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8.4D: Soil

  • Page ID
    49562
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    This page explains the role of soil in terrestrial food webs, highlighting its layers and the significance of topsoil for plant growth. It notes that tropical rainforest soils, although productive, tend to be nutrient-poor due to heavy rainfall and low humus levels, complicating cultivation efforts.
    Cross-section diagram of soil layers: topsoil, subsoil, weathered parent material, and parent material. Black and white illustration showing roots and organic matter in topsoil.
    Figure 17.2.4.1 Soil profile

    Topsoil

    The very top layer consists of partially decayed organic debris like leaves. Beneath this is the topsoil. This horizon is usually dark in color because of humus- partially decayed organic matter - which has been incorporated in it from above. Humus gives the soil a loose texture that holds water and allows air to diffuse through it. Oxygen is essential to permit cellular respiration in plant roots, decay organisms, and other inhabitants of the soil.

    Subsoil

    The subsoil is usually lighter in color that topsoil and often contains an accumulation of inorganic nutrients.

    Weathered parent material

    This represents the first steps in the chemical breakdown of rock into soil. Often the weathered parent material is underlain by the parent material itself, although in some places it has been carried from another location by wind, water, or glaciers.

    Parent material

    The chemical nature of the parent material, whether granite, limestone, or sandstone, for example, has a great influence on the fertility of the soil derived from it.

    The Effect of Water on Soil

    The Tropical Rain Forest

    The lushness of the jungle biome is somewhat illusory. While productivity is high, the soils themselves tend to be of very poor quality. Because of the high rainfall, nutrients are quickly washed out of the topsoil unless they are incorporated in the forest plants. As plant and animal debris falls to the ground, it is quickly decomposed because of the warmth and moisture there. Thus minerals are found mainly in the forest plants, not in the soil. When the plants are removed and cultivation attempted, the soils quickly lose fertility. The situation is made worse by the lack of humus (the topsoil may be no thicker than 2 in. [= 5 cm]) and the high iron and aluminum content of most of these soils. Once exposed to the sun, these lateritic soils soon bake into a bricklike material that cannot be cultivated.

    The most ancient (some might say primitive) way of working these soils is still the best:

    • clearing a small area of jungle
    • growing crops for only a year or two, and then
    • abandoning the area to jungle once again.

    This page titled 8.4D: Soil is shared under a CC BY 3.0 license and was authored, remixed, and/or curated by John W. Kimball via source content that was edited to the style and standards of the LibreTexts platform.

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