Basic Soil Orders Flashcards
Moderately weathered soils that form under boreal forest or broadleaf deciduous forest, rich in iron and aluminum
Alfisols (High Nutrient Soils)
Clay particles accumulate in a subsurface layer in response to leaching environments
Alfisols (High Nutrient Soils)
Fertile, productive soils, because they are neither too wet nor too dry
Alfisols (High Nutrient Soils)
Young soils in which the parent material is volcanic ash and cinders deposited by recent volcanic activity
Andisols (Volcanic Soils)
Soils that develop in dry places
Aridisols (Desert Soils)
Insufficient water to remove soluble minerals; may have an accumulation of calcium carbonate gypsum or salt in subsoil
Aridisols (Desert Soils)
Low organic content
Aridisols (Desert Soils)
Young soils having limited development and exhibiting properties of the parent material
Entisols (New Soils)
Productivity ranges from very high for some formed on recent river deposits to very low for those forming on shifting sand or rocky slopes
Entisols (New Soils)
Young soils with little profile development that occur in regions with permafrost
Gelisols (Permafrost Soils)
Low temperatures and frozen conditions for much of the year slow soil-forming processes
Gelisols (Permafrost Soils)
Organic soils with little or no climatic implications
Histosols (Organic Soils)
Can be found in any climate where organic debris can accumulate to form a bog soil
Histosols (Organic Soils)
Dark, partially decomposed organic material commonly referred to as peat
Histosols (Organic Soils)
Weakly developed young soil in which the beginning (inception) of profile development is evident
Inceptisols (Young Soils)