Enthalpy changes are absolutely everywhere in chemistry - from the...
Enthalpy Changes in WJEC A-Level Chemistry Unit 3 Explored

Enthalpy Changes and Energy Calculations
Enthalpy (ΔH) is simply the energy change that happens during chemical reactions. When ΔH is negative, the reaction gives out heat (exothermic) - think of burning wood or hand warmers. When ΔH is positive, the reaction absorbs heat (endothermic) - like the cooling effect in instant ice packs.
You'll use the formula ΔH = -mcΔT/n constantly in calculations. Here, 'm' is the mass of your solution, 'c' is the specific heat capacity, 'ΔT' is temperature change, and 'n' is moles of your limiting reactant. Always remember to use the smallest number of moles!
Standard conditions are crucial for comparing different reactions fairly. These are 1 ATM pressure, 298K (25°C), and 1 mol dm⁻³ for solutions. Think of these as the "referee's rules" that make sure everyone's playing the same game.
Quick Tip: Negative ΔH = heat out (exothermic), Positive ΔH = heat in (endothermic)
Types of Enthalpy Changes You Need to Know
There are loads of different enthalpy changes, but each one has a specific definition. Enthalpy of combustion is when exactly one mole burns completely in oxygen - perfect for comparing fuels. Enthalpy of formation shows the energy when one mole of compound forms from its elements in their natural states.
Hess' Law is your best friend for tricky calculations. It states that the total enthalpy change doesn't depend on the route you take - just like climbing a mountain, the height difference is the same whether you take the direct path or go round the scenic route.
For ionic compounds, you'll encounter lattice formation (always negative - energy released when ions come together) and lattice breaking (always positive - energy needed to separate ions). These are opposites of each other, which makes perfect sense when you think about it.
Exam Tip: Always check if enthalpy changes should be positive or negative - it's an easy way to spot mistakes in your calculations!
Measuring Enthalpy and Factors Affecting Lattice Energy
Calorimetry uses simple equipment - a polystyrene cup, thermometer, and your reaction mixture. The main problem is heat loss, so you'll need a lid with insulating material and take several temperature readings to get accurate starting temperatures.
Lattice energy measures how strongly ions are held together in ionic compounds. Two main factors affect this strength: ionic size and charge on the ion. Smaller ions pack closer together, creating stronger attractions and higher lattice energies.
Charge density (charge divided by ionic radius) is the key concept here. Higher charge density means stronger electrostatic forces between ions. This explains why MgO has a much higher melting point than NaCl - Mg²⁺ and O²⁻ have higher charges than Na⁺ and Cl⁻.
Real-World Connection: This is why salt (NaCl) dissolves easily in water but limestone (CaCO₃) doesn't - the lattice energy differences are huge!
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Enthalpy Changes in WJEC A-Level Chemistry Unit 3 Explored
Enthalpy changes are absolutely everywhere in chemistry - from the warmth you feel when hand warmers activate to the energy released when petrol burns in car engines. Understanding these energy transfers will help you predict whether reactions will happen and...

Enthalpy Changes and Energy Calculations
Enthalpy (ΔH) is simply the energy change that happens during chemical reactions. When ΔH is negative, the reaction gives out heat (exothermic) - think of burning wood or hand warmers. When ΔH is positive, the reaction absorbs heat (endothermic) - like the cooling effect in instant ice packs.
You'll use the formula ΔH = -mcΔT/n constantly in calculations. Here, 'm' is the mass of your solution, 'c' is the specific heat capacity, 'ΔT' is temperature change, and 'n' is moles of your limiting reactant. Always remember to use the smallest number of moles!
Standard conditions are crucial for comparing different reactions fairly. These are 1 ATM pressure, 298K (25°C), and 1 mol dm⁻³ for solutions. Think of these as the "referee's rules" that make sure everyone's playing the same game.
Quick Tip: Negative ΔH = heat out (exothermic), Positive ΔH = heat in (endothermic)
Types of Enthalpy Changes You Need to Know
There are loads of different enthalpy changes, but each one has a specific definition. Enthalpy of combustion is when exactly one mole burns completely in oxygen - perfect for comparing fuels. Enthalpy of formation shows the energy when one mole of compound forms from its elements in their natural states.
Hess' Law is your best friend for tricky calculations. It states that the total enthalpy change doesn't depend on the route you take - just like climbing a mountain, the height difference is the same whether you take the direct path or go round the scenic route.
For ionic compounds, you'll encounter lattice formation (always negative - energy released when ions come together) and lattice breaking (always positive - energy needed to separate ions). These are opposites of each other, which makes perfect sense when you think about it.
Exam Tip: Always check if enthalpy changes should be positive or negative - it's an easy way to spot mistakes in your calculations!
Measuring Enthalpy and Factors Affecting Lattice Energy
Calorimetry uses simple equipment - a polystyrene cup, thermometer, and your reaction mixture. The main problem is heat loss, so you'll need a lid with insulating material and take several temperature readings to get accurate starting temperatures.
Lattice energy measures how strongly ions are held together in ionic compounds. Two main factors affect this strength: ionic size and charge on the ion. Smaller ions pack closer together, creating stronger attractions and higher lattice energies.
Charge density (charge divided by ionic radius) is the key concept here. Higher charge density means stronger electrostatic forces between ions. This explains why MgO has a much higher melting point than NaCl - Mg²⁺ and O²⁻ have higher charges than Na⁺ and Cl⁻.
Real-World Connection: This is why salt (NaCl) dissolves easily in water but limestone (CaCO₃) doesn't - the lattice energy differences are huge!
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