CHEMISTRY INTERMEDIATE

Thermodynamics

Energy, heat, work, entropy — and the equations that tell you whether a reaction will happen. Thermodynamics is the framework that connects the microscopic world of atoms to measurable quantities like temperature, pressure, and spontaneity.

01 · Foundations

The four laws of thermodynamics

0th Law

Thermal equilibrium

If A is in thermal equilibrium with B, and B with C, then A is in equilibrium with C. This defines temperature as a measurable property.

1st Law

Conservation of energy

Energy cannot be created or destroyed, only converted between forms. ΔU = q + w (internal energy = heat + work).

2nd Law

Entropy increases

The total entropy of an isolated system always increases in a spontaneous process. The universe tends toward maximum disorder.

3rd Law

Absolute zero

The entropy of a perfect crystal at absolute zero (0 K) is zero. Absolute zero cannot be reached in finite steps.

The First Law (ΔU = q + w) is the starting point for all energy calculations. In chemistry, the most common work term is pressure-volume work: w = −pΔV. At constant pressure (typical of laboratory reactions open to atmosphere), heat flow equals the enthalpy change: qp = ΔH.

02 · Enthalpy

Enthalpy: heat at constant pressure

Enthalpy (H) is defined as H = U + pV. For a process at constant pressure, ΔH = ΔU + pΔV. The practical significance: ΔH is the heat that flows into or out of a reaction flask open to the atmosphere.

ΔH = H(products) − H(reactants)

Exothermic: ΔH < 0

Endothermic: ΔH > 0

Standard enthalpy values (ΔH°) are measured at 298 K and 100 kPa. Standard enthalpies of formation (ΔHf°) are tabulated for most compounds and allow calculation of reaction enthalpies via:

ΔH°rxn = Σ ΔHf°(products) − Σ ΔHf°(reactants)

Bond enthalpies provide an alternative route: breaking bonds requires energy (endothermic); forming bonds releases energy (exothermic). The net ΔH ≈ Σ bonds broken − Σ bonds formed. This connects to chemical bonding and explains why combustion (breaking weak C–H and O=O bonds, forming strong C=O and O–H bonds) is always exothermic.

03 · Entropy

Entropy and the Second Law

Entropy (S) measures disorder — more precisely, the number of microscopic arrangements (microstates) consistent with the observed macrostate. Boltzmann's relation: S = kB ln Ω.

Predicting the sign of ΔS:

  • ΔS > 0 — solid dissolves, gas is produced, number of gas moles increases, mixing occurs.
  • ΔS < 0 — gas condenses, precipitate forms, number of gas moles decreases.

The Second Law states that the entropy of the universe (system + surroundings) always increases in a spontaneous process: ΔSuniv > 0. This is why heat flows from hot to cold (never spontaneously the reverse), why gases expand to fill containers, and why concentrated solutions dilute.

In biology, living organisms maintain highly ordered states locally — but they do so by increasing the entropy of their surroundings (releasing heat from respiration). The net ΔSuniv remains positive. See Cellular respiration for how cells couple exothermic ATP hydrolysis to endothermic biosynthesis.

04 · Gibbs free energy

Gibbs free energy: the spontaneity criterion

The Gibbs free energy (G) combines enthalpy and entropy into a single spontaneity criterion for processes at constant temperature and pressure:

ΔG = ΔH − TΔS

ΔH ΔS ΔG Spontaneous?
−+Always −Yes, at all temperatures
+−Always +Never spontaneous
−−Depends on TOnly at low T (ΔH dominates)
++Depends on TOnly at high T (TΔS dominates)

At equilibrium, ΔG = 0, and the relationship to the equilibrium constant K:

ΔG° = −RT ln K

This connects thermodynamics to equilibrium (see the Equilibrium glossary entry and the Reaction rates guide) and to electrochemistry (ΔG° = −nFE°, see the Electrochemistry guide).

05 · Hess's law

Hess's law: calculating unmeasurable enthalpies

Enthalpy is a state function — its value depends only on the current state of the system, not the path taken to get there. This means enthalpy changes are additive: you can combine known reactions to calculate the enthalpy of a reaction that is difficult or impossible to measure directly.

Worked example: Calculate ΔH for C(s) + ½O₂(g) → CO(g) (difficult to measure directly — CO₂ is always produced as a byproduct).

(1) C(s) + O₂(g) → CO₂(g) ΔH₁ = −393.5 kJ/mol

(2) CO(g) + ½O₂(g) → CO₂(g) ΔH₂ = −283.0 kJ/mol

Target = (1) − (2): ΔH = −393.5 − (−283.0) = −110.5 kJ/mol

Hess's law is used in every Born–Haber cycle (lattice enthalpy calculation) and in calculating enthalpies of hydrogenation, combustion, and neutralisation from formation data. See Balancing equations for the stoichiometric manipulation needed.

Thermodynamics — common questions

Temperature measures average kinetic energy per particle. Heat (q) is the flow of energy from higher to lower temperature. The relationship is q = mcΔT for a substance with specific heat capacity c. An important distinction: heat is a process (energy in transit), not a property stored in a substance.

Thermodynamics predicts equilibrium

ΔG° = −RT ln K connects free energy directly to equilibrium position. The Reaction rates guide covers Le Chatelier's principle and how equilibrium shifts with conditions.

Reaction rates →