10- Microbiology of soil Flashcards

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1
Q

What is soil composed of? 2 broad groups; definition

A

• The loose outer material of Earth’s surface, distinct from bedrock.

• Soil can be divided into two broad groups:
– Mineral soils: derived from rock weathering and other inorganic materials.
– Organic soils: derived from sedimentation in bogs and marshes.

• Soils are composed of
– Inorganic mineral macer (~40% of soil volume)
– Organic macer (~5%)
– Air and water (~50%)
– Living organisms
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2
Q

What are the 4 soil horizons?

A

1) O horizon
2) A horizon
3) B horizon
4) C horizon

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3
Q

Soil; made of whut

A

• Most microbial growth takes place on the surfaces of soil
particles

• The availability of water is the most important factor influencing microbial activity in surface soils
– Sand: water drains quickly
– Silt: retains water to the right
extent
– Clay: water retained too well soil becomes anoxic.

• Nutrient availability is the most important factor in subsurface environments.

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4
Q

Microorganisms in soil; top cm; prokaryote; rhizosphere; mycorrhizae

A
• Top few centimeters:
– Bacteria/Archaea: up to 2.5 x 109
– Fungi: up to 2 x 105
– Protozoa: up to 3 x 104
– Algae: up to 2.5 x 104

• Prokaryotes are largely responsible for:
– the production of the humus
– release of minerals from soil particles (production of acids from organic compounds solubilize the minerals)
– cycling of nutrients (C, N, S)
– nitrogen fixation.

Rhizosphere: soil that surrounds plant roots and receive plant secretions.

Mycorrhizae: association of fungi with plant roots.

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5
Q

Explain nitrogen fixation

A
  • Only certain prokaryotes can fix nitrogen (N2); a lot of energy is required because of the triple bond (N≡N).
  • Nitrogen fixation is one of the most important microbial processes on earth. In the absence of fertilizers, other organisms are dependent on nitrogen fixers.
  • Some nitrogen fixers are free-living (ex.: Cyanobacteria) and others are symbiotic (ex.: Rhizobium).
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6
Q

Nitrogen fixation; catalyzed by?; electrons; final product

A

• Reaction is catalyzed by nitrogenase complex (metal
cofactors)

• 8 electrons (from pyruvate) are required, 2 are lost as H2 in the
process.

• Ammonia is the final product and is used to produce amino acids, etc.

• Dinitrogenase reductase is inhibited by the presence of
oxygen.

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7
Q

Explain free-living nitrogen fixers; Clostridium; Azotobacter; Cyanobacteria;

A
  • Azotobacter, Beijerinckia and Clostridium.
  • Widespread in soil, require a soil rich in organic macer to provide energy for nitrogen fixation.
  • Produce ammonia that can be used by plants (NH3, dissolves in water to produce ammonium NH4).
  • Clostridium: strict anaerobe.
  • Azotobacter: strict aerobe. The enzyme is protected by a very high rate of O2 consumption, which keeps the intracellular environment anaerobic.
  • Cyanobacteria: only some species are capable of N2 fixation. MAJOR nitrogen fixing organisms in nature. Cyanobacteria produce energy by oxygenic photosynthesis, oxygen is produced in the cell.
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8
Q

Explain cyanobacteria; heterocyst

A
  • Nitrogen fixation occurs in specialized anaerobic cells (heterocysts), which lack Photosystem II (does not produce O2).
  • The heterocysts have a thick cell wall that slow down the diffusion of O2.
  • The regular cells provide the heterocysts with carbohydrate (pyruvate).
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9
Q

Explain symbiotic nitrogen fixers

A

• The mutualistic relationship
between leguminous plants and nitrogen-fixing bacteria is one of the most important symbioses known.

  • Examples of legumes include soybeans, clover, alfalfa, beans, and peas.
  • Rhizobium is the best-known nitrogen-fixing bacteria engaging in these symbioses
  • Colonization of legume roots by nitrogen-fixing bacteria leads to the formation of root nodules that fix nitrogen.
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10
Q

Explain nodule formation (6 steps)

A
  • Step 1: Recognition and attachment of bacterium to root hairs
  • Step 2: Excretion of nod factors by the bacterium
  • Step 3: Bacterial invasion of the root hair
  • Step 4: Travel to the main root via the infection thread (tube composed of cellulose)
  • Step 5: Formation of bacteroid state within plant cell (swollen and misshapen bacteria - fix N2)
  • Step 6: Continued plant and bacterial division, forming the mature root nodule
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11
Q

Nodule formation; O2 levels; bacteroids

A

• Oxygen levels are controlled by the O2-binding protein leghemoglobin, produced by plant cells.

• Bacteroids are a terminal structure and cannot be shed
in the environment. The nodules contain regular

Rhizobium cells that serve to inoculate the environment.

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12
Q

Explain implication for agriculture

A
  • Most plants will use nitrogen compounds produced by free-living nitrogen fixers or by other organisms during ammonification (e.g. urine).
  • Nitrate is more soluble than ammonium and is more readily available to plants.
  • Nitrifying bacteria: NH3 à NO2- à NO3
  • If the soil is poorly drained and becomes waterlogged, the soil becomes anaerobic, which promotes denitrification: NO3 - à NO2 - à NO à N2O à N2.
  • Anaerobic conditions also promote sulfur and sulfate reduction which produce H2S (toxic for plants).
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