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The science and management

              of



      soil biology
            Joel Gruver
          WIU Agriculture
        j-gruver@wiu.edu
                            The Furrow
Is conventionally
 managed soil a
 biological ghost
      town?
Microherd
 Even soils receiving intensive tillage
and chemical inputs contain billions of
      bacteria per gram of soil

                                          Phil Brookes
The soil beneath our feet may be teeming with a hundred
 times more species of bacteria than previously thought,
       according to biologists in New Mexico, US.

  Measuring the bacterial biodiversity of soil is difficult
because only a few species can be cultured, according to
     Jason Gans of the Los Alamos National Lab.

   Fortunately, biologists can also estimate biodiversity
using a technique called DNA reassociation. This involves
 chemically unzipping the two strands of all the bacterial
 DNA in a sample, mixing them up and seeing how long
    they take to join up again with matching partners.
Their results reveal that there are a few
very common species in soil but lots of rare      SSSA
  species. "There is a very large number of
  low abundance species," says Gans. So
many rare species, in fact, that the estimate
 of bacterial biodiversity rises to ~ 1 million
           species per gram of soil.
How much of the C in these corn stalks
will return to the atmosphere within 1
                  year?

                           > 75%


 This is not possible without an active
          microbial community
Which trajectory for
                                SOM is most common      C
                                     in the US?
                                                        B


                                                        A




150 b/a
                 How is it possible for
                   residue levels to
    Corn yield




                 increase > 3x without
                    building SOM?
30 b/a


                                      1950
Broadbalk continuous wheat experiment
                                     Data modelled by RothC-26.3 (solid lines)

                   100
                           Organic C in soil NPK systems are both producing > 100 bu/a wheat
                            The manure and
                              (t C ha-1)                      Farmyard manure annually
                   80
Soil C (tons/ha)




                   60
                                                        Why has the NPK program
                                                      resulted in so little increase in
                   40
                                                                   SOM?                     NPK



                   20                                                               unfertilized
                                                                                   Unmanured


                    0
                    1820      1840     1860   1880   1900   1920    1940    1960     1980    2000   2020
                                                            Year
The current OM level in a soil is a
  result of the long-term balance
between organic inputs and outputs
The current OM level in a soil is a
  result of the long-term balance
between organic inputs and outputs


                        Organic outputs



   Yield enhancing practices will not build
       SOM if OM outputs increase at a
        comparable rate to OM inputs
Drainage + Tillage + Lime + N + harvest = Accelerated loss of SOM



 ”But with the removal of water through furrows, ditches, and
    tiles, and the aeration of the soil by cultivation, what the
 pioneers did in effect was to fan the former simmering fires…
      into a blaze of bacterial oxidation and more complete
   combustion. The combustion of the accumulated organic
 matter began to take place at a rate far greater than its annual
 accumulation. Along with the increased rate of destruction of
  the supply accumulated from the past, the removal of crops
lessened the chance for annual additions. The age-old process
was reversed and the supply of organic matter in the soil began
              to decrease instead of accumulating.”

            William Albrecht – 1938 Yearbook of Agriculture
How do these soils differ ??




                                  manure
                                cover crops
          crop residues        crop residues




20 years of similar tillage and total organic
input but different types of organic inputs
                                       Rodale Institute Farming Systems Trial
Granular crumb structure                        Poor structure




              The development of
               crumb structure is
                  a key step in
                 retaining SOM



       http://www.grdc.com.au/growers/gc/gc48/conference1.htm
We are well aware that a poorly
      balanced diet for humans results in
          heart disease, tooth decay,
            obesity… what are the
        consequences of feeding soil a
             “white bread” diet?

White bread diet for soil = very little diversity of organic inputs
Unfortunately this is the
            norm in agriculture
                 today :-<



 Acute
  root
          VS.
disease



                Chronic root
                malfunction
Dramatic effect of steam
sterilization and compost on
  growth of pepper plants
The digestive
 capacity of soil
microorganisms
greatly exceeds
organic inputs to
     soils.


      http://picturethis.pnl.gov/im2/8208417-5cn0/8208417-5cn.jpg
So
    why does
 organic matter
accumulate at all
    in soil?
In the long run
Nature, October 2011




 …it remains largely unknown why some SOM persists for
   millennia whereas other SOM decomposes readily…
    Recent analytical and experimental advances have
  demonstrated that molecular structure alone does not
control SOM stability: in fact, environmental and biological
                 controls predominate…
Mined humate products may
have value but are not the
same as old soil organic matter




                                   The traditional concept of
                                      large stable humus
                                      molecules has been
                                  rejected by most scientists
Organic matter accumulates under anaerobic conditions


     Blackland soils of
      North Carolina




                                        Lily (1981)
                   > 1 million acres
Impact of temperature on SOM accumulation


                             Organic matter accumulates
                             in climates that support high
                             biomass production but limit
  Organic matter dynamics




                                    decomposition




                                                       Temperature
Brady and Weil (2002)
Organic matter production   Impact of temperature on plant growth




                                               Temperature
Brady and Weil (2002)
Organic matter consumption   Impact of temperature on decomposition




                                                 Temperature
Brady and Weil (2002)
Visualizing soil
habitat at biologically
   relevant scales
Worm’s eye view?
Nematode’s eye view?
Bacteria occupy
< 5 % of soil surfaces
  and < 0.1% of soil
      porosity
              Visualizing soil habitat at
                   relevant scales
Most of the pores where soil
microorganisms reside are either
environmentally suppressive or
 lacking in suitable substrates.
Microorganisms have very limited ability to
       move within the soil matrix.
As a result,
    soil is a very sleepy place !




osmobiosis         anhydrobiosis
                                     thermobiosis
     anoxybiosis
                               cryobiosis
Most soil microorganisms are
     in a dormant state
           waiting…
For their prince charmings
         to arrive !
Roots

      Rain



  There are many types of prince charmings !


                                       Tillage




Organic Amendments
Dormant earthworm




             SSSAJ 69(3) cover
Earthworm cocoons
offer much more protection




http://soils.usda.gov/sqi/soil_quality/soil_biology/images/CE8a-cocoon_LR_small.jpg
Most plants in your
soils are in a state
   of dormancy
Seed dormancy    than
is much better   microbial
understood       dormancy
Who lives in the soil?
                Bacteria
 Body size      Fungi        Microflora
increasing      Algae
                Protozoa         Microfauna
                Nematodes
                Microarthropods         Mesofauna
                Enchytraeids
                Earthworms                 Macrofauna
                Ants, termites, spiders
                Mollusks
                                                Megafauna
                Others: rodents, snakes,
                  voles, amphibians, etc.
Most soil organisms widely in size
    Soil organisms vary are tiny !!!

               Bacteria
               Fungi        Microflora aka microbes
               Algae
               Protozoa         Microfauna
               Nematodes
               Microarthropods       Mesofauna
               Enchytraeids
               Earthworms
               Ants, termites, spiders
                                           Macrofauna
               Mollusks
               Others: rodents, snakes,       Megafauna
Abundance        voles, amphibians, etc.
Soil
   microbes
   carry out
  > 90% of all
decomposition
Soil animals have a
 disproportionate impact on
nutrient cycling, energy fluxes
       and plant growth
Soil animals are mobile
   but have limited digestive ability

Soil microbes are relatively immobile
      but have almost unlimited
           digestive ability
  fungi                         bacteria
3 main types of digestive interactions
occur between soil animals and microbes
Microbivory



             +                  NH4+
       NH4

                        NH4+



                 NH4+                  NH4+

                                NH4+            I want some
                                                bacteria for
                                                   lunch !
 Microfauna (e.g. protozoa and nematodes)
harness the microbes’s digestive abilities by
             grazing on them
External
                    rumen
                   digestion

When mesofauna feed on fresh litter, their fecal
pellets contain shredded, moistened and mixed
         but largely undigested residues

Reingestion of fecal pellets after a few days of
microbial activity greatly increases assimilation
Many
microarthropods
 use this digestive
      strategy
Leaf cutter ants are a more
  well known example of
 external rumen digestion
Internal rumen digestion
greatly enhances utilization
 of complex substrates by
      soil macrofauna
Macrofauna are also
ecosystem engineers
Do roots and
macrofauna play
similar ecological
      roles?
Microbial activation                    Structural modification


                           bacteria
                           root hair


                           rhizoplane




 Structural modification                   Microbial activation
Navigating the rhizosphere

       Rhizoplane                 End of the rhizosphere
   Endo-                                         Root free soil
Rhizosphere         Ecto-Rhizosphere




                        > 100 X
                       microbial
                        activity




                                                   (Lavelle and Spain, 2001)
Why do roots have a priming effect?


           Aggregate    Release of protected
           Disruption      organic matter
Growing                                               Priming
 Root                                                 Effect
            Exudation     Activation of
                         microorganisms




                                          (Lavelle and Spain, 2001)
Soil                                                   in
 organisms
    are                                                 HOT
concentrated
                                                    SPOTS !




           drilosphere            porosphere




   detritusphere    aggregatusphere          rhizosphere

                                      Adapted from Coleman et al. (19??)
casts                 middens




        Drilosphere
          Zone of
        earthworm
         influence
Detritusphere

        fungi



surface residue zone
Clean tillage
eliminates the
detritusphere




      Many soil organisms prefer to
           feed at the surface
3 main
               strategies for
Conservation   managing soil    Augmentation
                  biology




               Activation
Not all earthworms are sensitive to tillage…




but the ones that make vertical burrows
that connect the topsoil and subsoil are…
Earthworm functional
              continuum


Epigeic        Anecic      Endogeic
 worms           worms         worms
Myco = fungus        Mycorrhizal diversity
Rhiza = root
                           Ectomycorrhizae
                          Most woody plants

                                                AM endomycorrhizae

                                               Most herbaceous
    Arbutoid                                    plants including
    mycorrhizae                                  corn and soybeans




        Ericoid
        endomycorrhizae

                                        Orchid endomycorrhizae




                                                 Lavelle and Spain (2001)
Mycorrhizal Networks: Connecting
     plants intra- and interspecifically
                                       •Many plants are
                                       connected
                                       underground by
                                       mycorrhizal hyphal
                                       interconnections.

                                        •Mycorrhizal fungi
                                        are not very host
                                             specific.

 Illustration by Mark Brundrett

           Mycorrhizal inoculants are available
but conservation of established networks is more important
Increase nutrient uptake              suppress pathogens
     (especially P)




                       Mycorrhizae
Mediate plant competition            Improve soil structure




                                Glomalin
                               Superglue
                               of the soil ??
Are you conserving the beneficial
    fungi on your crop foliage?
Frogeye leafspot fungus resistance to strobilurin
chemistry a concern for Mid-South soybean growers
Hembree Brandon - Mar. 2, 2011 5:36am

Add another to the growing list of weeds, insects, and diseases that have
developed resistance to the chemicals that farmers rely on to control pests and
protect yields — strobilurin-resistant Cercospora sojina, the fungus that causes
frogeye leafspot in soybeans.

The strobilurin chemistry has been widely used as a first line of defense in
preventing yield loss from Frogeye leafspot.

―There was documentation in 2010 of strobilurin-resistant Cercospora in Illinois,
Kentucky, and Tennessee,‖ Tom Allen said at the annual conference of the
Mississippi Agricultural Consultants Association.
Roots

      Rain
   Irrigation

       Biological activation strategies


                                          Tillage




Organic Amendments
Innovative cover cropping
 is a great way to activate
     your soil biology!!
Bio-strip till
attempt #1
September 2008
Attempt #3




Radish planted on 30” rows using milo plates
            in mid-August 2010
Corn following cover crop experiment in
 2011 at the WIU Organic Research Farm

                                  Relative
   Cover crop system
                                 corn yield
    Volunteer oats                 79%
Radishes planted on 30‖            99%
Radishes drilled on 7.5‖           91%

   Corn planted on radish rows
Wheat + radish trial at the Allison farm
           November 2010


       3 lb/a = 2 lb/a = 1 lb/a > 0 lb/c
           ~ 2.5 bu/a yield boost



     Is this an activation effect?
Have you tried any
              biological seed
               treatments?



Augmenting soil biology
Old school inoculation
http://www.beckerunderwood.com/en/pages/scienceofinoculation
VOTiVO contains a naturally occurring soil bacteria, or rhizobacteria, that live
  and grow with the plant’s root system. The bacteria creating a biofilm that
  becomes a living barrier limiting the number of receptor sites which could
 otherwise be occupied by plant pathogens such as nematodes. Nematodes
  use gaseous and solid exudates from the root as means to detect a root’s
   proximity, so reduced levels of exudates can decrease the ability of the
   nematodes to locate the receptor sites on the roots. The bacteria further
   reduce viable nematode populations by consuming exudates, depriving
         nematodes of an additional source of energy and nutrients.
competition              parasitism




 Ask vendors to explain specifically
     how their product works!




antibiosis             induced resistance
Do recognize this scene?




      If you build it, they will come…
The most important biological management strategy

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Science and management of soil biology

  • 1. The science and management of soil biology Joel Gruver WIU Agriculture j-gruver@wiu.edu The Furrow
  • 2.
  • 3.
  • 4.
  • 5.
  • 6.
  • 7. Is conventionally managed soil a biological ghost town?
  • 8. Microherd Even soils receiving intensive tillage and chemical inputs contain billions of bacteria per gram of soil Phil Brookes
  • 9. The soil beneath our feet may be teeming with a hundred times more species of bacteria than previously thought, according to biologists in New Mexico, US. Measuring the bacterial biodiversity of soil is difficult because only a few species can be cultured, according to Jason Gans of the Los Alamos National Lab. Fortunately, biologists can also estimate biodiversity using a technique called DNA reassociation. This involves chemically unzipping the two strands of all the bacterial DNA in a sample, mixing them up and seeing how long they take to join up again with matching partners.
  • 10. Their results reveal that there are a few very common species in soil but lots of rare SSSA species. "There is a very large number of low abundance species," says Gans. So many rare species, in fact, that the estimate of bacterial biodiversity rises to ~ 1 million species per gram of soil.
  • 11. How much of the C in these corn stalks will return to the atmosphere within 1 year? > 75% This is not possible without an active microbial community
  • 12. Which trajectory for SOM is most common C in the US? B A 150 b/a How is it possible for residue levels to Corn yield increase > 3x without building SOM? 30 b/a 1950
  • 13. Broadbalk continuous wheat experiment Data modelled by RothC-26.3 (solid lines) 100 Organic C in soil NPK systems are both producing > 100 bu/a wheat The manure and (t C ha-1) Farmyard manure annually 80 Soil C (tons/ha) 60 Why has the NPK program resulted in so little increase in 40 SOM? NPK 20 unfertilized Unmanured 0 1820 1840 1860 1880 1900 1920 1940 1960 1980 2000 2020 Year
  • 14. The current OM level in a soil is a result of the long-term balance between organic inputs and outputs
  • 15. The current OM level in a soil is a result of the long-term balance between organic inputs and outputs Organic outputs Yield enhancing practices will not build SOM if OM outputs increase at a comparable rate to OM inputs
  • 16. Drainage + Tillage + Lime + N + harvest = Accelerated loss of SOM ”But with the removal of water through furrows, ditches, and tiles, and the aeration of the soil by cultivation, what the pioneers did in effect was to fan the former simmering fires… into a blaze of bacterial oxidation and more complete combustion. The combustion of the accumulated organic matter began to take place at a rate far greater than its annual accumulation. Along with the increased rate of destruction of the supply accumulated from the past, the removal of crops lessened the chance for annual additions. The age-old process was reversed and the supply of organic matter in the soil began to decrease instead of accumulating.” William Albrecht – 1938 Yearbook of Agriculture
  • 17. How do these soils differ ?? manure cover crops crop residues crop residues 20 years of similar tillage and total organic input but different types of organic inputs Rodale Institute Farming Systems Trial
  • 18. Granular crumb structure Poor structure The development of crumb structure is a key step in retaining SOM http://www.grdc.com.au/growers/gc/gc48/conference1.htm
  • 19. We are well aware that a poorly balanced diet for humans results in heart disease, tooth decay, obesity… what are the consequences of feeding soil a “white bread” diet? White bread diet for soil = very little diversity of organic inputs
  • 20. Unfortunately this is the norm in agriculture today :-< Acute root VS. disease Chronic root malfunction
  • 21. Dramatic effect of steam sterilization and compost on growth of pepper plants
  • 22. The digestive capacity of soil microorganisms greatly exceeds organic inputs to soils. http://picturethis.pnl.gov/im2/8208417-5cn0/8208417-5cn.jpg
  • 23. So why does organic matter accumulate at all in soil?
  • 24. In the long run
  • 25. Nature, October 2011 …it remains largely unknown why some SOM persists for millennia whereas other SOM decomposes readily… Recent analytical and experimental advances have demonstrated that molecular structure alone does not control SOM stability: in fact, environmental and biological controls predominate…
  • 26. Mined humate products may have value but are not the same as old soil organic matter The traditional concept of large stable humus molecules has been rejected by most scientists
  • 27. Organic matter accumulates under anaerobic conditions Blackland soils of North Carolina Lily (1981) > 1 million acres
  • 28. Impact of temperature on SOM accumulation Organic matter accumulates in climates that support high biomass production but limit Organic matter dynamics decomposition Temperature Brady and Weil (2002)
  • 29. Organic matter production Impact of temperature on plant growth Temperature Brady and Weil (2002)
  • 30. Organic matter consumption Impact of temperature on decomposition Temperature Brady and Weil (2002)
  • 31. Visualizing soil habitat at biologically relevant scales
  • 34. Bacteria occupy < 5 % of soil surfaces and < 0.1% of soil porosity Visualizing soil habitat at relevant scales
  • 35. Most of the pores where soil microorganisms reside are either environmentally suppressive or lacking in suitable substrates.
  • 36. Microorganisms have very limited ability to move within the soil matrix.
  • 37. As a result, soil is a very sleepy place ! osmobiosis anhydrobiosis thermobiosis anoxybiosis cryobiosis
  • 38. Most soil microorganisms are in a dormant state waiting…
  • 39. For their prince charmings to arrive !
  • 40. Roots Rain There are many types of prince charmings ! Tillage Organic Amendments
  • 41. Dormant earthworm SSSAJ 69(3) cover
  • 42. Earthworm cocoons offer much more protection http://soils.usda.gov/sqi/soil_quality/soil_biology/images/CE8a-cocoon_LR_small.jpg
  • 43. Most plants in your soils are in a state of dormancy
  • 44. Seed dormancy than is much better microbial understood dormancy
  • 45. Who lives in the soil?  Bacteria Body size  Fungi Microflora increasing  Algae  Protozoa Microfauna  Nematodes  Microarthropods Mesofauna  Enchytraeids  Earthworms Macrofauna  Ants, termites, spiders  Mollusks Megafauna  Others: rodents, snakes, voles, amphibians, etc.
  • 46. Most soil organisms widely in size Soil organisms vary are tiny !!!  Bacteria  Fungi Microflora aka microbes  Algae  Protozoa Microfauna  Nematodes  Microarthropods Mesofauna  Enchytraeids  Earthworms  Ants, termites, spiders Macrofauna  Mollusks  Others: rodents, snakes, Megafauna Abundance voles, amphibians, etc.
  • 47. Soil microbes carry out > 90% of all decomposition
  • 48. Soil animals have a disproportionate impact on nutrient cycling, energy fluxes and plant growth
  • 49. Soil animals are mobile but have limited digestive ability Soil microbes are relatively immobile but have almost unlimited digestive ability fungi bacteria
  • 50. 3 main types of digestive interactions occur between soil animals and microbes
  • 51. Microbivory + NH4+ NH4 NH4+ NH4+ NH4+ NH4+ I want some bacteria for lunch ! Microfauna (e.g. protozoa and nematodes) harness the microbes’s digestive abilities by grazing on them
  • 52. External rumen digestion When mesofauna feed on fresh litter, their fecal pellets contain shredded, moistened and mixed but largely undigested residues Reingestion of fecal pellets after a few days of microbial activity greatly increases assimilation
  • 53. Many microarthropods use this digestive strategy
  • 54. Leaf cutter ants are a more well known example of external rumen digestion
  • 55. Internal rumen digestion greatly enhances utilization of complex substrates by soil macrofauna
  • 57. Do roots and macrofauna play similar ecological roles?
  • 58. Microbial activation Structural modification bacteria root hair rhizoplane Structural modification Microbial activation
  • 59. Navigating the rhizosphere Rhizoplane End of the rhizosphere Endo- Root free soil Rhizosphere Ecto-Rhizosphere > 100 X microbial activity (Lavelle and Spain, 2001)
  • 60. Why do roots have a priming effect? Aggregate Release of protected Disruption organic matter Growing Priming Root Effect Exudation Activation of microorganisms (Lavelle and Spain, 2001)
  • 61. Soil in organisms are HOT concentrated SPOTS ! drilosphere porosphere detritusphere aggregatusphere rhizosphere Adapted from Coleman et al. (19??)
  • 62. casts middens Drilosphere Zone of earthworm influence
  • 63. Detritusphere fungi surface residue zone
  • 64. Clean tillage eliminates the detritusphere Many soil organisms prefer to feed at the surface
  • 65. 3 main strategies for Conservation managing soil Augmentation biology Activation
  • 66. Not all earthworms are sensitive to tillage… but the ones that make vertical burrows that connect the topsoil and subsoil are…
  • 67. Earthworm functional continuum Epigeic  Anecic  Endogeic worms worms worms
  • 68. Myco = fungus Mycorrhizal diversity Rhiza = root Ectomycorrhizae Most woody plants AM endomycorrhizae Most herbaceous Arbutoid plants including mycorrhizae corn and soybeans Ericoid endomycorrhizae Orchid endomycorrhizae Lavelle and Spain (2001)
  • 69. Mycorrhizal Networks: Connecting plants intra- and interspecifically •Many plants are connected underground by mycorrhizal hyphal interconnections. •Mycorrhizal fungi are not very host specific. Illustration by Mark Brundrett Mycorrhizal inoculants are available but conservation of established networks is more important
  • 70. Increase nutrient uptake suppress pathogens (especially P) Mycorrhizae Mediate plant competition Improve soil structure Glomalin Superglue of the soil ??
  • 71. Are you conserving the beneficial fungi on your crop foliage?
  • 72. Frogeye leafspot fungus resistance to strobilurin chemistry a concern for Mid-South soybean growers Hembree Brandon - Mar. 2, 2011 5:36am Add another to the growing list of weeds, insects, and diseases that have developed resistance to the chemicals that farmers rely on to control pests and protect yields — strobilurin-resistant Cercospora sojina, the fungus that causes frogeye leafspot in soybeans. The strobilurin chemistry has been widely used as a first line of defense in preventing yield loss from Frogeye leafspot. ―There was documentation in 2010 of strobilurin-resistant Cercospora in Illinois, Kentucky, and Tennessee,‖ Tom Allen said at the annual conference of the Mississippi Agricultural Consultants Association.
  • 73. Roots Rain Irrigation Biological activation strategies Tillage Organic Amendments
  • 74. Innovative cover cropping is a great way to activate your soil biology!!
  • 76. Attempt #3 Radish planted on 30” rows using milo plates in mid-August 2010
  • 77.
  • 78. Corn following cover crop experiment in 2011 at the WIU Organic Research Farm Relative Cover crop system corn yield Volunteer oats 79% Radishes planted on 30‖ 99% Radishes drilled on 7.5‖ 91% Corn planted on radish rows
  • 79. Wheat + radish trial at the Allison farm November 2010 3 lb/a = 2 lb/a = 1 lb/a > 0 lb/c ~ 2.5 bu/a yield boost Is this an activation effect?
  • 80. Have you tried any biological seed treatments? Augmenting soil biology
  • 83.
  • 84.
  • 85. VOTiVO contains a naturally occurring soil bacteria, or rhizobacteria, that live and grow with the plant’s root system. The bacteria creating a biofilm that becomes a living barrier limiting the number of receptor sites which could otherwise be occupied by plant pathogens such as nematodes. Nematodes use gaseous and solid exudates from the root as means to detect a root’s proximity, so reduced levels of exudates can decrease the ability of the nematodes to locate the receptor sites on the roots. The bacteria further reduce viable nematode populations by consuming exudates, depriving nematodes of an additional source of energy and nutrients.
  • 86.
  • 87. competition parasitism Ask vendors to explain specifically how their product works! antibiosis induced resistance
  • 88. Do recognize this scene? If you build it, they will come… The most important biological management strategy