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Zeolite

Zeolites are aluminosilicates formed by the vitrification of volcanic ash over millions of years. They have a high porosity and a high ion exchange capacity.
Leonardite

It is the substance composed of organic products, colloidal in nature, which comes from the decomposition of organic remains (fungi and bacteria). The fibrous mass was transformed into coal on which the thin layer of Leonardito was formed.
Phosphoric rock

It is a natural phosphate fertilizer of direct application, without chemical alterations, of high efficiency. It is characterized by providing the soil with a good percentage of phosphorus, from the moment it is applied, and in a gradual and sustained manner over time.
Bentonite

It is a natural clay that contains a high portion of Montmorrillonite, a hydrated colloidal aluminum silicate of natural origin, in which some aluminum and silicon atoms may have been replaced by other atoms, such as magnesium, calcium and iron.
Dolomite lime

In agriculture, dolomite lime is a source of magnesium and calcium that constitutes an indispensable fertilizer by modifying the pH of the soil, managing to regulate its acidity, improving it and increasing the yield of crops.