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  2. Tropical peat - Wikipedia

    en.wikipedia.org/wiki/Tropical_peat

    Tropical peat is a type of histosol that is found in tropical latitudes, including South East Asia, Africa, and Central and South America. [2] Tropical peat mostly consists of dead organic matter from trees instead of spaghnum which are commonly found in temperate peat. [3] This soils usually contain high organic matter content, exceeding 75% ...

  3. Mollisol - Wikipedia

    en.wikipedia.org/wiki/Mollisol

    Mollisol is a soil type which has deep, high organic matter, nutrient-enriched surface soil ( A horizon ), typically between 60 and 80 cm in depth. This fertile surface horizon, called a mollic epipedon, is the defining diagnostic feature of Mollisols. Mollic epipedons are created by long-term addition of organic materials derived from plant ...

  4. Bureau of Soils and Water Management - Wikipedia

    en.wikipedia.org/wiki/Bureau_of_Soils_and_Water...

    SRDC Building, the home of the Bureau of Soils and Water Management headquarters. Agency overview. Formed. June 5, 1951. Headquarters. SRDC Building, Visayas Avenue corner Elliptical Road, Vasra, Quezon City, Philippines. 14°39′16″N 121°02′48″E. /  14.65445°N 121.04659°E  / 14.65445; 121.04659. Agency executive.

  5. Histosol - Wikipedia

    en.wikipedia.org/wiki/Histosol

    Histosol. In both the World Reference Base for Soil Resources (WRB) [1] and the USDA soil taxonomy, [2] a Histosol is a soil consisting primarily of organic materials. They are defined as having 40 centimetres (16 in) or more of organic soil material starting within 40 cm from the soil surface. In Soil Taxonomy, Gelisols key out before ...

  6. Bulk soil - Wikipedia

    en.wikipedia.org/wiki/Bulk_soil

    Bulk soil is soil outside the rhizosphere that is not penetrated by plant roots. The bulk soil is like an ecosystem, it is made up of many things such as: nutrients, ions, soil particles, and root exudates. There are many different interactions that occur between all the members of the bulk soil. Natural organic compounds are much lower in bulk ...

  7. Aridisol - Wikipedia

    en.wikipedia.org/wiki/Aridisol

    Aridisol. Aridisols (or desert soils) are a soil order in USDA soil taxonomy. [ 1] Aridisols (from the Latin aridus, for "dry", and solum) form in an arid or semi-arid climate. Aridisols dominate the deserts and xeric shrublands, which occupy about one third of the Earth's land surface. Aridisols have a very low concentration of organic matter ...

  8. Physical properties of soil - Wikipedia

    en.wikipedia.org/wiki/Physical_properties_of_soil

    Soil bulk density is equal to the dry mass of the soil divided by the volume of the soil; i.e., it includes air space and organic materials of the soil volume. Thereby soil bulk density is always less than soil particle density and is a good indicator of soil compaction. [47] The soil bulk density of cultivated loam is about 1.1 to 1.4 g/cm 3 ...

  9. Unified Soil Classification System - Wikipedia

    en.wikipedia.org/wiki/Unified_Soil...

    The Unified Soil Classification System ( USCS) is a soil classification system used in engineering and geology to describe the texture and grain size of a soil. The classification system can be applied to most unconsolidated materials, and is represented by a two-letter symbol. Each letter is described below (with the exception of Pt ): If the ...

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