Participates in the formation of the soil structure and the more productive development of microflora.
Promotes the rapid restoration of degraded and depleted soil resulting from intensive farming.
Reduces the loss of water and nutrients in light sandy soil. Promotes the enrichment of such soil with humus.
Promotes the ventilation and loosening of heavy and clay soil, and thereby improves its supply of oxygen and enhances the workability of the soil.
Selectively activates the work of useful soil forming and nodule bacteria, while simultaneously inhibiting pathogenic microflora and fungal diseases in the soil.
Counteracts the covering of the soil with a crust as well as its erosion, due to the increased ability of the colloids to bind together.
Improves the moisture retention capacity of the soil by increasing its resistance to drought. Optimises the balance of water in the soil.
Promotes normalisation of the soil pH.
Acts as a chelator for the metal ions under alkaline conditions, thus creating the possibility for their perception by the roots.
Fixes soluble inorganic fertilisers in the root zones, while increasing the digestibility of the root system in the plant and reducing leaching.
Has an extremely high capacity for exchanges of cations, which promotes the transformation of NPK nutrients, as well as other trace
elements, into a form that can be perceived directly by the plants.
Irreversibly binds the salts of heavy metals and radionuclides to sedentary complexes, which are removed from the soil circulation, preventing them from entering plants and agricultural products.
Promotes the process of the utilisation of residues from plant protection chemicals and other harmful metabolites, which leads to a decrease in the chemical load on the soil.
Participates in the formation of the soil structure and the more productive development of microflora.