Microbes in Agricultural Soil
Section
By [Author Name]
At right is a sample image insertion. It works for any image uploaded anywhere to MicrobeWiki.
The insertion code consists of:
Double brackets: [[
Filename: PHIL_1181_lores.jpg
Thumbnail status: |thumb|
Pixel size: |300px|
Placement on page: |right|
Legend/credit: Magnified 20,000X, this colorized scanning electron micrograph (SEM) depicts a grouping of methicillin resistant Staphylococcus aureus (MRSA) bacteria. Photo credit: CDC. Every image requires a link to the source.
Closed double brackets: ]]
Other examples:
Bold
Italic
Subscript: H2O
Superscript: Fe3+
Sample citations: [1]
A citation code consists of a hyperlinked reference within "ref" begin and end codes.
To repeat the citation for other statements, the reference needs to have a names: "<ref name=aa>"
The repeated citation works like this, with a forward slash.[1]
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.
Soil organic Matter
One of the most nutrient rich portions of soil is the soil organic matter (SOM). Not only is SOM beneficial for microbes, but it also acts as a buffer for high acidity and increases water availability within the soil, acting as a sponge and releasing it for plant use [11]. Furthermore, SOM helps decompose excess pesticides and acts as a carbon sink, sequestering atmospheric carbon [5, 11]. SOM is composed of organic substances (those with carbon) in the soil. This includes plants, algae, microorganisms, and decomposing matter left from both plants and microorganisms [1].
The three main components of the SOM are the “living” (microorganisms), the “dead” (fresh residue) and the “very dead” (humus- long decomposed plant and animal substances) [1,11]. These components are then broken down into further classification. The SOM is composed of active (35%) and passive (65%) [1]. Active SOM consists of the “living” and “dead” plant and animal materials. These are composed of easily digested sugars and proteins, acting and food for the microbes within the soil [1]. The active layer contains the microbes that convert nutrients into a form more readily available for plants The passive SOM is unable to be decomposed by microbes and is higher in lignin [1]. Passive SOM is the portion that acts as a carbon sink.
Every point of information REQUIRES CITATION using the citation tool shown above.
Section 2
Include some current research, with at least one figure showing data.
Section 3
Include some current research, with at least one figure showing data.
Section 4
Conclusion
References
- ↑ 1.0 1.1 Hodgkin, J. and Partridge, F.A. "Caenorhabditis elegans meets microsporidia: the nematode killers from Paris." 2008. PLoS Biology 6:2634-2637.
- ↑ Bartlett et al.: Oncolytic viruses as therapeutic cancer vaccines. Molecular Cancer 2013 12:103.
- ↑ Hoorman, J and Islam, R. "Understanding Soil Microbes and Nutrient Recycling." 2010. Agriculture and Natural Resources.
Authored for BIOL 238 Microbiology, taught by Joan Slonczewski,at Kenyon College,2024
