Table of Contents
ToggleEnthalpy (H) is a key concept in thermochemistry that describes the total internal energy of a system, including the energy needed to change its temperature and pressure. In simple terms, enthalpy refers to the heat content of a system. When discussing chemical reactions, we focus on the change in enthalpy (ΔH), which is the difference between the enthalpy of the products and the reactants.
The enthalpy of reaction (ΔH) describes the energy change during a chemical reaction:
Key Examples:
Combustion of Propane (Exothermic):
Dissolution of Anhydrous CuSO₄ (Endothermic):
The sign of ΔH provides critical insight into the reaction’s heat flow direction:
Tip: While the temperature change in the surroundings can provide clues about a reaction’s enthalpy change, the total energy exchange depends on the system’s internal energy changes, not just temperature shifts.
Example Reactions:
While a negative ΔH (exothermic reaction) often suggests a thermodynamically favorable reaction, it’s not the sole determining factor. The Gibbs free energy change (ΔG) and the equilibrium constant (Kc) also play crucial roles.
ΔG = ΔH – TΔS, where:
1. Combustion of Methane (Exothermic)
Equation:
Description: ΔH is negative, indicating heat release.
2. Dissolution of Ammonium Nitrate (Endothermic)
Equation:
Description: ΔH is positive, indicating heat absorption.
Enthalpy of reaction (ΔH) is a crucial measure in thermodynamics, indicating whether a reaction absorbs or releases heat. It helps predict reaction feasibility, understand energy transfers, and quantify heat changes. Mastering these concepts provides a strong foundation for tackling energy calculations and real-world applications in thermochemistry.