The life in the soil is one of my favorite topics. I think it’s importance in cropping system is grossly underestimated. After all without the soil biology there would be no soil. However complex the soil biology is I think that it is best left to mother nature to balance out this ecosystem. That is why we practice a no-till production system. Lots of benefits come with preserving this soil life that you just can’t buy from the crop inputs supplier. I strongly recommend that every person attempting to grow anything in soil find themselves as many publications about soil boilogy like this one from Univeristy of Minnesota Extension titled Soil Scientist. The more you dig into this topic the more you appriciate the value of the soil life. We will be posting great information on this topic.
The Table Below was sourced from the University of Minnesota, Extension web site.
Description |
Size |
Diet |
Typical amt in ag soils |
Action in soil |
Bacteria
|
1 um (0.001 mm) |
Organic matter, especially simple carbon compounds |
100 mil. to 1 bil. in a teaspoon |
Decompose organic matter. Immobilize nutrients in the rooting zone.
|
Fungi
|
A few um wie, yards or miles long |
Organic matter, especially simple carbon compounds. Also, living plants |
Several yards in a teaspoon |
Decompose organic matter.
|
Protozoa
|
5-500 um |
Bacteria, primarily |
Several thousand in a teaspoon |
Stimulate and control growth of bacteria.
|
Nematodes
|
50 um wide, 1 mm long |
Bacteria, fungi, protozoa, other nematodes, and roots |
Ten to twenty in a teaspoon |
Control many disease-causing organisms.
|
Arthropods
|
Microscopic to inches |
All other organisms |
Several hundred in a cubic foot |
Shred plant residue, making it more accessible to bacteria and fungi.
|
Earthworms |
Inch or more long |
Bacteria, fungi, and organic matter |
Five to thirty in a cubic foot |
Shred plant residue.
|