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Library / Foundations: Chemistry / FCH-16

Foundations: Chemistry

Enthalpy change from calorimetry

Heat of reaction from the temperature rise of a solution.

Ref
FCH-16
Rev
v1
Field
Foundations: Chemistry
Result
ΔH [kJ/mol]

Q is the heat absorbed by the solution (in J), m its mass in g, c its specific heat capacity (4.18 J g⁻¹ K⁻¹ for water) and n the moles of the limiting reagent. The minus sign makes a temperature rise give a negative (exothermic) ΔH.

A reaction that warms the water has given out energy. The temperature rise tells you how much, and dividing by the moles gives the energy per mole.

Calculator

Solve for
kJ/mol
g
5500
J/(g K)
0.110
K
0.150
mol
0.0011
  • Heat absorbed by the solution1.359 kJ
  • Heat per gram of solution27.17 J/g

What drives the result

Each variable is moved across its typical range while the others stay at the values above. The longest bar is the key driver.

Enthalpy change (kJ/mol) current value −54.34 kJ/mol
nMoles of limiting reagentKey driver
−1,360−1.36
mMass of solution
−543−5.43
ΔTTemperature rise
−418−0.836
cSpecific heat capacity
−130−1.3
  • Neutralisation of a strong acid with a strong alkali gives about −57 kJ/mol; polystyrene cup losses make the measured value a little lower.
  • Heat lost to the surroundings is the main source of error, so insulate the cup and use a lid.
Chart data as tables

Ranked variables

VariableTypical rangeLowest resultHighest resultSwing (kJ/mol)Local stepChange in result
n Moles of limiting reagent0.001 to 1 mol−1,359−1.3591,357+10%−9.09 %
m Mass of solution5 to 500 g−543.4−5.434538+10%+10 %
ΔT Temperature rise0.1 to 50 K−418−0.836417.2+10%+10 %
c Specific heat capacity0.1 to 10 J/(g K)−130−1.3128.7+10%+10 %

Sweep of Temperature rise

Temperature rise (K)Enthalpy change (kJ/mol)
0.1−0.836
6.337−52.98
12.57−105.1
18.81−157.3
25.05−209.4
31.29−261.6
37.52−313.7
43.76−365.9
50−418

Sweep one variable

Enthalpy change (kJ/mol)Hover, touch, or use the arrow keys on the chart
−400−300−200−1000 1020304050 Temperature rise (K) now −54.34

Variables and how each one contributes

ΔH

Enthalpy change

Result · kJ/mol

What the equation gives you. Everything else feeds it.

m

Mass of solution

g · typical 5 to 500

Mass of solution heated (1 cm³ of water ≈ 1 g). Directly proportional to Q.

c

Specific heat capacity

J/(g K) · typical 0.1 to 10

4.18 for water-based solutions. Directly proportional to Q.

ΔT

Temperature rise

K · typical 0.1 to 50

Rise in temperature of the solution. Directly proportional to Q.

n

Moles of limiting reagent

mol · typical 0.001 to 1

Moles of the reagent that is used up. Inversely proportional.

Worked example with the values above

  1. Q = m c ΔT = 50 × 4.18 × 6.5 = 1,359 J = 1.359 kJ.
  2. Divide by the moles: 1.359 / 0.025.
  3. ΔH = −54.34 kJ/mol (negative: exothermic).

Assumptions and limits

  • Solution has the properties of water.
  • No heat lost to the surroundings.

Common mistakes

  • Dividing by the mass of reactants instead of the moles.
  • Giving the wrong sign.

Statistics and uncertainty

Heat loss and thermometer reading error (±0.5 K on 6.5 K is 8%) make ΔH from a simple cup experiment uncertain by 5–10%.

Where it is used

  • Measuring energy of fuels and reactions.
  • Checking neutralisation heats.

Maths you need

  • Specific heat capacity: Q = m c ΔT
  • Moles: n = c V

Related formulas

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