The Concept of Enthalpy (H)
In a chemistry lab, we often conduct reactions in open containers (like beakers) where the pressure is constant (atmospheric pressure). Under these constant pressure conditions, the heat transferred (q) is given a special name: Enthalpy change (ΔH) .
What is Enthalpy?
Enthalpy (H) is often described as the “total heat content” of a system. It’s a measure of the energy stored within a substance, primarily as chemical potential energy in the bonds between atoms.
However, we can never know the absolute enthalpy (H) of a system. It’s impossible to measure the total energy from scratch.
Why we measure changes (ΔH, not H):
Because we can’t measure absolute enthalpy, we always measure the change in enthalpy during a reaction. This change is represented by the symbol ΔH (Delta H).
ΔH tells us how much heat was absorbed or released by the chemical reaction at constant pressure.
The equation for calculating the enthalpy change of a reaction is::
ΔH = H(products) – H(reactants)
Let’s break down what this equation tells us about the reaction:
If ΔH is NEGATIVE (ΔH < 0):
This means
- H(products) < H(reactants).
- The products have less enthalpy (less heat content) than the reactants.
- The system has lost energy to the surroundings.
The excess energy is released, usually as heat.
This type of reaction is called exothermic (e.g., combustion, freezing).
If ΔH is POSITIVE (ΔH > 0):
This means
- H(products) > H(reactants).
- The products have more enthalpy (more heat content) than the reactants.
- The system has gained energy from the surroundings.
- The system absorbs heat from the surroundings.
This type of reaction is called endothermic (e.g., photosynthesis, melting ice).
This simple equation, ΔH = H(products) – H(reactants), is the cornerstone of thermochemistry and will be the foundation for the rest of our study.