When two opposing processes operate simultaneously and independently between two states (state 1 and state 2) with continuous interchange between them, the system may reach a condition called dynamic equilibrium. Dynamic equilibrium is represented by a double-headed arrow in a reversible process: A ⇌ B. Depending on the nature of the states involved, equilibria are classified as physical or chemical.
Dynamic equilibrium is the state of a system in which a reversible process continues to occur in both directions, but the macroscopic composition (concentrations, pressures, etc.) no longer changes with time because the forward and reverse rates are equal. Although there is continuous microscopic movement of particles between reactants and products, there is no net change in amounts. Systems in dynamic equilibrium are examples of steady states.
Static equilibrium refers to a condition in which all motion and change have ceased; forces or fluxes are balanced so that there is no microscopic exchange between states. In contrast, in dynamic equilibrium microscopic exchanges continue but produce no net macroscopic change because the opposing rates are equal. In both cases the resultant force or net rate is zero and no visible change is observed.



For the general reaction aA + bB ⇌ cC + dD at equilibrium, the quotient of the product of concentrations of products (each raised to its stoichiometric exponent) to the product of concentrations of reactants (each raised to its exponent) is constant at a given temperature. This constant is the equilibrium constant expressed in concentration terms and denoted by Kc:


For gaseous reactions, it is often convenient to use partial pressures instead of concentrations because at a fixed temperature the partial pressure of a gas is proportional to its concentration (by the ideal gas law). For the gaseous reaction aA(g) + bB(g) ⇌ cC(g) + dD(g), the pressure-based equilibrium constant is denoted Kp and defined as:

Unit of Kp = (pressure unit)Δng, commonly atmΔng or barΔng.
For the reaction N2(g) + 3H2(g) ⇌ 2NH3(g),


For the reaction aA + bB ⇌ cC + dD:


The relation between Kp and Kc is:
Kp = Kc(RT)Δng
where Δng = (c + d) - (a + b), R is the gas constant (0.08206 L·atm·K-1·mol-1 if pressure in atm and concentration in mol L-1), and T is absolute temperature in K.
Relation between Kc and Kp for different types of reactions:
(i) If Δng = 0, then Kp = Kc.
(ii) If Δng > 0, then typically Kp > Kc (for given R and T).
(iii) If Δng < 0, then typically Kp < Kc.

Example: Phosgene (COCl2) dissociates at high temperature into CO and Cl2. At 600 K, Kp = 0.0041 atm for the reaction COCl2(g) ⇌ CO(g) + 1/2 Cl2(g). Initially 0.124 atm of COCl2 is placed in the container and allowed to reach equilibrium. Find the equilibrium composition.
Sol.





PCO=x=0.00769 atm
PCl2=x/2=0.00385 atm
PCOCl2=0.124-x=0.124-0.00769=0.1163 atm
Example. For the reaction NOBr(g) ⇌ NO(g) + 1/2 Br2(g), Kp = 0.15 atm at 90°C. If partial pressures are NOBr = 0.5 atm, NO = 0.4 atm and Br2 = 2.0 atm at this temperature, will Br2 be consumed or formed?
Sol.
Compute Q using the instantaneous partial pressures and compare with Kp. Here Q > Kp, so the reaction shifts backward; therefore Br2 will be consumed.
Equilibrium constants are often related to the degree of dissociation (α) of weak electrolytes or molecular species. Using mole balance and the relation between average molecular mass (vapour density) and composition, α can be determined from experimental vapour density or equilibrium constant data.
Example. The vapour density of a mixture of PCl5, PCl3 and Cl2 is 92. Find the degree of dissociation (α) of PCl5 under the conditions of the measurement.
Sol.
Initial and equilibrium mole relations for PCl5 ⇌ PCl3 + Cl2 are used to express the average molecular mass and relate it to the observed vapour density.
From the algebra one obtains the molecular mass value and hence
so α = 0.13.
Q.1. Given the following equilibrium constants:
(1) CaCO3(s) → Ca2+(aq) + CO32-(aq); K1 = 10-8.4
(2) HCO3-(aq) → H+(aq) + CO32-(aq); K2 = 10-10.3
Calculate the value of K for the reaction CaCO3(s) + H+(aq) → Ca2+(aq) + HCO3-(aq)
Sol.
The net reaction is the sum of reaction (1) and the reverse of reaction (2):
Reaction (1): CaCO3(s) → Ca2+(aq) + CO32-(aq); K1 = 10-8.4
Reverse of reaction (2): H+(aq) + CO32-(aq) → HCO3-(aq); K-2 = 1 / K2 = 10+10.3
Net Reaction: CaCO3(s) + H+(aq) → Ca2+(aq) + HCO3-(aq)
K = K1 × K-2 = 10-8.4 × 10+10.3 = 10+1.9
Comment: This net reaction describes the dissolution of limestone by acid. The small intrinsic tendency of CaCO3 to dissolve is driven by removal of CO32- via protonation to HCO3-. Such coupled reactions are common, especially in biochemistry, where one reaction "pulls" another forward.
Q.2. The synthesis of HBr from hydrogen and liquid bromine has an equilibrium constant Kp = 4.5 × 1015 at 25°C. Given that the vapour pressure of liquid bromine is 0.28 atm, find Kp for the homogeneous gas-phase reaction at the same temperature.
Sol.
The heterogeneous synthesis (involving liquid Br2) and the vaporization equilibrium of Br2(l) ⇌ Br2(g) can be combined to give the homogeneous gas-phase reaction. Use equilibrium algebra (sum reactions and multiply corresponding equilibrium constants) to obtain the gas-phase Kp. The vapour pressure of liquid bromine (0.28 atm) serves to relate the heterogeneous and homogeneous K values via multiplication or division of equilibrium expressions as appropriate.
| 1. What is the difference between static and dynamic equilibrium? | ![]() |
| 2. What is the significance of the equilibrium constant? | ![]() |
| 3. How is the equilibrium constant calculated? | ![]() |
| 4. Can the equilibrium constant change with temperature? | ![]() |
| 5. How can the equilibrium constant be used to determine the position of equilibrium? | ![]() |