The soil type on your property is an important factor in determining how fast and how often water can be applied to the plant material.
Soil absorbs and holds water in much the same way as a sponge. A given texture and volume of soil will hold a given amount of moisture. The intake rate of the soil will influence the precipitation rate and type of sprinkler that can be used. The ability of soil to hold moisture, and the amount of moisture it can hold, will greatly affect the irrigation schedule.
Soil is made up of sand, silt and clay particles. The percentage of each of these three particles is what determines the actual soil texture. Because the percentage of any one of these three particles can differ, there is virtually an unlimited number of soil types possible.
The simplest way to determine the soil type is to place a moistened soil sample in your hand and squeeze. Take the sample from a representative part of the site, and from approximately the same depth to which you will be watering. In other words, if you want to water to a depth of 6 in (15 cm), dig down 6 in (15 cm) to take your soil sample.
The Jar Test
A more accurate way to determine the amount of sand, silt and clay in your soil is to conduct the jar test.
1. Remove 1 to 2 cups of soil from the zone to be irrigated.
2. Place into a glass jar, like a mason jar.
3. Fill the jar half way with water. Shake and let sit for
2 hours so the particles can settle. The heavier sand particles
will settle to the bottom, then silt, then clay on top.
4. Measure the height of all 3 layers of the soil then the height
of each layer; divide the height of each layer by the total
height to figure out the percentage of each soil in the jar.
5. Apply these figures to the “Soil Classification” chart. In the example, now you know the landscape soil is silt loam.
One of the most significant differences between different soil types is the way in which they absorb and hold water. Capillary action is the primary force in spreading water horizontally through the soil. Both gravity and capillary action influence vertical movement of water. In coarser soils, water is more likely to be absorbed vertically, but will not spread very far horizontally. The opposite is true for finer soils.
The table below lists the general characteristics of the three main soil types.
Look particularly at the information in the last three columns. The soil’s intake rate, or how fast it absorbs water, dictates how quickly water can be applied by the irrigation system. Coarse, sandy soil absorbs water very quickly while silts and clays have a very low intake rate. The fine textured soils, once wet, retain moisture longer than do the coarse grained soils. The main problem we wish to avoid is applying water faster than the soil can receive it. This causes runoff, erosion or soil puddling, all of which waste water and can cause damage.
Rolling terrain further complicates the problem of matching the application rate from the sprinklers with the intake rate of the soil. As the angle of slope increases, the intake rate decreases because of the higher potential for runoff.