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65% Humic Acid 4mm Flakes Natural Potassium Fertilizer

Minimum Order Quantity : 1MT Packaging Details : 1kg, 5kg, 10kg, 25kg
Delivery Time : 5-8 Work Days Payment Terms : L/C, D/P, T/T, Western Union
Supply Ability : 500 Metric Tons per Week
Place of Origin: CHINA Brand Name: New-Nutri
Certification: OMRI Model Number: YNPH05G10

Detail Information

Humic Acid: 65% Fulvic Acid: 3%~5%
Potassium-K2O: 12% Water Solubility: 100%
PH: 9.5 Appearance: Black Shiny Flakes
Size: 2-4mm
High Light:

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Product Description

Water Soluble Potassium Humate Fertilizer , Black Shiny Flakes , Humic Acid 65%

 

 

New-Nutri Potassium Humate Shiny Flakes is one of our best-selling products, there are many customers from India, Egypt, Turkey, Vietnam and other countries ordering it every year. It can be used in various irrigation systems. New-Nutri Potassium Humate shiny flakes is characterized by good water solubility, high humic acid and fulvic acid content, no sediment, no flocculation, and can be used together with most other fertilizers.

 

Specifications:

Water Solubility 100%
Humic Acid 65%
Fulvic Acid 3%
K2O 12%
pH 9-10

 

65% Humic Acid 4mm Flakes Natural Potassium Fertilizer 0

 

It is well known that potassium humate can regulate soil environment and effectively deal with soil hardening. But what causes the soil to harden?Now let's see.

  1. The content of organic matter is an important index of soil fertility and granule structure. The decrease of organic matter results in soil compaction.The low content of soil organic matter affects the activity of microorganisms, which influences the formation of soil aggregates and leads to soil compaction.
  2. Excessive application of potassium fertilizer into the soil, potassium ion displacement in potassium is particularly strong, can form the soil aggregates of polyvalent cation replacement out, but the monovalent potassium ion does not have bond bridge, the bond bridge of the soil aggregate structure was destroyed, also destroyed the aggregate structure, resulting in soil compaction.
  3. The aggregate structure of soil is an important index of soil fertility. The destruction of the aggregate structure of soil results in the decrease of soil water retention, fertilizer retention ability and permeability, resulting in soil hardening.
  4. The soil aggregate structure is formed by negatively charged soil clay and organic matter connected by positively charged polyvalent cation.
  5. Soil acidity or alkalinity is too large or too small, such as acid rain.

 

 

 

 

 

 

 

 

 

 

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