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  2. Rendzina - Wikipedia

    en.wikipedia.org/wiki/Rendzina

    Rendzina (or rendsina) is a soil type recognized in various soil classification systems, including those of Britain [1] and Germany [2] as well as some obsolete systems. They are humus-rich shallow soils that are usually formed from carbonate- or occasionally sulfate-rich parent material. [2] Rendzina soils are often found in karst and ...

  3. Agricultural lime - Wikipedia

    en.wikipedia.org/wiki/Agricultural_lime

    Some effects of agricultural lime on soil are: it increases the pH of acidic soil, reducing soil acidity and increasing alkalinity [1] it provides a source of calcium for plants; it improves water penetration for acidic soils; it improves the uptake of major plant nutrients (nitrogen, phosphorus, and potassium) of plants growing on acid soils. [2]

  4. Caliche - Wikipedia

    en.wikipedia.org/wiki/Caliche

    Salts can also build up in the soil due to the lack of drainage. Both of these situations are detrimental to plant growth. Second, the impenetrable nature of caliche beds excludes plant roots, limiting plant access to nutrients, water, and anchorage. Third, caliche beds can also cause the surrounding soil to be basic.

  5. Calcareous grassland - Wikipedia

    en.wikipedia.org/wiki/Calcareous_grassland

    Plants on calcareous grassland are typically short and hardy, and include grasses and herbs such as clover. Calcareous grassland is an important habitat for insects, particularly butterflies and ants, [ 2 ] and is kept at a plagioclimax by grazing animals , usually sheep and sometimes cattle.

  6. Chalk - Wikipedia

    en.wikipedia.org/wiki/Chalk

    Chalk and other forms of limestone may be used for their properties as a base. [23] Chalk is a source of quicklime by thermal decomposition, or slaked lime following quenching of quicklime with water. [24] In agriculture, chalk is used for raising pH in soils with high acidity. [25] Small doses of chalk can also be used as an antacid. [26]

  7. Calcareous - Wikipedia

    en.wikipedia.org/wiki/Calcareous

    These oozes form slowly under low-energy environments, and necessitate higher seawater saturation states or a deeper CCD (see supersaturation and precipitation vs. undersaturation and dissolution). Therefore, in shallow CCD conditions ( i.e. , undersaturation of calcium carbonate at depth), stable, non-calcareous sediments such as siliceous ...

  8. Ultisol - Wikipedia

    en.wikipedia.org/wiki/Ultisol

    Ultisol, commonly known as red clay soil, is one of twelve soil orders in the United States Department of Agriculture soil taxonomy. The word "Ultisol" is derived from "ultimate", because Ultisols were seen as the ultimate product of continuous weathering of minerals in a humid, temperate climate without new soil formation via glaciation .

  9. Chalk heath - Wikipedia

    en.wikipedia.org/wiki/Chalk_heath

    Chalk heath is a rare habitat, in the temperate grasslands, savannas, and shrublands biome, formed of a paradoxical mixture of shallow-rooted calcifuge ("calcium-hating") and deeper-rooted calcicole ("calcium-loving") plants, growing on a thin layer of acidic soil over an alkaline substrate. Chalk heath is intermediate between two much more ...