BIOESR SOIL FAMILY NOT ONLY IMPROVES SOIL FERTILITY BUT INCREASES HIGH CROP YEILD
Soil fitness is the foundation of organic farming systems. Fertile soil provides essential nutrients to plants, while assisting numerous and energetic biotic networks that allows the soil to withstand environmental degradation. Organic manufacturers face particular demanding situations in handling soil productivity. Current tips on nutrient control for organic farmers are pretty widespread in nature. Organic farmers rely on intuition and observation, recommendation from vendors, traditional soil tests, and their personal own experience to make choices about the amount and varieties of soil amendments to apply. As a result, there is tremendous variability in both the quantities of nutrients applied and the resulting soil fertility status on organically controlled farms. Organic farmers are searching to “construct the soil” or enhance its inherent fertility via means of the usage of crop rotations, animal and green manures, and cover crops. Crop rotation and tillage practices need to offer the right seedbed and pest manipulation even as minimizing erosion. Although the subsequent sections deal with nutrient control and soil constructing practices separately, those factors of control are in detail linked via a system of management. Organic farms that attain their goals keep soils and protect the environment while using modest quantities of inputs. Soil checks and easy budgeting tools can assist producers maintain stability to attain success.
The macronutrients with concentrations greater than 500 micrograms/g plant include nitrogen, phosphorus, potassium, sulfur, calcium, and magnesium . Micronutrients taken up in lower abundance are no less necessary but are not limiting to growth in most situations. Sandy soils with inherently low nutrient contents are an exception. The micronutrients include iron, zinc, manganese, copper, boron, chlorine, and molybdenum. Organic farmers use natural materials or, when possible, exploit biological processes to supply needed nutrients to soils.
One of the simplest things a producer can do is maintain optimal soil pH levels. This is critical as pH influences nutrient solubility, microbial activity, and root growth. High pH favors weathering of minerals and increases the release of cations but reduces the solubility of salts including carbonates and phosphates. Lower pH values prefer fungi while excessive pH favors bacteria. Soil pH can also affect the plant’s capability to take up nutrients directly. At very low pH values (<3), cell membranes are impaired and become leaky. For maximum crops, soil pH tiers are ideal among optimal between 6.0 and 7.0. Lime may be implemented to elevate the pH of acidic soils pH value less than 6 and supply calcium. Alkalinity, that’s tougher to correct, usually requires the use of sulfur, this treatment is usually temporary and costly than liming. When adjusting the pH, it is important to recognize the crop’s pH requirement since optimum pH levels vary by crop.
BIOESR S.O.L gives birth to soil organisms such as Earthworms, Good Bacteria and diversity of life in the soil. Earthworms transport soil material and Soil Organisms make up the nutrients from the subsoil to the topsoil and thus maintain the vitality of the soil. Earthworms promote the colonization and propagation of beneficial soil bacteria and fungi in their burrows and casts.
BIOESR S.O.L is a unique product for soil fertility that promotes root growth, hence increasing the yield, as well as quality. S.O.L improves the bioefficacy of plants and provides them with essential nutrients. They are highly effective for improving soil texture and structure.
BIOESR N PLUS contains a consortium of nitrogen-fixing bacteria . Nitrogen is a component of proteins and nucleic acids and is essential to life on Earth. Although nitrogen is abundant in the atmosphere, most organisms cannot use it in that form. Nitrogen-fixing bacteria’s accomplish more than 90 percent of all nitrogen fixation and thus play an important role in the nitrogen cycle. The free-living (nonsymbiotic) bacteria, includes the cyanobacteria (or blue-green algae) Anabaena and Nostoc and genera such as Azotobacter, Beijerinckia, and Clostridium.
The symbiotic nitrogen-fixing bacteria invade the root hairs of host plants, where they multiply and stimulate formation of root nodules, enlargements of plant cells and bacteria in intimate association Within the nodules the bacteria convert free nitrogen to ammonia, which the host plant utilizes for its development. To ensure sufficient nodule formation and optimum growth of legumes (eg, Paddy, Coconut Trees, beans, Corn , Millets, Turmeric and all types of crops), seeds are usually inoculated with commercial cultures of appropriate Rhizobium species, especially in soils poor or lacking in the required bacterium.
BIOESR P PLUS contains a consortium of Phosphate-fixing bacteria . Phosphorus (P) is a macronutrient required for the proper functioning of plants. Though soil possesses total P in the form of organic and inorganic compounds, most of them remain inactive and thus unavailable to plants. Phosphate solubilizing microbes (PSMs) are a group of beneficial microorganisms capable of hydrolyzing organic and inorganic insoluble phosphorus compounds to soluble P form that can easily be assimilated by plants. PSM by inoculating in soil appears to be an efficient way to convert the insoluble P compounds to plant-available P form, resulting in better plant growth, crop yield, and quality.
Bacillus, Pseudomonas, Rhizobium, Aspergillus, Penicillium, and AMR are the most efficient P solubilizers for increasing bioavailability of P in soil. Furthermore, PSMs acts as a biocontrol against plant pathogens via production of antibiotics, hydrogen cyanate (HCN), and antifungal metabolites. Thus, PSMs represent potential substitutes for inorganic phosphate fertilizers to meet the P demands of plants, improving yield in sustainable agriculture.
BIOESR K PLUS contains Group of Healthy Dense potash dissolving bacteria’s a essential nutrient and a major constituent within all living cells. Naturally, soils contain K in larger amounts than any other nutrients, however most of the K is unavailable for plant uptake. Application of chemical fertilizers has a considerably negative impact on environmental sustainability. It is known that potassium solubilizing bacterias (KSBs) can solubilize K bearing minerals and convert the insoluble K to soluble forms of K available to plant uptake. , such as Acidothiobacillus ferrooxidans, Paenibacillus spp., Bacillus mucilaginosus, B. edaphicus, and B. circulans have capacity to solubilize K minerals (e.g., biotite, feldspar, illite, muscovite, orthoclase, and mica) which dissolves insoluble inorganic potash and makes it available for plants.
After nitrogen (N) and phosphorus (P), potassium (K) is the most important plant nutrient that has a key role in the growth, metabolism, and development of plants. In addition to increasing plant resistance to diseases, pests, and abiotic stresses, K is required to activate over 80 different enzymes responsible for plant and animal processes such as energy metabolism, starch synthesis, nitrate reduction, photosynthesis, and sugar degradation.