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The Twelve USDA Soil Orders
Entisols
Inceptisols
Mollisols
Alfisols
Spodosols
Histosols
Andisols
Oxisols
Ultisols
Gelisols
Vertisols
Aridisols
Gelisols
Soils with permafrost or cryoturbation (mixing from frost heaving)
Cold or frozen much of the yearCan be organic or inorganic soils
9% worldwide 7% US
Entisols
Young, weakly developed soil Typically NO B horizon
(in some cases, can have a very coarse-textured, poorly formed Bw)
Typical profiles: C AC OC OACCommon on ridgetops, recent deposits (rivers,
beaches, ash…), urban areas
16% Worldwide12% US
A
C
Inceptisols
Relatively young soils – have B horizonsMore developed than Entisols but less developed
than any other soil order (soil doesn’t meet the criteria of other orders)
10% Worldwide 9% US
Andisols
Developed from volcanic materialA horizons that are rich in Al-humic materialsSecondary minerals are predominately amorphousRange in development from moderate
to well-developed
<1% Worldwide 2% US
Aridisols
Dry soils; arid to semi-arid environmentsTypically less plant growth, A horizon with less OMCan have many types of B horizons, but Bk’s are common
12% Worldwide 9% US
Mollisols
Have a ‘mollic’ A horizon (>50% Base Sat., with good physical properties)Usually under grasslandsVERY fertile soilsProfiles may be: A B_ C
A C or even A E B_ C
7% Worldwide22% US
Alfisols
Has a Bt horizon Moderate Base Sat. (< 50% and > 35%)Lower fertility than Mollisols, but still excellent soilCommon under deciduous forests, grasslandsA, E, Bt1, Bt2, C A, Bt1, Bt2, BC
10% Worldwide15% US
Ultisols
Old, highly weathered soil, acidicLow Base Sat. (< 35%)Has a Bt horizonLower fertility than AlfisolsCommon under forestsDevelop in wetter temperate areas or
tropical areas with lots of leachingO, A, Bt1, Bt2, Bt3, C
9% Worldwide10% US
Oxisols
Most highly weathered, old soilsLaterization – has an oxic B horizonOxides prevalent, kaolinite commonA horizon low in organic matterCommon in tropical areas with high
rainfall, stable landscape
8% Worldwide<1% US
Spodosols
Has a Spodic horizon (Bs, Bhs)Illuvial accumulation of Fe, Al, O.M.Usually has an E horizonAcidic, lower fertilityFound in cooler, temperate regions, areas of high
leaching, coarse textured soilO, E, Bhs, Bs, C
3% Worldwide3% US
Vertisols
High content of shrink/swell clay in the upper 1m of soilMontmorilloniteSoil expands and contractsCracks open in dry season, material falls in and cracks shut in wet season—mixes soilSubhumid to semi-arid areasDeep A horizon
2% Worldwide2% US
Histosols
Organic Soil (little mineral material)O horizonsFound in waterlogged areas of any type
of climate: WetlandsWhen drained, can be fertile but difficult to manage
due to poor physical propertiesOa, Oe, Oi
1% Worldwide1% US