🌡️thermodynamics

Calorimetry

q = mc(deltaT)

The calorimetry equation calculates heat absorbed or released using mass, specific heat capacity, and temperature change. It's fundamental for determining enthalpy changes experimentally.

Variables

q=Heat

Heat absorbed (+) or released (-) in joules

m=Mass

Mass of substance in grams

c=Specific Heat Capacity

Heat capacity in J/(g·°C)

deltaT=Temperature Change

Final temperature minus initial temperature

Example Calculation

Scenario

A 50.0 g sample of water is heated from 25.0°C to 75.0°C. Calculate the heat absorbed. (c_water = 4.18 J/g·°C)

Given Data

m:50.0 g
c:4.18 J/(g·°C)
deltaT:75.0 - 25.0 = 50.0°C

Calculation

q = mc(deltaT) = (50.0 g)(4.18 J/g·°C)(50.0°C)

Result

q = 10,450 J = 10.5 kJ

Interpretation

The water absorbed 10.5 kJ of heat energy. Water has a high specific heat, which is why it's commonly used in calorimetry and temperature regulation.

When to Use This Formula

  • Calculating heat absorbed or released
  • Determining enthalpy changes in reactions
  • Coffee cup calorimetry experiments
  • Finding specific heat capacity of unknown substance

Common Mistakes

  • Forgetting the sign of q (exo vs endo)
  • Using wrong specific heat value
  • Confusing mass of water with mass of reactant
  • Not converting units (J to kJ)

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FAQs

Common questions about this formula

For reactions in solution: q_solution = -q_reaction (heat gained by solution = heat lost by reaction). Calculate q for solution using m (mass of solution), c (usually water's value), and deltaT. Then deltaH = q_reaction / moles of limiting reagent.

Specific heat capacity (c) is the amount of heat needed to raise 1 gram of a substance by 1°C. Water has c = 4.18 J/(g·°C), which is unusually high. Metals typically have lower values (around 0.4-0.9 J/(g·°C)).

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