1/11
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai |
|---|
No analytics yet
Send a link to your students to track their progress
Oxisols (ox):
Tropical soils
Oxidized subsurface horizons: high iron and aluminum oxides (reddish / yellowish color)
Heavy precip. Leaches soluble minerals from A horizon
Low pH, low fertility
Lack of distinct horizons
Aridisols (id)
Desert soils
Largest single soil order (19% of Earth’s land surface)
Shallow soil horizons
Low precip., infreq. Leaching
Little vegetation, low org. Matter
Salinization: salts dissolved in soil water migrate to surface, despotited as water evaporates: damage / kill plants
Mollisols (oll)
Grassland soils
Mollis = soft
Rich soils, high organic matter (high humus content) - dark surface horizon
Cover more area in continental US than any other soil order
Alfisols (alf)
Moderately weathered (leached) forest soils
Most widespread soil order
5 suborders from equator to high latitudes
Semi-arid to moist (Mediterranean)
Soils of the Midwest: Continuum: Aridisols (west), mollisols (central), alfisols (east)
Ultisols (ult)
Highly weathered (leached) forest soils
High precipitation, subtropical (southeast US)
Ultimate weathering
Low pH, lower fertility
An Alfisol might evolve into an Ultisol
Reddish
Spodosols (od)
Northern coniferous forest soils
Northeast US, Northern Europe
Rarely found in Southern Hemisphere
Spodos = wood ash, grey color
Acidic, highly weathered (leached), sandy
E horizon: light colored, clay minerals leached out (eluviation)
Entisols (ent)
Recent (young)
Undeveloped soils
Lack vertical development of horizons
Occur in many climates
Poor ag. soils (except river silt deposits)
Form on active slopes, floodplains, poorly drained tundra, tidal mudflats, dune sands, glacial outwash plains
Inceptisols (ept)
Inceptum = beginning
Inception of B horizon
Weakly developed / minimal horizon development
More developed than Entisols
Young, infertile
Moist, eluvial: some loss
Found in most climates
Gelisols
Cold and frozen soils
Contain permafrost within 2m of surface
Temps at or below 0OC; soil dev. Is slow
Decomp. Is slow; store large amts of org. matter and carbon
Thick O horizons
Andisols (and)
Soil formed from volcanic parent materials (ash and glass)
High mineral content recharged by eruptions
Commonly found near or downwind or volcanoes: thick layer of ash deposited
Vertisols (ert)
Vert → invert
Horizons invert: bring lower horizons near surface
Soils that shrink and swell (expandable clays)
Crack when dry / swell when wet
High in nutrients, good for farming
Histosols (ist)
Wetland soils (bogs, peat beds)
Saturated year-round
Accumulate thick org. matter (no permafrost)
Form in former lakes or poorly drained depressions