Humic substances

Humic substances are a group of complex organic compounds that form as a result of the decomposition of plant and animal matter over long periods, typically in soils, sediments, and natural waters. They are a major component of soil organic matter and play a critical role in soil fertility, water retention, and the global carbon cycle. Humic substances are divided into three main categories based on their solubility:

  1. Humic Acids
    • Soluble in alkaline solutions but precipitate in acidic conditions.
    • They are dark brown to black in color and are responsible for much of the color of organic-rich soils.
    • Humic acids improve soil structure, increase water retention, and enhance nutrient availability.
  2. Fulvic Acids
    • Soluble in both acidic and alkaline conditions.
    • Lighter in color (yellow to brown) and smaller in molecular size compared to humic acids.
    • Fulvic acids are highly mobile in soil and water and can easily transport nutrients and minerals to plants.
  3. Humin
    • Insoluble in both acidic and alkaline conditions.
    • Humin is the most stable fraction and contributes to long-term carbon storage in soils.
    • It plays a role in improving soil structure and acts as a carbon reservoir.

Key Functions of Humic Substances

  • Soil Health: They improve soil texture, aeration, and water-holding capacity.
  • Nutrient Cycling: Humic substances bind with nutrients, making them more available to plants and reducing nutrient loss through leaching.
  • pH Buffering: They help stabilize soil pH, creating a favorable environment for plant growth.
  • Microbial Activity: They provide energy sources for soil microorganisms, which are essential for soil fertility.

In addition to their role in agriculture and ecology, humic substances are also used in water treatment, environmental remediation, and as supplements in animal feed and human health products due to their chelating and antioxidant properties.

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