Soil microbes offer nutrient-dense nourishment improved crop production and recycle soil solutions. They play an essential role in decomposing organic matter, cycling nutrients, and fertilizing the soil. Besides, they improve plant growth on various physiological parameters of plants by a number of mechanisms.
When the decay process in the soil outpaces the return of residues from plant primary productivity the result is a loss of soil organic matter resource.
The too ways of increasing soil organic matter is to increase the primary plant production resource while also reducing the rate of its decay.
Burining plant residues can lead to lost opportunity to gain soil organic matter.
When soils are tilled the crop residues may undergo faster more complete decay leading to lost soil organic matter.
Soil organic matter losses can result from erosion of the top soil by either water or wind.
The ability of mycorrhizal fungi to increase persistently in the soil hold the soil for erosion and produce protection sugal proteins which are resistance to rapid decay provide a biological mechanism of utilizing the natural symbiosis to improve soil organic matter effectivity at low cost.
Perennial living plant covers are very effective return of both cropresidues and compost/manures are effective biologically based recycling strategy with target the improvement of soils and the improvement of the environment.
Soil microorganisms promote the decomposition of organic matter by secreting enzymes. The changes of biochar on soil enzyme activity are affected by the interaction between biochar, enzymes, and enzyme substrates. The active sites of biochar can absorb or desorb enzymes and their substrates. Microorganisms regulate soil properties and fertility through different pathways: (1) microbes can activate soil nutrients and promote their availability; (2) nitrogen-fixing bacteria improve soil fertility by transforming the nitrogen elements; (3) the extracellular secretions of microbes. Plant microbiomes are agriculturally important bioresources for agriculture as beneficial microbes may enhance plant growth and improve plant nutrition uptake through solubilization of P, K, and Zn, nitrogen fixation, and other mechanisms including siderophore production. Within food plant cropping systems, microorganisms provide vital functions and ecosystem services, such as biological pest and disease control, promotion of plant growth and crop quality, and biodegradation of organic matter and pollutants. Free-living microbes including filamentous fungi of the genus Trichoderma and a variety of plant growth-promoting rhizobacteria (PGPR) are able to suppress soil-borne plant pathogens and to stimulate plant growth by different direct or indirect mechanisms, such as production of phytohormones, and mycoparasitism. These organisms have many tasks, and are central to crop fertility, purifying the environment from pollutants, regulating carbon storage stocks and production/consumption of many significant green house gases, such as methane and nitrous oxides. These microbes may reside in rhizosphere and promote plant growth. Soil microorganism also contributes to a wide range of application in sustainability of all ecosystems. These microbes reg- ulate nutrient cycling, regulation of dynamic of soil organic matter, and enhance efficiency of nutrient acquisition.
The main processes by which microorganisms break down large organic molecules into smaller ones are hydrolysis and acidogenesis, both of which rely on enzymes secreted by the microbes. Hydrolysis requires moisture to progress. They result in the release of sugar molecules, Volatile fatty acids, organic acids, alcohol molecules that undergo further decomposition leading to nutrient cycling. The processes appear to be enzymes-driven leading to nutrient-cycling; an important role of the microbes in soil health. During the processes the microbes benefit from the energy released.
Soil microbes are the most important candidature for enhancing soil fertility and health. The plant growth promoting microbes and arbuscular mycorrhizae (AM) are used for enhancing plant growth and yields of agricultural crops under normal and stress conditions. Soil microorganisms promote the decomposition of organic matter by secreting enzymes. The changes of biochar on soil enzyme activity are affected by the interaction between biochar, enzymes, and enzyme substrates. The active sites of biochar can absorb or desorb enzymes and their substrates. The soil microbes are bacteria, actinomycetes, viruses, fungi, nematode, and protozoa. They produce plant growth regulators and metabolites that affect the plant growth and development. Soil microbes are critical to decomposing organic residues and recycling soil nutrients. Soil microorganisms are responsible for most of the nutrient release from organic matter. When microorganisms decompose organic matter, they use the carbon and nutrients in the organic matter for their own growth. They release excess nutrients into the soil where they can be taken up by plants. These microorganisms play a crucial role in biological pest control by effectively infecting and controlling harmful pests. Beneficial microorganisms for pest control include fungi, bacteria and viruses that naturally occur in environments such as soil, water, and air. More importantly, root traits which can promote/ attract beneficial microbes such as mycorrhiza, P-solubilising, N2-fixing and plant growth promoting bacteria can have direct positive impacts on farm productivity. These associations are well documented for their positive impact on plant growth and yield. They are known as decomposers. By far the most important microscopic decomposers are bacteria, which do the lion's share of decomposition in the compost heap. But there are other microscopic creatures such as actinomycetes, fungi, and protozoa, that also play an important role.
The mycorhizal contribution need emphasis. They can extend the effective rooting zone up to 10,000 times. Under this optimized condition phosphorus is optimized at 20% of absent condition.water is the most limiting
Microorganisms: Decomposers and Nutrient Liberators
Microorganisms are tiny but vital players in soil health. While they do break down organic matter, this process is actually beneficial for plant growth and overall soil health. Here's how:
Decomposition: Microorganisms like bacteria and fungi are decomposers. They break down dead plant and animal matter in the soil through a process called decomposition. This might seem like a reduction of soil matter, but it's actually a necessary step in the nutrient cycle. By breaking down complex organic molecules, microbes release essential nutrients like nitrogen, phosphorus, and potassium into the soil. These become available for plants to absorb and use for growth.
Improved Crop Productivity: By releasing nutrients and making them accessible to plants, microbial activity directly contributes to improved crop productivity. Plants can't utilize nutrients locked up in dead organic matter. Microbes act as the middlemen, breaking down the material and releasing the nutrients in a usable form.
Healthy Soil Structure: In addition to nutrient cycling, microbes also play a role in maintaining good soil structure. They produce sticky substances that bind soil particles together, improving aeration and water drainage. This creates a healthy environment for plant roots to grow and access water and nutrients.
Overall, microorganisms are essential for a healthy and productive soil ecosystem. Their decomposing activities may reduce some organic matter, but this breakdown process is crucial for releasing nutrients that plants need to thrive.
There is also the important process of Mineralization. During metabolism, microbes release simpler inorganic compounds, such as ammonium (NH4+), nitrate (NO3-), phosphate (PO4^3-), and sulfate (SO4^2-), into the surrounding environment as byproducts. These inorganic compounds are then available back for uptake by plants and other organisms, completing the nutrient cycle and raising soil productivity. They are the very nutrients taken up by plants in large quantities. Thus the microbes play a crucial role in mineralization by breaking down complex organic matter and releasing essential nutrients into the the soil.