Juma, N. 1999. The pedosphere and its dynamics. Salmon Productions, - - PowerPoint PPT Presentation

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Juma, N. 1999. The pedosphere and its dynamics. Salmon Productions, - - PowerPoint PPT Presentation

Juma, N. 1999. The pedosphere and its dynamics. Salmon Productions, Edmonton, Alberta, Canada Soil Pore Solids Space Air 20 30% Mineral 45% Water 20 30% Organic 5% Capillary Fringe (est. thickness) Soil Range in Depth Avg.


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Juma, N. 1999. The pedosphere and its dynamics. Salmon Productions, Edmonton, Alberta, Canada

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Air 20 – 30% Water 20 – 30% Mineral 45% Organic 5% Pore Space Soil Solids

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Capillary Fringe

(est. thickness) <60 in. 5-10 ft. Clays <12 in. 0.5 – 5 ft. Silts 2 in. 0-3 in. Sands Avg. Range in Depth Soil

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Bedrock Solum O - Organic A – Mineral Mixed with

humus, dark colored

E - Horizon of maximum

eluviation of silicate clays, Fe, Al oxides

B - Horizon of maximum

illuviation of material

C - Zone of least weathering,

accumulation of Ca & Mg carbonates, cementation, etc.

R

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Coarse Sand 18” Fine Sand Silt Silt Clay Coarse Sand Silt 8” Silt Clay

Water Infiltration Water Infiltration Rapid Moderate/ slow Moderate Slow

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Juma, N. 1999. The pedosphere and its dynamics. Salmon Productions, Edmonton, Alberta, Canada

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Example of macropore formation due to soil shrinkage and cracking

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Example of surface sealing due to soil swelling.

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Jury, W.A., W.R. Gardner, and W.H. Gardner.

  • 1991. Soil physics, 5th ed. John Wiley & Sons, Inc.

New York.