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  2. Clay - Wikipedia

    en.wikipedia.org/wiki/Clay

    Clay is a type of fine-grained natural soil material containing clay minerals [1] (hydrous aluminium phyllosilicates, e.g. kaolinite, Al 2 Si 2 O 5 4). Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide. [2] [3]

  3. Claypan - Wikipedia

    en.wikipedia.org/wiki/Claypan

    The high moisture content results in wet and sticky clay texture. When the clay swells, the low saturated hydraulic conductivity prevents the vertical water infiltration to the deeper soil horizon. It leads to water perches above the claypan layer. [5] The water permeability is restricted in the claypan layer resulting in low soil aeration.

  4. List of Uchu Sentai Kyuranger characters - Wikipedia

    en.wikipedia.org/wiki/List_of_Uchu_Sentai...

    Uchu Sentai Kyuranger (宇宙戦隊キュウレンジャー, Uchū Sentai Kyūrenjā) is a Japanese tokusatsu series that serves as the 41st installment in the Super Sentai franchise and the 29th entry in the Heisei era.

  5. Physical properties of soil - Wikipedia

    en.wikipedia.org/wiki/Physical_properties_of_soil

    Bulk density (g/cm 3) Pore space (%) Tilled surface soil of a cotton field 1.3: 51 Trafficked inter-rows where wheels passed surface 1.67: 37 Traffic pan at 25 cm deep 1.7: 36 Undisturbed soil below traffic pan, clay loam 1.5: 43 Rocky silt loam soil under aspen forest 1.62: 40 Loamy sand surface soil 1.5: 43 Decomposed peat 0.55: 65

  6. Soil mechanics - Wikipedia

    en.wikipedia.org/wiki/Soil_mechanics

    The thickness of the zone of capillary saturation depends on the pore size, but typically, the heights vary between a centimeter or so for coarse sand to tens of meters for a silt or clay. [3] In fact the pore space of soil is a uniform fractal e.g. a set of uniformly distributed D-dimensional fractals of average linear size L.

  7. Takir (soil) - Wikipedia

    en.wikipedia.org/wiki/Takir_(soil)

    Gerasimov I.P. On “takhirs” and the process of takyr formation: (Materials for the knowledge of the desert-steppe soil-forming process) in Soil Science. 1931. No. 4. S. 5-13. Gerasimov I.P. On "takhirs", their genetic essence and the process of takyproerazovaniya // Soil Science. 1933. No. 5. P. 401-403. Uspanov, U. U., Genesis and ...

  8. Soil texture - Wikipedia

    en.wikipedia.org/wiki/Soil_texture

    Determining soil texture is often aided with the use of a soil texture triangle plot. [5] An example of a soil triangle is found on the right side of the page. One side of the triangle represents percent sand, the second side represents percent clay, and the third side represents percent silt. If the percentages of sand, clay, and silt in the ...

  9. Soil pH - Wikipedia

    en.wikipedia.org/wiki/Soil_pH

    A high mesh size (60 mesh = 0.25 mm; 100 mesh = 0.149 mm) indicates a finely ground lime that will react quickly with soil acidity. The buffering capacity of a soil depends on the clay content of the soil, the type of clay, and the amount of organic matter present, and may be related to the soil cation exchange capacity.

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