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  2. Atterberg limits - Wikipedia

    en.wikipedia.org/wiki/Atterberg_limits

    Soil is placed into the metal cup (Casagrande cup) portion of the device and a groove is made down at its center with a standardized tool of 2 millimetres (0.079 in) width. The cup is repeatedly dropped 10 mm onto a hard rubber base at a rate of 120 blows per minute, during which the groove closes up gradually as a result of the impact.

  3. Clay - Wikipedia

    en.wikipedia.org/wiki/Clay

    Clay is generally considered undesirable for agriculture, although some amount of clay is a necessary component of good soil. Compared to other soils, clay soils are less suitable for crops due to their tendency to retain water, and require artificial drainage and tillage to make suitable for planting.

  4. Humus - Wikipedia

    en.wikipedia.org/wiki/Humus

    Soil carbon sequestration is a major property of the soil, also considered as an ecosystem service. [24] Only when it becomes stable and acquires its multi-century permanence, mostly via multiple interactions with the soil matrix , molecular soil humus should be considered to be of significance in removing the atmosphere's current carbon ...

  5. Molding sand - Wikipedia

    en.wikipedia.org/wiki/Molding_sand

    Molding sand was used exclusively for bronze casts, which was pioneered by the ancient Chinese. The next major advancement came in India in 500 B.C. when cast-crucible steel was created. Eventually, Sir Humphry Davy first did aluminum castings in Great Britain, around 1808. [2]

  6. Soil moisture - Wikipedia

    en.wikipedia.org/wiki/Soil_moisture

    Water is pulled by capillary action due to the adhesion force of water to the soil solids, producing a suction gradient from wet towards drier soil [50] and from macropores to micropores. [51] The so-called Richards equation allows calculation of the time rate of change of moisture content in soils due to the movement of water in unsaturated ...

  7. Ultisol - Wikipedia

    en.wikipedia.org/wiki/Ultisol

    Map of the United States showing what percentage of the soil in a given area is classified as an Ultisol-type soil. The great majority of the land area classified in the highest category (75%-or-greater Ultisol) lies in the South and overlays with the Piedmont Plateau, which runs as a diagonal line through the South from southeast (in Alabama) to northwest (up into parts of Maryland).

  8. Shrink–swell capacity - Wikipedia

    en.wikipedia.org/wiki/Shrink–swell_capacity

    A COLE value of 0.06 means that 100 inches of soil will expand by 6 inches when wet. [2] Soils with this shrink-swell capacity fall under the soil order of Vertisols . [ 6 ] As these soils dry, deep cracks can form on the surface, which then allows water to penetrate to deeper levels of the soil. [ 7 ]

  9. Sapric - Wikipedia

    en.wikipedia.org/wiki/Sapric

    The soil is very light, so windbreaks are necessary to protect these fields in dry weather. It also can catch fire and burn underground for months. Oxidation also removes a portion of the soil each year, making it progressively shallower.