Heat Transfer

Site: Young Education
Cours: Thermal Energy and Gas Laws
Livre: Heat Transfer
Imprimé par: Guest user
Date: lundi 9 novembre 2026, 16:38

1. Thermal Equilibrium and Heat Flow

Learning outcomes
  • I can explain that heat flows naturally from warmer objects to cooler objects.

  • I can define thermal equilibrium and describe when it occurs.
  • I can predict the direction of heat transfer between two objects.
  • I can distinguish between heat transfer and temperature change.
  • I can identify examples of thermal equilibrium in everyday life.

Thermal Equilibrium and Heat Flow

Heat Flows from Warmer to Cooler Objects

When two objects at different temperatures interact, thermal energy is transferred from the warmer object to the cooler object.

This transfer of thermal energy is called heat transfer.

For example, if you place a metal spoon into a cup of hot tea:

  • the tea is initially warmer than the spoon
  • thermal energy transfers from the tea to the spoon
  • the spoon becomes warmer
  • the tea becomes slightly cooler

The transfer continues until the spoon and tea reach the same temperature.

At that point, they are in thermal equilibrium.

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Temperature and Particle Motion

Temperature is related to the average kinetic energy of the particles in a substance.

In a warmer object, particles generally have greater average kinetic energy than particles in a cooler object.

When warmer and cooler materials interact, collisions between particles allow energy to be transferred.

The overall result is:

warmer object → cooler object

The warmer object loses thermal energy while the cooler object gains thermal energy.

This process continues until there is no temperature difference driving a net transfer of thermal energy.


What Is Thermal Equilibrium?

Thermal equilibrium occurs when objects in thermal contact reach the same temperature and there is no net transfer of thermal energy between them.

For example, suppose a block at 80°C is placed in contact with a block at 20°C.

Initially:

80°C object → heat transfer → 20°C object

As energy is transferred:

  • the hot object cools
  • the cold object warms
  • the temperature difference decreases

Eventually, both objects reach the same final temperature.

At this point:

T₁ = T₂

The objects are in thermal equilibrium.

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Predicting the Direction of Heat Transfer

The direction of spontaneous heat transfer is determined by temperature, not by the size, mass or total internal energy of the objects.

The basic rule is:

Higher temperature → Lower temperature

For example:

Object A Object B Net heat transfer
80°C 20°C A → B
10°C 35°C B → A
25°C 25°C No net transfer
−10°C 5°C B → A

Even when both objects are cold, energy still transfers from the object with the higher temperature to the one with the lower temperature.

For example, an ice cube at −15°C placed in a freezer at −5°C will gain thermal energy from its surroundings because −5°C is warmer than −15°C.


Heat and Temperature Are Not the Same Thing

The words heat and temperature are sometimes used as though they mean the same thing, but in physics they describe different concepts.

Temperature

Temperature indicates the thermal state of an object and is related to the average kinetic energy of its particles.

Temperature can be measured in units such as:

  • degrees Celsius (°C)
  • kelvin (K)

Heat

Heat is thermal energy transferred between systems because of a temperature difference.

Heat is therefore energy in transfer.

Its SI unit is the joule (J).

A useful distinction is:

Temperature tells us how hot or cold something is.

Heat describes energy being transferred because of a temperature difference.


Heat Transfer vs Temperature Change

Heat transfer often causes temperature to change, but the two ideas are not identical.

Consider a cold metal block placed into hot water.

Thermal energy transfers:

hot water → metal block

The block gains energy and its temperature usually rises.

The water loses energy and its temperature usually falls.

However, the amount of heat transferred and the resulting temperature change depend on several factors, including:

  • mass
  • material
  • specific heat capacity
  • changes of state

Therefore, the same amount of transferred energy does not necessarily produce the same temperature change in different objects.


Mass Matters

Imagine heating:

  • one cup of water
  • an entire swimming pool

Raising both by 1°C requires vastly different amounts of energy.

The swimming pool contains much more water and therefore requires much more energy for the same temperature increase.

This demonstrates why temperature alone does not tell us the total thermal energy of an object.

A small cup of boiling water has a higher temperature than a swimming pool at 30°C, but the swimming pool contains vastly more internal energy overall.


Specific Heat Capacity Matters

Different materials require different amounts of energy to change their temperatures.

The relationship can be expressed as:

Q = mcΔT

where:

  • Q = energy transferred, in J
  • m = mass, in kg
  • c = specific heat capacity, in J/(kg·°C)
  • ΔT = temperature change, in °C or K

A material with a high specific heat capacity requires more energy to produce a particular temperature change.

Water has a relatively high specific heat capacity, which is one reason it warms and cools more slowly than many other materials.


Worked Example

A 2.0 kg object has a specific heat capacity of 500 J/(kg·°C). Its temperature increases by 10°C.

Calculate the energy transferred to the object.

Use:

Q = mcΔT

Substitute:

Q = 2.0 × 500 × 10

Q = 10,000 J

Therefore:

Q = 10,000 J

The object gained 10 kJ of energy.


Reaching Thermal Equilibrium

Suppose a hot object and a cold object are placed together inside an insulated container.

Initially:

T_hot > T_cold

Energy transfers from the hotter object to the colder object.

As time passes:

  • T_hot decreases
  • T_cold increases
  • the temperature difference becomes smaller
  • the rate of net heat transfer generally decreases

Eventually:

T_hot = T_cold

Thermal equilibrium has been reached.

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On a temperature-time graph, the temperatures of the two objects move toward the same equilibrium temperature.


Does Energy Transfer Stop Completely?

At thermal equilibrium, we usually say there is no net heat transfer between the objects.

At the microscopic level, particles are still moving, colliding and exchanging energy.

However, because both systems have the same temperature, energy is exchanged in both directions at equal average rates.

Therefore:

energy transfer in one direction = energy transfer in the opposite direction

The net transfer is zero.

This is an important distinction.


Everyday Example: A Hot Drink

Imagine making a cup of hot chocolate.

Initially:

  • drink = 80°C
  • room = 22°C

Because the drink is warmer:

drink → surroundings

Energy is transferred from the drink to the cup, air, table and other surroundings.

The drink gradually cools.

If left long enough, its temperature approaches the temperature of its surroundings.

The drink and surroundings are then approximately in thermal equilibrium.

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Everyday Example: Ice in Water

Suppose an ice cube at 0°C is placed into water at 25°C.

The water is warmer, so:

water → ice

The ice gains thermal energy.

Initially, much of this energy is used to melt the ice rather than raise its temperature.

This illustrates an important idea:

Heat transfer does not always cause an immediate temperature change.

During a change of state, energy can be transferred while temperature remains constant.


Everyday Example: A Thermometer

A thermometer works by reaching thermal equilibrium with the object being measured.

Suppose a thermometer initially at room temperature is placed into warm water.

Thermal energy transfers:

warm water → thermometer

The thermometer warms until its temperature becomes approximately equal to the temperature of the water.

Only then does it provide a reliable measurement.

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This explains why a thermometer sometimes needs time before its reading becomes stable.


Everyday Example: Food in a Refrigerator

Suppose warm leftovers are placed in a refrigerator.

The food is initially warmer than the air and other materials inside the refrigerator.

Therefore:

food → refrigerator surroundings

The food loses thermal energy and cools.

Eventually, its temperature approaches the temperature inside the refrigerator.

This is another example of a system moving toward thermal equilibrium.


Methods of Heat Transfer

Thermal energy can be transferred in three major ways.

Conduction

Conduction transfers thermal energy through particle interactions, particularly in solids.

Example:

A metal spoon becomes hot when one end is placed in hot soup.

Convection

Convection transfers thermal energy through the bulk movement of fluids.

Example:

Warm water rises and cooler water sinks in a heated pot.

Thermal Radiation

Thermal radiation transfers energy through electromagnetic waves.

Unlike conduction and convection, radiation does not require matter.

Example:

Energy from the Sun travels through space to Earth.

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All three processes can contribute to systems moving toward thermal equilibrium.


Thermal Equilibrium and Insulation

Insulation does not prevent thermal equilibrium forever.

Instead, insulation reduces the rate of energy transfer.

For example, a vacuum flask reduces energy transfer through:

  • conduction
  • convection
  • radiation

As a result, a hot drink remains hot for much longer.

However, given enough time, the drink and its surroundings will still tend toward thermal equilibrium.

This leads to an important distinction:

Insulation slows heat transfer; it does not change the natural direction of heat transfer.


Can Heat Flow from Cold to Hot?

Thermal energy naturally transfers from higher temperature to lower temperature.

However, devices such as refrigerators and air conditioners can move energy from cooler regions to warmer regions.

They can do this only by using an external energy supply.

For example, a refrigerator transfers thermal energy from its cold interior to the warmer room while consuming electrical energy.

This does not contradict the natural direction of spontaneous heat transfer because work is being done on the system.


Thermal Equilibrium and the Zeroth Law

Thermal equilibrium is connected to the Zeroth Law of Thermodynamics.

In simplified form:

If object A is in thermal equilibrium with object C, and object B is also in thermal equilibrium with object C, then A and B are in thermal equilibrium with each other.

Therefore:

If:

T_A = T_C

and:

T_B = T_C

then:

T_A = T_B

This principle makes temperature measurement possible.

A thermometer acts as the third system. Once it reaches thermal equilibrium with an object, its temperature can be used to determine the object's temperature.


Common Mistakes

Mistake: "Cold flows into an object."
In thermal physics, we normally describe thermal energy transferring from the warmer object to the cooler object.

Mistake: "Heat and temperature are the same thing."
Heat is energy transferred because of a temperature difference. Temperature describes the thermal state of a system.

Mistake: "A larger object must have a higher temperature."
Temperature does not depend simply on an object's size.

Mistake: "Thermal equilibrium means particles stop moving."
Particles continue moving. There is simply no net heat transfer between systems at the same temperature.

Mistake: "Insulation stops all heat transfer."
Real insulation reduces the rate of transfer but does not normally eliminate it completely.

Mistake: "If energy is transferred into something, its temperature must rise."
Not necessarily. During a change of state, energy can be transferred without a temperature change.


Key Terms

Thermal energy — energy associated with the microscopic motion and interactions of particles in a system.

Heat transfer — transfer of thermal energy resulting from a temperature difference.

Temperature — a measure related to the average kinetic energy of particles.

Thermal equilibrium — the condition in which systems have the same temperature and there is no net heat transfer between them.

Temperature difference — the difference in temperature between two systems that drives net thermal energy transfer.

Conduction — energy transfer through interactions between particles.

Convection — energy transfer through the movement of a fluid.

Thermal radiation — energy transfer by electromagnetic radiation.

Specific heat capacity — the energy required to raise the temperature of 1 kg of a substance by 1°C (or 1 K).

Insulation — material or a system designed to reduce the rate of thermal energy transfer.

Zeroth Law of Thermodynamics — the principle relating thermal equilibrium between multiple systems and providing the basis for temperature measurement.


Key Takeaways

  • Thermal energy naturally transfers from higher-temperature objects to lower-temperature objects.
  • A temperature difference drives net heat transfer.
  • Thermal equilibrium occurs when interacting systems reach the same temperature and there is no net heat transfer.
  • Heat and temperature are different concepts.
  • Heat describes energy transfer, while temperature describes the thermal state of a system.
  • Heat transfer does not always produce a temperature change, particularly during changes of state.
  • The temperature change produced by a given energy transfer depends on mass and specific heat capacity.
  • Conduction, convection and radiation can all transfer thermal energy.
  • Insulation slows heat transfer but does not reverse its natural direction.
  • A thermometer measures temperature by approaching thermal equilibrium with the object being measured.
  • Refrigerators can transfer energy from cooler to warmer regions because external energy is supplied.
  • Thermal equilibrium is fundamental to the Zeroth Law of Thermodynamics.

Check Your Understanding

  1. In which direction does thermal energy naturally transfer between objects at 70°C and 25°C?
  2. Define thermal equilibrium.
  3. Why does a hot drink eventually approach room temperature?
  4. Explain the difference between heat and temperature.
  5. Why does a thermometer need time to give an accurate reading?
  6. Two objects are both at 35°C and are placed in contact. Is there a net heat transfer between them? Explain.
  7. Why can energy be transferred into melting ice without increasing its temperature?
  8. Explain why insulation slows the approach to thermal equilibrium but does not prevent it indefinitely.
  9. A 0.50 kg object with a specific heat capacity of 800 J/(kg·°C) warms by 15°C. Calculate the energy transferred to it.
  10. Explain how a refrigerator can transfer thermal energy from its cold interior to a warmer room.

2. Conduction

Learning outcomes
  • I can describe conduction as heat transfer through direct particle collisions.

  • I can explain why conduction is most effective in solids.
  • I can compare thermal conductors and thermal insulators.
  • I can identify materials with high and low thermal conductivity.
  • I can apply conduction concepts to real-world situations.

Conduction

What Is Conduction?

Conduction is the transfer of thermal energy through a material by interactions between neighboring particles, without the material as a whole moving from one place to another.

When one part of an object is heated, particles in that region gain energy. They vibrate or move more rapidly and interact with nearby particles, transferring energy through the material.

The overall direction of thermal energy transfer is:

higher temperature → lower temperature

For example, if one end of a metal rod is placed in a flame, the heated end becomes hot first. Over time, thermal energy is conducted along the rod, causing the other end to become warmer.

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Conduction at the Particle Level

In a solid, particles are packed closely together in fixed positions.

They cannot move freely through the material, but they can vibrate about their equilibrium positions.

When part of a solid is heated:

  • particles in the hotter region gain kinetic energy
  • their vibrations become more energetic
  • they interact with neighboring particles
  • energy is transferred to those neighboring particles
  • the process continues through the material

As a result, thermal energy spreads from warmer regions toward cooler regions.

The particles themselves do not travel from the hot end to the cold end. It is the energy that is transferred.


Why Conduction Is Effective in Solids

Conduction can occur in solids, liquids and gases, but it is generally most effective in solids.

In solids, particles are:

  • closely packed
  • strongly interacting
  • able to transfer energy efficiently to neighboring particles

In gases, particles are much farther apart. Collisions occur less frequently, so conduction is generally much slower.

This is one reason trapped air can be a useful thermal insulator.

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Conduction in Metals

Metals are particularly effective thermal conductors.

Energy transfer in a metal occurs through both:

  • vibrations of the metal lattice
  • movement and collisions of delocalized electrons

Metals contain electrons that can move relatively freely through the material.

At the hot end of a metal object, these electrons gain energy. They move through the metal and transfer energy through interactions with other electrons and ions.

This makes thermal conduction in many metals much faster than in non-metallic solids.


Why Metals Feel Cold

Touch a metal object and a wooden object that have been sitting in the same room.

They may both be at exactly the same temperature, yet the metal often feels colder.

Why?

Your hand is warmer than both objects.

Thermal energy therefore transfers:

hand → object

Metal conducts this energy away from the contact point quickly, so your skin loses thermal energy rapidly.

Wood transfers the energy away much more slowly.

Therefore, the metal feels colder even though it may be at the same temperature as the wood.

This demonstrates an important idea:

How hot or cold something feels depends partly on the rate of heat transfer, not simply its temperature.


Thermal Conductors

A thermal conductor is a material through which thermal energy can be transferred relatively easily.

Many metals are excellent thermal conductors.

Examples include:

  • copper
  • aluminium
  • silver
  • iron
  • steel

Copper is particularly useful because it combines high thermal conductivity with practical properties such as durability and workability.

https://images.openai.com/static-rsc-4/ayFXJkyektUTyLmY2uJ8aHF8GE9-ISi_7j_3toedl6PwusnITjRAupAcoCeJJmzkp0NaQn3Nk_7olzDu-Zo3cPYbDpacf1Eb8n0JLLhYiSgiFIXSiwHKkWgYV0tWZzXZkInrSSPaF-pDMJfr4GMRW9J-EXHXAAAInR9XoLR2kUoFq_5ReDGdG-eZljkwoHmn?purpose=fullsize
 
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9

Thermal Insulators

A thermal insulator is a material that transfers thermal energy relatively slowly.

Examples include:

  • air
  • wood
  • plastic
  • rubber
  • foam
  • wool
  • fibreglass
  • cork

These materials have low thermal conductivity.

Insulators are useful whenever we want to reduce the rate of heat transfer.

For example, the plastic handle on a cooking pot reduces conduction from the hot metal pot to a person's hand.


Thermal Conductivity

The ability of a material to conduct thermal energy is described by its thermal conductivity.

The symbol commonly used for thermal conductivity is:

k

Its SI unit is:

W/(m·K)

A material with a large value of k is a good thermal conductor.

A material with a small value of k is a good thermal insulator.

Approximate values illustrate the enormous differences between materials:

Material Approximate thermal conductivity, W/(m·K) Behaviour
Copper 400 Excellent conductor
Aluminium 240 Excellent conductor
Steel 15–50 Conductor
Glass ~1 Poor conductor
Wood ~0.1 Insulator
Air ~0.025 Very good insulator

Exact values vary with temperature, composition and other conditions.


Factors Affecting the Rate of Conduction

The rate at which thermal energy is conducted depends on several factors.

Temperature Difference

A greater temperature difference generally produces a greater rate of energy transfer.

For example, a metal rod with one end at 200°C and the other at 20°C will initially conduct energy more rapidly than the same rod with its ends at 30°C and 20°C.

Thermal Conductivity

Materials with larger thermal conductivity transfer energy more rapidly.

larger k → faster conduction

Cross-Sectional Area

A thicker piece of material provides a larger area through which energy can be transferred.

larger area → faster conduction

Thickness or Length

Increasing the distance through which thermal energy must travel reduces the rate of conduction.

greater thickness → slower conduction


The Conduction Equation

For steady conduction through a flat material, the rate of thermal energy transfer can be approximated by:

P = kAΔT/L

where:

  • P = rate of energy transfer, in W
  • k = thermal conductivity, in W/(m·K)
  • A = cross-sectional area, in m²
  • ΔT = temperature difference, in K or °C
  • L = thickness of the material, in m

This equation shows why thick layers of low-conductivity materials are effective insulation.

Increasing L decreases the rate of heat transfer.

Decreasing k also decreases the rate of heat transfer.


Worked Example

A wall has:

k = 0.50 W/(m·K)

A = 10 m²

L = 0.20 m

The temperature difference between its two sides is:

ΔT = 20°C

Calculate the rate of thermal energy transfer through the wall.

Use:

P = kAΔT/L

Substitute:

P = (0.50 × 10 × 20) / 0.20

P = 500 W

Therefore:

P = 500 W

Thermal energy is being conducted through the wall at a rate of 500 J every second.


Cooking and Conduction

Cookware demonstrates how engineers use both conductors and insulators in the same object.

The base of a saucepan is usually made from metal because the base needs to transfer energy efficiently:

stove → saucepan → food

Aluminium and copper are particularly effective for spreading thermal energy across cookware.

The handle has a different purpose.

We want to reduce:

hot pan → hand

Therefore, handles may be made from materials such as plastic, silicone or wood.

https://images.openai.com/static-rsc-4/xiPN61tJawOH9Da6Op3QLBW77wnQf_PWRHfkRxfp-_nAXI8LtMzATYjGgL3Cj8I5gO8IdfrjknDworBf9S9QbD2u18mMUbkfrcawBh0OijSyOmdOfYRepywkyhVUi3DUUdnKzBqqBbs8RyJErvMYQOatngdiZ41o1AiNW5mWy3cdBXIQKVl6sFpOOeZGa93L?purpose=fullsize
 
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8

The same object therefore uses:

conductor where fast heat transfer is useful

and:

insulator where heat transfer should be reduced


Building Insulation

Buildings lose thermal energy through walls, windows, roofs and floors.

Insulation reduces this transfer.

Common insulating materials include:

  • fibreglass
  • mineral wool
  • foam
  • cellulose
  • trapped air

Many insulation materials contain numerous small pockets of air.

Air has very low thermal conductivity, so trapping it reduces conduction.

https://images.openai.com/static-rsc-4/YVcluGO49lXZFxFOthwZ0tiuFzaSuWgAfeufPyexq6L3H1iWrzHrRpBfX-PoSc6bWs202i0WuTlzMAUBpU7k9Tv0rbdVvUpYwdP-6Xr_qnJcR41HUATLB0W_a-9sWQfBZoO7JZtyrLygO1sutb5Q8TIqjrhd9wADutmULtXzfCSiBNdYhy5zhtf8jxr3iZcC?purpose=fullsize
 
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8

Insulation does not completely stop energy transfer. It reduces the rate at which thermal energy is conducted.


Double-Glazed Windows

Double-glazed windows contain two sheets of glass separated by a gap.

The gap contains air or another gas.

Because gases have relatively low thermal conductivity, the gap reduces conduction between the inside and outside of the building.

Some high-performance windows use gases such as argon because they can provide better insulation than ordinary air.

https://images.openai.com/static-rsc-4/YVucYyhvx02LJ_kr3WRcW8jzwgkkrSQhU4--Z5nnzpykKqCCqnrLBEGk4NBD8s5v4bgAU39sAHSrpjZQKzbwvdFD41d0bviKgNH15NcVmcSHjIlsX6iylIDn768ivWDSc8-8SnwfukdBcbIw52Y1o2odP3TMhTFbwQ2i3EwqGMe6NflUTtNtSH5eVMDPAl_R?purpose=fullsize
 
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7

The principle is:

trapped low-conductivity gas → reduced thermal conduction


Clothing and Conduction

Clothing does not normally keep you warm by producing thermal energy.

Instead, clothing reduces the rate at which your body loses energy to its surroundings.

Materials such as:

  • wool
  • fleece
  • down
  • synthetic insulation

trap layers or pockets of air.

Because air is a poor conductor, these trapped air pockets reduce thermal conduction.

This is why several layers of clothing can be more effective than one thin layer.


Vacuum Flasks

A vacuum flask is designed to reduce several forms of heat transfer.

The space between its walls contains very little matter.

Because conduction requires particles to transfer energy, removing most of the particles dramatically reduces conduction.

A vacuum also prevents convection across the gap.

Reflective surfaces are often added to reduce thermal radiation.

https://images.openai.com/static-rsc-4/heGBlcV3ZZfTYeqbCRiuSK0D_vy6QTYYuLHacmknzvCLnD4NOOdYNVPd6UAOIIAWJEWu12vSYBvdqVjAFEXnM-LUTEPWeQdzvpPJG8Yj1TZSIWgwKxUoFp2GB6mi0tmQi6XLCvoPwNgiH-wOFIUwzJtiDotq--90SJAw7KlH4h1B17togKdt2KS-x43T4idR?purpose=fullsize
 
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6

This makes vacuum flasks useful for keeping hot substances hot and cold substances cold.


Heat Sinks

Sometimes we want conduction to happen as rapidly as possible.

Electronic components such as computer processors generate thermal energy during operation.

A heat sink is usually made from a highly conductive metal such as aluminium or copper.

Thermal energy is conducted:

processor → heat sink

The heat sink then transfers energy to the surrounding air.

Fins increase the surface area, helping energy transfer from the heat sink to the surroundings.

https://images.openai.com/static-rsc-4/JpEGhmlknuzlNRSbzxlPqxkhaRUZbW8zG3uYD6yYKbFOrRX1an1FZbwHyN23FNGZZUEiDRYQYS9IgOe6mW8U0W9ZQXIZnxc4uWXJmWkVn-4V3Gxa280GIlqkhyzNv193smM5d9VFrmvzmocPyKXJL0saPd6UvYzWc7sFH_eHOtRTlhm2XGPDUVNj99Bd6nWn?purpose=fullsize
 
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9

Conduction in Different States of Matter

Solids

Conduction is generally most effective because particles are closely packed.

Metals are particularly effective because mobile electrons also transfer energy.

Liquids

Conduction occurs through particle interactions, but liquids often transfer substantial thermal energy through convection as well.

Gases

Gases are generally poor conductors because their particles are widely separated.

However, gases can transfer energy effectively through convection if they are free to circulate.

This explains why insulation works best when air is trapped rather than allowed to move freely.


Conduction vs Convection

These processes should not be confused.

Conduction:

Energy is transferred through particle interactions without bulk movement of the material.

Convection:

Energy is transferred by the bulk movement of a fluid.

Consider a pot of water on a stove.

Energy conducts:

stove → metal pot

Energy then conducts:

metal pot → nearby water

Movement of the water can then establish convection currents that distribute energy throughout the liquid.

Multiple heat-transfer processes can therefore occur at the same time.


Choosing Materials for Different Applications

There is no material that is always "better."

The correct material depends on whether we want thermal energy to move quickly or slowly.

Application Desired property Possible material
Saucepan base High conductivity Aluminium or copper
Saucepan handle Low conductivity Plastic or wood
Building insulation Low conductivity Fibreglass or foam
Heat sink High conductivity Aluminium or copper
Winter clothing Low conductivity Wool, fleece or trapped air
Oven glove Low conductivity Thick insulating fabric

Engineers therefore consider thermal conductivity when selecting materials.


Common Mistakes

Mistake: "Conduction means particles move from the hot side to the cold side."
The particles in a solid mainly remain in their positions. Energy is transferred through interactions and vibrations.

Mistake: "Only solids conduct heat."
Conduction occurs in solids, liquids and gases, although its effectiveness differs greatly.

Mistake: "Insulators do not conduct any energy."
Insulators still conduct thermal energy, but at a much lower rate.

Mistake: "Metal feels cold because its temperature is lower."
A metal and wooden object in the same room may have the same temperature. Metal often feels colder because it removes thermal energy from your hand more quickly.

Mistake: "Air is always a good insulator."
Air is most effective when it is trapped. If air can circulate, convection can increase energy transfer.


Key Terms

Conduction — transfer of thermal energy through interactions between neighboring particles without bulk movement of the material.

Thermal conductor — a material that transfers thermal energy relatively easily.

Thermal insulator — a material that transfers thermal energy relatively slowly.

Thermal conductivity — a measure of how effectively a material conducts thermal energy.

Delocalized electrons — mobile electrons in metals that help transfer thermal energy rapidly.

Temperature gradient — change in temperature with distance through a material.

Insulation — material used to reduce the rate of thermal energy transfer.

Heat sink — a conductive component designed to transfer thermal energy away from another object.

Vacuum — a region containing very little matter, greatly reducing conduction and convection.

Steady-state conduction — a condition in which the temperature distribution remains constant while energy continues to transfer through a material.


Key Takeaways

  • Conduction transfers thermal energy through interactions between particles.
  • Net thermal energy moves from regions of higher temperature to lower temperature.
  • Solids generally conduct better than gases because their particles are much more closely packed.
  • Metals are particularly good conductors because mobile electrons help transfer energy.
  • Copper and aluminium have high thermal conductivity.
  • Air, foam, wood and many plastics have low thermal conductivity.
  • Thermal insulators reduce heat transfer; they do not completely prevent it.
  • Greater temperature difference and larger area generally increase the rate of conduction.
  • Greater thickness reduces the rate of conduction.
  • Trapped air provides useful insulation because air has low thermal conductivity.
  • Engineers use conductors when rapid energy transfer is desirable and insulators when energy transfer should be reduced.
  • Everyday applications include cookware, building insulation, clothing, vacuum flasks and electronic heat sinks.

Check Your Understanding

  1. Describe conduction using the particle model.
  2. Why is conduction generally more effective in solids than in gases?
  3. Why are metals particularly good thermal conductors?
  4. Explain why a metal object may feel colder than a wooden object even when both are at the same temperature.
  5. Why are saucepan bases often metal while their handles may be plastic?
  6. Explain why trapped air is useful in building insulation.
  7. What happens to the rate of conduction if the thickness of an insulating wall increases?
  8. A material has a very high thermal conductivity. Would it be suitable for an oven glove? Explain.
  9. Calculate the rate of conduction through a material with k = 0.20 W/(m·K), A = 5.0 m², ΔT = 15°C and L = 0.10 m.
  10. Explain why aluminium or copper is commonly used in electronic heat sinks.
 
 
 

3. Convection and Phase Change

Learning outcomes

  • I can describe convection as heat transfer through moving fluids.
  • I can explain how convection currents form because of density differences.
  • I can distinguish between boiling and evaporation.
  • I can explain why evaporation causes cooling.
  • I can identify examples of convection and evaporation in nature and everyday life.

Convection and Phase Change

What Is Convection?

Convection is the transfer of thermal energy through the bulk movement of a fluid.

A fluid is a substance that can flow, so convection occurs in:

  • liquids
  • gases

Unlike conduction, where energy passes between neighboring particles without large-scale movement of the material, convection involves the particles themselves moving from one place to another.

For example, when water is heated in a saucepan, warmer water near the bottom rises while cooler water sinks. This movement transfers thermal energy throughout the liquid.

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7

Why Convection Currents Form

Convection currents form because heating and cooling can produce density differences within a fluid.

When a fluid is heated:

  • its particles gain kinetic energy
  • the particles generally spread farther apart
  • the fluid expands
  • its density decreases

The warmer, less-dense fluid tends to rise.

At the same time, cooler fluid is usually denser and tends to sink.

This creates continuous circulation called a convection current.

The basic cycle is:

fluid heated → expands → density decreases → rises

fluid cools → contracts → density increases → sinks

The process can repeat continuously while a temperature difference exists.

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7

Density and Convection

Density describes the amount of mass within a particular volume.

ρ = m/V

where:

  • ρ = density
  • m = mass
  • V = volume

If a fixed mass of fluid expands when heated, its volume increases.

Since:

density = mass ÷ volume

an increase in volume generally means the density decreases.

This helps explain why warmer regions of a fluid can rise relative to cooler regions.


Convection in a Pot of Water

Consider a saucepan of water being heated from below.

The sequence is:

  1. The stove transfers energy to the bottom of the saucepan.
  2. Energy conducts through the metal.
  3. Water near the bottom gains thermal energy.
  4. The heated water expands and becomes less dense.
  5. The warmer water rises.
  6. Cooler, denser water moves downward.
  7. The cooler water is heated.
  8. The cycle repeats.

A circulating convection current develops.

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6

Notice that several heat-transfer processes can occur together.

stove → pan: mainly conduction

pan → nearby water: conduction

movement through water: convection


Convection in Gases

Convection also occurs in gases.

When air is heated, it generally expands and becomes less dense than the surrounding cooler air.

The warmer air rises while cooler, denser air moves downward to replace it.

This process occurs in:

  • rooms
  • the atmosphere
  • ovens
  • chimneys
  • hot-air balloons

Heating a Room

A heater warms nearby air.

The warmer air expands, becomes less dense and rises.

Cooler air moves toward the heater and is warmed.

This creates convection currents that distribute thermal energy around the room.

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4

This is one reason heaters are often positioned relatively low in a room.


Sea Breezes

Convection plays an important role in weather.

During the day, land usually warms more rapidly than nearby water.

Air above the land becomes warmer and rises.

Cooler, denser air from above the water moves toward the land to replace it.

This produces a sea breeze.

https://images.openai.com/static-rsc-4/lZJ-QUACctndVqEwLeZLVyrw0lThbO00v8akSLK3R4LyXNr_fK5-kbXXILB6wZbQnbhaWJyRcK7Q5tf14GWGXVMu-eBA9TAX1yKLY-2P4Y_m-HeCMnLaPMIEDTCDx35sUkqq03u1SkXHkb0N1Bc4A5vtIR10obytnimwDpN3lQTBu4xOvlRRFJujw55xNbW-?purpose=fullsize
 
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6

At night, the situation can reverse because land usually cools more quickly than the sea, sometimes producing a land breeze.


Convection in Earth's Atmosphere

Solar energy does not heat Earth's surface evenly.

Differences in:

  • latitude
  • surface type
  • cloud cover
  • land and water distribution

create temperature differences.

These differences contribute to large-scale atmospheric convection.

Warm air rises while cooler air sinks, helping drive:

  • winds
  • clouds
  • thunderstorms
  • weather systems

Convection is therefore important far beyond a saucepan or classroom experiment.


Hot-Air Balloons

A hot-air balloon provides another example of density differences in gases.

A burner heats the air inside the balloon.

The warmer air becomes less dense than the surrounding cooler air.

The balloon can then experience enough upward buoyant force to rise.

https://images.openai.com/static-rsc-4/Nq-_GMdIicKzWrhvV1g4_L2C26enLeLpKbJEtoEYp-q6A_Uguf7ngqYB3k2FS8aox16DRJWI4ipnmjBtwjfX-BTr76TLK5DxuMBH03ZIzoI1RBqt0JM7SCEZzTVjLDwZ0xJt2kfF2MHx3_WeDWUQEkOjN5zpfI77l6-KlOte6n3Ac01QLpjkjrlW45PufTLH?purpose=fullsize
 
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6

The balloon rises because of buoyancy resulting from the density difference, rather than because "hot air naturally wants to go upward."


Phase Changes

A phase change, or change of state, occurs when matter changes from one physical state to another.

Common phase changes include:

  • melting: solid → liquid
  • freezing: liquid → solid
  • vaporization: liquid → gas
  • condensation: gas → liquid
  • sublimation: solid → gas
  • deposition: gas → solid

During a phase change, energy can be transferred without producing an immediate change in temperature.

For example, when boiling water receives energy, much of that energy is used to separate particles rather than increase their average kinetic energy.


Vaporization

Vaporization is the general process in which a liquid becomes a gas.

There are two important forms of vaporization:

evaporation

and

boiling

These processes both convert liquid into gas, but they occur differently.


Evaporation

Evaporation occurs at the surface of a liquid.

Particles in a liquid do not all have exactly the same kinetic energy.

Some surface particles have enough energy to overcome the attractive forces holding them in the liquid.

These particles escape into the gas phase.

Evaporation:

  • occurs at the surface
  • can occur below the boiling point
  • can occur at many temperatures
  • usually happens gradually

A puddle can therefore disappear on a warm day even though the water never reaches 100°C.

https://images.openai.com/static-rsc-4/yb_1NJkk6msNtB5yxyIkfg1x_bqhZtfh6Io0sA6Cs0tOfAXEAPAQYBvhgZIDwjAP6jdbyRwzUsfqK97ORDY5hPZCG7Al21h-sjlyyStLe_XrR2V0YB7h3vaLDl8Zt0XKpjPAN4KJROW3Pb82S3JkiM3tchiQTPeB2Y-1U0taWneUT6_Xr3sxWe1QnDkxsLFa?purpose=fullsize
 
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7

Boiling

Boiling occurs throughout a liquid rather than only at its surface.

During boiling, bubbles of vapor form within the liquid and rise toward the surface.

A liquid boils when its vapor pressure becomes equal to the external pressure.

At normal atmospheric pressure, pure water boils at approximately:

100°C

However, the boiling temperature changes when external pressure changes.

At high altitudes, atmospheric pressure is lower, so water boils at a lower temperature.


Boiling vs Evaporation

The distinction between these two processes is important.

Evaporation Boiling
Occurs at the surface Occurs throughout the liquid
Can occur at many temperatures Occurs at the boiling point for a given pressure
No bubbles required within the liquid Vapor bubbles form within the liquid
Usually relatively slow Can occur rapidly
Causes cooling of the remaining liquid Requires continuous energy input to continue

Both processes involve:

liquid → gas

but the mechanisms are different.

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5

Why Evaporation Causes Cooling

Evaporation produces an important effect: evaporative cooling.

Within a liquid, particles have a range of kinetic energies.

The faster-moving particles are more likely to have enough energy to escape from the surface.

When these higher-energy particles leave, the particles remaining in the liquid have a lower average kinetic energy.

Since temperature is related to average kinetic energy:

average kinetic energy decreases → temperature decreases

The remaining liquid therefore becomes cooler.


Sweating and Evaporative Cooling

Sweating uses evaporation to help regulate body temperature.

Sweat spreads across the skin.

Some water molecules with relatively high kinetic energy escape into the air.

Energy is required for this evaporation, and thermal energy is transferred from the skin and sweat.

The skin therefore cools.

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5

Sweating is most effective when sweat can evaporate quickly.


Why Humidity Matters

On a humid day, the air already contains a large amount of water vapor.

This reduces the rate at which additional water evaporates from the skin.

As a result:

  • sweat evaporates more slowly
  • evaporative cooling becomes less effective
  • the body may feel hotter

In dry air, evaporation can occur more rapidly.

This is why the same temperature can feel very different under different humidity conditions.


Wind and Evaporation

Moving air can also increase evaporation.

Air directly above a wet surface can become rich in water vapor.

Wind carries this humid air away and replaces it with drier air.

This allows evaporation to continue more rapidly.

That is why:

  • wet clothes often dry faster on windy days
  • sweat cools the body more effectively when air moves across the skin
  • blowing across hot food can sometimes help it cool faster

Drying Clothes

Wet clothes provide a familiar example of evaporation.

Liquid water within the fabric absorbs energy and escapes into the surrounding air as water vapor.

Clothes generally dry faster when:

  • temperature is higher
  • humidity is lower
  • air movement is greater
  • more surface area is exposed
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5

This combines several thermal and environmental processes.


Evaporative Coolers

Some cooling systems deliberately use evaporation.

An evaporative cooler passes warm air across water or wet material.

As some of the water evaporates, energy is taken from the water and surrounding air.

The air temperature decreases.

These systems are particularly effective in hot, dry climates, where evaporation occurs readily.


Refrigerators and Phase Change

Refrigerators and air conditioners also make use of phase changes.

A special fluid called a refrigerant repeatedly evaporates and condenses.

When the refrigerant evaporates, it absorbs energy.

When it condenses, it releases energy.

By controlling where these phase changes occur, a refrigerator can transfer thermal energy from its cool interior to the warmer surroundings.

This requires electrical energy to operate the compressor and other components.


Clouds and Convection

Convection and phase changes frequently occur together in Earth's atmosphere.

Warm, moist air near Earth's surface can rise through convection.

As the air rises:

  • atmospheric pressure decreases
  • the air expands
  • the air cools

If it cools sufficiently, water vapor can condense into tiny liquid droplets.

These droplets form clouds.

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6

Strong convection can produce tall clouds and contribute to thunderstorms.


Convection in Earth's Interior

Convection also occurs over enormous timescales inside Earth.

Heat from Earth's interior contributes to slow movement within the mantle.

Hotter material can become less dense and move upward while cooler material moves downward.

Mantle convection is one process associated with Earth's internal heat transfer and plate tectonics.

The mantle is not simply a liquid ocean beneath the crust. Much of it is solid rock that can deform and flow extremely slowly over geological timescales.


Convection and Conduction Together

Real systems often involve more than one type of heat transfer.

Consider water boiling in a metal saucepan:

Heating element → saucepan

Energy is transferred mainly through conduction.

Saucepan → water touching the bottom

Energy initially transfers largely through conduction.

Water circulating through the pot

Energy is distributed by convection.

Water surface → surrounding air

Energy can be transferred through evaporation, convection and radiation.

Thermal processes therefore often work together rather than occurring independently.


Factors Affecting Evaporation

Several factors influence the rate of evaporation.

Temperature

Higher temperature gives particles greater average kinetic energy.

Higher temperature → generally faster evaporation

Surface Area

A larger exposed surface allows more particles to escape.

Larger surface area → faster evaporation

Air Movement

Moving air removes water vapor from above the surface.

More air movement → faster evaporation

Humidity

High humidity means the surrounding air already contains substantial water vapor.

Higher humidity → slower evaporation

These factors explain many everyday observations about drying and cooling.


Common Mistakes

Mistake: "Convection occurs in all materials."
Convection requires bulk movement, so it occurs in fluids—liquids and gases—not in ordinary rigid solids.

Mistake: "Heat rises."
It is more accurate to say that warmer, less-dense fluid may rise, carrying thermal energy with it.

Mistake: "Hot air rises because heat has an upward force."
Warmer air often rises because it is less dense than surrounding cooler air and experiences a net buoyant force.

Mistake: "Evaporation only happens when water is hot."
Evaporation can occur at temperatures well below the boiling point.

Mistake: "Boiling and evaporation are the same process."
Both are forms of vaporization, but evaporation occurs at the surface while boiling occurs throughout the liquid.

Mistake: "Evaporation cools because cold particles escape."
Higher-energy particles are more likely to escape, lowering the average kinetic energy of the remaining liquid.


Key Terms

Convection — transfer of thermal energy through the bulk movement of a fluid.

Fluid — a substance capable of flowing, including liquids and gases.

Convection current — circulating fluid motion caused by differences in density, often resulting from temperature differences.

Density — mass per unit volume.

Buoyancy — the upward effect experienced by an object or region of fluid because of pressure differences in a surrounding fluid.

Phase change — physical change from one state of matter to another.

Vaporization — change from the liquid state to the gas state.

Evaporation — vaporization occurring at the surface of a liquid.

Boiling — rapid vaporization occurring throughout a liquid when its vapor pressure equals the external pressure.

Boiling point — temperature at which a liquid boils at a particular pressure.

Condensation — change from gas to liquid.

Evaporative cooling — reduction in temperature caused when higher-energy particles escape from a liquid during evaporation.

Humidity — measure related to the amount of water vapor present in air.

Refrigerant — fluid used in refrigeration systems to transfer thermal energy through processes including evaporation and condensation.


Key Takeaways

  • Convection transfers thermal energy through the movement of liquids and gases.
  • Heating a fluid can cause it to expand and become less dense.
  • Warmer, less-dense fluid may rise while cooler, denser fluid sinks, producing a convection current.
  • Convection occurs in cooking, room heating, the atmosphere and many natural systems.
  • Evaporation and boiling are both forms of vaporization but occur differently.
  • Evaporation occurs at the surface and can happen below the boiling point.
  • Boiling occurs throughout a liquid when conditions allow vapor bubbles to form.
  • Evaporation causes cooling because higher-energy particles are more likely to escape.
  • Higher temperature, greater surface area and increased air movement generally increase evaporation.
  • Higher humidity generally decreases evaporation.
  • Sweating cools the body through evaporation.
  • Convection and phase changes work together in processes such as cloud formation, refrigeration and weather.
  • Real thermal systems commonly involve conduction, convection, radiation and phase changes simultaneously.

Check Your Understanding

  1. Describe convection using the particle model.
  2. Why can heating a fluid cause its density to decrease?
  3. Explain how a convection current forms in a saucepan of water.
  4. Why does convection not normally occur in a rigid solid?
  5. Explain the difference between boiling and evaporation.
  6. Can water evaporate at 25°C? Explain.
  7. Why does evaporation cause the remaining liquid to cool?
  8. Why does sweating usually cool the body less effectively on a humid day?
  9. Explain how convection contributes to the formation of a sea breeze.
  10. A student says, "Heat rises." Explain why saying "warmer, less-dense fluid can rise" is more scientifically accurate.
 
 
 

4. Radiation

Learning outcomes
  • I can describe radiation as heat transfer by electromagnetic waves.
  • I can explain why radiation does not require a medium.
  • I can compare conduction, convection, and radiation.
  • I can explain how surface color and texture affect heat absorption and emission.
  • I can identify examples of radiative heat transfer in everyday life.

Radiation

What Is Thermal Radiation?

Thermal radiation is the transfer of energy by electromagnetic waves.

All objects with a temperature above absolute zero emit electromagnetic radiation. For objects at everyday temperatures, much of this radiation is in the infrared region of the electromagnetic spectrum.

Unlike conduction and convection, radiation does not require particles or a material medium.

This means thermal energy can be transferred through:

  • solids
  • liquids
  • gases
  • a vacuum

The transfer of energy from the Sun to Earth is one of the most important examples of thermal radiation.

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6

Why Radiation Does Not Need a Medium

Conduction and convection depend on matter.

In conduction, energy is transferred through interactions between particles.

In convection, energy is transferred through the movement of a fluid.

Radiation is different because electromagnetic waves can travel through empty space.

This is essential for Earth.

The space between the Sun and Earth is almost a vacuum. Conduction and convection cannot effectively transfer energy across this enormous distance.

Instead:

Sun → electromagnetic radiation → Earth

Solar radiation travels approximately 150 million km through space before reaching Earth.


Electromagnetic Radiation

Electromagnetic radiation consists of oscillating electric and magnetic fields.

The electromagnetic spectrum includes:

  • radio waves
  • microwaves
  • infrared
  • visible light
  • ultraviolet
  • X-rays
  • gamma rays

All electromagnetic waves can travel through a vacuum.

For thermal physics, infrared radiation is especially important.

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Objects at everyday temperatures emit strongly in the infrared region, which our eyes cannot see.


All Objects Emit Radiation

Every object above absolute zero emits thermal radiation.

This includes:

  • people
  • buildings
  • animals
  • ice
  • tables
  • planets
  • stars

A hotter object generally emits thermal radiation at a greater rate than a cooler object of the same size and surface properties.

A hot stove therefore emits more thermal radiation than the same stove when it is cold.

Very hot objects can emit enough visible radiation to glow.

For example:

  • heated metal may glow red
  • hotter metal may appear orange or yellow
  • stars emit large amounts of visible and infrared radiation

Absorption and Emission

Objects can both absorb and emit electromagnetic radiation.

Suppose an object receives radiation from its surroundings.

Some of that radiation may be:

  • absorbed
  • reflected
  • transmitted

Absorbed radiation transfers energy to the object.

At the same time, the object emits its own thermal radiation.

Whether the object becomes warmer or cooler depends partly on the balance between the energy it absorbs and the energy it emits.


Net Radiative Heat Transfer

Imagine a warm object placed in a cooler room.

The object:

  • absorbs radiation from the room
  • emits radiation toward the room

Because the object is warmer, it generally emits energy at a greater rate than it absorbs.

Therefore, there is a net transfer of energy from the warmer object to the cooler surroundings.

As the object cools, the difference becomes smaller.

At thermal equilibrium:

energy absorbed = energy emitted

There is then no net radiative energy transfer, even though radiation continues to travel in both directions.


Infrared Cameras

Although humans cannot see infrared radiation directly, special cameras can detect it.

A thermal imaging camera detects infrared radiation emitted by objects and converts the measurements into an image.

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7

Thermal imaging is used in:

  • building inspections
  • electrical maintenance
  • firefighting
  • industrial equipment monitoring
  • scientific research
  • search and rescue

Different colours in a displayed thermal image usually represent different measured temperatures or infrared intensities. The colours themselves are often added by the imaging software.


Surface Colour and Absorption

Surface properties affect how efficiently radiation is absorbed and emitted.

For visible and infrared wavelengths relevant to many everyday situations, dark, dull surfaces are generally good absorbers.

A dark surface exposed to strong radiation often absorbs more energy than a similar light or reflective surface.

For example, consider two objects placed in sunlight:

  • one has a dull black surface
  • one has a shiny reflective surface

Under otherwise similar conditions, the black surface will generally absorb radiation more effectively.

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6

This helps explain why dark surfaces can become very hot in direct sunlight.


Surface Texture and Emission

A surface that is a good absorber of particular wavelengths is also generally a good emitter at those wavelengths.

In simplified school-level thermal physics:

dark, dull surfaces → good absorbers and good emitters

light, shiny surfaces → poorer absorbers and poorer emitters

A polished metal surface is particularly effective at reflecting infrared radiation and is therefore a poor absorber and emitter compared with a dull dark surface.


Blackbody Radiation

An idealized object called a blackbody absorbs all electromagnetic radiation that falls on it.

A blackbody is also an ideal thermal emitter.

Real objects are not perfect blackbodies, but the concept provides a useful model for understanding thermal radiation.

As the temperature of a blackbody increases:

  • the total energy emitted each second increases
  • the wavelength at which emission is strongest changes

This helps scientists understand radiation from objects such as stars, planets and heated materials.


Radiation from the Human Body

Your body constantly emits infrared radiation.

Your surroundings also emit radiation toward you.

If your surroundings are colder than your skin, your body generally emits more thermal radiation than it absorbs.

The result is a net loss of thermal energy.

This is one reason you can feel cold near a cold surface even without touching it.

Similarly, you can feel the warmth of a fire from several metres away because radiation transfers energy from the fire to your body.

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6

Feeling Heat from a Fire

Suppose you stand near a campfire.

You are not touching the flames, so conduction through direct contact cannot explain most of the warming.

Hot gases rise, so convection transfers much of the heated air upward.

Yet you can feel substantial warmth while standing beside the fire.

A major reason is:

fire → infrared radiation → your body

Your skin and clothing absorb some of this radiation and gain thermal energy.


Radiation from the Sun

The Sun has an extremely high surface temperature and emits enormous amounts of electromagnetic radiation.

This radiation travels through space and reaches Earth.

Earth absorbs part of the incoming solar radiation.

This energy:

  • warms Earth's surface
  • contributes to atmospheric processes
  • drives much of Earth's weather and climate
  • supports photosynthesis
  • powers the water cycle
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6

Without radiative energy transfer, the Sun could not warm Earth across the vacuum of space.


Shiny Surfaces and Reflection

Shiny metallic surfaces can reflect a large fraction of incident infrared radiation.

Engineers use this property when they want to reduce radiative heat transfer.

Examples include:

  • reflective building insulation
  • emergency blankets
  • vacuum flasks
  • spacecraft thermal-control surfaces

A reflective surface sends much of the incoming radiation away rather than absorbing it.


Emergency Blankets

Emergency blankets are often made from thin plastic coated with a reflective metallic layer.

The shiny surface helps reduce energy loss through thermal radiation by reflecting infrared radiation.

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6

The blanket can also affect convection by limiting air movement close to the body.

This demonstrates that real thermal systems often involve several methods of heat transfer at once.


Vacuum Flasks

A vacuum flask uses several methods to reduce heat transfer.

Vacuum

The vacuum between the walls greatly reduces:

  • conduction
  • convection

because very few particles are present.

Reflective surfaces

Shiny surfaces reduce thermal radiation by reflecting infrared radiation.

Insulating stopper

The stopper reduces conduction and convection through the opening.

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6

A vacuum alone cannot stop radiation because electromagnetic waves can travel through a vacuum.

This is why reflective surfaces are also useful.


Solar Cookers

A solar cooker uses radiation from the Sun to heat food.

Reflective surfaces direct additional solar radiation toward the cooking container.

Dark cooking surfaces absorb radiation effectively and convert the absorbed energy into internal energy.

This demonstrates two useful principles:

reflective surfaces redirect radiation

and:

dark surfaces absorb radiation effectively


Buildings and Radiation

Radiative heat transfer is important when designing buildings.

A roof exposed to sunlight can absorb substantial solar radiation.

The amount absorbed depends on factors such as:

  • surface material
  • colour
  • reflectivity
  • angle of incoming sunlight

Reflective roofing materials can reduce the amount of solar energy absorbed by a building.

Windows can also transmit solar radiation into buildings, where surfaces absorb the radiation and warm.


Conduction, Convection and Radiation

The three major mechanisms of heat transfer are different.

Feature Conduction Convection Radiation
Requires matter? Yes Yes No
Requires fluid movement? No Yes No
Can occur through vacuum? No No Yes
Main mechanism Particle interactions Bulk movement of fluid Electromagnetic waves
Common example Metal spoon heating Warm air rising Sun warming Earth

In real situations, more than one process often occurs simultaneously.


Example: A Saucepan on a Stove

Consider water being heated in a saucepan.

Conduction

Energy is conducted through the metal base of the saucepan.

Convection

Warmer water rises while cooler water sinks, producing convection currents.

Radiation

The hot stove and saucepan emit infrared radiation.

All three mechanisms may therefore operate at the same time.


Example: A House on a Cold Day

A heated house can lose thermal energy through several mechanisms.

Conduction:
Energy passes through walls, windows and the roof.

Convection:
Warm air can escape while colder air enters.

Radiation:
Surfaces emit infrared radiation toward cooler surroundings.

Good building design attempts to reduce all three forms of heat transfer.


Example: The Human Body

The human body exchanges energy with its environment in several ways.

Conduction: direct contact with another material.

Convection: moving air carries energy away from the skin.

Radiation: the body emits infrared radiation.

Evaporation: sweat removes energy as it evaporates.

This is why changing wind, humidity, clothing and surrounding temperatures can greatly affect how warm or cold a person feels.


Temperature and Radiation

Hotter objects generally emit thermal radiation more intensely.

For an ideal blackbody, the total power emitted per unit area is described by the Stefan–Boltzmann law:

P/A = σT⁴

where:

  • P = power emitted
  • A = surface area
  • σ = Stefan–Boltzmann constant
  • T = absolute temperature in kelvin

The important relationship is:

radiated power ∝ T⁴

This means radiative emission increases very rapidly as absolute temperature increases.

For example, doubling the absolute temperature would increase the ideal emitted power per unit area by:

2⁴ = 16

So the object would emit 16 times as much power per unit area, assuming ideal blackbody behaviour.


Common Mistakes

Mistake: "Radiation means only dangerous nuclear radiation."
Radiation simply means energy transmitted through waves or particles. Thermal radiation is electromagnetic radiation, commonly infrared.

Mistake: "Radiation needs air to travel."
Electromagnetic radiation can travel through a vacuum.

Mistake: "Only hot objects emit radiation."
All objects above absolute zero emit electromagnetic radiation.

Mistake: "Cold objects do not radiate."
They do. They simply emit less thermal radiation than hotter objects of similar size and surface properties.

Mistake: "A vacuum prevents all heat transfer."
A vacuum greatly reduces conduction and convection but does not prevent radiation.

Mistake: "Black objects are always hotter."
Surface colour and texture affect absorption and emission, but an object's temperature also depends on its environment and energy balance.


Key Terms

Thermal radiation — transfer of energy by electromagnetic waves resulting from the thermal motion of matter.

Electromagnetic wave — a wave consisting of oscillating electric and magnetic fields that can travel through a vacuum.

Infrared radiation — electromagnetic radiation with wavelengths longer than visible red light, strongly associated with thermal emission at everyday temperatures.

Absorption — process in which incoming radiation transfers energy to a material.

Emission — release of electromagnetic radiation by an object.

Reflection — redirection of radiation from a surface.

Blackbody — an ideal object that absorbs all incident electromagnetic radiation and is an ideal thermal emitter.

Emissivity — measure of how effectively a real surface emits thermal radiation compared with an ideal blackbody.

Thermal imaging — detection of infrared radiation to investigate temperature patterns.

Net radiation transfer — overall energy transfer resulting from the difference between radiation emitted and absorbed.

Stefan–Boltzmann law — relationship showing that ideal thermal emission per unit area is proportional to the fourth power of absolute temperature.


Key Takeaways

  • Thermal radiation transfers energy through electromagnetic waves.
  • Radiation does not require a material medium.
  • Electromagnetic radiation can travel through a vacuum.
  • The Sun transfers energy to Earth primarily through radiation.
  • Objects at everyday temperatures emit significant infrared radiation.
  • All objects above absolute zero emit thermal radiation.
  • Objects simultaneously absorb and emit radiation.
  • Net thermal energy transfer is generally from warmer objects toward cooler surroundings.
  • Dark, dull surfaces are generally good absorbers and emitters of thermal radiation.
  • Shiny metallic surfaces tend to be good reflectors and relatively poor absorbers and emitters.
  • Thermal cameras detect infrared radiation emitted by objects.
  • A vacuum reduces conduction and convection but does not stop radiation.
  • Real thermal systems often involve conduction, convection and radiation simultaneously.
  • Increasing absolute temperature greatly increases the rate of thermal radiation emitted.

Check Your Understanding

  1. What is thermal radiation?
  2. Why can radiation transfer energy through empty space?
  3. Why cannot conduction transfer energy from the Sun to Earth?
  4. What region of the electromagnetic spectrum is especially important for thermal radiation at everyday temperatures?
  5. Why can you feel heat from a fire without touching it?
  6. Compare conduction, convection and radiation in terms of whether each requires matter.
  7. Why are shiny surfaces used inside some vacuum flasks?
  8. Which would generally absorb radiation more effectively: a dull black surface or a polished metallic surface?
  9. Explain why a thermal camera can detect a person in darkness.
  10. A student says, "A vacuum flask prevents all heat transfer because there are no particles in the vacuum." Explain why this statement is incomplete.

5. Applications of Heat Transfer

Learning outcomes
  • I can identify situations where conduction, convection, and radiation occur together.
  • I can explain how insulation reduces heat transfer.
  • I can describe how heat transfer is used in buildings, cooking, and engineering.
  • I can explain how evaporation can cool objects and living organisms.
  • I can evaluate methods of improving thermal efficiency in practical applications.

Applications of Heat Transfer

Heat Transfer in Real Systems

In most real situations, conduction, convection, and radiation occur at the same time.

The dominant method depends on:

  • the materials involved
  • whether liquids or gases can move
  • temperature differences
  • surface properties
  • the surrounding environment

For example, when cooking food in an oven:

  • conduction transfers energy through the baking tray and through the food
  • convection transfers energy through moving hot air
  • radiation transfers energy from the hot heating elements and oven surfaces

Understanding how these processes work together allows engineers to either increase heat transfer when it is useful or reduce it when energy needs to be conserved.

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5

Thermal Efficiency

Thermal efficiency describes how effectively a system uses transferred thermal energy for its intended purpose.

In many systems, some energy is transferred to places where it is not useful.

For example, when heating a house:

useful transfer: heating the rooms

unwanted transfer: thermal energy escaping through walls, windows, doors and the roof

Improving thermal efficiency usually means:

  • increasing useful energy transfer
  • reducing unwanted energy transfer
  • reducing energy consumption
  • reducing operating costs

The exact solution depends on the purpose of the system.

A saucepan should transfer energy quickly into food, while a thermos should transfer energy as slowly as possible.


Insulation

Thermal insulation reduces the rate of unwanted heat transfer.

Insulation does not completely stop energy transfer. Instead, it makes the transfer occur more slowly.

Effective insulation may reduce:

  • conduction
  • convection
  • radiation

Different methods are required for each mechanism.


Insulation and Conduction

Conduction can be reduced by using materials with low thermal conductivity.

Common thermal insulators include:

  • fibreglass
  • foam
  • wool
  • wood
  • plastic
  • cork
  • trapped air

Many insulating materials contain numerous small air pockets.

Air is a poor thermal conductor, so trapping air can greatly reduce conduction.

The air must remain relatively still because moving air could establish convection currents.

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Insulation and Convection

Convection requires the movement of a fluid.

It can therefore be reduced by preventing air or other fluids from circulating.

Examples include:

  • trapping air inside foam
  • using several layers of clothing
  • sealing gaps around windows
  • using lids on containers
  • creating narrow air spaces

A large open air space can allow convection currents to develop.

Many small trapped air pockets are generally much more effective because they restrict the movement of air.


Insulation and Radiation

Radiative heat transfer can be reduced using reflective surfaces.

Shiny metallic surfaces reflect much of the infrared radiation reaching them.

They are therefore used in:

  • vacuum flasks
  • reflective building insulation
  • emergency blankets
  • some spacecraft
  • thermal barriers

A reflective surface is particularly useful when radiation is an important heat-transfer mechanism.


Heat Transfer in Buildings

Buildings provide an excellent example of conduction, convection and radiation operating together.

A heated building can lose thermal energy through:

Conduction: through walls, windows, floors and the roof.

Convection: through moving air, ventilation and gaps around doors or windows.

Radiation: from warm surfaces toward cooler surroundings.

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Reducing these transfers can significantly improve a building's thermal efficiency.


Roof and Wall Insulation

Warm air inside a building can transfer energy to walls and ceilings.

Insulating materials slow the conduction of energy through these structures.

A thicker insulating layer generally provides greater thermal resistance.

Materials such as:

  • fibreglass
  • mineral wool
  • cellulose
  • rigid foam

are commonly used because they have low thermal conductivity.

Good insulation means heating or cooling systems do not need to operate as frequently to maintain a comfortable indoor temperature.


Double and Triple Glazing

Windows can be an important route for heat transfer.

A double-glazed window contains two panes of glass separated by a sealed gap.

The gap usually contains air or a gas such as argon.

The gas has relatively low thermal conductivity and is trapped so that large convection currents cannot develop.

Triple glazing adds another pane and insulating gap.

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8

Some energy-efficient windows also have special coatings that reduce radiative heat transfer.


Draught Proofing

Small gaps around:

  • doors
  • windows
  • pipes
  • vents

can allow warm indoor air to escape and cooler outdoor air to enter.

This increases energy transfer through air movement.

Draught proofing seals unnecessary gaps and reduces this exchange.

However, buildings still require appropriate ventilation for indoor air quality and moisture control.

Thermal efficiency therefore involves balancing several practical requirements.


Reflective Building Materials

Buildings exposed to strong sunlight can gain substantial energy through radiation.

Light-coloured or reflective roofs can reflect more incoming solar radiation and reduce heat absorption.

This can reduce the amount of energy needed for air conditioning in hot climates.

The best building design therefore depends partly on climate.

A design intended to retain thermal energy in a cold environment may differ from one intended to reduce solar heating in a hot environment.


Cooking

Cooking requires thermal energy to be transferred into food efficiently and safely.

Different cooking methods use different combinations of heat-transfer mechanisms.


Cooking on a Stove

Consider a metal saucepan containing water.

Energy travels through several stages:

stove → saucepan → water → food

Conduction

The metal pan conducts energy from the stove.

Convection

Heated water rises while cooler water sinks, establishing convection currents.

Radiation

Hot stove surfaces and the pan emit infrared radiation.

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6

The cookware is deliberately designed to manage these transfers.


Why Cookware Uses Different Materials

The base of a saucepan should conduct energy efficiently.

Materials such as:

  • aluminium
  • copper
  • steel

are therefore commonly used.

The handle has a completely different purpose.

We want to reduce:

hot pan → hand

Handles may therefore contain:

  • plastic
  • wood
  • silicone
  • other insulating materials

One object can therefore contain both a thermal conductor and thermal insulator, depending on the purpose of each part.


Convection Ovens

A convection oven contains a fan that circulates hot air.

Moving hot air increases energy transfer between the air and food.

This can:

  • reduce cooking time
  • produce more even heating
  • reduce large temperature differences within the oven
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7

Forced convection is also widely used in engineering whenever faster heat transfer is desirable.


Lids and Thermal Efficiency

Placing a lid on a cooking pot can improve efficiency.

A lid reduces:

  • convection from the water surface
  • evaporation
  • escape of warm water vapor

Less energy is transferred to the surroundings.

Therefore, less energy may be required to maintain the desired cooking temperature.

This is a simple example of improving thermal efficiency without changing the heat source.


Evaporation and Cooling

Evaporation can be deliberately used to cool objects and organisms.

During evaporation, higher-energy particles are more likely to escape from the surface of a liquid.

The remaining particles have a lower average kinetic energy.

Therefore:

evaporation → energy removed → cooling


Sweating

Humans use evaporative cooling to regulate body temperature.

Sweat glands release water onto the skin.

As the water evaporates, energy is required to separate the water molecules and allow them to enter the gas phase.

This energy comes partly from the skin.

The skin therefore loses thermal energy and cools.

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6

Sweating works most effectively when evaporation occurs rapidly.


Why Humidity Affects Cooling

High humidity reduces the rate of evaporation because the surrounding air already contains substantial water vapor.

As a result:

high humidity → slower evaporation → less evaporative cooling

This is one reason hot, humid conditions can feel particularly uncomfortable.

Moving air can have the opposite effect.

Wind or a fan removes humid air close to the skin and replaces it with less humid air.

This can increase evaporation.


Evaporative Cooling in Animals

Many animals also use evaporation for temperature regulation.

Dogs, for example, have relatively limited sweating compared with humans.

Instead, they can increase evaporation from moist surfaces of the mouth and respiratory system by panting.

Some animals use other strategies involving:

  • sweating
  • panting
  • licking their bodies
  • spreading water across body surfaces

All of these can increase evaporative heat loss.


Evaporative Coolers

An evaporative cooler deliberately evaporates water to cool air.

Warm, dry air passes across water or wet material.

Water evaporates and absorbs energy.

The outgoing air becomes cooler.

These systems can be effective in hot, dry environments but are less effective when humidity is already high.


Refrigerators

A refrigerator is designed to transfer thermal energy from a cold interior to warmer surroundings.

This does not happen spontaneously. Electrical energy is used to operate the system.

A refrigerant circulates through the refrigerator and repeatedly changes pressure and state.

In simplified terms:

inside refrigerator: refrigerant absorbs energy

outside refrigerator: refrigerant releases energy

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The coils at the back or underneath a refrigerator can become warm because energy removed from inside the refrigerator, plus energy supplied to the system, is ultimately released into the room.


Heat Sinks and Electronics

Electronic devices generate thermal energy during operation.

Excessive temperature can:

  • reduce performance
  • shorten component life
  • damage electronics

A heat sink transfers energy away from components such as processors.

Heat sinks are often made from aluminium or copper because these materials conduct thermal energy effectively.

Fins increase the surface area available for energy transfer to the surrounding air.

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8

A cooling fan can then increase convection.

The sequence may be:

processor → conduction → heat sink → convection → surrounding air

Radiation also contributes a smaller amount of energy transfer.


Car Engines

Vehicle engines produce large quantities of thermal energy.

Too much heat could damage engine components.

A cooling system therefore transfers thermal energy away from the engine.

Typically:

  1. Coolant absorbs energy from the engine.
  2. The heated coolant flows to the radiator.
  3. Energy conducts through the radiator material.
  4. Air moves across the radiator.
  5. Convection transfers energy to the surrounding air.

Radiators contain many thin fins to increase surface area.

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8

This is another example where good engineering means increasing, rather than reducing, heat transfer.


Vacuum Flasks

A vacuum flask is designed to do the opposite: minimize energy transfer.

It uses several methods simultaneously.

Vacuum

Reduces conduction and prevents convection between the walls.

Reflective surfaces

Reduce radiative energy transfer.

Insulating stopper

Reduces conduction and prevents air circulation through the opening.

Narrow neck

Reduces the area through which energy can escape.

A good thermal design therefore targets each possible heat-transfer pathway.


Thermos vs Radiator: Different Goals

Thermal efficiency does not always mean reducing heat transfer.

Consider two devices.

Vacuum Flask

Goal:

minimize heat transfer

Therefore engineers use:

  • insulation
  • vacuum
  • reflective surfaces

Car Radiator

Goal:

maximize heat transfer

Therefore engineers use:

  • conductive metals
  • large surface area
  • flowing coolant
  • moving air

The "best" thermal design depends on what the system is supposed to accomplish.


Improving Thermal Efficiency

Engineers can improve thermal performance in several ways.

Method Effect
Low-conductivity insulation Reduces conduction
Trapped air Reduces conduction and convection
Vacuum Greatly reduces conduction and prevents convection
Reflective surface Reduces radiative transfer
Double/triple glazing Reduces heat transfer through windows
Draught proofing Reduces unwanted air movement
Increased surface area Increases heat transfer when cooling is desired
Fans Increase forced convection
Conductive metals Increase conduction
Lids on containers Reduce convection and evaporation
Evaporation Provides cooling

The correct method depends on whether the goal is to retain thermal energy or remove it.


Evaluating a Thermal Design

Suppose an engineer wants to improve the insulation of a house.

Simply choosing the thickest insulation may not automatically be the best solution.

The engineer might consider:

  • thermal conductivity
  • insulation thickness
  • installation cost
  • durability
  • moisture resistance
  • fire safety
  • environmental impact
  • expected energy savings

A useful solution should therefore be evaluated according to both thermal performance and practical considerations.


Worked Example: Improving a House

A house loses significant thermal energy through its roof and windows.

Possible improvements include:

Roof insulation: reduces conduction.

Double glazing: reduces conduction and convection through the windows.

Reflective coatings: can alter radiative heat transfer.

Draught proofing: reduces unwanted air movement.

Suppose roof insulation is inexpensive and greatly reduces energy loss, while replacing every window is much more expensive for a smaller improvement.

The insulation may provide the better cost-to-benefit ratio.

Engineering decisions often involve such trade-offs rather than simply choosing the technology with the greatest theoretical performance.


Common Mistakes

Mistake: "Insulation stops heat transfer."
Insulation reduces the rate of heat transfer. It does not normally eliminate it.

Mistake: "Thermal efficiency always means preventing heat transfer."
Sometimes efficient design requires increasing heat transfer, as in radiators and heat sinks.

Mistake: "A vacuum stops all heat transfer."
A vacuum greatly reduces conduction and convection but electromagnetic radiation can still travel through it.

Mistake: "A fan makes air cold."
A fan mainly moves air. This can increase convection and evaporation, increasing the rate at which energy leaves a warm surface.

Mistake: "Sweat cools the body simply because sweat is cold."
The major cooling effect occurs when sweat evaporates.

Mistake: "Only one type of heat transfer occurs at a time."
Conduction, convection and radiation commonly occur simultaneously.


Key Terms

Thermal efficiency — measure of how effectively a system uses or controls thermal energy for its intended purpose.

Thermal insulation — materials or methods used to reduce the rate of unwanted heat transfer.

Thermal conductivity — measure of how effectively a material conducts thermal energy.

Conduction — energy transfer through particle interactions without bulk movement of matter.

Convection — energy transfer through the bulk movement of a fluid.

Thermal radiation — energy transfer by electromagnetic waves.

Evaporation — escape of particles from the surface of a liquid into the gas phase.

Evaporative cooling — cooling caused when higher-energy particles escape during evaporation.

Heat sink — device designed to transfer thermal energy away from a component.

Radiator — device designed to transfer thermal energy efficiently to its surroundings.

Double glazing — two panes of glass separated by an insulating gas layer.

Draught proofing — sealing unwanted gaps to reduce air movement and energy transfer.

Forced convection — convection enhanced by devices such as fans or pumps.

Reflective insulation — material designed to reduce radiative heat transfer by reflecting electromagnetic radiation.


Key Takeaways

  • Conduction, convection and radiation commonly occur together in real thermal systems.
  • Insulation reduces unwanted heat transfer rather than completely stopping it.
  • Low-conductivity materials reduce conduction.
  • Trapped air can reduce both conduction and convection.
  • Reflective surfaces can reduce radiative heat transfer.
  • Building insulation, glazing and draught proofing can reduce energy consumption.
  • Cooking systems deliberately use conduction, convection and radiation to transfer energy into food.
  • Lids can improve cooking efficiency by reducing convection and evaporation.
  • Evaporation cools surfaces because higher-energy particles escape from the liquid.
  • Sweating uses evaporation to help regulate body temperature.
  • High humidity reduces the effectiveness of evaporative cooling.
  • Heat sinks and radiators are designed to increase heat transfer.
  • Vacuum flasks are designed to decrease heat transfer.
  • Improving thermal efficiency requires identifying the important heat-transfer pathways and choosing appropriate methods to control them.
  • Practical engineering decisions must also consider factors such as cost, safety, durability and environmental impact.

Check Your Understanding

  1. Give an example in which conduction, convection and radiation occur at the same time.
  2. Why does trapped air make a useful thermal insulator?
  3. Explain how double glazing reduces heat transfer through a window.
  4. Why can reflective surfaces improve thermal insulation?
  5. Explain why a saucepan might have a metal base but a plastic handle.
  6. How does a convection oven increase the rate of heat transfer to food?
  7. Why does sweating cool the human body?
  8. Why is evaporative cooling less effective in humid conditions?
  9. Explain how a heat sink and fan work together to cool a computer processor.
  10. A designer can choose between making an insulating wall thicker or using a material with lower thermal conductivity. Explain how either change could reduce heat transfer.
  11. Why does putting a lid on a saucepan usually improve its thermal efficiency?
  12. Compare a vacuum flask and a car radiator. Explain why one is designed to minimize heat transfer while the other is designed to maximize it.