A hand warmer heats up when you snap it, an instant cold pack turns icy when you squeeze it, and a barbecue runs on the heat from burning propane. Every one of these is a chemical or physical change that moves energy into or out of its surroundings. In Grade 11 you balanced equations and counted moles; now you will attach an energy value to those equations, so you can predict exactly how many kilojoules a given amount of fuel will release, or how cold a cold pack will get. The key quantity is enthalpy change, written .
To track energy, chemists split the universe into two parts. The system is the set of chemicals you are studying — the reactants turning into products. The surroundings are everything else: the water they are dissolved in, the beaker, the air, your hand. Energy is conserved, so any energy the system loses is gained by the surroundings, and vice versa. That is why a thermometer placed in the surroundings can tell you what is happening inside the system.
- An open system can exchange both matter and energy with the surroundings (an open beaker).
- A closed system exchanges energy but not matter (a sealed flask).
- An isolated system exchanges neither — the ideal a calorimeter tries to approach.
Exothermic and Endothermic Changes
Enthalpy () is the total heat content of a system at constant pressure. You can never measure itself, but you can measure how much it changes: In an exothermic change the products have less enthalpy than the reactants, so energy leaves the system, the surroundings warm up, and is negative. In an endothermic change the products have more enthalpy, energy flows in from the surroundings, the surroundings cool down, and is positive.
- Products lower in enthalpy than reactants
- Surroundings get warmer
- Examples: combustion, neutralization, freezing, condensation
- Products higher in enthalpy than reactants
- Surroundings get cooler
- Examples: dissolving ammonium nitrate, photosynthesis, melting, boiling
Thermochemical Equations
A thermochemical equation is a balanced equation, with states of matter, that also reports the energy change. There are two equivalent ways to write it. You can write beside the equation, or you can write the energy as a term inside the equation — on the product side for an exothermic reaction (energy is released, like a product) and on the reactant side for an endothermic reaction (energy is absorbed, like a reactant). The value belongs to the equation exactly as written, in the mole amounts given by the coefficients.
Measuring Heat with a Calorimeter
When heat flows into a substance, its temperature rises by an amount that depends on three things: how much of it there is (mass ), how hard it is to heat (its specific heat capacity , the energy needed to warm 1 g by 1 °C), and the temperature change . So . Water has a large specific heat capacity, c = 4.18\text{ J/{(g}\cdot{}^\circ\text{C)}}, which is why it is the standard liquid in a calorimeter: it absorbs a lot of energy with a modest, easily measured temperature change. A simple coffee-cup calorimeter is two nested polystyrene cups with a lid and a thermometer. Polystyrene is a good insulator, so very little heat escapes, and the reaction happens right inside the water, which acts as the surroundings. You measure the temperature change of the water, calculate for the water, and then use conservation of energy: whatever the water gained, the reaction lost. For dilute aqueous solutions, assume the solution has the density () and specific heat capacity of pure water.
| Type of change | Example | Typical size of energy change |
|---|---|---|
| Physical (phase change) | Melting ice: ; boiling water at 100 °C: | Tens of kJ per mole — only intermolecular forces change |
| Chemical | Burning methane: | Hundreds to thousands of kJ per mole — chemical bonds break and form |
| Nuclear | Fission of uranium-235 | Roughly — millions of times larger, because nuclei change and a little mass becomes energy |