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Tim Reinbott
Bradford Research Center
College of Food and Natural
Resources
 Loss of Organic
Matter
• Soil structure
• Soil microbial biomass
 Release of CO2
 Soil Erosion
 Why Till?
• Weed Control
 This is what separates us
(Missouri) from Central Iowa,
Illinois, Minnesota, Indiana, etc
 In these areas climatic
conditions favor the
accumulation of Organic Matter
• Slower breakdown, long
history of deep rooted native
perennial plants
 SOM is derived from
• Plant residue (both
litter and roots)
• Animal remains and
excreta
• Living soil microbes
(microbial biomass)
 Over time fresh
organic material is
transformed into soil
organic matter
Crop
Residues
Bacteria
Fungi
Actinobacteria
SOM
8
20 – 40% of SOM is lost on cultivation
Management effects on SOM
• Tillage (disturbance) 
• Chemical Fertilization 
• Manure 
• Residue Retention 
• Crop 
• Crop Rotation 
• Cover Crop 
10
Decline in SOC from Sanborn
Field Plots showing increase
following the return of residues
beginning in 1950
Soil Micro Organisms
Soil Life (macro)
Help create soil structure and
break down larger plant
residues
• Earthworms
• Nematodes
• Beetles
• Ants
• Termites
• Springtails
One tablespoon of soil has approximately 1
billion soil microbes:
• Bacteria: 3,000,000 to 500,000,000
• Actinobacteria: 1,000,000 to 20,000,000
• Fungi: 5,000 to 1,000,000
• Yeast: 1,000 to 1,000,000
• Protozoa: 1,000 to 500,000
• Algae: 1,000 to 500,000
• Nematodes: 10 to 5,000
The soil microbes in the plow layer
has the mass equivalent of two
cows (2400 lbs) per acre that need
to be fed
Soil organisms are
much like cows, they
need inputs of plant
residues for food
and energy
Specifically, they
need the carbon that
is contained in plant
residue and soil
organic matter
 ManuresCompost
 Aerobic
• Earthy Smell
 -much of the nutrients are
kept in the compost and
not released
 Anaerobic
• Acidic smell
-release of methane
and Nitrous Oxide
26
Buckwheat
Crimson Clover
Oats
Early May Late May
LONG TERM PASTURE
TILLED IN A
CORN/SOYBEAN/WHEAT ROTATION
Scientists describe 3 pools of soil organic matter
**really is a continuum of decomposition
41
Passive SOM
500 – 5000 yrs
C/N ratio 7 – 10
Active SOM
1 – 2 yrs
C/N ratio 15 – 30
Slow SOM
15 – 100 yrs
C/N ratio 10 – 25
• Recently deposited organic material
• Rapid decomposition
• 10 – 20% of SOM
• Intermediate age organic material
• Slow decomposition
• 10 – 20% of SOM
• Very stable organic
material
• Extremely slow
decomposition
• 60 – 80% of SOM
Results are read in a spectrometer in lab or
field or from a color card
Potassium
Permanganate Test
KMnO4 oxidizes active carbon. The
purple color of the chemical
changes to pink the more active
carbon there is in a soil sample.
No-Till With Cover Crops
No-Till In A Corn/Soybean Rotation
Tilled Each Year in a Corn/Soybean Rotation
Fencerow
Native Warm Season Grass
Cool Season Grass Mix
Restored Native Prairie
Tilled No-Till No-Till w/ Cover Crops
Healthier
Soil!
What Could
She Have
Done?
Tim Reinbott
884-7945
Bradford.cafnr.org

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Cover Crops, compost, and no-till. A formula for good soil health

  • 1. Tim Reinbott Bradford Research Center College of Food and Natural Resources
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  • 6.  Loss of Organic Matter • Soil structure • Soil microbial biomass  Release of CO2  Soil Erosion  Why Till? • Weed Control
  • 7.  This is what separates us (Missouri) from Central Iowa, Illinois, Minnesota, Indiana, etc  In these areas climatic conditions favor the accumulation of Organic Matter • Slower breakdown, long history of deep rooted native perennial plants
  • 8.  SOM is derived from • Plant residue (both litter and roots) • Animal remains and excreta • Living soil microbes (microbial biomass)  Over time fresh organic material is transformed into soil organic matter Crop Residues Bacteria Fungi Actinobacteria SOM 8
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  • 10. 20 – 40% of SOM is lost on cultivation Management effects on SOM • Tillage (disturbance)  • Chemical Fertilization  • Manure  • Residue Retention  • Crop  • Crop Rotation  • Cover Crop  10 Decline in SOC from Sanborn Field Plots showing increase following the return of residues beginning in 1950
  • 12. Soil Life (macro) Help create soil structure and break down larger plant residues • Earthworms • Nematodes • Beetles • Ants • Termites • Springtails
  • 13. One tablespoon of soil has approximately 1 billion soil microbes: • Bacteria: 3,000,000 to 500,000,000 • Actinobacteria: 1,000,000 to 20,000,000 • Fungi: 5,000 to 1,000,000 • Yeast: 1,000 to 1,000,000 • Protozoa: 1,000 to 500,000 • Algae: 1,000 to 500,000 • Nematodes: 10 to 5,000
  • 14. The soil microbes in the plow layer has the mass equivalent of two cows (2400 lbs) per acre that need to be fed Soil organisms are much like cows, they need inputs of plant residues for food and energy Specifically, they need the carbon that is contained in plant residue and soil organic matter
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  • 22.  Aerobic • Earthy Smell  -much of the nutrients are kept in the compost and not released  Anaerobic • Acidic smell -release of methane and Nitrous Oxide
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  • 40. LONG TERM PASTURE TILLED IN A CORN/SOYBEAN/WHEAT ROTATION
  • 41. Scientists describe 3 pools of soil organic matter **really is a continuum of decomposition 41 Passive SOM 500 – 5000 yrs C/N ratio 7 – 10 Active SOM 1 – 2 yrs C/N ratio 15 – 30 Slow SOM 15 – 100 yrs C/N ratio 10 – 25 • Recently deposited organic material • Rapid decomposition • 10 – 20% of SOM • Intermediate age organic material • Slow decomposition • 10 – 20% of SOM • Very stable organic material • Extremely slow decomposition • 60 – 80% of SOM
  • 42. Results are read in a spectrometer in lab or field or from a color card Potassium Permanganate Test KMnO4 oxidizes active carbon. The purple color of the chemical changes to pink the more active carbon there is in a soil sample.
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  • 46. No-Till With Cover Crops No-Till In A Corn/Soybean Rotation Tilled Each Year in a Corn/Soybean Rotation
  • 47. Fencerow Native Warm Season Grass Cool Season Grass Mix Restored Native Prairie
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  • 49. Tilled No-Till No-Till w/ Cover Crops
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