“The easiest and most dramatic way to improve any garden is to improve the soil.” Joy Jones, OSU Extension Service.
Never did I dream that I would get excited about dirt! However, my Master Gardener class on soil was so enlightening, that I actually got excited. The complexities of soil are often not understood, and we tend to overlook its significant contribution to our lives. But it is in fact, a unique habitat specifically designed to support plant life. Soil helps to provide moisture, nutrients, heat, and support to all plants. If we understand it, our gardens will reap the benefits of our knowledge! So, in today’s blog post, I want to share with you some basic facts about soil and maybe some helpful ideas to improve your garden.
What exactly is soil? This pie chart shows the breakdown of ingredients. Soil is 50% solid and 50% pore space. Of the solid portion, 45% is decomposed rock (minerals) and 5% is organic matter. Ideally, the pore space has equal portions of air and water.
Productive soil allows water to permeate it and then supplies water to the plants. Pores can be created by earthworm and root channels as well as by the aggregation of soil particles. Pores can be large (they let water permeate) and they can be small and hold water against gravity making it available to the plant roots. Soils that have a balance of large and small pores have the ability to both allow water in and the ability to hold water for supply as needed by plants.
Porosity is of huge importance to maintaining plant health, and there are factors that affect soil porosity. The texture of the soil is one factor. There are coarse and fine particles than make up soil. Sand is the largest particle and is visible to the eye. Silt is a smaller particle that is similar in size to an individual particle of white flour. Clay particles are the smallest, and they can only be seen with a microscope. Both sand and silt are rounded and look like little rocks, but clay is flattened and the particles stick together like slices of buttered bread. These particles all seem small, but the relative difference in their sizes is very large. If a clay particle were the size of a penny, a sand particle would be the size of a house!
So, pore sizes in sandy soils tend to be large and in silt or clay soils, the pores are smaller due to the particles size differences. Sandy soils are easy to permeate, but they are fast-draining and not able to retain water. Silt or clay soils allow water to be held, but they do not allow permeability.
The perfect combination of pore sizes and particle sizes would be created with roughly equal parts of sand, silt and clay. This ideal soil is called loam. Most garden soils are not ideal but a combination of sand, silt and clay in other ratios that might make the soil more challenging to work with.
Good soil structure is also vitally important to allow water and air movement. Structure is the aggregation of individual particles of sand, silt and clay. The particles will bind together with “glue” from organic matter and provide structure to the soil. If the structure is good, the soil is acting like a sponge, allowing water to enter and soak in and letting excess water drain down. However, structure is fragile and can be damaged or destroyed by compaction. Compaction will cause the soil structure to resist water movement and root penetration as well.
What causes compaction? Compaction often occurs during site preparation or house construction. It’s often difficult to establish a garden and landscape in a new housing development. Although large earth-moving equipment is not the only thing that damages soil structure. Excessive tilling or tilling when the soil is too wet can cause compaction. Heavy foot traffic or running a heavy wheel-barrow over and over will also cause compaction.
So, where does all this information lead us to? We all want productive soil that is permeable to water and is able to supply water to plants when it is needed. But, maybe we live in an area where our soil is sandy, and water soaks in but our plants dry out quickly. Or maybe we just remodeled our home and trucks hauling building supplies drove over our garden space several times. Sometimes there are just circumstances that are beyond our control.
One very important action that we can take to improve the porosity of our soil is to add several inches of organic matter to the soil each year. Adding organic matter will:
- Stabilize soil structure. Humus is actually what holds particles together.
- Increase water holding capacity in sandy soils.
- Improve pore space in clay soils making it more permeable.
- Provide nutrients to plants once it decomposes.
- Provide a food source for beneficial micro organisms.
To keep soils from compaction:
- Do not till or spade soil when it is too wet. It must be dry and crumbly before tilling.
- Do not overwork soil with a rototiller. One pass is usually enough.
- Use raised beds and paths. By using paths you limit the area being walked on and the plant roots are never walked on.
- Grow a cover crop, especially one that produces deep roots like annual rye.
- Increase or maintain applications of organic matter.
- Aerate your soil, especially lawn areas that have heavy foot traffic.
- Double dig your soil. Here’s a great video to explain this concept: http://www.youtube.com/watch?v=W85QmZgDxFk
I hope this information is useful to you. Next week, I will share some more information from my soil class on amending soils.
Question for the week: What type of soil do you have?
Diagram of soil ingredients from: http://www.vanaturally.com/guide/soil.html
Diagram of soil particle size from: http://pnwmg.org/mgsoils.html



