By John Brennan, Updated Mar 24, 2022
Image credit: tonuacatic/iStock/GettyImages
Calorimetry is a cornerstone of experimental thermochemistry, allowing scientists to determine reaction enthalpies and heat capacities. While many students are comfortable measuring the final temperature (T_f) of a calorimeter experiment, a common classroom challenge is predicting T_f when the reaction enthalpy (ΔH_rxn) and the heat capacities of all components are known. This article walks through that calculation in a clear, systematic way.
Carefully read the problem statement. You’ll typically find:
In an ideal, adiabatic calorimeter, no heat is lost to the surroundings. All heat released by the reaction is absorbed by the calorimeter and its contents.
Because the calorimeter and its contents reach the same final temperature, the heat released equals the heat absorbed:
ΔH_rxn = [C_p,contents × m_contents + C_cal] × (T_i – T_f)
Note the subtraction order: (T_i – T_f). Reaction enthalpies are negative for exothermic processes, so this sign convention keeps the algebra straightforward.
Rearrange the equation:
ΔH_rxn / [C_p,contents × m_contents + C_cal] = T_i – T_f
Flip the sign and add T_i:
T_f = T_i – ΔH_rxn / [C_p,contents × m_contents + C_cal]
Example: ΔH_rxn = –200 kJ, C_p,contents = 0.00418 kJ g⁻¹ K⁻¹, m_contents = 200 g, C_cal = 2 kJ K⁻¹, T_i = 25 °C.
T_f = 25 – [–200 / (0.00418 × 200 + 2)]
= 25 – [–200 / 2.836]
= 25 + 70.5
= 95.5 °C
The final temperature is 95.5 °C.