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Gelisols (el)
- contains permafrost
- depend on climates
- do not have a diagnostic horizon
permafrost
can undergo soil processes
Gelisols found mostly in
-polar regions
-mostly on island and cont. edge
- high elevations
Entisols (ent)
- immature soil
- recent soils
- no genetic horizons, only a weak A
-little development
setting of entisols
places that have new parent material
inceptisols(ept)
- inception of B horizon
- weakly developed profile
- more developed than entisols
inceptisols setting
- widely distributed (found anywhere)
- steep slopes, mt. regions, young geomorphic surfaces
- resistant parent materials
what soil order supports over 20% of the global population
inceptisols
Andisols(ands)
-developed from volcanic material, particularly ash
- contain glass, many short-lived unstable colloids
- high water-holding capacity
-buried soil horizons are common
Histosols(ist)
organic soils
- 20-30% OM
- @ least 40cm thick
-low bulk density
-wetland soils
Histosols distribution
- in northern locations b/c cold inhibits the recycling/decomposition
Aridisols(ids)
- dry much of the year
- accumulation of CaCO3, gypsum, quartz, NaCl, evaporitic material
Mollisols(olls)
-grassland soils
- organic-rich
- thick surface horizon and deep
- thick A horizon not O horizon
Vertisols(erts)
- clay rich
-shrink-swell
-vertical cracking
Alfisols(alfs)
-moderately leeched
- relatively high native fertility
-forests
-accumulated clays in subsurface
Spodosols(ods)
- e horizon
-subsurface accumulation of humus
- complexed with Fe and Al
-coarse parent material
-forest
-naturally low fertility
-not much oxidation
Spodosols(ods) setting
wet and cold areas
Utisols(ults)
-Old soils which have been leached low fertility
-lot of development
- low LEC
-accumulation of clays
- red
Utisols setting
humid areas, temperate to tropical
oxisols
intensely weathered soils of tropical and subtropical environments, lateraliation
-very red
-low LEC
- high in Fe, Al
- chem weathering
- lack of OG parent material