Getting Dirty with SOILS
Older than dirt????!!!!
Why Care?
I. Soil Profile the horizons…… O A E B C R
R E
Organics: Chelators Increases water absorption Releases high amounts of CO2
E
E
Diagnostic properties (B horizon) Texture Structure Color
Texture
Structure
Diagnostic properties (B horizon) Texture Structure Color
Munsell Color Chart
R
I. Soil Profile II. Soil Classification A. Method: non genetic
I. Soil Profile II. Soil Classification A. Method: non genetic B. Orders: 12 total
Soil Orders Entisols Inceptisols Mollisols Spodosols Alfisols Ultisols Oxisols Aridisols Vertisols Histosols Andesols Gelisols
Entisol
Inceptisol
Ultisols
Alfisols
Oxisol
Mollisol
Vertisol
Aridisols
Spodosols
Histosols
Gelisols
Andisols
Soils III. Pedogenic Controls and Regimes A. Factors of Soil Formation (Jenny, 1951)
Soils III. Pedogenic Controls and Regimes A. Factors of Soil Formation 1.Climate
Soils III. Pedogenic Controls and Regimes A. Factors of Soil Formation 1.Climate 2. Biota
Soils III. Pedogenic Controls and Regimes A. Factors of Soil Formation 1.Climate 2. Biota 3. Parent material
Soils III. Pedogenic Controls and Regimes A. Factors of Soil Formation 1.Climate 2. Biota 3. Parent material 4. Slope
Soils III. Pedogenic Controls and Regimes A. Factors of Soil Formation 1.Climate 2. Biota 3. Parent material 4. Slope 5. Time
III. Pedogenic Controls and Regimes A. Factors of Soil Formation B. Podzolization “refers to the removal of iron and/or aluminum from the A horizon downward to the B Horizon” Most common when annual ppt. exceeds 70 cm (27.6 in)
III. Pedogenic Controls and Regimes A. Factors of Soil Formation B. Podzolization C. Laterization Intense oxidation Organic accumulation is inhibited Silica is leached from the system
III. Pedogenic Controls and Regimes A. Factors of Soil Formation B. Podzolization C. Laterization D. Calcification
Soil Catena
IV. Factor of Time V. Geomorphic Sig. of Soils e.g.: building foundations hydrologic responses to ppt. permanence of road construction
The contrast…….