Soil Organic Matter
Section C
Soil Fertility and Plant Nutrition
Review - Soil organisms
• Bacteria– Most numerous, smallest– Aerobic and anaerobic
• Actinomycetes– Share characteristics of bacteria and fungi– Active in degradation of resistant compounds
• Fungi– Aerobic only, filamentous– Active in degradation of resistant compounds
Major Soil Organisms
Bacteria 108/gram
Actinomycetes 107/gram
Fungi 106/gram
Soil Microorganisms
• Can be classified according to C and energy sources and their oxygen requirement:– photoautotrophs
• Energy from sunlight & C from CO2
• Some bacteria and algae only– chemoautotrophs
• Energy from oxidizing inorganic material, C from CO2
• Some bacteria only– chemoheterotrophs
• Energy and C from oxidation of organic materials• Most bacteria, all fungi and actinomycetes
Soil Microorganisms• Oxygen requirement
– aerobic• Require free O2 for respiration
• All fungi and actinomycetes, most bacteria
– anaerobic• Must use alternative electron acceptors instead of O2
– NO3 -, SO4 2-, Fe3+ , CO2
• Some bacteria are anaerobic
– facultative• Can be aerobic or anaerobic. Some bacteria
Decomposition of Plant Residues(Under aerobic conditions)
PlantResidues
CO2
NH4+, SO4
2-, etc. (inorganic waste)
Humus (organic waste)
+DeadMicroorganisms
More microbial biomass
Soil Organic Matter
• Soil organic matter: all organic matter in the soil, including humus, microbial biomass, and plant and animal residues in various stages of decomposition.– Composed of a wide range of organic
materials, from highly decomposable to resistant to decomposition.
Roles of Soil Organic Matter
• Microbial substrate• Nutrient reserve (esp. N, P, S)• CEC • Water-Holding capacity• Soil structure
Humus
• The stable portion of soil organic matter that results from microbial degradation of residues.– Dark colored– About 58% C, 5% N– Complex chemical structure, aromatic plus
aliphatic functional groups– Difficult to break down because of structure– high CEC
Humus
• The major organic “waste” by-product of OM degradation.
• The percentage of a residue that will become humus is approx. proportional to its lignin content.
Lignin
Humus
Carbon
Hydrogen
Oxygen
Nitrogen
Decomposition of Organic Matter
• Organic materials are decomposed by heterotrophic microorganisms. The organic matter is a source of _______, __________, and _____________ to these organisms.
carbon
energy nutrients
Humus and Nutrients
• Humus contains about 58% C, 5%N, 0.6% P, and 0.6% S
• How much humus in soils?
• How much OM does this represent?An Aridisol with 0.5% SOM in the top 30 cm will contain 3000 m3/ha x 1500 kg/m3 x 0.005 = 22,500 kg/ha (top 30 cm)
A Mollisol with 5.0% SOM in the top 30 cm will contain 3000 m3/ha x 1500 kg/m3 x 0.05 = 225,000 kg/ha (top 30 cm)
An Aridisol might contain 0.5% SOM by weight, a Mollisol 3-5% by weight
Decomposition of Humus• The rate of decomposition of humus is most strongly
affected by soil moisture and temperature (<1 to >5%/yr).
• Humus is chemically complex and has a C:N ratio of about 11:1
• High soil temperatures, abundant (but not excessive) moisture encourages “rapid” humus breakdown
• In soils where OM content is not decreasing, synthesis of “new” humus approximately equals decomposition of “old” humus.
Decomposition (Mineralization) of Humus
• Releases N as NH4+ , available for plants
• If 2.5% of the N in SOM is mineralized each year, how much N would be released for plant uptake?
• Aridisol (from previous example)– 22,500 kg SOM/ha x 0.05 kg N/kg SOM x 0.025 (% min)
= 28 kg N/ha
• Mollisol (from previous example)– 225,000 kg SOM/ha x 0.05 kg N/kg SOM x 0.025 (%
min) = 280 kg N/ha
Decomposition of Plant Residues(Under aerobic conditions)
PlantResidues
CO2
NH4+, SO4
2-, etc. (inorganic waste)
Humus (organic waste)
+DeadMicroorganisms
More microbial biomass
What Happens to Residues?
CO2
Biomass
Waste
CO2
Biomass
Waste
Chemically simple residues
Chemically complexresidues
Decomposition of Plant Material
• The rate of decomposition of plant residues is governed mostly by:– Chemical makeup of the residue– C:N ratio– Available soil N– Temperature, moisture, oxygen, and other
environmental conditions that affect microbial growth
Chemical Composition of Plant Residues
Sugars Complex proteins Hemicellulose Cellulose LigninSimple proteins WaxesStarchs
Increasing chemical complexity
Increasing rate of decomposition
C:N Ratio
• Why is the C:N ratio important?– Microorganisms need C and N in fixed ratios,
because C and N are used to synthesize proteins, nucleic acids, etc.
– Bacterial cell C:N is 5:1 to 8:1. Since about 50% of the C in an organic material is converted to CO2, they need roughly a C:N of 10:1 to 16:1 in the residue they consume.
– Fungi need a C:N of about 40:1 in their diet
decomposition
C:N Ratio
50 g C20 g as CO2
20 g as biomass
Microbial biomass has an averageC:N of 10:1, therefore how much Nis needed to balance the new biomassC?
10 g as waste
2 g
Therefore, if the residuecontaining 50 g of Ccontains < 2 g of N (C:N>25:1), it will haveinsufficient N for microbial needs. What about >2 g N (C:N <25:1)
C:N Ratios
• High C:N material:– Woody – Grain crop residue– Mature plant tissues
• Low C:N material:– Green– Young plant tissues– Legume residues– Composts– Manures
C:N Ratio and Residue Mgmt.
• What are the implications of the C:N ratio of crop residues for nutrient management?
Immobilization
The conversion of inorganic (available) N (NH4+, NO3
-) to microbial biomass N. Results from...
NH
4+ a
nd
NO
3- )
Time
CO
2 rele
ase
C:N ratio of residues
Mineralization
The conversion of organic (unavailable) N to NH4+ .
Results from...
NH
4+
Time
CO
2 rele
ase
C:N ratio of residues
Soil Organic Matter Content
• In “undisturbed” soils:SOM = f (I, O)– Inputs = plant residues– Outputs = decomposition, erosion
• In managed soils:SOM = f (I, O, M)– M = management practices such as tillage,
cultivation ,residue management, etc.
Soil Organic Carbon
Soil Organic Matter Content
• The amount of organic matter in a soil tends to be difficult to change, and reflects an equilibrium between additions and losses over long periods of time.
• In the absence of changes in management or climate, soil organic matter content tends to remain relatively constant (steady state). In this case, the low amounts broken down each year are replaced by new humus.
Management Effects on SOM
• Agricultural management of soils usually _____________ amounts of SOM (compared to undisturbed soils) because:
– tillage increases aeration and aerobic microbial activity
– liming, where practiced, increases microbial activity– irrigation may increase microbial activity– erosion
decreases
Effects of Cropping on SOM - Oklahoma
0
0.5
1
1.5
2
2.5
1880 1900 1920 1940 1960 1980 2000
So
il %
C
Unfertilized Wheat Wheat + manure
Conserving SOM
• Management practices that can help conserve or build SOM:– Reduced (minimum) tillage– Cover crops – Growing high residue crops– Adding organic materials to soils– Practicing crop rotation
Effect of Cropping Practices
Effect of FertilizersManitoba
Illinois
Organic Materials
• Animal Manures– Solids, liquids
• Human Manures– Solids (sewage sludge, biosolids)– Liquids (effluent)
• Composts• Reasons for applying to soils:
– –
Animal Manures
• Were a major source of plant nutrients (especially ____ and _____) before widespread use of commercial fertilizers
• Manures average 0.5 to 1% N, 0.25 to 0.5% P• Significant environmental problems are
associated with storage and disposal of animal manures.
N P
Human Waste
• In some parts of the world, have historically been an important fertilizer source
• Average 4% N, 3% P, 0.3% K• Soil disposal is one of the few options for
disposal• Use is becoming more common
Composting
• Compost is formed from the aerobic breakdown of organic materials which results in a mass of partly decomposed organic matter.
• Can be a valuable soil amendment. Most valuable for organic-matter building in soils. Not nutrient-rich.
“Sustainable Agriculture”
• A general term that is often applied to agricultural practices deemed “organic”. Usually means that organic fertilizer sources are emphasized.
• “Organic” agriculture means that only organic fertilizer sources are used.
• In organic agriculture, the proper use and management of organic inputs is critical