Skip to content
Exit presentation

Heat Transfer in Nature

Water seeping into the ground

Rain falls on a field. Some of it disappears into the ground. Where does it go?

Loading lab…

The idea

Rain falls on the ground.
Step 1 of 5
  1. Rain falls on the ground.
  2. It seeps (soaks slowly) down through soil and rock. This is infiltration.
  3. It fills the gaps of an underground layer. This layer is an aquifer.
  4. A well reaches the aquifer. We draw water from it.
  5. A recharge pit lets rain soak in and refill the aquifer.

The rain soaks down and fills an underground layer.

Gravel is made of small stones. Gravel lets water through fastest. Sand is slower. Clay is slowest. Wide gaps let water through faster. These rules are for packed ground.

Packed ground is pressed down firmly.

Water stored in an aquifer is groundwater. Pumping means taking water out with a pump. Pumping out more water than rain refills can empty the aquifer.

Jump to lesson

This track

  1. 0 Start here
  2. 1 Heat and temperature are different
  3. 2 Heat moves from hot to cold
  4. 3 Through a solid: conduction
  5. 4 In liquids and gases: convection
  6. 5 Across empty space: radiation
  7. 6 Three ways, every day
  8. 7 Checkpoint: how heat moves
  9. 8 The water cycle
  10. 9 Water seeping into the ground
  11. 10 Sea breeze and land breeze
  12. 11 Ice stupas
  13. 12 Checkpoint: water, breezes and ice
  14. 13 The big picture
  15. 14 Track quiz

Other tracks