Sand-based athletic fields

Sand-based athletic fields are sporting grounds constructed on sand, which have certain advantages over those built on native soils. Highly maintained areas of turf, such as those on an athletic field or on golf greens and tees, can be grown in native soil or sand-based systems. There are advantages and disadvantages to both that need to be considered before deciding what type of soil to grow turf in. Native soils offer many positive qualities, such as high nutrient holding capacity, water holding capacity, and sure footing. However, native soil fields are typically very poorly drained. This causes problems with growing turf and maintaining a safe surface for players. Sand-based systems provide all of the above qualities, and also improved drainage. They allow the turf manager better control over moisture management and resist soil compaction.

Construction

Sand-based systems are composed of a sand-based root zone, a gravel layer, and a drainage system. Although the root zone of a sand-based system is mostly sand, amendments are often added to increase the organic matter content and add stability to the root zone. Peat moss is the most common root zone amendment used, but other inorganic amendments can also be used. Peat moss is used because it increases water and nutrient holding capacity and decreases bulk density. The most common ratio of sand to peat moss is 8:2. This ratio will allow a water holding capacity of 15 to 26% and increase nutrient holding capacity greatly (Kussow, 1987).

100% sand root zones are used often and are more cost effective. Selection of the type of sand is very crucial. Sand suitable for a root zone should be a medium to coarse (0.15-1.0 mm) particle size and should have sub-angular or sub-rounded shape. If sub-angular sand is chosen, it can deter some insects from making their homes in the soil. The shape makes it harder for them to move around in the soil. Rounded sands are not suitable because they do not pack and cannot provide a firm enough seedbed. Angular sands are not suitable because they become too firm and can potentially cut into roots. Once a sand is selected and it is determined if an amendment will be used, the layout of the root zone profile must be determined.

In the United States, the most common specifications for constructing a sand-based system are laid out by the United States Golf Association, or the USGA. The specifications for a sand-based athletic field are the same as what is typically used for USGA golf greens. These specifications consist of a 12 to 16 inch sand root zone. The choice of sand type and the addition of an amendment depend on the designer. When an amendment is used, it must be thoroughly incorporated with the sand. The sand overlays a 4-inch gravel layer (Ferro and Otto, 2001). This creates a perched water table above the gravel that helps keep the root zone moist during dry conditions. A drainage system should be installed below the gravel to carry excess water away from the field.

Aeration and Topdressing for Proper Thatch Management

Aeration on a sand-based system is used more to control the thickness of the thatch layer than to relieve compaction. A thick thatch layer on a sand-based athletic field can be detrimental. These layers prevent essential nutrients and water from reaching the plant. Further, fertilizers, fungicides, and insecticides can not penetrate the surface and reach the soil. This can obviously be devastating if a field is consumed by a soil borne disease or insect. Water penetration can also be deterred by a thick thatch layer. When there is a thick mat of organic matter near the surface of a field a second perched water table will form. This will cause roots to stay in the top couple of inches of soil because they do not need to search for water at greater depths. Without a deep root system, a field can become unsafe due to footing issues.

Core aerification is the most conventional way to control thatch. Taking up plugs and removing them from the surface eliminates much of the organic matter that is in the soil. The most common aerificaiton tines used are usually a half inch in diameter, normally penetrate about four inches, and are hollow. If the holes are on 2 inch center, 36 holes will be punch per square foot. After a field is aerified, the cores can either be raked up and removed, or left on the surface to break down. Solid tines will punch holes into surface but are only a temporary solution. This is because they do not reduce the organic layer, but merely displace it. Another common method of reducing thatch is vertical mowing. This consists of vertical blades tearing into the soil and pulling out organic matter. It is very effective at reducing thatch, but is also very disruptive. This can lead to a long recovery time for the turf. Reducing the amount of thatch at the surface allows nutrients and pesticides to penetrate into the soil more effectively. Collecting grass clippings will not reduce the formation of a thatch layer. Thatch layers are made up of decomposed vegetative parts of grass plants like stolons and rhizomes.

Once a field is aerified, and there are holes in the surface, a field should be topdressed with the same sand that was used in the construction of the field. Refilling the aerification holes with sand improves the macroporosity of the soil and allows better penetration of water. This will allow the turf manager to water deeper and therefore improve the root system. Introducing sand into the thatch layer allows the growth media to be suitable for play. Without sand mixed with the thatch layer, divots would readily kick out and the field would not be safe for any type of sport.

Nutrient management in sand-based athletic fields

Nutrient management is essential in maintaining a healthy stand of turfgrass, and is much more difficult to achieve effectively in a sand-based system. Unlike with native soil fields, leaching of nutrients is a major concern when managing a sand-based turf system.

Nutrient leaching occurs more readily in a sand-based system because sand has a relatively low cation exchange capacity, or CEC. This refers to the sand's ability to retain nutrient particles. Soil particle "hold on" to positively charged nutrient particles because they are negatively charged. The opposite charges cause the nutrients to adhere to soil particles which can then be taken up by plants (UMN Extension, 2004). Sand has virtually no CEC, whereas clay and organic matter have relatively high CEC. This means that the higher the clay and organic matter of a soil, the more nutrients it will hold.

Low CEC is a major concern when an athletic field is constructed with 100% sand because substantial amounts of nutrients will be unavailable to the turf. The pure sand base will not hold on to nutrients until there is substantial organic matter incorporated into the soil to keep nutrients from leaching. Eventually, organic matter levels will rise as the plants begin to mature and dead vegetative matter decomposes.

The best way to avoid this problem is to incorporate some type of organic matter into the root zone mix during construction. The most common, as noted above, is peat moss. Mixing peat moss into the root zone mixture greatly increases nutrient holding capacity. This will greatly increase the chances of establishing a healthy stand of turfgrass because the soil will be able to retain both nutrients and water.

Because the nutrient holding capacity is low, soil tests are crucial for sand-based athletic fields. Soil tests should be taken frequently to measure what nutrients are lacking. Fertility programs should then be based on the soil tests. Unlike a native soil field, where most nutrients that are applied stay in the soil, sand-based fields nutrient status fluctuates. That is why a yearly fertilizer program can not be followed (Mayer, 1998). It is more important to obtain soil tests during the establishment of a new field because organic matter will be low and amounts of nutrients will fluctuate even more.

Water management in sand-based athletic fields

One of the many advantages of sand-based systems is extremely good drainage. A well constructed sand-based system can drain excessive amounts of rainfall very quickly. The good drainage that sand-based systems exhibit also offer the turf manager better control over soil water content.

The large size of sand particles allow water to flow freely which, in turn, allows sand-based system to drain extremely well. This is beneficial because it allows fields to be used during inclement weather. Sand-based systems will drain multiple inches of water within a short period of time. This allows a sporting event to be played through a rain or after a short delay. Native soil fields, on the other hand, do not drain well and many games have to be cancelled or postponed due to puddling on the field.

The good drainage of a sand-based system allows turf managers better control over their irrigation. Once the turf manager learns how his/her field drains, they will know, fairly accurately, when the field will need water. This allows them to make an irrigation plan that provides the turf with just enough water to maintain its health.

Localized dry spots, more commonly known as hot spots, are a common occurrence on sand-based turf systems. Hot spots are small areas of turf that are dry and often become hydrophobic. They can be first seen when the grass plants in the area begin to wilt. If the hot spot is not taken care of, the turf in that area will eventually die. Once the soil becomes hydrophobic, it is very hard to get water to penetrate. The best way to alleviate a hot spot is through long, light irrigation or rainfall (Vincelli and Eshenaur, 1994). It may also help to use a pitchfork to poke holes into the soil to increase percolation.

References

*Ferro, S., and D. Otto. 2001. Drainage Problems: Sand-based rootzones help golf courses and athletic fields find ‘soil solutions.’ Ground Maintenance Magazine June, 2001. [http://www.turfdiag.com/drainage_problems.htm Link]

*Kussow, W.R. 1987. Peat in Greens: Knowns, Unknowns, and Speculations. Online Posting. Michigan State Turf. [http://turf.lib.msu.edu/1980s/1987/870905.pdf Link]

*Mayer, Eugene. 1998. Compaction Resistance and Drainage: The Driving Force Behind Sand Based Root Zones. Turf Magazine. [http://www.invisiblestructures.com/GP2/GP2GRAPHICS/sandrootzone/compaction.pdf Link]

*University of Minnesota Extension. 2004. Soil Test Interpretations and Fertilizer Management for Lawns, Turf, Gardens, and Landscape Plants: Cation Exchange Capacity. Revised 2004. University of Minnesota. [http://www.extension.umn.edu/distribution/horticulture/components/1731-06.html Link]

*Vincelli, Paul, and Brian Eshenaur. 1994. Localized Dry Spot. Online Posting. Jul., 1994. UK Extension Service. [http://www.ca.uky.edu/agcollege/plantpathology/ext_files/PPFShtml/PPFS-OR-T-5.pdf Link]