14.3 - Specific heat capacity

14.3 - Specific heat capacity

Learn why equal energy inputs can produce different temperature rises, how to calculate those changes and how to measure specific heat capacity electrically. You will check an energy balance and explain what heat losses and the apparatus do to an experimental result.

Energy for a temperature rise

Why do equal masses of water and aluminium not warm by the same amount when they receive the same energy? The materials require different amounts of energy for each kilogram to rise by one kelvin. That difference is measured by their specific heat capacities.

Specific heat capacity

The specific heat capacity of a substance is the energy required per unit mass to raise its temperature by one kelvin, with no change of state.

The word specific means per unit mass. A large sample needs more energy than a small sample of the same material for the same temperature rise. Heat capacity, without “specific”, refers to the whole object's energy requirement per kelvin and has unit J K−1\mathrm{J\,K^{-1}}. Specific heat capacity has unit J kg−1 K−1\mathrm{J\,kg^{-1}\,K^{-1}}.

Heating without a change of state

Q=mcΔTQ=mc\Delta T

Here QQ is energy transferred by heating in joules, mm is mass in kilograms, cc is specific heat capacity in J kg−1 K−1\mathrm{J\,kg^{-1}\,K^{-1}}, and ΔT\Delta T is the temperature rise in kelvin. Use the appropriate cc for the substance and stated conditions, approximating it as constant over the temperature interval. The same numerical temperature difference can be used in degrees Celsius.

Not on the data sheet: learn it.

For fixed QQ and mm, a larger cc gives a smaller rise. Using representative values of 4200 J kg−1 K−14200\,\mathrm{J\,kg^{-1}\,K^{-1}} for water and 900 J kg−1 K−1900\,\mathrm{J\,kg^{-1}\,K^{-1}} for aluminium, each 0.50 kg0.50\,\mathrm{kg} sample receiving 4500 J4500\,\mathrm{J} would rise by about 2.1 K2.1\,\mathrm{K} and 10 K10\,\mathrm{K}, respectively. This is why energy input alone does not determine temperature change.

Heating is an energy transfer, not a quantity called heat stored in the sample. A temperature rise is evidence of a change in the material's state; internal energy is a property of the material. In the next lesson you will see a case where energy is transferred while temperature stays constant during a change of state.

Watch out

Use a temperature difference, not an absolute temperature, in this equation. A rise from 15 to 35 degrees Celsius is 20 kelvin; adding 273.15 to that difference creates an error.

State what the definition means in a physical situation.

Heating calculations and energy balances

Begin with the system and the energy transfers, then choose the equation. A mass in grams must become kilograms if cc is in J kg−1 K−1\mathrm{J\,kg^{-1}\,K^{-1}}. A cooling object loses energy; it is often simplest to calculate the positive amount lost from the positive temperature drop and state its direction separately.

Worked example 1: warming a metal sample

Question. A 0.250 kg0.250\,\mathrm{kg} sample has c=390 J kg−1 K−1c=390\,\mathrm{J\,kg^{-1}\,K^{-1}}. Calculate the energy required for a temperature rise of 20.0 K20.0\,\mathrm{K}, with no change of state.

Plan. Multiply mass, specific heat capacity and temperature rise.

Q=(0.250)(390)(20.0)=1950 JQ=(0.250)(390)(20.0)=1950\,\mathrm{J}

Answer. 1.95×103 J1.95\times10^3\,\mathrm{J}. Check. The unit product is kg×J kg−1 K−1×K=J\mathrm{kg}\times\mathrm{J\,kg^{-1}\,K^{-1}}\times\mathrm{K}=\mathrm{J}.

When a hot object enters cooler water, write energy lost by the hot object equals energy gained by the cooler parts, provided there is negligible transfer to the surroundings. Include the container if its thermal response is significant. You do not obtain the common temperature by averaging the starting temperatures unless the two total heat capacities are equal.

Worked example 2: a common final temperature

Question. A 0.100 kg0.100\,\mathrm{kg} metal sample at 80.0 ∘C80.0\,{}^{\circ}\mathrm{C}, with cm=900 J kg−1 K−1c_m=900\,\mathrm{J\,kg^{-1}\,K^{-1}}, is placed in 0.200 kg0.200\,\mathrm{kg} water at 20.0 ∘C20.0\,{}^{\circ}\mathrm{C}, with cw=4200 J kg−1 K−1c_w=4200\,\mathrm{J\,kg^{-1}\,K^{-1}}. Find the final equilibrium temperature, neglecting the container and transfers to the surroundings.

Plan. Let the final Celsius temperature be θ\theta. The metal cools by 80.0−θ80.0-\theta; the water warms by θ−20.0\theta-20.0.

(0.100)(900)(80.0−θ)=(0.200)(4200)(θ−20.0)90(80.0−θ)=840(θ−20.0)24000=930θ\begin{aligned} (0.100)(900)(80.0-\theta)&=(0.200)(4200)(\theta-20.0)\\ 90(80.0-\theta)&=840(\theta-20.0)\\ 24000&=930\theta \end{aligned}

Answer. θ=25.8 ∘C\theta=25.8\,{}^{\circ}\mathrm{C}.

Check. The result lies between the initial temperatures and is nearer the water's starting temperature because the water's total heat capacity is much larger. This is a model energy balance; appreciable environmental transfer or container heating would need extra terms.

For a constant useful heating power PP acting for time tt, the transferred energy is PtPt. The power relation is not on the data sheet: recall power as energy transferred per unit time. Combining it with Q=mcΔTQ=mc\Delta T gives Pt=mcΔTPt=mc\Delta T, with PP in watts and tt in seconds. It applies only when PP is the power actually heating the stated sample.

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