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All lessons Thermodynamics22 min

Specific Heat Capacity

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← Temperature and HeatThermal Expansion →
01
Hook
02
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Formalize
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Practice
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Challenge
Interactive simulation
01

Hook

You stir your coffee with a metal spoon — both the spoon and the coffee are at the same 80 °C temperature. Yet the spoon burns your fingers almost instantly while the coffee feels merely hot. If they're the same temperature, why does one hurt and the other doesn't?

02

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Spoilers

Specific Heat Capacity — summary and key formula

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The question

You stir your coffee with a metal spoon — both the spoon and the coffee are at the same 80 °C temperature. Yet the spoon burns your fingers almost instantly while the coffee feels merely hot. If they're the same temperature, why does one hurt and the other doesn't?

Temperature tells you how energetic the particles are on average, but it says nothing about how much energy a material holds in total. Different substances store very different amounts of heat energy for the same temperature rise — and that hidden capacity is what separates a material that scorches you from one that warms you gently. This property, called specific heat capacity, governs everything from cooking to climate.

The key idea

Specific heat capacity (c) is the amount of energy needed to raise 1 kg of a material by 1 °C (or 1 K). Materials with a high specific heat capacity absorb a lot of energy before their temperature rises much — water is the classic example. Materials with a low specific heat capacity, like metals, heat up quickly with relatively little energy input. The same mass of two different substances can hold very different amounts of thermal energy at the same temperature.

Q = mcΔT lets you calculate how much energy is needed to heat (or cool) any substance. Rearranged: ΔT = Q/(mc) tells you the temperature rise you'll get; m = Q/(cΔT) tells you how much mass you need. Water has one of the highest specific heat capacities of any common substance — c ≈ 4 200 J/(kg·K) — which is why it takes so long to boil and why oceans stabilise coastal climates. Iron and aluminium have c values of around 450–900 J/(kg·K), which is why metal cookware heats up fast. In calorimetry experiments, heat lost by a hot object equals heat gained by a cold one: m₁c₁ΔT₁ = m₂c₂ΔT₂.

The formula

Q=mcΔTQ = mc\Delta TQ=mcΔT
  • ·Q = heat energy transferred in joules (J)
  • ·m = mass in kilograms (kg)
  • ·c = specific heat capacity in J/(kg·°C) or J/(kg·K)
  • ·ΔT = change in temperature in degrees Celsius (°C) or kelvin (K)