IV. Soil Description Flashcards
Moderately weathered soils that form under boreal or deciduous forests, rich in iron and aluminum
Alfisols
Clay particles accumulate in a subsurface layer in response to leaching in moist environments
Alfisols
Fertile, productive soils because they are neither too wet nor too dry
Alfisols
Young soils formed from volcanic ash and cinders
Andisols
Soils that develop in dry places
Aridosols
Insufficient water to remove soluble minerals
Aridosols
May accumulate calcium carbonate, gypsum, or salt in the subsoil
Aridosols
Low organic content
Aridosols
Young soils with limited development, exhibiting properties of the parent material
Entisols
Productivity ranges from very high in river deposits to very low in shifting sand or rocky slopes
Entisols
Young soils with little profile development found in regions with permafrost
Gelisols
Low temperatures and frozen conditions slow soil formation
Gelisols
Organic soils with little or no climatic implications
Histosols
Found in climates where organic debris accumulates to form bog soil
Histosols
Dark, partially decomposed organic material, commonly known as peat
Histosols
Weakly developed young soils with beginning profile development
Inceptisols
Most common in humid climates, occurring from the Arctic to the tropics
Inceptisols
Native vegetation is most often forest
Inceptisols
Dark, soft soils developed under grass vegetation, found in prairie areas
Mollisols
Humus-rich surface horizon, high in calcium and magnesium
Mollisols
Excellent soil fertility
Mollisols
Also found in hardwood forests with significant earthworm activity
Mollisols
Range from boreal and alpine to tropical climates
Mollisols
Dry seasons are common
Mollisols
Soils that occur on old land surfaces unless strongly weathered before deposition
Oxisols
Generally found in tropical and subtropical regions
Oxisols
Rich in iron and aluminum oxides, heavily leached, poor for agriculture
Oxisols
Found only in humid regions on sandy material
Spodosols
Common in northern coniferous and cool humid forests
Spodosols
A light-colored horizon of leached material beneath dark organic matter
Spodosols
Soils resulting from long periods of weathering
Ultisols
Water percolation concentrates clay in the lower horizons
Ultisols
Restricted to humid climates in temperate and tropical regions
Ultisols
Extensive leaching results in poorer soil quality
Ultisols
Contain large amounts of clay, shrinking upon drying and swelling with water
Vertisols
Found in subhumid to arid climates with periodic water saturation
Vertisols
Soil expansion and contraction exert stress on human structures
Vertisols