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Copper Sulfate
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Copper sulfate, commonly referred to simply as copper sulfate, is the ionic chemical compound or white anhydrous salt formed by the copper cation and sulfate anion, characterized by the chemical formula CuSO₄. It is marketed in anhydrous form or in hydrated forms.
SULFUR
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Sulfur, represented by the formula S₈, is a non-metallic chemical element that naturally occurs in various forms and is essential for many chemical reactions and industrial processes.
Sulfate de Fer
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Iron sulfate is a chemical compound in the form of a pale green to blue-green crystalline solid.
Chélates de Fer
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Iron chelates are available as a fine powder, typically light brown or beige in color, odorless, and highly water-soluble.
Zinc Chelates
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Zinc chelates are available as a white crystalline or slightly granular powder, odorless, stable, and highly bioavailable.
Molybdate D'ammonium
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Ammonium Molybdate appears as a white crystalline powder, odorless, and slightly hygroscopic.
Lime
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Lime appears as a white crystalline powder or granules. It is odorless, mildly caustic, and soluble in water, where it forms an alkaline solution known as limewater.
Fulvic Acid
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Fulvic acid is a naturally occurring organic compound, primarily extracted from soil humates, and is a part of the humic acid family. It typically appears as a brown to black powder (depending on the source) and is generally odorless.
Leonardite
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Leonardite is a naturally occurring organic material, primarily composed of humus, lignite, and other fossil organic matter. It typically presents as a fine brown to black powder, with a faint odor, and is insoluble in water
Humic Acid
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Humic Acid appears as a brown to black powder, odorless, and slightly soluble in water under certain conditions. It is primarily extracted from lignite, peat, or organic-rich soils. While weakly soluble in water, it easily dissolves in alkaline solutions.
Biochar
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Biochar is a solid material, typically in the form of black or dark gray powder, derived from the pyrolysis of organic biomass under controlled low-oxygen conditions.
Peat
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Peat appears as a brown or black, often moist, organic material formed under low-oxygen conditions. It is a natural substance composed of partially decomposed plant debris.