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Factors which affect soil structure

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Factors which affect soil structure Organic Matter Content Soil Organisms Soil Colloids Tillage Freezing and Thawing Water Movement Organic Matter Content May be ... – PowerPoint PPT presentation

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Title: Factors which affect soil structure


1
Factors which affect soil structure
  • Organic Matter Content
  • Soil Organisms
  • Soil Colloids
  • Tillage
  • Freezing and Thawing
  • Water Movement

2
Organic Matter Content
  • May be increased by
  • Adding manure
  • Growing cover crops
  • May be decreased by
  • Tillage
  • Hot,
  • Humid
  • environment

3
Soil Organisms
  • Bacteria in soil have sticky
  • substance on cell wall.
  • This glue holds soil particles
  • to bacteria and to each other.
  • This binds soil particles into larger particles.
  • Fungi produce thread-like structures called
    mycelia which bind soil particles and peds
    making larger particles.

4
Soil Colloids
  • Very small particles with a weak electric charge.
    o o-
  • The charge causes water to bind to particles.
  • As water evaporates, colloids and larger
    particles draw together, creating even larger
    particles.

5
Tillage
  • Positive effect
  • Creates air space in soil, allowing organisms
    needed oxygen
  • Negative effect
  • Disrupts the soil structure and kills the larger
    organisms such as earthworms.
  • If done when too wet or dry, may destroy the soil
    structure of the tillage zone.

6
Freezing and Thawing
  • As water in soil freezes it expands, pushing soil
    particles apart.
  • This opens pore spaces for air.
  • As water thaws, pore spaces tend to remain
    temporarily.
  • This can be enough to encourage soil organisms,
    by allowing more oxygen.

7
Water Movement
  • Positive
  • As water moves vertically through the soil some
    of the water is stored, and can be used by crops.
  • Negative -
  • Vertical movement of water can cause leaching of
    minerals.
  • Vertical movement in soil freshly tilled may
    cause collapse and less pore space.
  • Vertical movement in clay can result in a hard
    pan.
  • Horizontal movement may cause erosion.

8

9
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10
pH
  • pH is the measure of the concentration of
    hydrogen ions.
  • It is measure on a logarithmic scale going from
    1-14 with 1 being the most acidic (most hydrogen
    ions) and 14 the most basic (least hydrogen
    ions).
  • pH of soil is important because certain chemical
    reactions only occur in certain range.
  • Not as important for organic systems, because
    they depend on biological reactions more than
    chemical reactions.
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