Percolation is the movement of water through soil, and the percolation rate is the speed at which that movement occurs. Percolation tests, or perc tests, measure percolation rates. Soil laboratory professionals usually measure percolation rates in terms of minutes per inch, typically in the context of septic tank testing. Many do-it-yourself tests, however, measure percolation rates in terms of inches per hour, which is perfectly adequate for garden care. You can use percolation rates to make various soil and plant selection and management decisions for your garden and yard.
Soil percolation is related to, but distinct from, soil infiltration. Although percolation is the movement of water through soil, infiltration is the movement of water into soil. A third term, permeability, describes both a soil's infiltration and percolation.
Percolation Rate by Soil Category
Percolation speed depends greatly on the soil type.
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- Sandy soils usually have very high percolation rates, measured in the range of 1 to 8 inches or more per hour. That means sandy soils dry out very quickly, heat up very quickly and do not hold nutrients for very long.
- Silty soils, including loam, have moderate percolation speeds, ranging from 0.1 to 1 inch per hour. This is the "Goldilocks" situation, in which a soil holds water and nutrients long enough for plant roots to absorb them, but the soil does not easily become waterlogged.
- Clay soils have notoriously slow percolation speeds of 0.1 inch or less per hour. These soils easily become waterlogged, and plant roots can suffocate as a result.
Any soil can vary significantly from the percolation rate averages. This variation can be due to issue that include soil compaction, organic matter content and/or soil temperature. Yet soil types are by far the single biggest determinant for percolation rates.
Percolation Rate Measurement
You can estimate percolation speed based on general knowledge of your soil's type and/or through casual observation of how well it drains. You also, however, can easily do a simple percolation test to determine a more precise percolation rate.
Things You'll Need
Yardstick or tape measure
Bucket or hose
Wooden board, several feet long
Wristwatch or clock
Step 1: Dig the Test Hole
Dig a hole in the desired soil percolation rate testing area. The hole should be 18 to 24 inches deep by 12 inches wide. If the testing area is large, dig several holes, spacing them throughout the area.
Step 2: Saturate the Test Hole
Fill the test hole, or holes, with water, and wait for the water to drain into the soil. The water may drain relatively rapidly, in less than one hour, or it may take a number of hours to drain.
Step 3: Refill the Hole
Ensure the water has drained completely, and refill each hole with water up to within 1 inch of its top.
Step 4: Measure the Initial Water Level
Lay a wood board that is several feet long across the top of each hole. The board is the measuring baseline. Insert a yardstick or tape measure to the hole's bottom. Measure the distance from the measuring baseline -- the board -- to the water level. Write down this initial distance in a notebook along with the current time. Leave the board in position for subsequent measurements. Remove the yardstick or tape measure.
Step 5: Measure the Water Level Change
Return to the test hole in 30 minutes, and insert the yardstick or tape measure to the hole's bottom. Measure the new distance from the board to the water level. Write down that measurement along with the current time.
Step 6: Repeat Measurements
Continue to measure the distance between the water level and the board every 30 minutes for at least three additional measurements. Write down each new measurement and the time it was taken. After taking several measurements, determine how much the water level dropped between each measurement. The amount of change per hour is the soil's percolation rate. If, for instance, the water level dropped an average of 1 inch every 30 minutes, then the percolation rate would be 2 inches per hour.
Percolation Rate Modifications
You can change you particular soil's percolation speed to provide better growing conditions for plants. If the soil drains too quickly, then mix it with loam, compost or even clay to slow percolation. For soil that drains too slowly, add loam, compost or sand. Incorporating compost aids either situation by adding organic content.
Modifying percolation speed by adding sand, clay, compost or loam can be done all at once prior to installing a garden. If a garden already has plants, then apply thin sheets of compost as a top-dressing -- on the soil surface -- each year. That method will slowly but steadily improve the soil's percolation speed over time as the compost works into the soil.
- Bartlett Tree Research Laboratories: Technical Report -- Soil Drainage
- The Lawn Institute: Soil Types Make a Difference in Lawn Irrigation
- Today's Homeowner with Danny Lipford: DIY Soil Drainage Perk Test for Your Yard
- Iowa Storm Water Education Program et al.: Rain Gardens -- Iowa Rain Garden Design and Installation Manual
Kathryn Kerby has been gardening, farming and/or ranching since the 1980s. She currently owns and manages Frog Chorus Farm in Washington state. Ms. Kerby has written extensively about gardening and sustainable agriculture, with articles in Permaculture Today and various sustainability newsletters. She is author of "The Chicken Coop Manual."