chapter 7 Flashcards

1
Q

soil organic matter

A

broad term for soil organic materials, including living and dead animals, plants, microorganisms, insects, pests, manures, and crop residues and other organic materials

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2
Q

5 fractions of OM

A

fresh and partly decomposed plant and animal remains
lignin- part of cell wall plants
OM adsorbed on colloids
biomass of microbial cells and by-products
humus

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3
Q

characteristics of humus (1-6)

A
  1. dark brown
  2. complex structure
  3. amorphous
  4. colloidal
  5. resistant to further microbial action
  6. modified lignin, polysaccharides
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4
Q

characteristics of humus (7-12)

A
  1. high specific surface area
  2. colloidal surface are negatively charged (pH dependent)
  3. at high pH, CEC is high (150-300)
  4. OM has 4-5 times higher water-holding capacity
  5. low plasticity and cohesion
  6. C:N ratio ranges bet. 10:1 and 12:1
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5
Q

physical benefits of OM

A
  1. enhanced soil aggregate stability, water infiltration, aeration, reduce run-off
  2. improve water-holding capacity
  3. reduces stickiness, easy to till
  4. reduce surface crusting, seedbed preparation
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6
Q

chemical benefits

A
  1. increase soil CEC
  2. improve buffering capacity
  3. accelerate decomposition of soil minerals
  4. increase N supply capacity
  5. holds organic nutrients (N,P, S) and makes them available to plants
  6. reduces NH3 volatilization in alkaline soils
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7
Q

biological benefits

A
  1. provides foods for organisms
  2. enhances soil microbial biodiversity and activity, helps disease and pests suppression
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8
Q

in summary OM:

A

increases soil fertility
improves soil physical condition
improves microbiological health of soil

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9
Q

sources of OM

A
  1. crop residue
  2. animal manure
  3. compost
  4. cover crops (green manure)
  5. perennial grasses and legumes
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10
Q

factors that affect rate of decomposition

A
  1. nature of organic material
  2. availability of nutrients, particularly N
  3. moisture
  4. aeration
  5. temperature
  6. pH
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11
Q

moisture
aeration
temperature
pH

A

field capacity
aerobes
30-40 C
neutral pH

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12
Q

what destroys OM

A
  1. decrease in biomass production
  2. decrease in OM supply
  3. increased decomposition rates
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13
Q

decrease in biomass production

A
  1. replacement of perennial vegetation
  2. replacement of mixed vegetation with monoculture pf crops and pastures
  3. high harvest index
  4. use of bare fallow
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14
Q

decrease in OM supply

A
  1. burning of natural vegetation and crop residues
  2. overgrazing
  3. removal of crop residues
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15
Q

increased decomposition rates

A
  1. tillage practices
  2. drainage- slow on poorly aerated soils
  3. fertilizers and pesticide use
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16
Q

OM Management

A
  1. use conservation tillage practices
  2. rotation of annual row crops with perennial grasses or legumes
  3. establishment of legume cover crops
  4. avoid soil compaction
  5. zero tillage
  6. agro-forestry
  7. composting
17
Q

relationship between C:N ratio and decomposition rate

A

higher C:N ratio, slower decomposition rate
lower C:N ration, faster decomposition rate