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.
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.
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.
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.
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.
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.
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
- In which direction does thermal energy naturally transfer between objects at 70°C and 25°C?
- Define thermal equilibrium.
- Why does a hot drink eventually approach room temperature?
- Explain the difference between heat and temperature.
- Why does a thermometer need time to give an accurate reading?
- Two objects are both at 35°C and are placed in contact. Is there a net heat transfer between them? Explain.
- Why can energy be transferred into melting ice without increasing its temperature?
- Explain why insulation slows the approach to thermal equilibrium but does not prevent it indefinitely.
- 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.
- 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.
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.
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.
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.
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.
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.
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.
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
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.
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.
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
- What is thermal radiation?
- Why can radiation transfer energy through empty space?
- Why cannot conduction transfer energy from the Sun to Earth?
- What region of the electromagnetic spectrum is especially important for thermal radiation at everyday temperatures?
- Why can you feel heat from a fire without touching it?
- Compare conduction, convection and radiation in terms of whether each requires matter.
- Why are shiny surfaces used inside some vacuum flasks?
- Which would generally absorb radiation more effectively: a dull black surface or a polished metallic surface?
- Explain why a thermal camera can detect a person in darkness.
- 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.