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soils 

Components- Minerals, Organic matter ,Water ,Air

  • Hans Jenny’s factors 1941 – Climate CL , Biological agents O, Relief/ topography R, Parent Material P, time T Cl O R P T

    Topography - affects drainage

  • Loess – a wind blow silt parent material of dust

    soil profiles/ horizons

  • O - organic material

  • A- some organic material, mostly mineral, ideal for plant growth, hydrolysis happens in this layer

  • E - washed out layer, mineral material, Hydrolysis happens here

  • B - accumulations, clay particles and oxides ( all the stuff from hydrolysis ends up here)

  • C- parent material, weathered bed rock

  • R - bedrock

  • A build up of calcium carbonate is sometimes called K horizon.

    How to describe soil

    1. Horizon designation

    2. Horizon boundary depths

    3. Color

    4. Texture

    5. Structure

    6. Clay films and oxidation/ reduction features

    7. Calcium carbonate accumulations

    8. Rock fragments

      Pedon – a column of soil taken from specific location, extending from the ground surface all the way down into C

      Solum- where soil development is most active AEB (not C)

      12 orders of Soil - Alfisols, Andisols, Aridisols, Entisols, Gelisols, Histosols, Inceptisols, Mollisols, Oxisols, Spodosols, Ultisols, Vertisols

      Alfisols -  moderately leached soils that have relatively high native fertility, high base status forest soils with argillic horizons

      Andisols- soils that have formed in volcanic ash or other volcanic ejecta

      Aridisols -  CaCO3-containing soils of arid regions that exhibit subsurface horizon development, soils of dry regions

      Entisols- recently formed soils, soils of recent origin

      Gelisols- soils of very cold climates that contain permafrost within two meters of the surface, soils of permafrost, cryoturbation, and ice segregation

      Histosols,- soils that are composed mainly of organic materials

      Inceptisols -  soils that exhibit minimal horizon development,embryonic soils with few diagnostic features

      Mollisols - soils of grassland ecosystems, grassland soils of steppes and prairies

      Oxisols- sesquioxide-rich, highly weathered soils of the intertropical regions, very highly weathered soils that are found primarily in the intertropical regions of the world

      Spodosols - acid soils characterized by a subsurface accumulation of humus that is complexed with Al and Fe, soils with subsoil accumulations of humus and sesquioxides

      Ultisols - low base status forest soils, strongly leached, acid forest soils with relatively low native fertility

      Vertisols - shrinking and swelling dark clay soils, clay-rich soils that shrink and swell with changes in moisture content


CE

soils 

Components- Minerals, Organic matter ,Water ,Air

  • Hans Jenny’s factors 1941 – Climate CL , Biological agents O, Relief/ topography R, Parent Material P, time T Cl O R P T

    Topography - affects drainage

  • Loess – a wind blow silt parent material of dust

    soil profiles/ horizons

  • O - organic material

  • A- some organic material, mostly mineral, ideal for plant growth, hydrolysis happens in this layer

  • E - washed out layer, mineral material, Hydrolysis happens here

  • B - accumulations, clay particles and oxides ( all the stuff from hydrolysis ends up here)

  • C- parent material, weathered bed rock

  • R - bedrock

  • A build up of calcium carbonate is sometimes called K horizon.

    How to describe soil

    1. Horizon designation

    2. Horizon boundary depths

    3. Color

    4. Texture

    5. Structure

    6. Clay films and oxidation/ reduction features

    7. Calcium carbonate accumulations

    8. Rock fragments

      Pedon – a column of soil taken from specific location, extending from the ground surface all the way down into C

      Solum- where soil development is most active AEB (not C)

      12 orders of Soil - Alfisols, Andisols, Aridisols, Entisols, Gelisols, Histosols, Inceptisols, Mollisols, Oxisols, Spodosols, Ultisols, Vertisols

      Alfisols -  moderately leached soils that have relatively high native fertility, high base status forest soils with argillic horizons

      Andisols- soils that have formed in volcanic ash or other volcanic ejecta

      Aridisols -  CaCO3-containing soils of arid regions that exhibit subsurface horizon development, soils of dry regions

      Entisols- recently formed soils, soils of recent origin

      Gelisols- soils of very cold climates that contain permafrost within two meters of the surface, soils of permafrost, cryoturbation, and ice segregation

      Histosols,- soils that are composed mainly of organic materials

      Inceptisols -  soils that exhibit minimal horizon development,embryonic soils with few diagnostic features

      Mollisols - soils of grassland ecosystems, grassland soils of steppes and prairies

      Oxisols- sesquioxide-rich, highly weathered soils of the intertropical regions, very highly weathered soils that are found primarily in the intertropical regions of the world

      Spodosols - acid soils characterized by a subsurface accumulation of humus that is complexed with Al and Fe, soils with subsoil accumulations of humus and sesquioxides

      Ultisols - low base status forest soils, strongly leached, acid forest soils with relatively low native fertility

      Vertisols - shrinking and swelling dark clay soils, clay-rich soils that shrink and swell with changes in moisture content