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Published bySilas Briggs Modified over 9 years ago
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Soil Analysis Objectives To understand how soil is formed To know the different soil horizons Be able to characterize soil based on: Color Texture Structure and pH Be able to identify the type based on its constituent particle size
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Soil Constituents: Air Water Nutrients Organic matter Disintegrated rock and Microorganisms Soil Formation Rate: 1inch/500-1000 years Soil Erosion: Natural and Anthropogenic Cropland: 1inch/15-30 years (US,1990)
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Desertification Soil compaction Overgrazing Depletion of water resources and Drought Salinization Climate Change
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Climate ◦ High in warmer and wetter climate Organisms ◦ Microbial decomposition ◦ Vegetation Topographic relief ◦ Mountain/valleys: slope, wind, water, sun Parent materials ◦ Based on geological material Time
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Weathering ◦ Physical ◦ Chemical ◦ Biological
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Texture ◦ Loam Mixture of sand, silt and clay ◦ Soil Porosity Sizes of spaces between soil particles Crop production Characteristics ◦ Color (dark, red, white) ◦ Structure (aggregated and clumped) ◦ pH ( 0-14 acidic, neutral, alkaline) Soil and nutrients ◦ Nitrogen (N), Phosphorus (P), Potassium (K) ◦ Eutrophication ComponentsParticle Size Clay<0.002mm Silt0.002-0.05mm Sand0.05-2.0 mm
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Place soil in top sieve Swirl for about 2 minutes Discard top sieve (sieve #5) Weigh and combine next 2 sieves ◦ (#10 + #60) = sand Weigh 4 th sieve (#230) = silt Weigh 5 th sieve (bottom)= clay Calculate percentages Use triangle method to determine texture
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