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Heat Transfer

Thermal energy can be transferred by conduction, convection, and radiation.

Thermal energy

Thermal energy

  • If there is a temperature difference between objects, heat will transfer.
  • A common misconception is that heat travels ‘up’. This is wrong.
  • Heat transfers from a hotter object to a colder object.
  • The greater the temperature difference, the faster the transfer of heat.
  • Heat transfer will stop when both objects are the same temperature.
  • Other factors that affect the thermal energy transfer rate include:
    • The surface area.
    • The material.
  • There are three ways in which heat is transferred.
Radiation

Radiation

  • All objects emit infrared radiation.
  • The hotter the object is, the more radiation it emits.
  • Radiation does NOT need particles, so it can travel through a vacuum.
  • Space is a vacuum and we can feel the Sun's radiation.
  • Infrared radiation is part of the electromagnetic spectrum.
  • Dark-matt surfaces are the best emitters and absorbers of radiation.
  • Shiny surfaces reflect radiation.
  • Thermal imaging cameras use infrared radiation to take photographs.
  • You feel the heat of a light bulb by radiation.
Conduction

Conduction

  • Conduction occurs when particles in a solid are heated.
  • If a substance is able to conduct heat well, such as a metal, it is a good conductor of heat.
  • If a substance is unable to conduct heat well, such as plastic or newspaper, it is a poor conductor or an insulator.
    • Plastic insulation is wrapped around electrical wires to prevent electric shocks.
How conduction works

How conduction works

  • As particles are heated, they gain energy and vibrate more.
  • As they vibrate, they collide and so transfer energy to the next particle.
  • Examples of this can be seen if you leave a cold spoon in a hot cup of tea:
    • The spoon will become hot.
  • Pans become hot when you are cooking due to conduction.
  • A snowball will melt in your hand.
Convection

Convection

  • Convection occurs when particles in a fluid (liquids or gases) are heated.
  • As particles are heated, they gain energy.
    • As they gain energy, they move around more and so take up more space and become less dense.
  • Less dense fluid will rise and be replaced by more dense fluid.
  • Examples are:
    • A radiator.
    • Central heating.
    • Convection currents causing wind.
    • The movement of the mantle inside the Earth.
Heat transfer

Heat transfer

  • No heat transfer is ever 100% efficient.
  • You will always lose heat from an object.
  • We say that this heat is 'dissipated' into the surroundings.
    • The heat is transferred to the air around you by convection, conduction, and radiation.
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