The math formula for enthalpy is H = U + PV. The letter U stands for internal energy, P is pressure, and V is volume. Most chemistry experiments take place in open beakers or flasks on a lab bench.
Because they are open to the room, the atmospheric pressure stays perfectly constant. Under these open conditions, the change in enthalpy (ΔH) exactly equals the heat absorbed or released. You can easily measure this heat flow using a simple device called a calorimeter.
If a reaction releases heat into the room, it has a negative ΔH value. We call this an exothermic reaction, and it will feel hot to the touch. If a chemical reaction absorbs heat, it has a positive ΔH value.
We call this an endothermic reaction, and it makes the surroundings feel cold. Enthalpy is also known as a thermodynamic state function. This means the total heat change depends only on your starting and ending points.
It does not matter how many chemical steps the reaction takes to get there. This helpful rule is famously known in chemistry as Hess’s law.
