analyze bond enthalpies to explain why a reaction is exothermic or endothermic at the molecular level. |
| Assume constant pressure (open cup). | Distinguish between enthalpy (constant pressure) and internal energy (constant volume, bomb calorimeter). |
| Focus on enthalpy (ΔH) alone to judge reaction feasibility. | Combine ΔH with entropy (ΔS) to calculate Gibbs free energy (ΔG) and predict spontaneity. |
How this lesson connects to future IB Chemistry topics
As you progress through the IB course, you will discover that enthalpy is only one piece of the puzzle for predicting whether a reaction will occur. The concept of entropy (the degree of disorder in a system) and Gibbs free energy will give you a complete picture. For now, mastering calorimetry and understanding enthalpy changes gives you the essential first step in answering the question: what drives chemical reactions?
SECTION 9
Practice Problems
Question 1: CONCEPTUAL
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Question 2: BASIC CALCULATION
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Question 3: INTERMEDIATE
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Question 4: APPLIED
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Question 5: CRITICAL THINKING
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SUMMARY
Lesson Summary
Summary
Enthalpy change (ΔH) is the heat energy transferred during a chemical reaction at constant pressure, measured in kJ mol⁻¹. Reactions that release heat are exothermic (ΔH < 0), causing the surroundings to warm up, while reactions that absorb heat are endothermic (ΔH > 0), causing the surroundings to cool down. We measure ΔH experimentally using calorimetry, typically with a coffee-cup calorimeter that records the temperature change of an aqueous solution.
The two key equations are q = m × c × ΔT (to find the heat absorbed by water) and ΔH = −q ÷ n (to find the molar enthalpy change). The negative sign accounts for the direction of heat flow between the system and surroundings. Experimental values often differ from literature values due to heat loss, incomplete reactions, or assumptions about the solution's properties. These skills form the foundation for Hess's Law, bond enthalpy calculations, and Gibbs free energy analysis later in the IB course.