Soil Biology and Organic Matter. I.Overview A.Soil is….. Minerals (the body) Organisms (the life)...

Soil Biology and Organic Matter

I. Overview

A. Soil is…..

• Minerals (the body)

• Organisms (the life)

Vital to soil formation and development

I. Overview

A. Soil is…..

• Minerals (the body)

• Organisms (the life)

Vital to soil formation and development

B. Teems with life• 1 million bacterial in each cubic cm of topsoil• 1 million earthworms per acre• More Biomass beneath our feet than above

II. Plants (Macro and Micro)

III. Animals (Macro and Micro)

II. Plants

A.Microflora

Why important?

II. Plants

A.Microflora

Why important?

•Most crucial life forms in soils (by far, the most abundant in number)

II. Plants

A.Microflora

Why important?

•Most crucial life forms in soils•They generate their energy by breaking down complex organic tissue, thereby freeing vital nutrients for other plants.•(Without these critters, these nutrients could be locked up indefinitely in complex organic compounds)

II. Plants

A.Microflora

•Bacteria

Single celled organisms;Greater number of organisms present than all others combined

II. Plants

A.Microflora

•Bacteria

oHeterotrophic – derive energy by consuming complex organic debris (leaves, roots, stems, animal tissue)—releases ammonium for plants

Requiring organic compounds of nitrogen and oxygen for nourishment

Rhizobium Bacteria—fix Nitrogen from air (Legumes)

II. Plants

A.Microflora

•Bacteria

oHeterotrophic – derive energy by consuming complex organic debris (leaves, roots, stems, animal tissue)—releases ammonium for plantsoAutotrophic – oxidize inorganic materials (sulfer, iron, carbon, ammonia).—releases nitrate and nitrite.Producing complex organic nutritive compounds from simple inorganic sources by photosynthesis

A. Microflora

• Actinomycetes (Act-tin-o-my-ce-tes)o Single-celled organisms slightly larger

than bacteria (fine, thread-like)o Decompose complex organic materials

in later stages in conversion to humus.o Capable of producing antibiotics

A. Microflora

• Fungio Heterotrophic organisms capable of

decomposing highly-resistant and complex organic compounds.

o Dominant flora when pH is less than 5

also…mycorrhizae fungus (Mi-cor-rizie)

Extension ofPlant roots

A. Microflora

• AlgaeSimplest green plant (needs sun and water)

Blue-Green Algae most common

Aids in adding organic matter

Old ham sandwich residue from GeologyClub fridge……

A. Microflora

Factors Limiting Microflora

• Adequate supply of organic matter

• Temperature (Peat Bogs too cool, desert too hot)

• Moisture

• pH (6-8 optimal—Rizobium bacteria very sensitive)

• Oxygen Availability (most microflora aerobic)

Whereas microflora are affected by the ambient temperature and moisture, MACROFLORA tend to form in response to climate, parent material, and slope conditions.....

II. Plants

B. Macroflora

•Grasses

•Shrubs

•Trees

Function:

•Produce an array of complex organic materials (leaves, roots, stems, bark, wood, seeds)—affect soil chemistry, water retention, pH, organic matter, etc.

Function:

•Produce an array of complex organic materials (leaves, roots, stems, bark, wood, seeds)—affect soil chemistry, water retention, pH, organic matter, etc.

•Aid in rock weathering and soil formation

•Protect soil from erosion

III. Animals

A.Microfauna

Protozoa (amoebae, ciliates, flagellates)

Single-celled organisms, need moisture (dormant when dry)

“grazers, eat bacteria”—digestion aids organic decomposition.

III. Animals

A.Microfauna

Nematodes (“eel worms”)

•More complex than protozoa

•Dine on decomposing organic matter, living soil animals, living plant roots

•Destructive to crops

III. Animals

A.Macrofauna

Ants and Earthworms

Major mixers of soil

Openings allow air and water movement

III. Animals

A.Macrofauna

Springtails, Mites, Mammals, Humans

“mix, mechanically alteradd organics…”

IV. Soil Organic Matter

A.Sources

IV. Soil Organic Matter

A.Sources

•Predominantly from plant tissue

•Animals (minor source)

•Earthworms, centipedes, ants process and move plant residues

IV. Soil Organic Matter

B. Humus Formation1. Term used for organic matter which has gone under extreme decomposition

Raw OrganicMatter Humus

Extensive decomposition

Great source of N, P, S

IV. Soil Organic Matter

B. Humus Formation

2. The ingredients of humus…

(N Compound)

(Humus)

Proteins—stores and slowly releases N in soilAlso find concentrations of P, S, and high CECAbility to absorb large volumes of water

IV. Soil Organic Matter

B. Humus Formation3. Carbon/Nitrogen relationships

Raw OrganicMatter Humus

Extensive decomposition

800 Carbons1 Nitrogen

10 Carbons1 Nitrogen

Why not use sawdust or raw vegetation?

Why not use sawdust or raw vegetation?•Raw vegetation invites large microbial population (they feed on C).•Compete for N, and make it less available to higher plant communities.

Why not use sawdust or raw vegetation?•Raw vegetation invites large microbial population.•Compete for N, and make it less available to higher plant communities.

•Decomposition of organics (CO2 gas), and many critters die and decompose. Nitrogen remains.•N fixed as protein in the microbes is now available to plants•Resultant humus is highly enriched in N relative to the original raw vegetation, and has a greater surface area (higher CEC)

So…should we add sawdust to a garden?

C:N = 400/1

C:N = 10/1

4. Carbon Cycle

IV. Soil Organic Matter

C. Amount and Distribution

C. Amount and Distribution

1. Influence of Climate and Vegetation

Metric tons of organic matter per ha of 1 meter depth

Wisconsin study of prairie vs. forestsoils.

Practical Implications•Clear and burn method of woodlands removes the majority of organics•Cropping grasslands reincorporates organic matter into the system

IV. Soil Organic Matter

C.Composting

1. (Compost)—organic material that has undergone significant biological decomposition

IV. Soil Organic Matter

C.Composting

1.(Compost)—organic material that has undergone significant biological decomposition

2.Benefits:

•Reduces volume of organic wastes by 5-10x.

•Heat generated during decomposition kills many disease-causing microbes

•Lowers C:N

•Serves as excellent soil conditioner

3. Methods

V. Soil Fertility

A.Fertilizers

V. Soil Fertility

A.Fertilizers

A. Fertilizers 5 – 10 – 5N P K

V. Soil FertilityA. FertilizersNitrogen

Sources: ammonium, nitrate

V. Soil FertilityA. FertilizersNitrogen

* darker, stronger leaves

V. Soil FertilityA. FertilizersNitrogen

* darker, stronger leaves* helps with uptake of other

nutrients

V. Soil FertilityA. FertilizersPhosphorous

Sources: ??

V. Soil FertilityA. FertilizersPhosphorous

* strengthens stems and roots

V. Soil FertilityA. FertilizersPhosphorous

* strengthens stems and roots* enhances flowering, and seed

production

V. Soil FertilityA. FertilizersPhosphorous

* strengthens stems and roots* enhances flowering, and seed

production* increases plant’s resistance to

certain diseases

V. Soil FertilityA. FertilizersPotassium (Potash)

V. Soil FertilityA. FertilizersPotassium (Potash)

* strengthens cell walls and stemsof plants.

V. Soil FertilityA. FertilizersPotassium (Potash)

Sources??

V. Soil FertilityA. FertilizersPotassium (Potash)

* strengthens cell walls and stemsof plants.

* helps in plant respiration and uptake of other minerals.

V. Soil FertilityA. FertilizersB. Organic Matter

V. Soil FertilityA. FertilizersB. Organic MatterC. Lime

D. Other Essential Element for PlantsFe, Cu, Zn Mg, Mn, B, Mo, Cl, S,