Microbes in Agricultural Soil
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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.
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.
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Symbiosis
Many of the benefits of soil microbes, including the conversion of nutrients into a readily available form, are a result of a symbiotic relationship. One example is the relationship between the hyphae of soil fungus and plants. The fungi possess a root-like structure, hyphae, that forms a network of structure that helps soil particles bind together, thereby improving both the stability and the structure of the soil for plants [6]. This is not the only example of symbiotic relationship within the soil, many of which involve essential soil microbes.
Mycorrhizal fungi
Another example of a symbiotic relationship within the soil results in nitrogen fixation. Nitrogen fixation is a crucial process that is essential for life and is carried out primarily by nitrogen-fixing bacteria and archaea within the soil [3]. However, this process would not be possible within the symbiotic relationship between soil microbes and arbuscular mycorrhizal fungi. Arbuscular mycorrhizal fungi are also beneficial in getting nutrients to plants. Nitrogen fixing-bacteria and phosphate-solubilizing bacteria work with the mycorrhizal fungi to increase nutrient availability for plants. The bacteria fix the nitrogen, converting it from molecular form to a usable form like ammonia, as well as solubilize phosphorus ions, making them more soluble for plant uptake [2]. Finally, the arbuscular mycorrhizal fungi, which are spread through the soil, transport these nutrients directly to the plants [2]. Without this symbiotic relationship, plant nutrient uptake would not be as successful
Rhizosphere
Similar to the SOM, the rhizosphere is a crucial component of the soil, serving as the nutrient-rich portion surrounding the plant roots. A variety of symbiotic relationships within this portion of the soil aids in plant health. In fact, the aforementioned mycorrhizal fungi extended from within the rhizosphere and throughout the bulk soil. Microbial activity within the rhizosphere performs a number of activities including nitrogen-fixation, nutrient solubilization, suppression of pests and pathogens, tolerance of plant stress, decomposition of organic residue, and the recycling of soil nutrients [4]. Microbes in the rhizosphere establish a number of symbiotic relationships with host plants, including beneficial (like arbuscular mycorrhizal fungi), neutral, and detrimental [2,4]. The symbiotic relationship between rhizobia and legumes is a mutualistic form of symbiosis, benefitting both [3]. Rhizobia, a type of nitrogen-fixing bacteria, can live in the soil on decaying matter or on the root nodules of their host legumes as a symbiont [3]. The rhizobia fix atmospheric nitrogen for their host, converting it to a usable form, while the host supplies rhizobia with the carbon from photosynthesis [3]. Though this is one example of many, the microbes within the soil are crucial components in promoting plant growth. Unfortunately, the microbes are susceptible to disturbance in response to aggressive environmental conditions and farming practices.
Sustainable Farming
When farming, not only is it important to consider plant health but also soil health. Natural soil processes regenerate soil over time, but the rate of formation is slow [7]. In order to best conserve soil, many have begun to consider it a nonrenewable resource. As a result, there's been a movement for sustainable agriculture, a method that provides the most beneficial services for agroecosystems and emphasizes the long-term, rather than short term and often detrimental, production of food supplies [7]. A number of farming methods have been encouraged that not only conserve soil, but regenerate it, reintroducing the microbes and nutrients within.
Sustainable Practices
Many agricultural practices following the industrial revolution become extractive, drawing out nutrients without replenishing them. Agricultural processes of planting and harvesting alter nutrient cycling within the soil. Generally, SOM, the nutrient rich portion of soil and vital for bacterial and plant health, is highest in areas where disturbance to soil is minimized [11]. Intensive cultivation and crop harvesting for humans and animals mine soil nutrients away from plants [7]. As a result, soil amendments are being used to maintain fertility and crop yields. Unfortunately, some amendments are used in excess and instead serve the opposite of their intended function. For example, using 80kg/ha of nitrogen fertilizer can reduce soil microbial populations by 25%, and phosphorus rich fertilizers can reduce the positive effects of mycorrhizal fungi [6]. Furthermore, high nitrogen levels can also reduce humus levels, the substance in the passive portion of the SOM responsible for increasing water holding capacity. One study found that “for every 1kg of excess Nitrogen applied, 100kg of soil humus is destroyed” [6]. One way to offset the negative consequences of overuse of fertilizers and pesticides is to use bio alternatives.
Microbial Management
Microbial bioalternatives have been used in sustainable agriculture, including biofertilizers, biopesticides, bioherbicides, and bioinsecticides among others [2]. Biofertilizers, for example, improve aquatic holding capacity, carbon storage, root growth, availability and cycling of essential nutrients, as well as filtering pollutants [2]. The use of microbial management is a growing field, taking care not just of crops but of soil and the microbes within.
Microbial Addition
The goal of microbial addition is to increase the overall number of beneficial microbes in the soil, introduce specific microbes to aid a specific crop, or introduce specific microbes that can increase nutrient ability [8]. Increasing nutrient availability can be done via biofertilizers and biostimulants, pest suppression can be achieved via biopesticides, and the stimulation of plant growth can be achieved via hormone signaling through the use of plant growth promoters or biostimulants [2,8]. Using commercial products can add microbes targeted for specific functions, [8]. One such commercial product seeks to enhance the aforementioned symbiotic relationships, inoculation with rhizobia being the most common and well-researched [8]. There are also products that increase symbiosis via the inoculation of arbuscular mycorrhizal fungi. These products typically contain the species Glomus [8]. Microbial addition can also be done with on-farm microbial mixtures for a less targeted approach. These mixtures, often compost or manure, generally contain microbes that are unknown to the farmer. The mixture can contain the beneficial microbes, acting as biofertilizers and biopesticides, but they might also contain pathogens that might not be beneficial to the soil or crop [8]. Microbes get into soils constantly and naturally via dust, animals, and rain, but when microbial communities become too harmful to the soil or plants, some farmers opt to rid the soil of them entirely.
Microbial Suppression
When pathogenic microbes within the soil become rampant and harmful, outcompeting the beneficial microbes and posing threats to crops and human health, some farmers mitigate the consequences the blanket approaches that reset the microbial communities within the soil. Certain microbial pathogens can result in total crop failure, and the aforementioned approaches seek to rid the soil not only of these microbes but also neutral and beneficial ones as well [8]. Non sustainable agriculture might approach blanket eradication through the use of chemical pesticides or even soil fumigation [8]. Another, more organic form of suppression is called anaerobic soil disinfestation (ASD). This method uses large quantities of organic matter covered in a tarp, forming anaerobic conditions and allowing the microorganisms to degrade [12]. As previously mentioned, the use of pesticides harms the ability of soils to retain not only microbes but also important nutrients [6]. However, microbes that were killed off release resources that are quickly taken up by incoming microbes, such as those brought in naturally via dust, rain, or animals [8]. Microbes can quickly repopulate the now cleared soil within days or weeks. One such microbe is Bacillus, using location to quickly travel through soil that is sufficiently saturated [8]. Due to the aggressive nature of the treatment, some farmers follow microbial suppression with microbial addition, using compost or other sources of beneficial bacteria. Once these beneficial microbes are established, they are better able to outcompete the more harmful, pathogenic ones, as they have already taken available space and resources [8]. Once the beneficial microbes return, the associated benefits quickly follow.
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
