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Soil Compaction

    diagram showing an apparatus for measuring the pressure exerted by a growing root. A pot holds a seedling, with a root protruding down into a solid block that deflects a sheet of some material as the root elongates.
    Device used by Wilhelm Pfeffer in 1893 to measure the pressure generated by a growing root. Biodiversity Heritage Library (public domain image).

    Growing roots exert a pressure of up to 25 atmospheres – equal to the pressure you’d feel 800 feet under water. Yet compacted soil will stop roots dead in their tracks. This article will discuss how soil gets compacted, and how to mitigate and prevent compaction in lawns, vegetable gardens, and landscape areas.

    A brief primer on soil structure

    The fundamental particles of soil are tiny bits of various minerals – essentially, weathered rock. Organic matter holds these soil particles together, forming aggregates. Tiny aggregates themselves associate into larger aggregates, again held together by organic matter (see picture). Fungal hyphae and fine root hairs also help to generate aggregates.

    The amount of aggregation determines the structure of the soil. If a soil has many large aggregates, there will be many large pores between the aggregates because the aggregates can’t fit tightly together. In a healthy, well-structured soil, pores make up half the volume of the soil. Soils with poor aggregation have less pore volume because their small aggregates pack tightly together (see picture).

    Diagram showing, on the left, a small soil aggregate made of mineral particles held together by organic matter. On the right, small soil aggregates are held together by organic matter, plant roots, and fungal hyphae to form larger soil aggregates. Pores within the large aggregate hold air and water.
    Left, small soil aggregates are made of mineral particles held together by organic matter. Right, large soil aggregates are made of small aggregates held together by organic matter, roots, and fungal hyphae. Pores within aggregates hold air and water. CC BY-NC 4.0
    Diagram showing soil compaction. Top panel, well-structured soil with large aggregates and lots of pores containing roots, fungal hyphae, air, and water. Bottom, compacted soil with small aggregates that pack tightly together and exclude air, water, roots, and hyphae.
    Top, a well-structured soil with large aggregates and plenty of pore space for air and water. Bottom, a compacted soil: broken-down aggregates, containing little organic matter, pack tightly together and exclude air and water. The box and the total amount of “solid material” are the same in both cartoons but the smaller pieces in the bottom drawing can pack more tightly together. CC BY-NC 4.0

    Pores are essential for plant growth:

    (1) Pores are filled with air and water. Pores usually contain about equal amounts of each, depending on how wet the soil is. Roots absorb nutrients dissolved in the water, for example potassium, calcium, and iron. Roots also absorb the air in the pores, providing the oxygen that roots need to grow.

    (2) Pores provides pathways for root growth.

    Compaction, on the other hand, destroys soil pores by squeezing aggregates together – which, as discussed above, is easier when aggregates are small. This starves plants of nutrients and creates a physical barrier to root growth. Two practices can prevent, and to some extent reverse, compaction:

    (1) Promote aggregation by giving soil plenty of organic matter. 5% organic matter is a typical level for a healthy soil. A soil test can measure organic matter. Soil test kits can be picked up at the VCE office at the Albemarle County office building at 460 Stagecoach Road in Charlottesville.

    (2) Avoid physically compressing soil by minimizing foot and machine traffic. If traffic is unavoidable, wait until the soil is dry before walking or driving on it.

    Below are recommendations for mitigating and preventing soil compaction in a few locations around the home.

    Vegetable gardens

    a picture of a 4-tined broadfork loosening brown dirt.
    Broadforks also are useful for removing stones. Image: Wikimedia Commons. CC BY-SA 3.0

    Preserve organic matter by eliminating or minimizing tillage. No-till is counterintuitive (and controversial). Tillage certainly softens the soil’s top layer in the short term. In the long run, though, tillage depletes the soil’s organic matter by over-aerating the top few inches of soil. Soil microbes respond to the increase in oxygen and consume the soil’s organic matter. This, in turn, causes soil aggregates to fall apart. (Some experts do suggest one-time tilling of compost into new beds to speed up soil improvement.)

    Instead of tilling, add organic matter by spreading compost or mulch over the surface of the soil. The organic matter will work its way into the soil over time. Accelerate the infiltration of organic matter by loosening the soil with a spading fork, broadfork, or garden rake. This opens up small gaps in the top few inches of soil, but without excessive aeration and aggregate breakdown .

    Two long white radishes with green fronds at their tops, against a black background.
    Tillage radishes excel at pushing through the soil. Image: Joseph Amsili CC-BY-ND 2.0

    Cover crops are another effective way to add organic matter and loosen the soil. There isn’t space here for an-depth discussion of cover crops, but Piedmont Master Gardener Cleve Campbell has written a great introduction to cover cropping. Cover crops’ roots add organic matter to the soil. Clovers, and legumes like hairy vetch, boost soil nitrogen as well. Cover crops’ roots also break apart compacted soil. Forage radishes are particularly good at punching holes in heavy soils.

    Terminating cover crops is another complex topic, covered in detail here. It’s important to terminate cover crops before they go to seed and become weeds! Don’t till cover crop residue back into the soil, for the reasons mentioned above. Rather, cut the cover crop at the soil’s surface using a stirrup hoe or hand sickle – or even a lawnmower. Compost the cover crop residue or simply leave it on the soil surface, a practice termed green manure. The residue will decay and release organic matter into the soil.

    Finally, minimize foot or machinery traffic on the cultivated parts of the garden. Paths between the garden beds are a good way to keep traffic off the cultivated beds. If you must stand or kneel on the beds, support your weight on a board to spread the pressure out.

    Lawns

    Aeration is the best way to alleviate compaction in lawns. Usually this is done with a rented machine. Find a device with hollow tines or spoons that bring soil cores up to the surface. Spikes or blades that cut into the soil aren’t as effective: they let some air into the soil, but also create compaction around the holes they cut. Spiked shoes also are not a good solution, for the same reason.

    After aerating, it’s not necessary to remove the cores. If you don’t mind the appearance, simply wait for them to fall apart. A faster method is to wait a few days, until the cores have dried a bit, then rake them into tiny pieces and compost or leave in place. If desired, follow up aeration with overseeding, fertilizing, and liming. (Don’t apply lime without first doing a soil test to measure soil pH.)

    The best time to aerate is when the grass is growing at its maximum rate. In other words, aerate in spring or fall for cool-season grasses and summer for warm-season grasses. Also, don’t aerate when the ground is very dry; this will decrease the effectiveness of the aerator and may even damage the tines. Also avoid aeration when the ground is very wet; this can make compaction even worse.

    a lawn aerator with coring attachments mounted on a rotating cylinder
    This hollow core aerator cuts and removes plugs of soil. Image: Wikimedia Commons (public domain image).

    How often should you aerate? A home lawn shouldn’t need aeration more than once a year. If you notice water puddling, this is an obvious sign that compaction is a problem. Similarly, heavy thatch – the layer of mixed living and dead material between the grass blades and the soil – is a sign of compacted soil. If the thatch is more than an inch thick, it’s time to aerate.

    Prevent compaction by minimizing foot and machine traffic. Of course, foot traffic is a main reason for having a lawn! Paradoxically, one solution is to concentrate traffic in a small area, for example by making pathways of mulch or stepping stones in high-traffic areas. Similarly, sometimes machine traffic is unavoidable. Don’t drive machinery across lawns when the soil is very wet. Drive machinery on boards or sheets of wood to spread out the weight.

    Landscapes

    Compaction in landscaping is tricky because these areas don’t lend themselves to invasive methods. Moreover, trees and shrubs are particularly sensitive to compaction because their roots extend quite far from their trunks.

    Alleviate compaction by adding organic matter to the surface, in the form of mulch. The mulch will break down and organic matter will, slowly but surely, fall into the soil below. Wood chips, shredded bark, and mulched leaves are good choices, inexpensive (or free) and easy to obtain. Allow leaves to decompose in place under trees. If leaving leaves in place is for one reason or another unacceptable, rake the leaves onto some grass, shred them with a lawnmower, and return them to the area under the trees.

    Side-by-side photos of trees properly and improperly mulched. On the left, the properly mulched tree has a relatively thin layer of mulch that goes out to the "drip line", the outer extent of the branches, and doesn't touch the trunk of the tree; on the right, the improperly mulched tree has a big pile of mulch going up the trunk a foot or more.
    Properly (left) and improperly (right) mulched trees. Note that the mulch extends as far out as the branches. Image: North Dakota State University. CC-BY-NC-SA 2.0

    Under trees, mulch should extend to the outer extent of the branches (see picture). This perimeter is called the drip-line of the tree. The mulch should be only 2-4” deep. Any deeper and it will impede decomposition and release of organic matter into the soil. Don’t mound any mulch against the base of the tree trunk – the notorious “mulch volcano” (see picture). If mulch covers the bark, moisture can cause the bark to rot, and animals may gnaw on the covered bark. The root flare – the widening of the trunk where it begins to divide into roots – should be visible.

    A professional arborist may use an air spade to loosen heavily compacted soil around a tree. An air spade uses supersonic jets of air that remove soil – even when heavily compacted – but leave roots largely undamaged. After removing a few inches of compacted soil, higher-quality soil, with plenty of organic matter, is added in its place. Needless to say, this is an extreme, and expensive, solution.

    Given the difficulty of remedying compacted soil in landscape areas, prevention is critical. Mulch works very well for this because it discourages foot traffic. Direct foot traffic away from trees and shrubs using pathways of mulch or stones. Don’t drive or park heavy machinery near landscaped areas.

    Closing thoughts

    Soil compaction is a serious problem anywhere humans have disturbed the soil, whether in a yard, a cityscape, or a farm. Prevention is by far the best way to combat compaction because compaction is hard to reverse, particularly in a short time. Adding organic matter to the soil, in one way or another, is the primary way to alleviate compaction. This, as discussed in the “primer” section above, promotes aggregation of soil particles and a robust network of pores that allow root growth and infiltration of air and water into the soil. The other key practices are an observant eye, for signs and symptoms of compaction, and, of course, patience.

    References and further reading

    Elements of the Nature and Properties of Soils, 4th Edition. Ray R. Weill and Nyle C. Bandy
    Air trench digging or loosening soil. University of Florida
    Assessing and addressing soil compaction in your yard. New Jersey Agricultural Experiment Station
    The Biology of Soil Compaction. Ohio State University Extension
    Cover crops. Cleve Campbell, Piedmont Master Gardener
    Forage radishes, a hard-working cover crop. Cleve Campbell, Piedmont Master Gardener
    How to control thatch in your lawn. University of Minnesota Extension
    Management of compaction – coring. University of Massachusetts Extension Turf Program
    Managing soil compaction. Oregon State Extension
    Mulching landscape trees. Penn State Extension
    Physical Root-Soil Interactions Physical Biology 2017 (PDF). Evelyne Kolb et al.
    Problems caused by compacted soil. University of Maryland Extension
    Restore compacted soils. University of Colorado and U.S. Botanic Garden
    Scraping: scuffle hoes. University of California Agriculture and Natural Resources
    Strategies to avoid and manage soil compaction. University of California Agriculture and Natural Resources
    Understanding soil compaction. New Jersey Agricultural Experiment Station
    Virginia Tech Soil Testing Lab
    Walkways in the landscape. University of Florida
    What to do about compacted soils. Michigan State University Extension
    Featured image: Volker Prasuhn, Wikimedia Commons (public domain image).

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