Humic Acid

Classification	:	Humic Acid
Country Of Origin	:	Jorden
Certificate of Analysis (CoA)	:	Available
Form	:	Powder
Shelf Life	:	2 Years
Storage	:	Dry Place
Brand Name	:	Russian Organic Fertilizer
Purity	:	98%
Packaging type	:	Plastic Bag
Manufacturing Capacity	:	500 Ton per Month
Packing Size	:	25, 50,100 Kg.
MOQ	:	100 Kg

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Humic Acid

Humic acids are the organic substances that coagulate when the strong-base extract is acidified while fulvic acids are the organic substances that remain soluble when the strong-base extract is acidified.

Humic acid is a chemical produced by decaying plants. People use it to make medicine. People take humic acid for stimulating the immune system and treating the flu (influenza), avian flu, swine flu, and other viral infections.

Humic acid buffers soil pH to 5.5 to 7.5 levels which is ideal for plant development and nutrient absorption. Thus acting as a natural chelator, they help plant roots to absorb nutrients more efficiently to create a long-term positive effect on soil quality and productivity.

Humic acid increases nutrient uptake, drought tolerance, and seed germination. It increases the microbial activity in the soil, making it an excellent root stimulator. Humic acid increases the availability of nutrients in our fertilizers and in those already existing in your soil.

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Humic acid neutralizes both acidic and alkaline soils and regulates the pH level of soils and it promotes the conversion of nutrient elements like N, P, K, Fe, Zn into available forms due to increased cation exchange capacity.

improve and optimize the uptake of nutrients and water by plants. increase buffering properties of soil. act as a natural chelator for metal ions under alkaline conditions and promote their uptake by the roots. rich in both organic and mineral substances essential to plant growth.

Humic acid and fulvic acid represent up to 80% of the TOC – dissolved organics – of natural waters. Humic substances are weak acidic electrolytes with carboxylic- and phenolic-OH groups with a micelle-like structure and with a molecular weight between 500 (fulvic) and 100,000 (humic). They become hydrophobic as pH decreases and thus foul hydrophobic membranes more. Humic fouling in the case of natural waters is aggravated by the presence of calcium (Ca+) by forming a bridge between the membrane and the negatively charged membrane surface, and/or between negatively charged carboxyl groups of the humic acid. Other organic components that foul membranes include microbial slime, polyhydroxy aromatics, and polysaccharides.

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Powder Fertilizer | Bio-Feed | Microelements | Special Formulation

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