Calculate equilibrium constants at different temperatures using Van't Hoff equation
Enter values in the left panel and click Calculate to see results
The Van't Hoff equation relates the temperature dependence of the equilibrium constant:
Where K is the equilibrium constant, ΔH is the enthalpy change, R is the gas constant (8.314 J/mol·K), and T is temperature in Kelvin.
Use our Equilibrium Constant vs Temperature Calculator to predict K at different temperatures using Van't Hoff equation. Ideal for chemistry students and professionals studying reaction equilibria and enthalpy changes.
The equilibrium constant (K) describes how far a chemical reaction proceeds towards products at equilibrium. However, K changes with temperature, governed by the Van't Hoff equation. This calculator helps you calculate K at a new temperature from known values or determine the enthalpy change (ΔH) from two K values at different temperatures. Essential for understanding exothermic and endothermic reactions in chemistry and industrial processes.
Van't Hoff Equation: ln(K₂/K₁) = -ΔH/R × (1/T₂ - 1/T₁)
Rearranged for ΔH: ΔH = -R × ln(K₂/K₁) / (1/T₂ - 1/T₁)
Where K₁, K₂ are equilibrium constants, ΔH is enthalpy change (J/mol), R = 8.314 J/mol·K, T₁, T₂ in Kelvin.
Calculations are one-dimensional, focusing on temperature scalars. Here's the process:
In 2D/3D contexts like reaction modeling, this extends to multi-variable systems, but basics are scalar.
Given: K₁ = 1.0 at T₁ = 298 K, ΔH = -5000 J/mol, T₂ = 308 K
ln(K₂/1.0) = -(-5000)/8.314 × (1/308 - 1/298) ≈ 0.602 × (-0.00097) ≈ -0.00058
K₂ ≈ 1.0 × e^(-0.00058) ≈ 0.9994
K slightly decreases for exothermic reaction as temperature rises.
Given: K₁ = 2.0 at T₁ = 300 K, K₂ = 1.5 at T₂ = 310 K
ln(1.5/2.0) = ln(0.75) ≈ -0.2877
1/T₂ - 1/T₁ = 1/310 - 1/300 ≈ -0.00097
ΔH = -8.314 × (-0.2877) / (-0.00097) ≈ 2450 J/mol
Positive ΔH indicates endothermic reaction.
It quantifies how equilibrium constants change with temperature, linking to reaction enthalpy.
Kelvin is absolute scale; differences are the same, but equations use absolute temperatures.
The equation assumes constant ΔH; for large ranges, use integrated forms or experimental data.
Accurate for ideal cases; real systems may have deviations due to non-ideal behavior.
For further understanding and validation of the formulas used above, we recommend exploring these authoritative resources: