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  2. Soil structure - Wikipedia

    en.wikipedia.org/wiki/Soil_structure

    Soil structure describes the arrangement of the solid parts of the soil and of the pore spaces located between them (Marshall & Holmes, 1979). [1] Aggregation is the result of the interaction of soil particles through rearrangement, flocculation and cementation.

  3. Soil horizon - Wikipedia

    en.wikipedia.org/wiki/Soil_horizon

    A soil layer is a zone in the soil, approximately parallel to the soil surface, with properties different from layers above and/or below it. If at least one of these properties is the result of soil-forming processes, the layer is called a soil horizon. In the following, the term layer is used to indicate the possibility that soil-forming ...

  4. Solum - Wikipedia

    en.wikipedia.org/wiki/Solum

    The solum (plural, sola) in soil science consists of the surface and subsoil layers that have undergone the same soil forming conditions. The base of the solum is the relatively unweathered parent material. Solum and soils are not synonymous. Some soils include layers that are not affected by soil formation. These layers are not part of the solum.

  5. Stonelayer - Wikipedia

    en.wikipedia.org/wiki/Stonelayer

    While the model has greatly aided soil science, and spatially explains generalized soil-environmental relationships on landscapes, the device—supremely attractive in its parsimony—has constrained pedologic interpretation because its genetic-interpretive domain is constrained by its broad factorial (landscape context) tenets.

  6. Soil formation - Wikipedia

    en.wikipedia.org/wiki/Soil_formation

    The type and amount of precipitation influence soil formation by affecting the movement of ions and particles through the soil, and aid in the development of different soil profiles. Soil profiles are more distinct in wet and cool climates, where organic materials may accumulate, than in wet and warm climates, where organic materials are ...

  7. Topsoil - Wikipedia

    en.wikipedia.org/wiki/Topsoil

    [8] [9] Soil horizons are layers parallel to the soil surface whose physical, chemical and biological characteristics differ from the layers above and beneath. The depth of the topsoil layer is measured as the depth of the surface to the first densely packed soil layer, known as subsoil .

  8. Soil morphology - Wikipedia

    en.wikipedia.org/wiki/Soil_morphology

    Since the origin of agriculture, humans have understood that soils contain different properties which affect their ability to grow crops. [4] However, soil science did not become its own scientific discipline until the 19th century, and even then early soil scientists were broadly grouped as either "agro-chemists" or "agro-geologists" due to the enduring strong ties of soil to agriculture.

  9. Pedosphere - Wikipedia

    en.wikipedia.org/wiki/Pedosphere

    Soil is well developed in the forest as suggested by the thick humus layers, rich diversity of large trees and animals that live there. Forest soils can form a thick soil carbon sponge. In forests, precipitation exceeds evapotranspiration which results in an excess of

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