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    • B horizon

      • The B horizon, or subsoil, is an accumulation of mostly fine material that has moved downward, resulting in a dense layer in the soil. In some soils, the B horizon contains nodules or a layer of calcium carbonate.
  1. Feb 17, 2023 · There is the significant importance of soil horizon in soil science. It allows one to understand the several processes that play a role in soil development and determine the different soil types. It also forms the basis for soil classification.

  2. soilsofcanada.ca › soil-formation › horizonsHorizons - Soils of Canada

    Horizons. The action and interaction of soil-forming processes as influenced by soil-forming factors gives rise to distinct soil horizons. These layers are assigned distinctive alphabetic symbols as a form of shorthand for their characteristics.

  3. Soil horizons are typically categorized into three main layers: the A horizon (topsoil), B horizon (subsoil), and C horizon (parent material). The characteristics of each soil horizon can vary significantly depending on climate, vegetation, and land use practices.

  4. Jun 7, 2020 · What Are Soil Horizons? Soil horizons, according to Britannica, are layers of soil that are underground, which “develop from the combined actions of living organisms and percolating water.” This definition basically means that many living creatures and other forces of nature shape the soil in a way that creates identifiable layers.

  5. Dec 24, 2022 · In some soils, the B horizon contains nodules or a layer of calcium carbonate. The C horizon, or soil base, includes the parent material, plus the organic and inorganic material that is broken down to form soil.

  6. May 24, 2024 · Calcium nodules are found near the base of the soil as calcium carbonate precipitates out of soil water. Mollisols are found in the drier portions of the humid continental climate through the steppe climate.

  7. Apr 27, 2024 · In some soils the B horizon is enriched with calcium carbonate in the form of nodules or as a layer. This occurs when the carbonate precipitates out of downward moving soil water or from capillary action. The diagram below illustrates the effect of climate on eluviation and illuviation.

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