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USDA soil classification system
Based on observable properties
Connected with climate and vegetation
Climate: hot & humid; tropical rainy (Af & Aw)
Vegetation: tropical forest (broadleaf evergreen & tropical semi-deciduous)
Location: equatorial Africa & South America
Very highly weathered
Horizons not very distinctive
Silica and nutrients leached from soil
Organic/nutrient poor; low CEC
Rich in aluminum & iron; formation of laterite
Image credit:U.S. Department of Agriculture, Natural Resources Conservation Service, http://soils.usda.gov/technical/classification/orders/oxisols.html
Climate: hot to temperate & humid; tropical rainforest (Af) & humid subtropical (Cfa)
Vegetation: tropical & temperate forests (broadleaf evergreen & broadleaf deciduous)
Location: equatorial Africa & South America, southeastern USA
Similar to oxisols, but not as highly weathered
Horizons more distinctive than oxisols
Image credit:U.S. Department of Agriculture, Natural Resources Conservation Service, http://soils.usda.gov/technical/classification/orders/ultisols.html
Climate: hot to temperate & humid to subhumid; tropical wet & dry (Aw), humid subtropical (Cfa), humid continental (Dfa, Dfb)
Vegetation: temperate forest (broadleaf deciduous)
Location: southern Great Lakes south to the Gulf of Mexico
Moderately leached; relatively fertile
Thin O horizon; A horizon more well-developed than in ultisols
Eluviation of clay from A & E horizons
Illuviation of clay in B horizon
photo credit: http://soils.usda.gov/technical/classification/orders/alfisols.html replace
Oxisols, Ultisols & Alfisols all have similar processes at work
They form a sequence from most (oxisols) to least (alfisols) weathered
Degree of weathering affects profile appearance; partly a function of age (time)
Climate: cool & humid; humid continental (Dfb, Dfc) although they can occur in other climates
Vegetation: needleleaf forest
Location: New England
Thick, acidic O horizon
Thin A horizon
Sandy, ash-grey E horizon
Clay & iron rich, red B horizon
photo credit: http://soils.usda.gov/technical/classification/orders/spodosols.html
Climate: cold; humid subarctic (Dfc, Dfd, Dw)
Vegetation: low-growing plants
Location: high latitudes
Permafrost
Dark A horizon due to presence of decaying plant litter
Cryoturbation: vertical mixing due to freeze-thaw
photo credit: http://soils.usda.gov/technical/classification/orders/gelisols.html
Climate: temperate to cool & subhumid to steppe; Cfa, Dfa, Dfb, BSk
Vegetation: prairie grassland
Location: midlatitudes; central USA from Texas to Canada & on into Canada
Thick, organic rich A horizon
Not leached of nutrients
Formation of calcium carbonate in B horizon
photo credit: http://soils.usda.gov/technical/classification/orders/mollisols.html
Climate: dry; subtropical desert (BWh) and midlatitude desert (BWk)
Vegetation: desert vegetation
Location: subtropics, leeward side of mountains, continental interiors, dry west-coasts
Weak A horizon
Minimally weathered
Minimally leached
Accumulation of salts
photo credit: http://soils.usda.gov/technical/classification/orders/aridisols.html
Climate: varies
Vegetation: varies
Location: widespread
Little horizon development
insufficient time
highly resistant parent material
active environments
Climate: varies; cool humid
Vegetation: water tolerant
Location: waterlogged environments such as bogs; most commonly in subarctic & arctic locations
Organic soils
photo credit: http://soils.usda.gov/technical/classification/orders/histosols.html
Climate: varies, but most well developed in climates with a seasonal moisture regime
Vegetation: varies
Location: places with expansive clays (clays that swell & shrink with wetting & drying)
Profile inversion due to mixing as cracks open & close
photo credit: http://soils.usda.gov/technical/classification/orders/vertisols.html
Climate: varies
Vegetation: varies
Location: volcanic regions
Parent material: volcanic ash & pyroclasts
Rich in humus
Soil orders associated with climates:
oxisols - Af, Aw
ultisols - Af, Aw, Cfa
alfisols - Aw, Cs, Cfa, Dfa, Dfb,
spodosols - Dfb, Dfc (& needleleaf forests)
gelisols - Dfc, Dfd, Dw (permafrost)
mollisols - Cfa, Dfa, Dfb, BSk
aridisols - BWh, BWk
Soil orders associated with special conditions:
spodosols - needleleaf forests
gelisols - permafrost
entisols & inceptisols - active environments; young soils
histosols - bogs
vertisols - expansive clay parent material
andisols - volcanic parent material