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Soils

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... deposit resting on the mineral soil ... Small biomass of soil animals. Mull (broadleaf) ... Soil animals more diverse = humification. More mixed ... – PowerPoint PPT presentation

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Title: Soils


1
Soils
2
Soil Profiles
  • General soil profile
  • Letters represent horizons
  • Numbers are layers within those horizons
  • Code
  • 0 litter
  • A area of leaching and organic matter
    accumulation
  • B area of accumulation
  • C parent material
  • R bedrock

See Text, Fig. 2.8
3
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4
Soil formation
  • Five main groups of soil forming factors
  • climate (present as well as past
  • vegetation (influenced by climate and soil fauna)
  • parent material
  • type of relief
  • time

5
Mor (coniferous) typical profile
  • Prominent organic deposit resting on the mineral
    soil
  • Sharp distinction between 0 and A horizons
  • Fungi are the main decomposers
  • Small biomass of soil animals

6
Mull (broadleaf) typical profile
  • Bacteria are the chief decomposers
  • Soil animals more diverse gt humification
  • More mixed upper horizons
  • Animal activity also affects the soil porosity

7
0
Gradual change
Mor soil
Mull soil
8
Components of soil
  • Sand (gravel consists of elements over 2 mm)

Silt (.05 - .002 mm)
Clay (less than .002 mm)
Humus (organic)
9
Litter build up
  • Climate effects the amount of litter and humus
    found in an ecosystem.

10
Organic Matter in Soil
  • Benefits of Organic Matter
  • Improves aggregation and structure
  • Improves infiltration
  • Improves water holding capacity
  • Improves rooting environment
  • Slow-release nutrients

11
Spaces for Gas and Water
  • Particle size effects spaces for gases and water.
  • Water movement is dependent on the spaces

12
  • Adhesion and cohesive forces
  • This is called capillary water

13
Water movement in different soils
Distance from center of furrow
Sandy Loam
Clay Loam
14
  • Field capacity vs. gravitational water
  • Hygroscopic water vs. available water

15
Soil Components
16
Nutrient exchange
  • Negative charges on clay micelles, humus
    particles and to a lesser extent on silt
    particles
  • Cations (K,Ca, Mg, etc.) are attracted to
    the negative charges

K
Ca
Ca
Ca
K
K
Ca
Ca
K
17
  • Differences in sand, silt, clay, humus
  • Size and charge of ion vs. tenacity with which it
    is held
  • Order of tenacity with which the cations are
    held
  • H gt Ca gt Mg gt K gt Na

18
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