Soil Effects
→It improves the physical, chemical, and biological structure of the soil, providing a suitable growth environment for plants.
→It increases the activity of beneficial microorganisms and provides a source of NUTRITION and ENERGY for soil organisms.
→It chelates vital plant nutrients such as phosphorus, calcium, zinc, iron, and manganese, which are bound in the soil and unavailable to plants, making them active for plants.
→It revitalizes the soil and plants in the growing environment with its high amounts of humic-fulvic acid and potassium.
→It reduces the effects of salinity caused by heavy fertilization and other causes.
→It prevents soil hardening, prevents the formation of crusts, loosens the soil, and increases its aeration and water-holding capacity. This promotes good rooting. It also prevents rapid water evaporation in sandy soils.
→It retains plant nutrients in the root zone, ensuring the plant receives as much as it needs. This prevents excessive fertilizer use.
→It also helps improve soils with low organic matter and high lime content, contributing to the creation of an ideal environment for growth.