Soil Organic Matter Section C Soil Fertility and Plant Nutrition

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