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-Alfa
Alfisols
-Ands
Andisols
-Ids
Aridisols
-Ents
Entisols
-NONE
Gelisols
-Ists
Hisosols
-Epts
Inceptisols
-Olls
Mollisols
-OX
Oxisols
-Ods
Spodisols
-Ults
Ultisols
-Erts
Vertisols
Entisols Def.
Very Young Soils from alluvial deposition
Alfisols Def.
Cool, moist climate.
Light Colored
Moderately Acidic
Andisols Def.
Soils derived from volcanic material
Dark color
Fertile
Aridisols Def.
Common Western United States
Thin or no O or A horizon
Often Alkaline
Gelisols Def.
Solis grown in areas with permafrost within 100 cm of surface
Only in Alaska
Histosols Def.
Organic soils
Mostly soils that are commonly called bogs, moors, or peats and mucks
Inceptisols Def.
Young soils
Humid or sub-humid
Horizons that only form quickly
Weak B horizon
Mollisols Def.
Prarie Soils
Dark, thick, with good structure
Low to moderate rainfall
Oxisols Def.
Highly weathered tropical soils
low in weathered material
High in aluminum
Only occur in Hawaii and Puerto Rico
Spodisols Def.
Light-colored
Acid forest
soils in cool regions
generally infertile
Ultisols Def.
Highly weather soils
warm climates
Often leached, acid, and infertile
Common to southeastern U.S.
Vertisols Def.
High in swelling clays
when dry, large, deep cracks form
Found in southern states especially Texas
(Dry Clay Soil)
Particle Size Impacts
Internal Surface Area
The smaller the particle size, the larger the surface area = higher water-holding capacity
Number and Sizes of pore spaces
Sand
<2 mm but >0.05 mm
Of one mineral
Silt
<0.55 mm but > 0.002 mm
particles not visible
not gritty
Smooth, when wet not sticky
Clay
<0.002 mm
Great specific surface area
Particles stick
Particle Density
Mass per unit of SOLID soil volume
Bulk Density
Function of weight and volume of unit of dry soil
= mass of solids + pores
Soil Porosity
Measure of soil volume that holds air and water
SP = wet weight (g) – dry weight (g) / soil volume cm3
X 100
Soil Permability
Ease which water, air, roots move through
soil