getting dirty with soils

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Getting Dirty with SOILS

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Getting Dirty with SOILS. Older than dirt????!!!!. Why Care?. Why Care?. I . Soil Profile the horizons…… O A E B C R. E. R. Organics: Chelators Increases water absorption Releases high amounts of CO2. E. E. Diagnostic properties (B horizon). Texture Structure Color. Texture. - PowerPoint PPT Presentation

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Page 1: Getting Dirty with SOILS

Getting Dirty with

SOILS

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Older than dirt????!!!!

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Why Care?

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Why Care?

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 I. Soil Profile

the horizons……OAEBCR 

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R

E

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Organics:•Chelators•Increases water absorption•Releases high amounts of CO2

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E

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E

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Diagnostic properties (B horizon)

• Texture• Structure• Color

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Texture

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•Structure

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Diagnostic properties (B horizon)

• Texture• Structure• Color

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Munsell Color Chart

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R

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 I. Soil Profile II. Soil Classification A. Method: non genetic

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 I. Soil Profile II. Soil Classification A. Method: non genetic B. Orders: 12 total

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Soil Orders

EntisolsInceptisolsMollisolsSpodosolsAlfisolsUltisolsOxisols

AridisolsVertisolsHistosolsAndesolsGelisols

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Entisol

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Inceptisol

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Ultisols

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Alfisols

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Oxisol

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Mollisol

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Vertisol

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Aridisols

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Spodosols

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Histosols

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Gelisols

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Andisols

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Soils

III. Pedogenic Controls and RegimesA.   Factors of Soil Formation (Jenny, 1951)

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Soils

III. Pedogenic Controls and RegimesA.   Factors of Soil Formation

1.Climate

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Soils

III. Pedogenic Controls and RegimesA.   Factors of Soil Formation

1.Climate2. Biota

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Soils

III. Pedogenic Controls and RegimesA.   Factors of Soil Formation

1.Climate2. Biota3. Parent material

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Soils

III. Pedogenic Controls and RegimesA.   Factors of Soil Formation

1.Climate2. Biota3. Parent material4. Slope

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Soils

III. Pedogenic Controls and RegimesA.   Factors of Soil Formation

1.Climate2. Biota3. Parent material4. Slope5. Time

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III. Pedogenic Controls and RegimesA.   Factors of Soil FormationB. Podzolization“refers to the removal of iron and/or aluminum from the A horizon downward to the B Horizon”

Most common when annual ppt. exceeds70 cm (27.6 in)

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III. Pedogenic Controls and RegimesA.   Factors of Soil FormationB. PodzolizationC. Laterization

•Intense oxidation•Organic accumulation is inhibited•Silica is leached from the system

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III. Pedogenic Controls and RegimesA.   Factors of Soil FormationB. PodzolizationC. Laterization D. Calcification

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 V. Geomorphic Sig. of Soils 

fertilitybuilding foundationshydrologic responses to ppt.permanence of road construction

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The contrast…….