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Soil
The growing medium of plants

Soil: Main Index


  • Cover Crops
  • Cultivation
  • Humus
  • Mulch
  • Natural Mulches
  • Preparing a Seedbed
  • Soil Amendments
  • Soil Preparation / Maintenance
  • Soil Preparation
  • Tillers
  • Tilling the Soil
  • Turning the soil

  • What is Soil?

    Before we set about changing soil, we need to know what soil is.

    Traditionally, soil's relationship to the earth is compared with the rind's relationship to an orange. The analogy is apt if you imagine an orange with a rind that is highly irregular in width, color, texture and composition. Be it deep or shallow, red or black, sand or clay, the soil is the link between the rock shell of the earth and the living things on its surface. We are dependent on soils for life itself.

    Soil is part of the earth's crust

    Geologists are primarily concerned with the earth's crust—a shell of solid rock about 20 to 30 miles thick surrounding the earth. Soil scientists, on the other hand, are concerned with the thin layer of loose material that covers this shell. This layer, the soil, can be anywhere from a few inches to a few feet thick. Every solid rock, when it is exposed at the surface of the earth, slowly disintegrates into loose material through the process called weathering.

    The formation of soil

    Rocks are broken up into smaller particles by frost action, by the expansion and contraction caused by temperature changes, by the grinding action of streams, glaciers and wind, and by the force of large tree roots.

    This physical weathering is aided by chemical weathering processes, which cause the rock minerals to dissolve slowly and change by the action of water, carbon dioxide, oxygen, organic acids, and the effects of microbial activity.

    The Nature of Soil

    So here is this rather thin layer of loose material—mineral elements from weathered rocks, dead and living organic matter (both flora and fauna), air and water—lying on top of a thick layer of solid rock and constantly undergoing change from the effects of weather, chemical processes, microbes, plants and man. This, then, is soil. Or is it? When, in fact, does the loose material become soil? There is no definite answer, but it is usually called soil if it is supporting plant life.

    There is no minimum or maximum thickness necessary for material to be called soil. What is required is that the material be a medium in which seeds and transplants can grow and from which they can obtain water, air and the nutrient elements essential to plant growth.

    Types of Soils

    There are many kinds of garden soils, from sand, to loam, to clay. You can find a plant to grow in any soil, or by soil preparation you can alter the soil to grow any plant—the choice is up to you.

    Long-time gardeners know their plot of ground, the characteristics of the soil, how much to water, when to get the soil ready for planting, and what garden fertilizers to use. Some of the most valuable gardening knowledge is based on experience.



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