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
Horizon designation
Horizon boundary depths
Color
Texture
Structure
Clay films and oxidation/ reduction features
Calcium carbonate accumulations
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
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
Horizon designation
Horizon boundary depths
Color
Texture
Structure
Clay films and oxidation/ reduction features
Calcium carbonate accumulations
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