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Groundwater Movement: Porosity and Permeability

Goal: To discover the rates at which water moves through different types of soils.

Definitions:

Permeability: The capability of rock or soil to transmit water.

Porosity: The degree to which the total volume of soil or rock is permeated with spaces or cavities through which water or air can move.

SOIL TYPE Time water
is poured
Time of
first drop
Appearance Amt. of water
at 2 minutes
SAND
GRAVEL
CLAY



1.

Which soil sample is the most permeable (allows water to flow through the fastest)?

2.

Which soil sample is the least permeable?

3. If you mixed the gravel and clay together, would the rate of water moving through the soil be faster or slower than the clay alone?
4.

Which soil retained the most water after 2 minutes (the most porous)?

5.

If it took 30 seconds for 7 ml of water to pass through the clay, how many ml would pass through in one hour?

6.

Can soil type protect groundwater? How? Which one?

7.

If an accidental chemical spill ocurred in an area of sandy soils, would there be a potential for groundwater contamination? If the same spill occurred in an area of clay soils, would you expect to see any difference?

ACTIVITY

Purpose: To demonstrate that water percolates through soils with different grain sizes at different rates.

Materials Needed:

  • Five plastic columns, 100 cm long and 5 cm in diameter.
  • Five guaze pads and rubber bands.
  • Five beakers to catch the water that percolates through each column.
  • Samples of clay, course sand, fine sand, gravel, and top soil.
  • Or five gradulated sizes of plastic beads, about 2 cups of each.
  • A stopwatch

Procedure:

  1. Secure a guaze pad to the bottom of each column with a rubber band.
  2. Place different soil sample or size of bead in each column until the column is about ½ full. Make sure all columns are filled to the same level.
  3. Pour 100 mL of water through the columns, one by one.
  4. Time the passage of the water through each column.
  5. Measure the amount of water that passes through each column.
  6. If using soil samples, note the color of the water in the collection beaker.

    Questions for Discussion:

    • Did the water go through all of the columns at the same rate?
    • If no, why not?
    • Describe the relationship between the rate at which water passes through the soil and the size of its grains.




 

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