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PRINCIPLES OF SOIL SCIENCE Soil Science 1 To my Baby Sister “shannon kamille Matalog”.. Hehe… :D
Definition ,[object Object],[object Object]
Definition ,[object Object],[object Object],[object Object]
5-4-4-5
5 -4-4-5 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
5- 4 -4-5 ,[object Object],[object Object],[object Object],[object Object],[object Object]
5-4- 4 -5 ,[object Object],[object Object],[object Object],[object Object],[object Object]
5-4-4- 5 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Composition of soil by volume   ,[object Object],[object Object],[object Object],[object Object],[object Object]
SOM ,[object Object],[object Object],[object Object],[object Object],[object Object]
Soil Air ,[object Object],[object Object],[object Object],[object Object],[object Object]
Soil Quality ,[object Object]
Causes of Soil Quality Degradation ,[object Object],[object Object],[object Object],[object Object],[object Object]
Mechanisms of soil quality degradation ,[object Object],[object Object],[object Object],[object Object]
Rocks and Minerals ,[object Object],[object Object]
Classes of Rocks ,[object Object],[object Object],[object Object]
Classification of some igneous rocks in relation to mineralogical composition and rock texture. Rock Texture Light-colored Minerals Dark-colored Minerals Feldspars, muscovite Quartz Hornblende, augite, biotite Coarse Granite Diorite Gabbro Peridotite/ Horblendite Inter-mediate Rhyolite Andesite Basalt Fine Felsite/Obsidian Basalt glass
Some of the More Important Sedimentary and Metamorphic Rocks and the Dominant Minerals Dominant Mineral Sedimentary Metamorphic Calcite  CaCO 3 Dolomite CaCO 3 .MgCO 3 Quartz  SiO 2 Clays Variable Variable Limestone Dolomite Sandstone Shale Conglomerate Marble Marble Quartzite Slate Gneiss Schist
The More Important Minerals Found in Soils Listed in Order of Decreasing Resistance to Weathering (1) Primary Minerals Secondary Minerals Quartz  SiO 2 Muscovite   K Al 3 Si 3 O 10 (OH) 2 Microcline  K AlSi 3 O 8 Orthoclase  K AlSi 3 O 8 Goethite  Fe OOH Hematite  Fe 2 O 3 Gibbsite  Al 2 O 3 .3H 2 O Clay minerals (Al silicates)
The More Important Minerals Found in Soils Listed in Order of Decreasing Resistance to Weathering (2) Primary Minerals  Secondary Minerals Biotite  K Al( Mg,Fe ) 3 (AlSiO 3 O 10 )(OH) 2 Albite  NaAlSi 3 O 8 Hornblende  Ca 2 Al 2 Mg 2 Fe 3 Si 6 O 22 (OH) 2 Augite  Ca 2 (Al, Fe) 4 ( MgFe ) 4 Si 6 O 24 Anorthite  Ca Al 2 Si 2 O 8 Olivine  ( Mg,Fe ) 2 SiO 4 Dolomite ( Ca CO 3 . Mg CO 3 ) Calcite ( Ca CO 3 ) Gypsum ( CaS O 4 .2H 2 O)
[object Object],[object Object]
Essential Elements Macronutrients Micronutrients from soil solids ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Iron Manganese Boron Zinc Copper Chlorine Cobalt Molybdenum Nickel
Essential Element, Macro- and Micronutrients   ,[object Object],[object Object],[object Object]
Rocks Weather to Soil ,[object Object],[object Object]
Physical Weathering ,[object Object],[object Object],[object Object],[object Object],[object Object]
Chemical Weathering ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Parent Materials ,[object Object],[object Object]
Parent Materials ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Origin of residual materials and soil texture Origin Texture Basalt, andesite, volcanic tuff Clayey soils Granite, coarse sandstones Loamy and sandy  Siltstones, fine-grained sandstones  Silt loam and silty clay loam textures
Climate ,[object Object],[object Object],[object Object],[object Object]
Topography ,[object Object],[object Object],[object Object]
Factors that retard soil profile development ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
What happens to a soil with time ,[object Object],[object Object],[object Object],[object Object]
Soil Pedon & Soil Profile ,[object Object],[object Object],[object Object]
Eluviation & Illuviation ,[object Object],[object Object],[object Object]
Organic Horizons ,[object Object],[object Object],[object Object],[object Object]
Mineral Soil Horizons ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Lowercase letter symbols to designate subordinate distinction within master horizons. ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
n - sodium accumulation p - plowing - only used with A q - silica accumulation - very  weathered or old soil r - soft rock - used with C or Cr s – an accumulation of illuvial iron t – accumulation of illuvial clay  w - color or structure development (Bw) x - Fragipan - hard, dense layer that developed with time y - gypsum accumulation (CaSO 4 ) z – accumulation of soluble salts  Lowercase letter symbols (cont’d).
Sand ,[object Object],[object Object],[object Object],[object Object]
Silt ,[object Object],[object Object]
Clay ,[object Object],[object Object],[object Object],[object Object],[object Object]
Clay ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Determining Soil Texture – Hydrometer Method ,[object Object],[object Object],[object Object],[object Object],[object Object]
Soil Structure ,[object Object]
Soil Structure ,[object Object],[object Object],[object Object],[object Object]
Particle Density ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Bulk Density ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Bulk Density ,[object Object],[object Object],[object Object],[object Object]
Porosity ,[object Object],[object Object],[object Object],[object Object]
PD, BD & Porosity ,[object Object],[object Object],[object Object],[object Object],[object Object]
Soil Aggregates ,[object Object]
What influences aggregate stability? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
What influences aggregate stability? ,[object Object],[object Object],[object Object],[object Object]
What influences aggregate stability? ,[object Object],[object Object]
What influences aggregate stability? ,[object Object],[object Object],[object Object],[object Object]
Adhesion & Cohesion ,[object Object],[object Object]
Capillary Water ,[object Object],[object Object],[object Object]
Water Potential ,[object Object]
Soil Water Classification ,[object Object],[object Object],[object Object],[object Object],0 bar  -0.33  -15  -100  -10000 Saturated  Field Cap  Wilt point  air dry  oven dry AWC
Some Points on Water Movement ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Calculating Soil Moisture ,[object Object],[object Object],[object Object],[object Object],[object Object]
Calculating Soil Moisture ,[object Object],[object Object],[object Object],[object Object],[object Object]
Calculating Soil Moisture ,[object Object],[object Object]
Sample Problem ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Sample Problems ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object]
What Determines Plant Available Water Capacity (AWC) AWC = FC-PWP ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Soil Water Measurement - Water Content ,[object Object],[object Object],[object Object],[object Object]
Soil Water Measurement - Water Potential ,[object Object],[object Object],[object Object]
Soil Consistence & Consistency ,[object Object],[object Object]
Soil Consistence & Consistency ,[object Object],[object Object],[object Object]
Wet Consistence ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Causes of Soil Colors ,[object Object],[object Object],[object Object],[object Object],[object Object]
Causes of Soil Colors ,[object Object],[object Object],[object Object],[object Object]
Soil Color ,[object Object],[object Object],[object Object]
Soil Color ,[object Object],[object Object],[object Object],[object Object],[object Object]
Soil Colors and Soil Attributes Soil Color Soil Attributes Brown to black (surface horizon) Accumulation of OM, humus Black (subsoil) Accumulation of Mn Parent material (e.g. basalt) Yellow to reddish Fe 3+   Well-aerated soils
Soil Colors and Soil Attributes Soil Color Soil Attributes Gray, bluish-green Fe 2+ Poorly drained soils White to gray Accumulation of salts White to gray Parent material: marl, quartz

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Review A 08

  • 1. PRINCIPLES OF SOIL SCIENCE Soil Science 1 To my Baby Sister “shannon kamille Matalog”.. Hehe… :D
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  • 17. Classification of some igneous rocks in relation to mineralogical composition and rock texture. Rock Texture Light-colored Minerals Dark-colored Minerals Feldspars, muscovite Quartz Hornblende, augite, biotite Coarse Granite Diorite Gabbro Peridotite/ Horblendite Inter-mediate Rhyolite Andesite Basalt Fine Felsite/Obsidian Basalt glass
  • 18. Some of the More Important Sedimentary and Metamorphic Rocks and the Dominant Minerals Dominant Mineral Sedimentary Metamorphic Calcite CaCO 3 Dolomite CaCO 3 .MgCO 3 Quartz SiO 2 Clays Variable Variable Limestone Dolomite Sandstone Shale Conglomerate Marble Marble Quartzite Slate Gneiss Schist
  • 19. The More Important Minerals Found in Soils Listed in Order of Decreasing Resistance to Weathering (1) Primary Minerals Secondary Minerals Quartz SiO 2 Muscovite K Al 3 Si 3 O 10 (OH) 2 Microcline K AlSi 3 O 8 Orthoclase K AlSi 3 O 8 Goethite Fe OOH Hematite Fe 2 O 3 Gibbsite Al 2 O 3 .3H 2 O Clay minerals (Al silicates)
  • 20. The More Important Minerals Found in Soils Listed in Order of Decreasing Resistance to Weathering (2) Primary Minerals Secondary Minerals Biotite K Al( Mg,Fe ) 3 (AlSiO 3 O 10 )(OH) 2 Albite NaAlSi 3 O 8 Hornblende Ca 2 Al 2 Mg 2 Fe 3 Si 6 O 22 (OH) 2 Augite Ca 2 (Al, Fe) 4 ( MgFe ) 4 Si 6 O 24 Anorthite Ca Al 2 Si 2 O 8 Olivine ( Mg,Fe ) 2 SiO 4 Dolomite ( Ca CO 3 . Mg CO 3 ) Calcite ( Ca CO 3 ) Gypsum ( CaS O 4 .2H 2 O)
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  • 29. Origin of residual materials and soil texture Origin Texture Basalt, andesite, volcanic tuff Clayey soils Granite, coarse sandstones Loamy and sandy Siltstones, fine-grained sandstones Silt loam and silty clay loam textures
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  • 39. n - sodium accumulation p - plowing - only used with A q - silica accumulation - very weathered or old soil r - soft rock - used with C or Cr s – an accumulation of illuvial iron t – accumulation of illuvial clay w - color or structure development (Bw) x - Fragipan - hard, dense layer that developed with time y - gypsum accumulation (CaSO 4 ) z – accumulation of soluble salts Lowercase letter symbols (cont’d).
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  • 83. Soil Colors and Soil Attributes Soil Color Soil Attributes Brown to black (surface horizon) Accumulation of OM, humus Black (subsoil) Accumulation of Mn Parent material (e.g. basalt) Yellow to reddish Fe 3+ Well-aerated soils
  • 84. Soil Colors and Soil Attributes Soil Color Soil Attributes Gray, bluish-green Fe 2+ Poorly drained soils White to gray Accumulation of salts White to gray Parent material: marl, quartz