Gibbs Free Energy Calculator
Calculate Gibbs free energy with ΔG = ΔH - TΔS.
Returns spontaneity, the equilibrium constant K, and the crossover temperature where the reaction flips.
How Gibbs Free Energy Is Calculated
Gibbs Free Energy (G) predicts whether a chemical reaction occurs spontaneously at constant temperature and pressure, which is to say under the conditions almost every reaction in chemistry and biology actually runs.
Gibbs Free Energy Formula:
ΔG = ΔH − TΔS
Where:
- ΔG = change in Gibbs free energy (kJ/mol)
- ΔH = enthalpy change (kJ/mol), negative means exothermic
- T = temperature in Kelvin (K = °C + 273.15)
- ΔS = entropy change. Enter it in J/mol·K, the unit tables use. The formula needs kJ/mol·K, so the calculator divides your value by 1000 before subtracting.
Spontaneity Rules:
- ΔG < 0: spontaneous (reaction proceeds forward)
- ΔG > 0: non-spontaneous (requires energy input)
- ΔG = 0: equilibrium (no net change)
Worked Example: Melting Ice at 25°C:
- ΔH = +6.01 kJ/mol (endothermic, absorbs heat)
- ΔS = +22.0 J/mol·K = +0.0220 kJ/mol·K
- T = 25 + 273.15 = 298.15 K
- ΔG = 6.01 − (298.15 × 0.0220) = 6.01 − 6.56 = −0.55 kJ/mol
ΔG < 0 confirms ice melts spontaneously at 25°C. At 273.15 K, which is 0°C, the same arithmetic gives ΔG = 6.01 − (273.15 × 0.0220) = 0.00 kJ/mol. That is equilibrium, and it is why ice and water coexist at exactly that temperature and nowhere else.
The crossover temperature
Set ΔG to zero and the formula rearranges to T = ΔH / ΔS, the single temperature where the reaction flips between spontaneous and not. For the ice numbers above that comes out at 273.2 K, the melting point, which is a satisfying way to see that the melting point is not an arbitrary fact about water but a consequence of its enthalpy and entropy of fusion.
Which side of the crossover is the spontaneous one depends on the signs:
| ΔH | ΔS | Result |
|---|---|---|
| negative | positive | Spontaneous at every temperature |
| positive | negative | Never spontaneous at any temperature |
| negative | negative | Spontaneous below the crossover |
| positive | positive | Spontaneous above the crossover |
The last two are the interesting ones, and they are where a crossover temperature is worth knowing.
Standard Conditions vs Real Conditions:
ΔG = ΔG° + RT × ln(Q)
where Q is the reaction quotient, R = 8.314 J/mol·K.
At Equilibrium: ΔG = 0, so ΔG° = −RT × ln(K), allowing calculation of the equilibrium constant K.
The electrochemistry link. For a redox reaction in a battery or fuel cell, Gibbs free energy connects directly to the cell voltage: ΔG° = −nFE°, where n is the moles of electrons transferred per mole of reaction, F is Faraday’s constant (96,485 C/mol), and E° is the standard cell potential in volts. A positive cell voltage means a negative ΔG°, so the reaction is spontaneous and will deliver electrical work.
Watch the degree symbol in that expression, because it is easy to lose. E° and ΔG° are standard values, fixed for a given reaction at a given temperature, and they do not change as a battery runs down. What changes is the actual cell potential E, which the Nernst equation ties to the reaction quotient: E = E° − (RT/nF) ln Q. As a fresh AA cell (≈1.5 V) discharges, products build up, Q climbs, E falls toward zero, and ΔG = −nFE rises toward zero with it. At E = 0 the cell has reached equilibrium and there is no usable free energy left, which is what a dead battery physically is.
How we build and check this calculator
This calculator runs entirely in your browser, so the numbers you enter stay on your device. The math behind it is written by hand and tested against worked examples and standard references before the page goes live.
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