This document discusses soil microorganisms and their classification. It notes that soil microorganisms play important roles in soil nitrogen utilization, organic matter decomposition, nutrient transformations, and soil formation. The microorganisms are classified as bacteria, actinomycetes, fungi, and algae. Bacteria are the most abundant and play key roles such as organic matter decomposition and enzymatic reactions. Actinomycetes are filamentous bacteria that also decompose organic matter. Fungi possess filamentous mycelium and are important for organic matter decomposition. Algae are photoautotrophs that fix carbon and are present in soils.
he rhizosphere is the narrow region of soil or substrate that is directly influenced by root secretions and associated soil microorganisms known as the root microbiome.
The phyllosphere is a term used in microbiology to refer to the total above-ground portions of plants as habitat for microorganisms.
Microbial interactions are ubiquitous, diverse, critically important in the function of any biological community.
The most common cooperative interactions seen in microbial systems are mutually beneficial. The interactions between the two populations are classified according to whether both populations and one of them benefit from the associations, or one or both populations are negatively affected.
Soils give a mechanical support to plants from which they extract nutrients. soil provides shelters for many animal types, from invertebrates such as worms and insects up to mammals like rabbits, moles, foxes and badgers. It also provides habitats colonised by a staggering variety of microorganisms. This module is about the microbial life in soils.
Mycorrhiza Biofertilizer is also known as VAM (Myco = Fungal + rrhiza = roots) adheres to plants rhizoids leading to development of hyphae. Hyphae boost development and spreading of white root in to soil leading to significant increase in rhizosphere. These hyphae further penetrate and form arbuscules within the root cortical. VAM fungi form a special symbiotic relationship with roots of plant that can enhance growth and survivability of colonized plants. Mycorrhiza Biofertilizer is very useful in organic farming as well as normal commercial farming
Plant microbe interaction by dr. ashwin chekeAshwin Cheke
PLANT MICROBE – INTERACTIONS AND THEIR MUTUAL BENEFITS IN ENHANCING SOIL HEALTH AND AGRICULTURAL PRODUCTION ,
IT ALSO INCREASE CROP PRODUCTIVITY AND IMPROVE SOIL HEALTH
he rhizosphere is the narrow region of soil or substrate that is directly influenced by root secretions and associated soil microorganisms known as the root microbiome.
The phyllosphere is a term used in microbiology to refer to the total above-ground portions of plants as habitat for microorganisms.
Microbial interactions are ubiquitous, diverse, critically important in the function of any biological community.
The most common cooperative interactions seen in microbial systems are mutually beneficial. The interactions between the two populations are classified according to whether both populations and one of them benefit from the associations, or one or both populations are negatively affected.
Soils give a mechanical support to plants from which they extract nutrients. soil provides shelters for many animal types, from invertebrates such as worms and insects up to mammals like rabbits, moles, foxes and badgers. It also provides habitats colonised by a staggering variety of microorganisms. This module is about the microbial life in soils.
Mycorrhiza Biofertilizer is also known as VAM (Myco = Fungal + rrhiza = roots) adheres to plants rhizoids leading to development of hyphae. Hyphae boost development and spreading of white root in to soil leading to significant increase in rhizosphere. These hyphae further penetrate and form arbuscules within the root cortical. VAM fungi form a special symbiotic relationship with roots of plant that can enhance growth and survivability of colonized plants. Mycorrhiza Biofertilizer is very useful in organic farming as well as normal commercial farming
Plant microbe interaction by dr. ashwin chekeAshwin Cheke
PLANT MICROBE – INTERACTIONS AND THEIR MUTUAL BENEFITS IN ENHANCING SOIL HEALTH AND AGRICULTURAL PRODUCTION ,
IT ALSO INCREASE CROP PRODUCTIVITY AND IMPROVE SOIL HEALTH
Biological control is the suppression of one organism by another. There are two modes of mechanisms namely direct and indirect. Here I focused on the direct mechanisms such as parasitism, predatism, antibiotic-mediated suppression, lytic enzymes and unregulated-waste products. with the help of these various direct mechanisms, the bio-control agents will compete the pathogen's activity.
Soil organic matter has long been recognized as one of the most important components in maintaining soil fertility, soil quality, and agricultural sustainability. The soil zone strongly influenced by plant roots, the rhizosphere, plays an important role in regulating soil organic matter decomposition and nutrient cycling. Processes that are largely controlled or directly influenced by roots are often referred to as rhizosphere processes. These processes may include exudation of soluble compounds, water uptake, nutrient mobilization by roots and microorganisms, rhizosphere-mediated soil organic matter decomposition, and the subsequent release of CO2 through respiration. Rhizosphere processes are major gateways for nutrients and water. At the global scale, rhizosphere processes utilize approximately 50% of the energy fixed by photosynthesis in terrestrial ecosystems, contribute roughly 50% of the total CO2 emitted from terrestrial ecosystems, and mediate virtually all aspects of nutrient cycling. Therefore, plant roots and their rhizosphere interactions are at the center of many ecosystem processes. However, the linkage between rhizosphere processes and soil organic matter decomposition is not well understood. Because of the lack of appropriate methods, rates of soil organic matter decomposition are commonly assessed by incubating soil samples in the absence of vegetation and live roots with an implicit assumption that rhizosphere processes have little impact on the results. Our recent studies have overwhelmingly proved that this implicit assumption is often invalid, because the rate of soil organic matter decomposition can be accelerated by as much as 380% or inhibited by as much as 50% by the presence of live roots. The rhizosphere effect on soil organic matter decomposition is often large in magnitude and significant in mediating plant-soil interactions.
Agricultural Microbiology: Role of microbes in soil fertilitySarthakMoharana
Description on different microbes which plays role in maintaining soil fertility.
Fertile soils teem with microorganisms, which directly contribute to the biological fertility of that soil.
Biological fertility is under-studied and our scientific knowledge of it is incomplete.
In addition to fertility, soil microorganisms also play essential roles in the nutrient cycles that are fundamentally important to life on the planet.
In the past, agricultural practices have failed to promote healthy populations of microorganisms, limiting production yields and threatening sustainability.
Scientific research is exploring new and exciting possibilities for the restoration and promotion of healthy microbial populations in the soil.
‘Soil is essential for the maintenance of biodiversity above and below ground. The wealth of biodiversity below ground is vast and unappreciated: millions of microorganisms live and reproduce in a few grams of topsoil, an ecosystem essential for life on earth…’
From: Australian Soils and Landscape, An Illustrated Compendium
An entomopathogenic fungus can act as a parasite of insects and kills or seriously disables them.Targets are distributed among 10 insect orders:
Hemiptera (59.6%), Coleoptera (40.9%), Lepidoptera (17.5%), Thysanoptera (14.6%), Orthoptera (9.4%), Diptera (7.0%), Hymenoptera (2.9%), Isoptera (2.3%), Siphonoptera (1.2%), and Blattodea(0.6%).
Biological control is the suppression of one organism by another. There are two modes of mechanisms namely direct and indirect. Here I focused on the direct mechanisms such as parasitism, predatism, antibiotic-mediated suppression, lytic enzymes and unregulated-waste products. with the help of these various direct mechanisms, the bio-control agents will compete the pathogen's activity.
Soil organic matter has long been recognized as one of the most important components in maintaining soil fertility, soil quality, and agricultural sustainability. The soil zone strongly influenced by plant roots, the rhizosphere, plays an important role in regulating soil organic matter decomposition and nutrient cycling. Processes that are largely controlled or directly influenced by roots are often referred to as rhizosphere processes. These processes may include exudation of soluble compounds, water uptake, nutrient mobilization by roots and microorganisms, rhizosphere-mediated soil organic matter decomposition, and the subsequent release of CO2 through respiration. Rhizosphere processes are major gateways for nutrients and water. At the global scale, rhizosphere processes utilize approximately 50% of the energy fixed by photosynthesis in terrestrial ecosystems, contribute roughly 50% of the total CO2 emitted from terrestrial ecosystems, and mediate virtually all aspects of nutrient cycling. Therefore, plant roots and their rhizosphere interactions are at the center of many ecosystem processes. However, the linkage between rhizosphere processes and soil organic matter decomposition is not well understood. Because of the lack of appropriate methods, rates of soil organic matter decomposition are commonly assessed by incubating soil samples in the absence of vegetation and live roots with an implicit assumption that rhizosphere processes have little impact on the results. Our recent studies have overwhelmingly proved that this implicit assumption is often invalid, because the rate of soil organic matter decomposition can be accelerated by as much as 380% or inhibited by as much as 50% by the presence of live roots. The rhizosphere effect on soil organic matter decomposition is often large in magnitude and significant in mediating plant-soil interactions.
Agricultural Microbiology: Role of microbes in soil fertilitySarthakMoharana
Description on different microbes which plays role in maintaining soil fertility.
Fertile soils teem with microorganisms, which directly contribute to the biological fertility of that soil.
Biological fertility is under-studied and our scientific knowledge of it is incomplete.
In addition to fertility, soil microorganisms also play essential roles in the nutrient cycles that are fundamentally important to life on the planet.
In the past, agricultural practices have failed to promote healthy populations of microorganisms, limiting production yields and threatening sustainability.
Scientific research is exploring new and exciting possibilities for the restoration and promotion of healthy microbial populations in the soil.
‘Soil is essential for the maintenance of biodiversity above and below ground. The wealth of biodiversity below ground is vast and unappreciated: millions of microorganisms live and reproduce in a few grams of topsoil, an ecosystem essential for life on earth…’
From: Australian Soils and Landscape, An Illustrated Compendium
An entomopathogenic fungus can act as a parasite of insects and kills or seriously disables them.Targets are distributed among 10 insect orders:
Hemiptera (59.6%), Coleoptera (40.9%), Lepidoptera (17.5%), Thysanoptera (14.6%), Orthoptera (9.4%), Diptera (7.0%), Hymenoptera (2.9%), Isoptera (2.3%), Siphonoptera (1.2%), and Blattodea(0.6%).
HORTICULTURAL BOOKS by VANANGAMUDI K. pdfVanangamudiK1
HORTICULTURAL BOOKS
Dr. K. Vanangamudi
PUBLISHED BY NIPA
A HANDBOOK OF HORTICULTURAL SCIENCES VOL. 1: PRINCIPLES & PRACTICES OF HORTICULTURE AND FRUIT SCIENCE
HORTICULTURAL SCIENCES VOL. 2: VEGETABLE SCIENCE AND ORNAMENTAL HORTICULTURE
A HANDBOOK OF HORTICULTURAL SCIENCES VOL. 3: SPICES, PLANTATION, MEDICINAL, AROMATIC CROPS AND POST-HARVEST MANAGEMENT
MCQ's ON HORTICULTURE
FACTS AND FIGURES OF FRUIT CROPS - AN OVERVIEW.pdfVanangamudiK1
FACTS AND FIGURES OF FRUIT CROPS
COMMON NAME, SCIENTIFIC NAME, FAMILY, CHROMOSOME NUMBER, ORIGIN, INFLORESCENCE, FRUIT TYPE, FLOWERING
AND FRUITING PERIOD OF FRUIT CROPS
PROTECTION OF PLANT VARIETY AND FARMERS RIGHT ACT.pdfVanangamudiK1
PROTECTION OF PLANT VARIETY & FARMERS RIGHT ACT
Plant breeding
K Vanangamudi
TNPSC AO, HO, ADH, AAO, AHO EXAMS
ICAR AIEEA JRF & SRF for PG admissions exams
ICAR NET, ARS & STO (T-6) exams
IBPS – AFO exams
PPV & FR Act 2001
Notable features of PPV & FR Act
Farmers rights
Breeders Rights
Extant variety
Essentially Derived Variety (EDV)
Researchers right
Registration of plant varieties
National Gene Fund
Plant Variety Journal of India (PVJ of India)
INTELLECTUAL PROPERTY RIGHTS
Plant breeding
K Vanangamudi
TNPSC AO, HO, ADH, AAO, AHO EXAMS
ICAR AIEEA JRF & SRF for PG admissions exams
ICAR NET, ARS & STO (T-6) exams
IBPS – AFO exams
Protective umbrella of TRIPS covers
Orthodox or conventional IPR’s
Cyber Law
Geographical Indications of goods
Organizations involved in IPR
Variety release
Plant breeding
K Vanangamudi
TNPSC AO, HO, ADH, AAO, AHO EXAMS
ICAR AIEEA JRF & SRF for PG admissions exams
ICAR NET, ARS & STO (T-6) exams
IBPS – AFO exams
Official release of the varieties at Central and State levels
Procedure for release of the varieties at Central level
Organizational setup of Varietal Identification Committee (VIC)
Central Seed Committee (CSC)
Central Sub-Committee on Crop Standards, Notification and Release of Varieties for Agricultural Crops
Notification of varieties
Procedure for release of State variety
State Varietal Identification System
State Seed Subcommittee for Agricultural Crops
VARIETAL SEED PRODUCTION IN MAIZE
Seed Science & Technology
K Vanangamudi
ICAR AIEEA JRF & SRF for PG admissions exams
ICAR NET, ARS & STO (T-6) exams
IBPS – AFO exams
Zenia and metazenia in maize
Pre sowing seed treatment in maize
HYBRID SEED PRODUCTION IN MAIZE\
Seed Science & Technology
K Vanangamudi
ICAR AIEEA JRF & SRF for PG admissions exams
ICAR NET, ARS & STO (T-6) exams
IBPS – AFO exams
Detasseling
Single cross hybrid, Double cross hybrid, Single cross hybrid, Single cross hybrid, Three way hybrid, Double top cross hybrid
VARIETAL SEED PRODUCTION IN PADDY
Seed Science & Technology
K Vanangamudi
ICAR AIEEA JRF & SRF for PG admissions exams
ICAR NET, ARS & STO (T-6) exams
IBPS – AFO exams
SEED VILLAGE
Seed Science & Technology
K Vanangamudi
ICAR AIEEA JRF & SRF for PG admissions exams
ICAR NET, ARS & STO (T-6) exams
IBPS – AFO exams
Concept, Features, History, Establishment and advantages of seed villages
Establishing seed processing unit
Advanta India seed village (Indian tobacco co-operation)
MSSRF seed village
Association of Indian development (AID) – seed village
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
Synthetic Fiber Construction in lab .pptxPavel ( NSTU)
Synthetic fiber production is a fascinating and complex field that blends chemistry, engineering, and environmental science. By understanding these aspects, students can gain a comprehensive view of synthetic fiber production, its impact on society and the environment, and the potential for future innovations. Synthetic fibers play a crucial role in modern society, impacting various aspects of daily life, industry, and the environment. ynthetic fibers are integral to modern life, offering a range of benefits from cost-effectiveness and versatility to innovative applications and performance characteristics. While they pose environmental challenges, ongoing research and development aim to create more sustainable and eco-friendly alternatives. Understanding the importance of synthetic fibers helps in appreciating their role in the economy, industry, and daily life, while also emphasizing the need for sustainable practices and innovation.
How to Make a Field invisible in Odoo 17Celine George
It is possible to hide or invisible some fields in odoo. Commonly using “invisible” attribute in the field definition to invisible the fields. This slide will show how to make a field invisible in odoo 17.
The Roman Empire A Historical Colossus.pdfkaushalkr1407
The Roman Empire, a vast and enduring power, stands as one of history's most remarkable civilizations, leaving an indelible imprint on the world. It emerged from the Roman Republic, transitioning into an imperial powerhouse under the leadership of Augustus Caesar in 27 BCE. This transformation marked the beginning of an era defined by unprecedented territorial expansion, architectural marvels, and profound cultural influence.
The empire's roots lie in the city of Rome, founded, according to legend, by Romulus in 753 BCE. Over centuries, Rome evolved from a small settlement to a formidable republic, characterized by a complex political system with elected officials and checks on power. However, internal strife, class conflicts, and military ambitions paved the way for the end of the Republic. Julius Caesar’s dictatorship and subsequent assassination in 44 BCE created a power vacuum, leading to a civil war. Octavian, later Augustus, emerged victorious, heralding the Roman Empire’s birth.
Under Augustus, the empire experienced the Pax Romana, a 200-year period of relative peace and stability. Augustus reformed the military, established efficient administrative systems, and initiated grand construction projects. The empire's borders expanded, encompassing territories from Britain to Egypt and from Spain to the Euphrates. Roman legions, renowned for their discipline and engineering prowess, secured and maintained these vast territories, building roads, fortifications, and cities that facilitated control and integration.
The Roman Empire’s society was hierarchical, with a rigid class system. At the top were the patricians, wealthy elites who held significant political power. Below them were the plebeians, free citizens with limited political influence, and the vast numbers of slaves who formed the backbone of the economy. The family unit was central, governed by the paterfamilias, the male head who held absolute authority.
Culturally, the Romans were eclectic, absorbing and adapting elements from the civilizations they encountered, particularly the Greeks. Roman art, literature, and philosophy reflected this synthesis, creating a rich cultural tapestry. Latin, the Roman language, became the lingua franca of the Western world, influencing numerous modern languages.
Roman architecture and engineering achievements were monumental. They perfected the arch, vault, and dome, constructing enduring structures like the Colosseum, Pantheon, and aqueducts. These engineering marvels not only showcased Roman ingenuity but also served practical purposes, from public entertainment to water supply.
Acetabularia Information For Class 9 .docxvaibhavrinwa19
Acetabularia acetabulum is a single-celled green alga that in its vegetative state is morphologically differentiated into a basal rhizoid and an axially elongated stalk, which bears whorls of branching hairs. The single diploid nucleus resides in the rhizoid.
Operation “Blue Star” is the only event in the history of Independent India where the state went into war with its own people. Even after about 40 years it is not clear if it was culmination of states anger over people of the region, a political game of power or start of dictatorial chapter in the democratic setup.
The people of Punjab felt alienated from main stream due to denial of their just demands during a long democratic struggle since independence. As it happen all over the word, it led to militant struggle with great loss of lives of military, police and civilian personnel. Killing of Indira Gandhi and massacre of innocent Sikhs in Delhi and other India cities was also associated with this movement.
Honest Reviews of Tim Han LMA Course Program.pptxtimhan337
Personal development courses are widely available today, with each one promising life-changing outcomes. Tim Han’s Life Mastery Achievers (LMA) Course has drawn a lot of interest. In addition to offering my frank assessment of Success Insider’s LMA Course, this piece examines the course’s effects via a variety of Tim Han LMA course reviews and Success Insider comments.
Palestine last event orientationfvgnh .pptxRaedMohamed3
An EFL lesson about the current events in Palestine. It is intended to be for intermediate students who wish to increase their listening skills through a short lesson in power point.
Overview on Edible Vaccine: Pros & Cons with Mechanism
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.