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SOIL MICROORGANISMS
Dr. K. VANANGAMUDI
Formerly Dean (Agriculture), AC & RI, Coimbatore
Dean, Adhiparashakthi Agricultural College, Kalavai
Professor and Head - Seed Science and Technology,
Tamil Nadu Agricultural University,
Coimbatore 641 04, Tamil Nadu, India.
1. Role of soil microorganisms
 Soil N utilization by plants.
 Dead organic matters decomposed.
 Nutrient transformation.
 Physical and chemical properties of soil.
 CO2 content.
 Soil formation.
2. Classification
 Soil organisms are classified broadly into soil flora and soil fauna.
 Subdivided into micro and macro flora.
 Micro flora again classified into bacteria, actinomycetes, fungi and algae.
1. Bacteria
 Single celled.
 Rod shaped and spherical.
 About 1 µm wide and up to 3 µm long and about 2 µm in diameter.
 Most abundant microorganism in the soil.
3.Classification of bacteria
a). Based on O2 requirement:
 Aerobic facteria: Bacillus subtilis, Azotobacter, Arthrobacter, Mycobacterium.
 Anaerobic bacteria: Actinomycetes, Clostridium, Propionibacterium, Bacterioides,
Fusobacterium, Bifidobacterium.
b) Based on temperature:
 Facultative: Optimal. An organism that can use only O2 but has anaerobic method of
energy production.
 Facultative aerobes – Chlorobium limicola.
 Facultative anaerobes – Escherichia coli, Bacillus anthracisis, Pseudomonas,
Klebsiella, Staphylococcus spp, Streptococcus spp, Salmonella, Listeria.
 Psychrophiles: Grows best at moderate temperature close to freezing.
 Arthrobacter, Psychrobacter, Chryseobacterium greenlandensis.
 Mesophiles: Grows best at moderate temperature.
 Listeria, Thiobacillus novellus, E.coli, Clostridium
 Theromophile: Grows best at high temperature.
 Chloroflexus aurantiacus, Thermus thermophilus, pyrolobus fumari
c) Based on their food preparation:
 Autotroph: Able form nutritional organic substances form inorganic substances such
as carbon dioxide.
 Cyanobacteria, Green and purple sulfur bacteria, Nitrosomonas.
 Heterotroph: Derives nutritional requirements from complex organic substances.
 Clostridium, Mycobacterium, Rhizobium.
 Chemoautotroph: Obtains energy by the oxidation of reduced compounds.
 Nitrosomonas, Thiobacillus thiooxidans.
 Obligate chemoautotrophs: Prefer specific substrates,
 Nitrobacter – Nitrite as substrate,
 Nitrosomonas – Ammonia as substrate,
 Thiobacillus - Converts sulphur compounds to SO4.
 Ferrobacillus – Converts ferrous to ferric,
d)Based on symbiotic relationship
Symbiotic N fixers:
 Associated with a host plant.
 Both the host and the bacteria get the benefits.
 Fix atmospheric N.
 Rhizobium (Legume association)
 Bradyrhizobium (Soybean association)
 Azorhizobium (Sesbania rostrata association)
 Anabaend azollae (Azolla – Anabaena)
 Frankia (Casuarina association)
Non symbiotic N fixers:
 Bacteria present without the association of a plant.
 But fix atmospheric N.
 Symbiotic, non symbiotic and cellulose decomposers come under Heterotrophs.
 Nitrifiers, denitrifiers nitrate formers and sulphur oxidizers are autotrophs.
 Azotobactor, Beijerinckia (named after scientist Beijerinck), Clostridium, Chlorobium,
Rhodopseudomonas, Desulphovibro, Thiobacillus, Nostoc.
2. Role of bacteria
 Bacteria carryout the decomposition of organic matter and synthesis of humus .
 Enzymatic transformations are carried out by bacteria
 Bacteria oxidizes or reduces many chemical reactions such as N fixation, sulphur
oxidation, nitrification etc.,
2. Actinomycetes
 Unicellular like bacteria.
 Have same size as bacteria.
 Filamentous and profusely branched.
 Mycelial threads are smaller than those of fungi.
 No nuclear membrane as in bacteria.
 Also called as filamentous.
 Sensitive to acid soils.
 Potato scab, a disease due to actinomycetes, can be controlled by lowering the soil pH
by applying sulphur.
 Heterotrophic - optimum temperature 25-30oC, pH 6.5 – 8.0.
 Actionomycetes are important for organic matter decomposition.
 Chitin and phospholipids are reduced to simple compounds.
 Aroma of freshly ploughed land at certain times of the year is probably due to
actinomycetes as well as certain molds.
 Actinomycete population in soil exceeds all other organisms except bacteria.
 Their proportion increases with soil depth. Their population and biomass are almost
equal to that of bacteria.
 Eg. Frankia family (Actinobacteria).
 Streptomyces flavovirens.
3. Fungi
 Soil fungi may be parasitic or saprophytic.
 Possess filamentous mycelium composed of individual hyphae which are 5-20 µm in
diameter and several centimeters in length.
 Most fungi are heterotrophic and hence, they depend on the organic matter content of
the soil.
 Dominant in acid soils and some can tolerate a pH upto 9.0.
 Strictly aerobic.
 Classified into phycomycetes, ascomycets, basidiomycetes and fungi imperfecti.
 Fungi may also may be classified as molds, yeast and mushrooms.
Molds: Filamentous microscopic molds develop vigorously in all types of soils.
 In acid forest soils, involves in decomposing of organic matter.
 Common genera - Mucor, Fusarium and Aspergillus.
 Average population is 10-200 billion / m2.
 In humus formation and aggregate stabilization, molds are more important than
bacteria.
 Continue to decompose complex organic substances, after bacteria and actinomycetes
have stopped their function.
Yeast: Group of fungi which exist as an unicellular organism.
 Reproduce by fission or budding.
 Used as food supplement and also for the production of alcoholic beverages.
 Yeast is not common in soils but produce several plant diseases.
Mushroom: Present in forests and grasslands where ample moisture and organic residues are
present.
 Some mushrooms are edible.
 Mushrooms are also not common in cultivated soils.
 Their fruiting body is above the ground.
3. Algae
 Filamentous, 10µm in diameter. Population in soil is around 1-10 billion / m2.
 Their mass in soil may be 50-600 kg/ha.
 Algae are photoautotrophs.
 Divided into 4 general groups - blue green, green, yellow green and diatoms.
 Blue green algae are numerous in rice soils.
 Blue green algae growing within the leaves of aquatic fern.
 Azolla can also fix atmospheric N.

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SOIL MICROORGANISMS.pptx

  • 1. SOIL MICROORGANISMS Dr. K. VANANGAMUDI Formerly Dean (Agriculture), AC & RI, Coimbatore Dean, Adhiparashakthi Agricultural College, Kalavai Professor and Head - Seed Science and Technology, Tamil Nadu Agricultural University, Coimbatore 641 04, Tamil Nadu, India. 1. Role of soil microorganisms  Soil N utilization by plants.  Dead organic matters decomposed.  Nutrient transformation.  Physical and chemical properties of soil.  CO2 content.  Soil formation. 2. Classification  Soil organisms are classified broadly into soil flora and soil fauna.  Subdivided into micro and macro flora.  Micro flora again classified into bacteria, actinomycetes, fungi and algae. 1. Bacteria  Single celled.  Rod shaped and spherical.  About 1 µm wide and up to 3 µm long and about 2 µm in diameter.  Most abundant microorganism in the soil. 3.Classification of bacteria a). Based on O2 requirement:  Aerobic facteria: Bacillus subtilis, Azotobacter, Arthrobacter, Mycobacterium.  Anaerobic bacteria: Actinomycetes, Clostridium, Propionibacterium, Bacterioides, Fusobacterium, Bifidobacterium.
  • 2. b) Based on temperature:  Facultative: Optimal. An organism that can use only O2 but has anaerobic method of energy production.  Facultative aerobes – Chlorobium limicola.  Facultative anaerobes – Escherichia coli, Bacillus anthracisis, Pseudomonas, Klebsiella, Staphylococcus spp, Streptococcus spp, Salmonella, Listeria.  Psychrophiles: Grows best at moderate temperature close to freezing.  Arthrobacter, Psychrobacter, Chryseobacterium greenlandensis.  Mesophiles: Grows best at moderate temperature.  Listeria, Thiobacillus novellus, E.coli, Clostridium  Theromophile: Grows best at high temperature.  Chloroflexus aurantiacus, Thermus thermophilus, pyrolobus fumari c) Based on their food preparation:  Autotroph: Able form nutritional organic substances form inorganic substances such as carbon dioxide.  Cyanobacteria, Green and purple sulfur bacteria, Nitrosomonas.  Heterotroph: Derives nutritional requirements from complex organic substances.  Clostridium, Mycobacterium, Rhizobium.  Chemoautotroph: Obtains energy by the oxidation of reduced compounds.  Nitrosomonas, Thiobacillus thiooxidans.  Obligate chemoautotrophs: Prefer specific substrates,  Nitrobacter – Nitrite as substrate,  Nitrosomonas – Ammonia as substrate,  Thiobacillus - Converts sulphur compounds to SO4.  Ferrobacillus – Converts ferrous to ferric, d)Based on symbiotic relationship Symbiotic N fixers:  Associated with a host plant.  Both the host and the bacteria get the benefits.  Fix atmospheric N.  Rhizobium (Legume association)  Bradyrhizobium (Soybean association)  Azorhizobium (Sesbania rostrata association)
  • 3.  Anabaend azollae (Azolla – Anabaena)  Frankia (Casuarina association) Non symbiotic N fixers:  Bacteria present without the association of a plant.  But fix atmospheric N.  Symbiotic, non symbiotic and cellulose decomposers come under Heterotrophs.  Nitrifiers, denitrifiers nitrate formers and sulphur oxidizers are autotrophs.  Azotobactor, Beijerinckia (named after scientist Beijerinck), Clostridium, Chlorobium, Rhodopseudomonas, Desulphovibro, Thiobacillus, Nostoc. 2. Role of bacteria  Bacteria carryout the decomposition of organic matter and synthesis of humus .  Enzymatic transformations are carried out by bacteria  Bacteria oxidizes or reduces many chemical reactions such as N fixation, sulphur oxidation, nitrification etc., 2. Actinomycetes  Unicellular like bacteria.  Have same size as bacteria.  Filamentous and profusely branched.  Mycelial threads are smaller than those of fungi.  No nuclear membrane as in bacteria.  Also called as filamentous.  Sensitive to acid soils.  Potato scab, a disease due to actinomycetes, can be controlled by lowering the soil pH by applying sulphur.  Heterotrophic - optimum temperature 25-30oC, pH 6.5 – 8.0.  Actionomycetes are important for organic matter decomposition.  Chitin and phospholipids are reduced to simple compounds.  Aroma of freshly ploughed land at certain times of the year is probably due to actinomycetes as well as certain molds.  Actinomycete population in soil exceeds all other organisms except bacteria.  Their proportion increases with soil depth. Their population and biomass are almost equal to that of bacteria.  Eg. Frankia family (Actinobacteria).
  • 4.  Streptomyces flavovirens. 3. Fungi  Soil fungi may be parasitic or saprophytic.  Possess filamentous mycelium composed of individual hyphae which are 5-20 µm in diameter and several centimeters in length.  Most fungi are heterotrophic and hence, they depend on the organic matter content of the soil.  Dominant in acid soils and some can tolerate a pH upto 9.0.  Strictly aerobic.  Classified into phycomycetes, ascomycets, basidiomycetes and fungi imperfecti.  Fungi may also may be classified as molds, yeast and mushrooms. Molds: Filamentous microscopic molds develop vigorously in all types of soils.  In acid forest soils, involves in decomposing of organic matter.  Common genera - Mucor, Fusarium and Aspergillus.  Average population is 10-200 billion / m2.  In humus formation and aggregate stabilization, molds are more important than bacteria.  Continue to decompose complex organic substances, after bacteria and actinomycetes have stopped their function. Yeast: Group of fungi which exist as an unicellular organism.  Reproduce by fission or budding.  Used as food supplement and also for the production of alcoholic beverages.  Yeast is not common in soils but produce several plant diseases. Mushroom: Present in forests and grasslands where ample moisture and organic residues are present.  Some mushrooms are edible.  Mushrooms are also not common in cultivated soils.  Their fruiting body is above the ground. 3. Algae  Filamentous, 10µm in diameter. Population in soil is around 1-10 billion / m2.  Their mass in soil may be 50-600 kg/ha.  Algae are photoautotrophs.  Divided into 4 general groups - blue green, green, yellow green and diatoms.
  • 5.  Blue green algae are numerous in rice soils.  Blue green algae growing within the leaves of aquatic fern.  Azolla can also fix atmospheric N.