Hess's Law Calculator: Sum Steps or Formation Enthalpies

Two routes to reaction enthalpy: sum reaction steps with reverse and multiply, or subtract standard formation enthalpies you can override. Signed kJ, method and sources shown.

At a glance

Computes
Reaction enthalpy by summing reversed and multiplied steps, or from formation enthalpies.
You supply
Step enthalpies with multipliers, or reactants and products with formation values.
Use when
You need a reaction enthalpy that cannot be measured directly in one step.
Assumes
Standard-reference-form elements have zero formation enthalpy at 298.15 K and 1 bar.

Combine the reaction steps you already have, or read a reaction enthalpy straight off a formation table. Both routes give the same ΔH°rxn, because enthalpy is a state function.

Method

Reaction steps

One row per step. A negative multiplier reverses that step and its magnitude scales it, so 0.5 is allowed. ΔH is the step enthalpy as written, in kJ.

StepMultiplierΔH (kJ) Actions

Cumulative enthalpy (kJ) against Reaction step; reference at Starting enthalpy

0.00.51.01.52.0−100−80−60−40−200Starting enthalpyCumulative enthalpy

Reaction enthalpy ΔH°rxn

Enter a reaction

Choose a method, fill the table, and calculate.

Export

ΔH°rxn = Σ n*ΔHf°(products) - Σ n*ΔHf°(reactants) How?

How this is calculated

Method. Enthalpy is a state function, so the enthalpy change of a reaction is independent of the path taken. The summation route adds the enthalpies of any set of steps that combine to the target reaction, reversing a step (which flips the sign of its ΔH) and scaling it (which scales the magnitude) as needed. The formation route reads the same ΔH°rxn from a table of standard formation enthalpies as Σ n*ΔHf°(products) minus Σ n*ΔHf°(reactants).

Conventions. Formation values are tabulated at 298.15 K and 1 bar. 1 bar is the IUPAC standard pressure adopted in 1982; older tables use 1 atm, a difference of about 1.3 percent that is negligible here. ΔHf° for an element in its most stable reference form is 0 by definition: carbon as graphite (diamond is +1.9 kJ/mol), oxygen as O2 (ozone is nonzero), and white phosphorus as the reference for P. A negative ΔH°rxn releases heat (exothermic); a positive value absorbs it (endothermic). The result is per mole of reaction exactly as written, so scaling the equation scales ΔH.

Values shown. The bundled ΔHf° table is OpenStax Chemistry 2e, Appendix G, at 298.15 K. It only pre-fills a field you can overwrite, because published tables disagree at the second decimal and you are graded against your own textbook: OpenStax lists CH4 as -74.6 kJ/mol where other tables use -74.8. The calculation reads only the numbers in the table on this page, never the bundled library.

Formula: ΔH°rxn = Σ n*ΔHf°(products) - Σ n*ΔHf°(reactants)

Sources

  1. OpenStax Chemistry 2e, 5.3 Enthalpy. OpenStax. Retrieved .
  2. OpenStax Chemistry 2e, Appendix G: Standard Thermodynamic Properties. OpenStax. Retrieved .
  3. LibreTexts General Chemistry, 5.6 Hess's Law. LibreTexts. Retrieved .