1. Soil:
unconsolidated mass of organic & inorganic material, water and air
inorganic material is measurably different from its parent material in physical and chemical properties
exhibits layering
2. last lecture examined weathering processes that would alter the physical and chemical properties of parent material
3. today we'll examine:
the soil profile
soil characteristics
soil classification & distribution
1. Processes affecting profile formation
additions
transformations: weathering & decomposition of organic matter
vertical transfers: eluviation and illuviation; capillary rise; bioturbation
removals: erosion; leaching
2. Horizons
O Horizon: litter layer; common in forests
A Horizon: topsoil; dark; nutrient rich
E Horizon: eluvial horizon
clay, iron & aluminum eluviated most often
sand & silt concentrated here
light colored
B Horizon: illuvial horizon
clay, iron & aluminum illuviated here
C Horizon: weathered parent material
R Horizon: consolidated bedrock
1. Color
2. Texture
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proportion of clay, silt & sand
inherited from parent material
affected by weathering
3. Organic Matter
CO2 generated during decomposition; helps promote chemical weathering
affects water holding capacity & cation exchange capacity
5. Bulk Density: weight of soil per unit volume
6. Soil Water Retention & Movement
7. Chemical Properties
cation exchange capacity
pH
1. Based on observable properties:
degree of profile development
amount of organic matter
often distinguished based on a particular horizon or combination of horizons
often correlated with climate and time
gelisols: soils with permafrost within 2 meters of the surface
andisols: soils formed in volcanic ash
histosols: organic soils
vertisols: soils rich in expansive clays
entisols: soils with little or no horizon development
inceptisols: soils with a weakly developed profile
aridisols: soils of desert environments; salinization
mollisols: grassland soils; calcification
spodosols: acidic soils of needleleaf forests; podzolization
alfisols: soils of humid & subhumid environments; higher in percent base saturation (i.e. more fertile) than ultisols
ultisols: moderately weathered soils of humid environments; lower percent base saturation than alfisols
oxisols: highly weathered soils of tropical & subtropical environments; laterization
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©
K.A. Lemke (klemke@uwsp.edu)
Last modified November 15, 2002 |