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Equilibrium Constant and Gibbs Energy Change as Functions of Temperature

General Chemistry • Chemical Equilibrium

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Gibbs Energy, Equilibrium Constant, and Temperature

Use standard enthalpy change ΔrH° and standard entropy change ΔrS° to solve for equilibrium constant K, temperature T, or standard Gibbs change ΔrG°. This model assumes ΔrH° and ΔrS° are approximately constant over the chosen temperature range.

Solve

K from T
Compute K and see whether products or reactants are favored.

Solve

T from K
Find the temperature required to reach a specified equilibrium constant.

Solve

ΔrG° from T
Evaluate spontaneity and compare it with the equilibrium position.

Use positive, physically meaningful values for temperature and equilibrium constant. Scientific notation such as 2.5e-7 is supported.

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Main equations

\[ \begin{aligned} \Delta_r G^\circ &= \Delta_r H^\circ - T \cdot \Delta_r S^\circ \\ \ln K &= -\frac{\Delta_r G^\circ}{R \cdot T} \end{aligned} \]

Gas constant

\[ R = 8.314462618\ \mathrm{J \cdot mol^{-1} \cdot K^{-1}} \]

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Batch / CSV mode

Paste one numeric value per line, or import a CSV file. Use this to compute many temperatures or many K values at once.

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Frequently Asked Questions

How are K and ΔrG° related at a given temperature?

They are linked by ΔrG° = -R T ln(K), where R is the gas constant and T is in kelvin. If K > 1 then ln(K) is positive and ΔrG° is negative at that temperature.

How does this calculator model the temperature dependence of K?

It uses ΔrG°(T) = ΔrH° - TΔrS° and then computes K(T) = exp[-ΔrG°(T)/(R T)]. This assumes ΔrH° and ΔrS° do not change with temperature over the range you use.

How do I solve for temperature from a known K value?

The rearranged form is T = ΔrH°/(ΔrS° - R ln K). If the denominator equals zero (ΔrS° = R ln K), there is no finite temperature solution under the constant-ΔrH° and constant-ΔrS° approximation.

Why does the calculator require temperature in kelvin for the equations?

Thermodynamic relationships use absolute temperature to keep units consistent in terms like R T and TΔrS°. If you enter °C, it is converted to K using T(K) = t(°C) + 273.15.

When is the constant ΔrH° and ΔrS° assumption not accurate?

It can break down over wide temperature ranges or when heat capacities vary significantly, causing ΔrH° and ΔrS° to change with temperature. For higher accuracy in such cases, temperature-dependent data or activity-based corrections may be needed.