Phase: the dividing idea
A phase is a region of matter that is uniform in both chemical composition and physical state. A mixture of gases is a single phase, however many gases it contains, because the molecules are intermingled at the molecular level. A clear aqueous solution is likewise one phase. A lump of solid sitting in a gas, by contrast, presents two phases with a sharp boundary between them. The number of phases present at equilibrium is the single fact that sorts every equilibrium system into one of two classes.
When all reactants and products occupy the same phase, the equilibrium is homogeneous. When the system contains more than one phase, the equilibrium is heterogeneous. This is not a cosmetic label: it changes which species are permitted to appear in the equilibrium-constant expression, and therefore changes the numerical value and even the units of $K$.
A single-phase gas mixture (left) versus a two-phase system with a solid floor and a gas above it (right). In the heterogeneous case only the gas-phase species enter the equilibrium constant.
Homogeneous equilibria
In a homogeneous system every reactant and product is in the same phase, so every concentration term is genuinely variable and every species appears in $K$. NCERT gives the all-gas synthesis of ammonia as the canonical example:
$$\ce{N2(g) + 3H2(g) <=> 2NH3(g)}$$
All three species are gases, so all three enter the constant. In terms of molar concentrations and partial pressures respectively,
$$K_c = \dfrac{[\ce{NH3}]^2}{[\ce{N2}][\ce{H2}]^3}, \qquad K_p = \dfrac{p_{\ce{NH3}}^2}{p_{\ce{N2}}\,p_{\ce{H2}}^3}$$
Homogeneous equilibria need not be gaseous. NCERT also cites reactions that are entirely in aqueous solution, such as the esterification equilibrium and the formation of the blood-red thiocyanate complex, where every species is dissolved in the same solution phase:
$$\ce{CH3COOC2H5(aq) + H2O(l) <=> CH3COOH(aq) + C2H5OH(aq)}$$ $$\ce{Fe^3+(aq) + SCN^-(aq) <=> [Fe(SCN)]^2+(aq)}$$
The first of these is worth a closer look, because it contains liquid water. When water is the bulk solvent of a dilute solution it behaves as a near-pure liquid and is treated as a constant, so in practice the working $K_c$ for hydrolysis or esterification omits the water term. The principle that does this omission is exactly the one that governs heterogeneous systems, taken up below.
Heterogeneous equilibria
Equilibrium in a system having more than one phase is called heterogeneous equilibrium. NCERT §6.5 opens with the simplest possible case — the equilibrium between liquid water and its own vapour in a closed container:
$$\ce{H2O(l) <=> H2O(g)}$$
Here a liquid phase and a gas phase coexist. A second standard example is a sparingly soluble solid in contact with its saturated solution, which spans a solid and an aqueous phase:
$$\ce{Ca(OH)2(s) <=> Ca^2+(aq) + 2OH^-(aq)}$$
Heterogeneous equilibria very often involve a pure solid or a pure liquid, and that is precisely what allows their equilibrium expressions to be simplified. The reasoning is given its own section because it is the most heavily tested idea in this subtopic.
Why pure solids and liquids drop out
The molar concentration of a pure solid or a pure liquid is fixed — it equals density divided by molar mass, both of which are constants for a given substance at a given temperature. Crucially, this value is independent of the amount present: a gram of calcium carbonate and a kilogram of it have the same molar concentration. NCERT states the rule directly — if a substance "X" is involved, then $[\ce{X(s)}]$ and $[\ce{X(l)}]$ are constant whatever amount of X is taken, whereas $[\ce{X(g)}]$ and $[\ce{X(aq)}]$ vary as the amount in a given volume varies.
Because the concentration of a pure condensed phase is a constant, it is absorbed into the equilibrium constant rather than written as a variable. In the modern language of activities, the activity of any pure solid or pure liquid is taken as exactly 1, so it contributes a factor of 1 and disappears from both $K_c$ and $K_p$.
Thermal dissociation of calcium carbonate in a closed vessel. The two solids form a bed at the base; only the carbon dioxide above it is a variable phase, so the equilibrium constant reduces to the pressure of CO₂.
Apply this to NCERT's headline example, the thermal dissociation of calcium carbonate:
$$\ce{CaCO3(s) <=> CaO(s) + CO2(g)}$$
Writing the full expression and then striking out the two constant solid terms gives a strikingly compact result:
$$K_c = \dfrac{[\ce{CaO(s)}]\,[\ce{CO2(g)}]}{[\ce{CaCO3(s)}]} \;\longrightarrow\; K_c' = [\ce{CO2}], \qquad K_p = p_{\ce{CO2}}$$
Solids are omitted from K, but must still be physically present
Students correctly drop $\ce{CaCO3(s)}$ and $\ce{CaO(s)}$ from the expression, then wrongly conclude the solids are irrelevant. NCERT is explicit: for a heterogeneous equilibrium to exist, the pure solid or liquid must be present at equilibrium, however small the amount. If all the $\ce{CaCO3}$ has decomposed, there is no equilibrium left to speak of — the system has simply run to completion.
Rule: omit pure solids/liquids from the value of $K$, but never from the existence condition. No solid present ⇒ no heterogeneous equilibrium.
The same logic strips constant terms from other multi-phase systems. In the purification of nickel via its volatile carbonyl, the nickel metal is a pure solid and is omitted:
$$\ce{Ni(s) + 4CO(g) <=> Ni(CO)4(g)}, \qquad K_c = \dfrac{[\ce{Ni(CO)4}]}{[\ce{CO}]^4}$$
And in a reaction that mixes solid, aqueous and liquid species, only the aqueous terms survive — the solid oxide and the liquid water both drop out:
$$\ce{Ag2O(s) + 2HNO3(aq) <=> 2AgNO3(aq) + H2O(l)}, \qquad K_c = \dfrac{[\ce{AgNO3}]^2}{[\ce{HNO3}]^2}$$
The mechanics of building $K_c$ and converting to $K_p$ are covered in Equilibrium Constant — Kc and Kp.
Worked example: CaCO₃ decomposition
For $\ce{CaCO3(s) <=> CaO(s) + CO2(g)}$, the pressure of $\ce{CO2}$ in equilibrium with the two solids is found to be $2.0 \times 10^5$ Pa at 1100 K. Compute $K_p$ using the standard state of 1 bar ($= 10^5$ Pa).
Both solids are omitted, so $K_p = p_{\ce{CO2}}$ expressed relative to the standard state.
$$K_p = \dfrac{p_{\ce{CO2}}}{p^\circ} = \dfrac{2.0 \times 10^5\ \text{Pa}}{10^5\ \text{Pa}} = 2.00$$
The result is a pure number once referenced to the standard state. Note the physical meaning: at 1100 K the equilibrium $\ce{CO2}$ pressure over the solids is fixed at $2.0 \times 10^5$ Pa no matter how much $\ce{CaCO3}$ or $\ce{CaO}$ is present — the defining signature of a heterogeneous equilibrium with pure solids.
Homogeneous vs heterogeneous: K expressions
The table below collects the standard NCERT examples and shows, for each, the full expression before omission and the simplified expression after pure condensed phases are removed. Comparing the two columns is the fastest way to internalise the rule.
| Type | Equilibrium | K expression (after omitting pure solids/liquids) |
|---|---|---|
| Homogeneous (gas) | $\ce{N2(g) + 3H2(g) <=> 2NH3(g)}$ | $K_c = \dfrac{[\ce{NH3}]^2}{[\ce{N2}][\ce{H2}]^3}$ — all species retained |
| Homogeneous (aqueous) | $\ce{Fe^3+(aq) + SCN^-(aq) <=> [Fe(SCN)]^2+(aq)}$ | $K_c = \dfrac{[\ce{[Fe(SCN)]^2+}]}{[\ce{Fe^3+}][\ce{SCN^-}]}$ — all species retained |
| Heterogeneous (solid + gas) | $\ce{CaCO3(s) <=> CaO(s) + CO2(g)}$ | $K_c = [\ce{CO2}]$, $\;K_p = p_{\ce{CO2}}$ — both solids omitted |
| Heterogeneous (solid + gas) | $\ce{Ni(s) + 4CO(g) <=> Ni(CO)4(g)}$ | $K_c = \dfrac{[\ce{Ni(CO)4}]}{[\ce{CO}]^4}$ — Ni(s) omitted |
| Heterogeneous (liquid + gas) | $\ce{H2O(l) <=> H2O(g)}$ | $K_p = p_{\ce{H2O}}$ — liquid water omitted |
| Heterogeneous (solid + aq + liq) | $\ce{Ag2O(s) + 2HNO3(aq) <=> 2AgNO3(aq) + H2O(l)}$ | $K_c = \dfrac{[\ce{AgNO3}]^2}{[\ce{HNO3}]^2}$ — Ag₂O(s) and H₂O(l) omitted |
| Heterogeneous (solid + gas) | $\ce{CO2(g) + C(s) <=> 2CO(g)}$ | $K_p = \dfrac{p_{\ce{CO}}^2}{p_{\ce{CO2}}}$ — graphite omitted |
Δn and Kp = Kc(RT)^Δn
The general bridge between the two constants, derived in NCERT §6.4.1 from the ideal-gas relation $p = [\text{gas}]RT$, is
$$K_p = K_c\,(RT)^{\Delta n}, \qquad \Delta n = \big(\text{moles of gaseous products}\big) - \big(\text{moles of gaseous reactants}\big)$$
The phrase "gaseous" is doing real work here. Because solids and liquids never enter either $K_p$ or $K_c$, they also play no part in $\Delta n$. For $\ce{CaCO3(s) <=> CaO(s) + CO2(g)}$ the only gas is the single mole of $\ce{CO2}$ on the product side, so $\Delta n = 1$ and $K_p = K_c(RT)$. For $\ce{H2(g) + I2(g) <=> 2HI(g)}$ the gas moles balance ($2 - 2 = 0$), so $\Delta n = 0$ and $K_p = K_c$, both dimensionless. This is why the NEET 2024 item below singles out $\ce{PCl5 <=> PCl3 + Cl2}$, the one reaction in its list with a nonzero $\Delta n$.
Counting non-gaseous species in Δn
A frequent slip is to include solid or aqueous species when computing $\Delta n$ for the $K_p = K_c(RT)^{\Delta n}$ conversion. Only gas-phase moles count. Including a solid product such as $\ce{CaO(s)}$ in the tally inflates $\Delta n$ and corrupts every downstream value.
Rule: $\Delta n = \Delta n_{\text{gas}}$ only. Solids, liquids and aqueous solutes are invisible to $\Delta n$ just as they are invisible to $K$.
Homogeneous & Heterogeneous Equilibria
- Homogeneous = all species one phase (all-gas $\ce{N2 + 3H2 <=> 2NH3}$, or all-aqueous); every species appears in $K$.
- Heterogeneous = more than one phase (e.g. $\ce{CaCO3(s) <=> CaO(s) + CO2(g)}$, $\ce{H2O(l) <=> H2O(g)}$).
- The concentration of a pure solid or pure liquid is constant (activity = 1), so it is omitted from $K_c$ and $K_p$.
- $\ce{CaCO3}$ decomposition reduces to $K_p = p_{\ce{CO2}}$; at 1100 K, $K_p = 2.00$.
- Omitted species must still be physically present for the equilibrium to exist.
- In $K_p = K_c(RT)^{\Delta n}$, only gaseous moles count toward $\Delta n$.