Why does low soil biological activity destroy crop efficiency?
Low biological activity of the soil causes blockage of nutrient circulation, which is a consequence prevents plants from taking up minerals provided in artificial fertilisers. A sterilized substrate lacks beneficial bacteria and fungi that decompose organic residues and transform them into forms available to the root system. A decrease in the population of microorganisms leads to the degradation of the lumpy structure, which makes the soil compact, susceptible to drought and poorly aerated. Instead of nourishing the plants, the minerals administered are depleted or washed into the deeper layers of the soil profile. Restoring microbial life is the only way to stop this process and rebuild the natural fertility of the site.
How to check the level of humus and the microbiological condition of the substrate?
The microbiological condition and the level of caries are checked by: performing preventive laboratory tests of soil samples taken from the arable and sub-arable layer. Basic chemical analysis determines the percentage of organic matter, but a full picture of the biological condition is provided by tests of the enzymatic activity of the substrate.
The farmer can also perform a simplified visual-field assessment, verifying the lumpy structure, the presence of earthworms and the rate of straw decomposition after harvest. The dark color of the earth and its specific, forest smell are natural indicators of the high concentration of humus compounds. Regular monitoring of biological parameters allows for quick implementation of regenerative actions before a drastic decline in yield occurs.
Regeneration of the sorption complex and the absorption of mineral fertilisers
Regeneration of the sorption complex directly determines the soil’s ability to retain and transfer nutrients to plants delivered in pure mineral form. Increasing the sorption capacity means that potassium, magnesium and calcium cations are more strongly bound by soil colloids and are not lost. This process directly improves bioavailability of mineral fertilisers, reducing the phenomenon of soil salinity and aluminum toxicity. The higher cation exchange capacity acts as a natural buffer that stabilizes the pH and optimizes the nutrition of crops in critical stages of development. The introduction of organic compounds into agrotechnics allows for permanent reconstruction of the physicochemical properties of even very light sites.
Improving soil conditions with Humus Active – how does it work in practice?
Improving soil conditions with Humus Active is based on simultaneous supply of concentrated humic acids to the substrate and active strains of lactic acid bacteria, actinomycetes and nitrogenous bacteria. The preparation works in two ways: it immediately improves the physical structure of the earth and initiates long-term humification processes. The introduced microorganisms immediately colonize the root zone, where they begin to multiply intensively and process the remaining organic matter.
Thanks to its liquid formula, the product quickly penetrates deep into the profile, binding loose dust particles into stable soil aggregates. The effect of this action is better aeration of the root layer and a significant increase in its ability to store rainwater.
What is stable humus in the soil and how to rebuild it permanently?
Stable humus in the soil is a high-molecular complex of organic compounds resistant to rapid microbiological decomposition, which determines the long-term fertility and water retention of the substrate. It consists mainly of humins and humic acids, which are produced in the long-term process of humification of plant remains with the participation of specialized microorganisms.
To permanently rebuild it in degraded sites, organic carbon should be regularly supplied and intensive, deep plowing that aerates the substrate should be avoided. It is helpful to introduce catch crops and regularly use humus preparations, which accelerate the synthesis of durable organic-mineral compounds. This process creates an optimal environment for the development of beneficial microflora and stabilizes yields for years.
Agricultural gold – what are Humico Active humic acids?
Humico Active humic acids natural, highly reactive macromolecular compounds with a unique chemical structure, constituting the most important active ingredient of professional soil improvers. They have an exceptionally high density of functional groups, thanks to which they have a sorption capacity many times higher than ordinary organic matter from manure. These substances act as a natural chelator, combining with minerals in the soil and facilitating their transport into plant cells. This ingredient stimulates the development of beneficial soil microorganisms, providing them with a direct source of energy and shelter. Their constant presence in the soil profile prevents the degradation of the site and protects crops against the effects of drought stress.
Stimulation of the root system, i.e. the foundation of a strong plant
The root system is stimulated through direct influence of growth substances and humate acids on cell division in the root growth cone. This action causes a rapid increase in root mass, with particular emphasis on the most valuable hairy roots responsible for water uptake. The extensive underground zone allows the plant to penetrate deeper layers of the soil, which drastically increases its resistance to periodic moisture deficiencies. A strong root also secretes more exopolysaccharides and organic acids, which further activate the microflora around the plant. The development of the underground foundation translates directly into better vigor of the above-ground part and stable building of crop biomass.
How to reduce costs and increase the efficiency of NPK fertilisation by 50%?
High efficiency of NPK fertilisation can be achieved by: optimization of biological processes, which prevent blocking and washing out of elements from the root zone. When the soil is functioning properly, doses of traditional chemical fertilisers can be reduced without the risk of reducing the harvested crop.
Providing humic substances ensures that minerals are supplied to the plant in a continuous and balanced manner. This allows for maximum use of each unit of nitrogen, phosphorus and potassium introduced into the soil. Reducing fertiliser losses is the simplest method to reduce the overall costs of plant production on the farm.
Unlocking yield potential thanks to crop residues
Unlocking the yield potential of a site requires: proper management of straw and roots remaining in the field after harvesting the main crop. Harvest residues are a valuable, natural source of macro- and microelements, but their decomposition without the participation of appropriate bacteria is too slow or generates putrefactive processes. The use of microbiological preparations accelerates the mineralization of straw, transforming it into biomass that is easily digestible for plants. This process allows you to retain valuable elements in the top layer of soil and re-introduce them into the nutritional cycle. Proper management of cover crops and plant residues provides a free foundation for building high yields in the next season.
Liquid improvers and granulates – choose a product for your field
The choice of the appropriate form of soil preparation depends on the specific technical equipment of the farm, the structure of sowing and the current needs of a specific location. Liquid soil improvers provide immediate action because the humate acids and microorganisms contained in them immediately penetrate the soil profile and start regenerative processes. In turn, granulated organic-mineral fertilisers are characterized by an extended release time of active substances, which is useful for starter fertilisation or on lighter soils.
When to use Humus Active and when to use Plonar Active?
Humus Active liquid form should be used primarily on stubble, before post-harvest cultivation or in early spring, to quickly activate microorganisms and accelerate the decomposition of organic matter. In turn, granulated Plonar Active jis recommended for pre-sowing or row application, especially in sites with extremely low phosphorus and potassium content, where simultaneous application of minerals and humates is required.
Humus Active is perfect for large-area treatments using sprayers, ensuring even coverage of the soil with biological life. Plonar Active is an irreplaceable solution in crops where the technology assumes precise, mechanical dosing of granulated fertiliser straight into the ground. The choice depends on the existing machinery and the expected moment of application of the preparation.
Summary – is it worth choosing soil biologization with Agrizaz?
Investing in biological regeneration of the substrate is a strategic decision that allows you to make your farm independent of the constantly increasing prices of traditional artificial fertilisers. Restoring microbiological efficiency and rebuilding stable humus translates directly into higher profitability of plant production, better lumpy structure and higher resistance of crops to weather anomalies.
The experience of Agrizaz experts proves that natural methods bring measurable economic and agrotechnical benefits. Start successfully managing the fertility of your fields and visit our home page at https://www.agrizaz.pl/to learn about the full portfolio of modern solutions for agriculture.
Frequently asked questions (FAQ)
How to remove heavy metals from the soil?
Effective removal of heavy metals from the soil solution involves their permanent immobilization and binding into chemically inactive chelate complexes using humic acids. Humate compounds have the ability to sorb metals such as lead, cadmium and chromium, which blocks their uptake by the root system of crop plants. Additionally, this process can be supported by phytoremediation, i.e. the cultivation of specific cover crops that accumulate pollutants in their aboveground biomass. Regularly increasing the content of stable humus is the most effective method of protecting the biological purity of the crop in contaminated sites.What causes nutrient imbalance in the soil?
The main cause of the disturbance of the balance of nutrients in the soil is intensive, one-sided NPK mineral fertilisation with a simultaneous lack of regular supply of organic matter. Long-term use of only artificial fertilisers leads to acidification of the soil, which directly causes the depletion of phosphorus and blocking of microelements. This problem is aggravated by simplified rotation, lack of use of catch crops and complete removal of straw from the field without its biological compensation. In such conditions, low biological activity of the soil prevents the natural release of mineral reserves locked in the ground.How does soil retain nutrients?
The soil retains nutrients through the phenomenon of physicochemical sorption occurring on the surface of soil colloids, which create a mineral-organic sorption complex. Humus particles and clay minerals have a negative electric charge, thanks to which they attract and bind positively charged cations of potassium, calcium, magnesium and ammonium forms of nitrogen. The higher the content of stable humus in the soil profile, the higher the water and fertiliser capacity of the entire site. This process prevents minerals from being irreversibly washed deep into the ground during heavy rainfall.
