Model of a Well

Grade Level: K-4


Source: Nebraska Earth Systems Education Network, School of Natural Resources
By Marianne Bonnemier

Background

Groundwater is contained in the zone of saturation below the land surface. The top of this zone is known as the water table. People can tap into this source of water by drilling wells. The depth of the well and level of the water table greatly influences the wells productivity.

Objective

Demonstrate the relationship of groundwater to wells.

Materials

Pencil, fine wire screening, small wire for fastening, medicine dropper, drinking glass, water, coarse sand, and food coloring (optional).

Procedure:

  1. Roll a piece of screening around a pencil to make a cylinder.
  2. Enlarge the cylinder to approximately 1 cm in diameter. Fasten cylinder with a piece of wire around it to keep it from unrolling.
  3. Place the cylinder upright in a glass with sand, keeping the sand out of the cylinder.
  4. Pour water into the sand. The sand will take up water, but the water will also go into the cylinder--the well.
  5. Remove water from the well with the medicine dropper.
  6. After you remove water from the cylinder (your well), notice the level of water in the sand. Your well will also be lower at first but will eventually fill up again.
  7. Add more water to your sand and observe your well.
  8. Observe your well and record your observations in number 1 in the conclusion.

Conclusion

Observations from step 8 in the procedure.

Extending the Concept