Leonardita del Ebro
Give back to the earth what it gives you, LIFE!
High-quality leonardite, suitable for organic farming.
Organic amendment
Mejora la fertilidad del suelo
Humic and Fulvic Acids
Mejora la estructura del suelo a largo plazo
100% Natural
Apta para cultivos ecológicos
What is leonardite?
It is a natural organic mineral formed from the oxidation of lignite over millions of years, resulting from the slow decomposition of ancient plant matter. It is found in surface and underground deposits, usually associated with layers of soft coal, and stands out for its high content of stabilized organic matter.
Benefits of Leonardite and Humic Acids in Your Crops
Improves Soil Structure
Enhances Nutrient Absorption
Stimulates Growth
Why Choose Us?
At Leonardita del Ebro, we are committed to agriculture based on quality and respect for the soil. Our natural leonardite comes from our own deposits in Mequinenza, selected for their high humic acid and organic matter content. Through a screening process, we ensure a consistent and reliable organic amendment designed to improve soil structure and optimize nutrient absorption in crops.
We offer a direct mine-to-farmer approach, providing in-depth technical knowledge and a strong commitment to sustainable agriculture and land regeneration, ensuring trust and focusing on long-term results.
International Export and Distribution of Leonardite
At Leonardita del Ebro, we currently export to 8 countries, including the United Kingdom, France, Portugal, Brazil, Saudi Arabia, and the United Arab Emirates. Our leonardite has been recognized for its high quality across different climates and crop types.
We continue to grow and open new international expansion channels, with the goal of bringing more sustainable agriculture to every corner of the world.
Success Stories: Agricultural Companies That Trust Our Organic Amendment
We also want to acknowledge the hundreds of small and medium-sized farmers who have trusted us to enhance their crops in an eco-friendly and soil-sustainable way.
