Enthalpy change (ΔH) is the term scientists use to describe the heat energy exchange during a chemical reaction under constant pressure. It is a central concept in thermodynamics and an integral part of understanding energy flow within chemical systems. The enthalpy change can be endothermic (absorbing heat) or exothermic (releasing heat).
For the slaked lime decomposition described above, the reaction is endothermic since it requires the absorption of heat. The enthalpy change is positive, marked by a ΔH value of +109 kJ/mol. This signifies that energy is absorbed from the surroundings to break the bonds in calcium hydroxide while forming new bonds in calcium oxide and water vapor.
Understanding the enthalpy change gives insights into:
- The energy required to initiate a reaction, or the heat produced as a reaction by-product.
- Predicting whether a reaction will be spontaneous or needs external energy to proceed.
- Designing energy-efficient industrial processes and calculating the heat exchange in chemical reactions for various applications like heating and cooling systems.
Note that the enthalpy change correlates directly to the stoichiometry of the reaction. That’s why it’s crucial to associate the enthalpy change to the correct amount of reactants, just as the stoichiometric coefficients in the thermochemical equation illustrate.