Chemistry · Equilibrium

Homogeneous & Heterogeneous Equilibria

Equilibrium constants are written differently depending on whether every species shares one phase or whether the system spans several. Following NCERT Class 11 §6.4 and §6.5, this note separates single-phase (homogeneous) systems from multi-phase (heterogeneous) systems, and establishes the rule that pure solids and pure liquids are omitted from $K_c$ and $K_p$ because their activity is taken as 1. The one-mark NEET item that asks you to write a correct $K$ expression for a system like $\ce{CaCO3}$ decomposition turns entirely on this distinction.

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 $K$.

Figure 1 Homogeneous (1 phase) all gases intermingled — all appear in K Heterogeneous (2 phases) solid phase gas → in K · solid → omitted

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 $K_p$.

Figure 2 CaCO₃(s) + CaO(s) CO₂(g) K_p = p(CO₂) closed vessel · fixed T · solids omitted from K

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:

$$K_c = \dfrac{[\ce{CaO(s)}]\,[\ce{CO2(g)}]}{[\ce{CaCO3(s)}]} \;\longrightarrow\; K_c' = [\ce{CO2}], \qquad K_p = p_{\ce{CO2}}$$

NEET Trap

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:

$$\ce{Ag2O(s) + 2HNO3(aq) <=> 2AgNO3(aq) + H2O(l)}, \qquad K_c = \dfrac{[\ce{AgNO3}]^2}{[\ce{HNO3}]^2}$$

Go deeper

The mechanics of building $K_c$ and converting to $K_p$ are covered in Equilibrium Constant — Kc and Kp.

Worked example: CaCO₃ decomposition

Worked Example

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.

TypeEquilibriumK 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 $\Delta n$.

NEET Trap

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 $K$.

Quick Recap

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 $\Delta n$.

NEET PYQ Snapshot — Homogeneous & Heterogeneous Equilibria

Real NEET items where the phase of each species — and the omission of pure solids — decides the answer.

NEET 2024

In which of the following equilibria are $K_p$ and $K_c$ NOT equal?

  1. $\ce{PCl5(g) <=> PCl3(g) + Cl2(g)}$
  2. $\ce{H2(g) + I2(g) <=> 2HI(g)}$
  3. $\ce{CO(g) + H2O(g) <=> CO2(g) + H2(g)}$
  4. $\ce{2BrCl(g) <=> Br2(g) + Cl2(g)}$
Answer: (1)

$K_p = K_c(RT)^{\Delta n}$, so the constants differ only when $\Delta n \ne 0$. Options 2, 3 and 4 each have equal gas moles on both sides ($\Delta n = 0$). Only $\ce{PCl5 <=> PCl3 + Cl2}$ has $\Delta n = 2 - 1 = 1$, so there $K_p \ne K_c$.

NEET 2017

A 20 L container at 400 K holds $\ce{CO2(g)}$ at 0.4 atm with excess $\ce{SrO}$ (solid volume negligible). The piston is moved in. For $\ce{SrCO3(s) <=> SrO(s) + CO2(g)}$, $K_p = 1.6$ atm. The maximum container volume when the $\ce{CO2}$ pressure reaches its maximum value is:

  1. 2 L
  2. 5 L
  3. 10 L
  4. 4 L
Answer: (2)

Both solids are omitted, so $K_p = p_{\ce{CO2}}$. The maximum $\ce{CO2}$ pressure is fixed at $K_p = 1.6$ atm (any further compression just deposits $\ce{SrCO3}$). At constant $T$, $p_1V_1 = p_2V_2 \Rightarrow 0.4 \times 20 = 1.6 \times V_2 \Rightarrow V_2 = 5$ L.

Concept

For $\ce{CO2(g) + C(s) <=> 2CO(g)}$, $K_p = 3.0$ at 1000 K with initial $p_{\ce{CO2}} = 0.48$ bar and $p_{\ce{CO}} = 0$, pure graphite present. The equilibrium partial pressures are closest to:

  1. $p_{\ce{CO}} = 0.66$ bar, $p_{\ce{CO2}} = 0.15$ bar
  2. $p_{\ce{CO}} = 0.48$ bar, $p_{\ce{CO2}} = 0.33$ bar
  3. $p_{\ce{CO}} = 0.15$ bar, $p_{\ce{CO2}} = 0.66$ bar
  4. $p_{\ce{CO}} = 0.33$ bar, $p_{\ce{CO2}} = 0.48$ bar
Answer: (1)

Graphite is a pure solid and is omitted, so $K_p = p_{\ce{CO}}^2/p_{\ce{CO2}}$. With a decrease $x$ in $p_{\ce{CO2}}$: $(2x)^2/(0.48 - x) = 3 \Rightarrow 4x^2 + 3x - 1.44 = 0 \Rightarrow x = 0.33$. Hence $p_{\ce{CO}} = 2x = 0.66$ bar and $p_{\ce{CO2}} = 0.48 - 0.33 = 0.15$ bar.

Concept

Which equilibrium-constant expression is correct for $\ce{Ag2O(s) + 2HNO3(aq) <=> 2AgNO3(aq) + H2O(l)}$?

  1. $K_c = \dfrac{[\ce{AgNO3}]^2[\ce{H2O}]}{[\ce{Ag2O}][\ce{HNO3}]^2}$
  2. $K_c = \dfrac{[\ce{AgNO3}]^2}{[\ce{HNO3}]^2}$
  3. $K_c = \dfrac{[\ce{AgNO3}]^2[\ce{H2O}]}{[\ce{HNO3}]^2}$
  4. $K_c = \dfrac{[\ce{AgNO3}]^2}{[\ce{Ag2O}][\ce{HNO3}]^2}$
Answer: (2)

$\ce{Ag2O}$ is a pure solid and $\ce{H2O}$ here is a pure liquid; both have activity 1 and are omitted. Only the aqueous species remain, giving $K_c = [\ce{AgNO3}]^2/[\ce{HNO3}]^2$.

FAQs — Homogeneous & Heterogeneous Equilibria

The most common doubts students raise on phases and the omission rule.

What is the difference between homogeneous and heterogeneous equilibrium?

In a homogeneous equilibrium all reactants and products are present in the same phase, for example the all-gas system N2(g) + 3H2(g) ⇌ 2NH3(g) or an all-aqueous solution. In a heterogeneous equilibrium the system contains more than one phase, such as the decomposition CaCO3(s) ⇌ CaO(s) + CO2(g), which involves both solid and gas phases.

Why are pure solids and pure liquids omitted from the equilibrium constant expression?

The molar concentration of a pure solid or a pure liquid is constant and independent of the amount present, because density and molar mass are fixed. Since this term is a constant, it is merged into the equilibrium constant rather than written separately. In modern terms the activity of a pure solid or pure liquid is taken as 1, so it does not appear in the Kc or Kp expression.

Write the Kp expression for CaCO3(s) ⇌ CaO(s) + CO2(g).

Both CaCO3 and CaO are pure solids, so they are omitted. Only the gaseous CO2 remains, giving Kp = pCO2 and Kc = [CO2]. This means that at a fixed temperature the equilibrium pressure of CO2 over the solids is constant, regardless of how much solid is present. At 1100 K the measured pressure gives Kp = 2.00.

Must pure solids and liquids still be present even though they are omitted from K?

Yes. For a heterogeneous equilibrium to exist, the pure solid or liquid must be physically present at equilibrium, however small the amount. Its concentration or partial pressure does not appear in the equilibrium constant, but if the solid or liquid is entirely consumed the system is no longer at equilibrium and K loses meaning.

Does omitting solids change the relation Kp = Kc(RT)^Δn?

No. The relation Kp = Kc(RT)^Δn still holds, but Δn must be calculated using only the gaseous species, because solids and liquids never enter either Kp or Kc. For CaCO3(s) ⇌ CaO(s) + CO2(g) there is one mole of gas on the right and none on the left, so Δn = 1.

Why is liquid water omitted from Kc in aqueous reactions but counted in gaseous systems?

When water is the bulk solvent and remains a pure liquid, its concentration is essentially constant and it is omitted from Kc, as in Ag2O(s) + 2HNO3(aq) ⇌ 2AgNO3(aq) + H2O(l). However, when water appears as a gaseous species, such as in H2O(l) ⇌ H2O(g), the vapour H2O(g) is a variable gas phase and does appear in the expression as Kp = pH2O.