ChemBioTube

Thermochemistry Calculator

Heat from calorimetry, Hess's law reaction enthalpy, and Gibbs free energy with the equilibrium constant.

q = m·c·ΔT (J); ΔH = −q/n. Hess: ΔHrxn = Σ(coef·ΔHf)products − Σ(coef·ΔHf)reactants. Gibbs: ΔG = ΔH − T·ΔS/1000 (kJ/mol); K = exp(−ΔG·1000/(R·T)) with R = 8.314 J/(mol·K).

Enter the values for this tab to see the result.

Description

A three-mode thermochemistry calculator: measure the heat of a process with q = m·c·ΔT, combine standard formation enthalpies into a reaction enthalpy with Hess's law, or convert ΔH and ΔS into Gibbs free energy and the equilibrium constant. Every mode shows intermediate sums so you can check the arithmetic.

How to use

Pick the tab for the quantity you need. In Calorimetry enter the solution mass, its specific heat (4.18 J/(g·K) for water), the temperature change and, optionally, the moles of limiting reagent to also get ΔH per mole. In Hess's law add one row per species, choose product or reactant, and enter its coefficient and standard enthalpy of formation. In Gibbs enter ΔH in kJ/mol, ΔS in J/(mol·K) and the temperature in kelvin.

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What it does

Thermochemistry answers three questions that look different but share the same energy bookkeeping: how much heat a process exchanges, what the enthalpy change of a reaction is when it cannot be measured directly, and whether a reaction is spontaneous at a given temperature. The calculator handles each with the standard textbook relations, so it is useful for checking homework, planning a calorimetry experiment, or sanity-checking a reported value before you trust it.

When to use it

Use calorimetry mode to turn a measured temperature rise into joules and, when the amount of reactant is known, into a molar enthalpy. Use Hess's law mode to add up tabulated formation enthalpies for a reaction that is hard to run cleanly in a calorimeter, such as a combustion or a synthesis with side products. Use Gibbs mode to see how a reaction's spontaneity changes with temperature, or to estimate the equilibrium constant behind a ΔG° value from a database.

FAQ

What does the sign of q mean in calorimetry?
A positive q is heat absorbed by the system, a negative q is heat released. The tool uses q = m·c·ΔT with mass in grams, specific heat in J/(g·K) and ΔT in kelvin or degrees Celsius, which are numerically the same interval. If the heat came from a reaction, the reaction enthalpy is ΔH = −q/n: the reaction releases what the solution absorbed, so the sign flips.
How is Hess's law applied here?
Each Hess row is one species with its stoichiometric coefficient and standard enthalpy of formation. The tool sums coefficient × ΔHf over the products, subtracts the same sum over the reactants, and the difference is ΔHrxn. Formation enthalpies of elements in their standard states are zero, so an O₂ row contributes nothing.
How do ΔG, ΔH, ΔS and temperature relate?
ΔG = ΔH − T·ΔS, with ΔH in kJ/mol, ΔS in J/(mol·K) and T in kelvin, so the entropy term is divided by 1000 to match units. A negative ΔG means the forward reaction is spontaneous at that temperature, and because T multiplies ΔS, a reaction can switch direction as the temperature changes.
Why is the equilibrium constant so large or so small?
K = exp(−ΔG°/(R·T)) is exponential: at 298 K a ΔG of −20 kJ/mol gives K ≈ 3×10³, while +20 kJ/mol gives about 3×10⁻⁴. A few kJ/mol moves K by orders of magnitude, and values beyond roughly 10³⁰⁰ are shown as ∞ because the reaction is effectively quantitative.