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GES175, Science of Soils. Physical Properties of Soils. Particle Size. * Physical properties are influenced by particle size Size Classification (USDA): Soil < 2 mm Sand, 2 - 0.05 mm Silt, 0.05 - 0.002 mm Clay, <0.002 mm . Textural Triangle. Clay. Percent Silt. 40.
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GES175, Science of Soils Physical Properties of Soils
Particle Size * Physical properties are influenced by particle size Size Classification (USDA): Soil < 2 mm Sand, 2 - 0.05 mm Silt, 0.05 - 0.002 mm Clay, <0.002 mm
Textural Triangle Clay Percent Silt 40 Percent Clay 55 Silty Clay Sandy Clay 60 35 Silty Clay Loam Clay Loam Sandy Clay Loam 75 20 Loam Silt Loam Sandy Loam 90 10 Loamy Sand Silt Sand 50 70 20 Percent Sand
Clay 40 55 Silty Clay Sandy Clay 60 Silty Clay Loam Clay Loam Clayey Soil (fine textured)
60 35 Silty Clay Loam Sandy Clay Loam 75 20 Loam Silt Loam 90 Silt 50 70 20 Loamy/Silty Soils (medium textured)
20 Sandy Loam 10 Loamy Sand Sand 50 70 Sandy Soils (coarse textured)
Soil Structure granular Cause and Effect (description in laboratory) prismatic
+ Creating Structure Flocculation (chemical)
Surface Area vs - large grain - aggregate of small particles
Creating Structure - organic and inorganic ‘glues’ Aggregation
Stress Forces (what breaks the ‘glue’) Vertical Lateral
Soil Structure: Surface Horizons Spheriodal Granular
Massive Poor Management Granular
Compaction of Surface Horizons compaction - Platy Structure -
Structure: Subsurface ---- Prizmatic ---- Increased length in vertical direction - lateral stress > vertical stress
Blocky Structure: (subsurface horizons) • Increased (relative) age equates stress fractures
Bulk Densities Organic soil Db» 0.8 Mg/m3
Bulk Densities Organic soil Db» 0.8 Mg/m3 versus Compacted Subsoil è Db» 1.7 Mg/m3
Macroporosity Clay Aggregates Well Sorted Sand
+ Flocculation Aggregation Internal Porosity Micropores
Timber Harvest Volcanic Ash Soil