Microbes in Agricultural Soil: Difference between revisions

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==Introduction==
==Introduction==
</b> Many agroecologists have said that in order to feed an ecosystem you need to feed the soil. Under this logic, innovations with microorganisms, something already present in the soil, can aid future research towards more sustainable, less extractive, agriculture. Soil microbes serve a variety of functions including pest and disease control, increasing both plant growth and quality, and biodegradation of organic matter and other pollutants [1]. In addition to the number of activities that promote-plant health, microbes are also directly beneficial to plant health [2]. Forming symbiotic relationships with plants, rhizobia enables plants to obtain oxygen while phosphate-stabilizing bacteria enable plants to obtain phosphate [2]. Microbes not only help ensure the healthy growth of plants, but they are also useful for regenerating tainted soils. Microorganisms are metabolic capabilities that can serve a useful bioremediation tool for soil contaminated with heavy metal or organic pollutants [1].  
</b> Many agroecologists have said that in order to feed an ecosystem you need to feed the soil.Microbes can be found across a variety of environments, including in the soils. In fact, it’s been said that there are more microbes in a teaspoon of soil than there are people on Earth [1]. These microbes serve a multitude of ecosystem functions. Soil microbes are beneficial in determining the nutrient content of food, and this is often done through the transformation of degradable organic compounds to an inorganic, readily available form for crops [2]. Some examples of these microbes include Bacillus, Azotobacter, Microbacterium, Erwinia, Beijerinckia, Enterobacter, Flavobacterium, Pseudomonas, and Rhizobium bacteria, which are all examples of phosphate solubilizers [2]. A phosphate solubilizer turns phosphate, a crucial nutrient, from an inaccessible form to one that is easily taken in and stored by plants. Some other examples include cyanobacteria (Anabaena, Nostoc, Calothrix), Azotobacter, Azospirillum, and Gluconacetobacter, which are nitrogen-fixing endophytes, a type of symbiote [2]. Similar to phosphate solubilizers, nitrogen-fixers convert nitrogen to a form more easily accessible to plants. Many farmers have even turned to the application of microbes to promote and maintain soil health [2]. In addition to microorganisms, earthworms also play a role in soil health. Both microorganisms and earthworms leave castings, the end product of digestion, and residuals that serve to increase plant nutrients [6]. When compared to soil devoid of these, soil that had been shaped by microorganism and earthworm activity showed a significant increase in nutrient levels [6]. The presence and activity of such organisms is crucial not just for plant health but also human and animal health.
 
The abundance and diversity of species as well as their activity vary drastically depending on the soil environment. The optimal environment for soil organisms is that of a natural and healthy soil, in which the biomass of microbes can amount to 4 to 5 tonnes per hectare [6]. However, soil health and fertility is declining in places as a result of increasing fertilizer use, tillage, and crop protectants [6]. As a result of the soil disruption, populations of soil organisms are subject to decline. Many farmers have begun utilizing sustainable farming techniques that limit fertilizer and soil disruption as well as actively introducing healthy microbes to the soil.
 
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Revision as of 23:52, 13 April 2024

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Magnified 20,000X, this colorized scanning electron micrograph (SEM) depicts a grouping of methicillin resistant Staphylococcus aureus (MRSA) bacteria. See PHIL 617 for a black and white view of this image. Phoro credit: CDC.
Magnified 20,000X, this colorized scanning electron micrograph (SEM) depicts a grouping of methicillin resistant Staphylococcus aureus (MRSA) bacteria SOIL. See PHIL 617 for a black and white view of this image. Phoro credit: CDC.

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Introduction

Many agroecologists have said that in order to feed an ecosystem you need to feed the soil.Microbes can be found across a variety of environments, including in the soils. In fact, it’s been said that there are more microbes in a teaspoon of soil than there are people on Earth [1]. These microbes serve a multitude of ecosystem functions. Soil microbes are beneficial in determining the nutrient content of food, and this is often done through the transformation of degradable organic compounds to an inorganic, readily available form for crops [2]. Some examples of these microbes include Bacillus, Azotobacter, Microbacterium, Erwinia, Beijerinckia, Enterobacter, Flavobacterium, Pseudomonas, and Rhizobium bacteria, which are all examples of phosphate solubilizers [2]. A phosphate solubilizer turns phosphate, a crucial nutrient, from an inaccessible form to one that is easily taken in and stored by plants. Some other examples include cyanobacteria (Anabaena, Nostoc, Calothrix), Azotobacter, Azospirillum, and Gluconacetobacter, which are nitrogen-fixing endophytes, a type of symbiote [2]. Similar to phosphate solubilizers, nitrogen-fixers convert nitrogen to a form more easily accessible to plants. Many farmers have even turned to the application of microbes to promote and maintain soil health [2]. In addition to microorganisms, earthworms also play a role in soil health. Both microorganisms and earthworms leave castings, the end product of digestion, and residuals that serve to increase plant nutrients [6]. When compared to soil devoid of these, soil that had been shaped by microorganism and earthworm activity showed a significant increase in nutrient levels [6]. The presence and activity of such organisms is crucial not just for plant health but also human and animal health.

The abundance and diversity of species as well as their activity vary drastically depending on the soil environment. The optimal environment for soil organisms is that of a natural and healthy soil, in which the biomass of microbes can amount to 4 to 5 tonnes per hectare [6]. However, soil health and fertility is declining in places as a result of increasing fertilizer use, tillage, and crop protectants [6]. As a result of the soil disruption, populations of soil organisms are subject to decline. Many farmers have begun utilizing sustainable farming techniques that limit fertilizer and soil disruption as well as actively introducing healthy microbes to the soil.



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Authored for BIOL 238 Microbiology, taught by Joan Slonczewski,at Kenyon College,2024