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Why does it take so long to boil a full kettle but only moments to warm a single spoonful of water? Why does the sand on a beach become scorching in the midday sun while the sea stays cool? The answer lies in specific heat capacity — a property that measures how much energy a material needs to change its temperature. Some materials warm up readily with only a little energy; others, like water, need a great deal. This lesson, part of Topic P1 (Matter) of OCR Gateway Science A, explains how heating raises a substance's internal energy, defines specific heat capacity, works through the equation E=mcΔθ in every direction, and walks through the required practical for measuring it.
By the end of this lesson you should be able to explain how heating raises internal energy, define specific heat capacity, use and rearrange E=mcΔθ, describe the required practical to determine a specific heat capacity, and identify the main sources of error in it.
Recall that the internal energy of a substance is the total kinetic and potential energy of its particles. When you transfer energy to a substance by heating it, you raise its internal energy, and one of two things happens:
This lesson deals with the first case — heating that raises the temperature. How much the temperature rises for a given amount of energy depends on three things: the mass of the substance, the energy supplied, and a property of the material called its specific heat capacity.
Exam Tip: Be clear which "energy" is which. Heating raises internal energy; when this increases the particles' kinetic energy the temperature goes up. Temperature is a measure of the average kinetic energy of the particles, not the total internal energy.
The specific heat capacity of a material is the energy needed to raise the temperature of 1 kg of the material by 1°C (equivalently, by 1 K — a change of one kelvin is the same size as a change of one degree Celsius). It is given the symbol c and its unit is J/kg°C (joules per kilogram per degree Celsius).
A material with a high specific heat capacity needs a lot of energy to warm up (and releases a lot when it cools); a material with a low specific heat capacity warms up and cools down easily. Water has an unusually high specific heat capacity of about 4200 J/kg°C, which is why it is used in central-heating systems and car radiators (it can carry a lot of energy) and why coastal climates are milder (the sea stores energy in summer and releases it slowly in winter).
| Material | Specific heat capacity / J/kg°C |
|---|---|
| Water | 4200 |
| Aluminium | 900 |
| Iron / steel | 450 |
| Copper | 385 |
| Lead | 130 |
Exam Tip: Specific heat capacity is the energy to raise 1 kg by 1°C. Water's high value (≈ 4200 J/kg°C) means it takes a lot of energy to heat and stores a lot of energy — link this to its use as a coolant and to mild coastal climates.
The energy needed to change the temperature of a substance is given by:
E=mcΔθ
where E is the energy transferred (in J), m is the mass (in kg), c is the specific heat capacity (in J/kg°C), and Δθ is the change in temperature (in °C). The symbol Δθ (delta theta) means "the change in temperature" — always the final temperature minus the starting temperature.
The equation rearranges to make any quantity the subject:
E=mcΔθc=mΔθEΔθ=mcEm=cΔθE
How much energy is needed to raise the temperature of 2 kg of water from 20°C to 70°C? (Specific heat capacity of water =4200 J/kg°C.)
Step 1 — find the temperature change: Δθ=70−20=50°C.
Step 2 — write the equation: E=mcΔθ.
Step 3 — substitute: E=2×4200×50.
Step 4 — calculate: E=420000 J (which is 420 kJ).
Answer: 420000 J.
Calculate the energy needed to raise the temperature of a 0.5 kg aluminium block by 30°C. (Specific heat capacity of aluminium =900 J/kg°C.)
Step 1 — the temperature change is already given: Δθ=30°C.
Step 2 — write the equation: E=mcΔθ.
Step 3 — substitute: E=0.5×900×30.
Step 4 — calculate: E=13500 J.
Answer: 13500 J (= 13.5 kJ).
A 2 kg block of metal is given 39000 J of energy and its temperature rises by 50°C. Calculate the specific heat capacity of the metal and suggest what it might be.
Step 1 — rearrange for c: c=mΔθE.
Step 2 — substitute: c=2×5039000=10039000.
Step 3 — calculate: c=390 J/kg°C.
Answer: c=390 J/kg°C, which is very close to the value for copper (385 J/kg°C).
A 1.5 kg iron block is given 33750 J of energy. By how much does its temperature rise? (Specific heat capacity of iron =450 J/kg°C.)
Step 1 — rearrange for Δθ: Δθ=mcE.
Step 2 — substitute: Δθ=1.5×45033750=67533750.
Step 3 — calculate: Δθ=50°C.
Answer: the temperature rises by 50°C.
Exam Tip: Always work out Δθ as final − start first, and make sure the mass is in kilograms (so 500 g becomes 0.5 kg). Mixing up grams and kilograms is the commonest error in these calculations and gives an answer 1000 times too big or too small.
A key P1 required practical is to measure the specific heat capacity of a material — usually a metal block, but the same method works for water. The idea is to supply a measured amount of electrical energy to a known mass and measure the resulting temperature rise, then calculate c.
The apparatus is a metal block with two holes drilled in it: one for an electric heater (immersion heater) and one for a thermometer. The heater is connected through a joulemeter (or, equivalently, an ammeter and voltmeter together with a timer so the energy can be calculated).
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