Skip to content
Dabour HubLEARN · PRACTICE · EXPLORESign inStudent

4.1.2Atomic Structure

The Absorption and Emission of EM Radiation — AQA GCSE Combined Science Trilogy 8464 - Physics Revision Notes & Topical Questions

5 min read 7 parts Lesson 3 of 23

🩺
100% Curriculum Specification Match Lesson Doctor Verified
The only platform with 100% curriculum specification match and verified interactive question banks.
0%read

Part 1 of 5Emission and absorption

All objects emit
  • All objects emit Every object emits infrared radiation, and the hotter the object, the more radiation it emits each second.
All objects absorb
  • All objects absorb Objects also absorb radiation from their surroundings.
Net effect
  • Net effect An object hotter than its surroundings emits more than it absorbs, so it cools.
    • A cooler object absorbs more than it emits, so it warms.
Steady temperature
  • Steady temperature When absorbing and emitting at the same rate, the temperature remains constant.

Part 2 of 5Effect of surface

SurfaceAbsorption of infraredEmission of infraredReflection
Matt blackBest absorberBest emitterPoor
Dull darkGoodGoodPoor
Shiny white or silverPoor absorberPoor emitterBest reflector

Part 3 of 5Earth's temperature

1Sun's radiation arrives
  • Sun's radiation arrives Short-wavelength radiation passes through the atmosphere and warms the surface.
2Surface re-emits
  • Surface re-emits Earth emits longer-wavelength infrared radiation back towards space.
3Gases absorb some
  • Gases absorb some Greenhouse gases such as carbon dioxide and methane absorb part of this infrared radiation.
4Balance shifts
  • Balance shifts More greenhouse gas means more radiation is retained, so the average temperature rises.

Part 4 of 5Radiation and atoms

1
When radiation is absorbed, electrons in the atom can gain energy and move to a higher energy level.
2
If the energy is large enough, an electron leaves the atom entirely and the atom becomes a positive ion.
3
When electrons drop back to lower energy levels, they emit electromagnetic radiation.
4
Higher frequency radiation such as ultraviolet, X-rays and gamma can ionise atoms.

Part 5 of 5Investigating emission (practical idea)

Comparing surfaces
Set-up
  • Set-up Use identical containers (Leslie cubes) of hot water, each with a different surface colour or finish.
Measurement
  • Measurement Place an infrared detector the same distance from each side and compare the readings.
Control
  • Control Keep the water temperature, distance and detector the same;
    • the matt black surface gives the highest reading.

Key terms

TermMeaning
Infrared radiationElectromagnetic radiation emitted by all objects due to their temperature.
AbsorberA surface that takes in radiation, increasing the energy of the object.
EmitterA surface that gives out radiation.
Greenhouse gasA gas in the atmosphere that absorbs infrared radiation from Earth.
IonisationThe removal of an electron from an atom, creating an ion.

Avoid these mistakes

1
Saying only hot objects emit infrared; all objects do, although cold ones emit much less.
2
Thinking shiny surfaces are the best emitters — they are poor emitters and absorbers but good reflectors.
3
Claiming greenhouse gases block the Sun's radiation from reaching Earth; they absorb the infrared leaving it.
4
Confusing reflection with emission when explaining why a silver surface stays cooler.

Last updated: