askvity

How do microorganisms increase soil fertility?

Published in Soil Biology 3 mins read

Microorganisms increase soil fertility primarily by decomposing organic matter, cycling nutrients, and improving soil structure.

Microorganisms, including bacteria, fungi, archaea, and protozoa, play a crucial role in enhancing soil fertility. Their activities directly impact nutrient availability, soil structure, and plant health. Here's a detailed breakdown of how they achieve this:

Decomposition of Organic Matter

Microbes are nature's recyclers. They break down complex organic materials, such as dead plant matter, animal waste, and other organic residues, through a process called decomposition. This process releases essential nutrients back into the soil in forms that plants can readily absorb.

Nutrient Cycling

  • Nitrogen Fixation: Certain bacteria, like Rhizobium in association with legumes, convert atmospheric nitrogen (N2) into ammonia (NH3), a usable form of nitrogen for plants. This is a vital process as nitrogen is often a limiting nutrient for plant growth.
  • Phosphorus Solubilization: Many microorganisms, including bacteria and fungi, can solubilize insoluble forms of phosphorus in the soil, making it available to plants. Phosphorus is crucial for plant energy transfer and root development.
  • Potassium Mobilization: Similarly, certain microbes can mobilize potassium, another essential macronutrient, from insoluble mineral forms in the soil.
  • Sulfur Oxidation and Reduction: Microorganisms facilitate the cycling of sulfur by oxidizing and reducing various sulfur compounds, making it available for plant uptake.

Improving Soil Structure

  • Aggregation: Fungi, particularly mycorrhizal fungi, play a key role in soil aggregation. Their hyphae (thread-like filaments) bind soil particles together, creating stable aggregates. This improves soil porosity, water infiltration, and aeration.
  • Production of Polysaccharides: Bacteria and fungi produce polysaccharides (sugars) that act as "glues," binding soil particles and contributing to soil structure stability.
  • Increased Water Retention: Well-aggregated soil retains more water, making it available to plants during dry periods.

Enhanced Plant Growth

  • Production of Plant Growth Regulators: Some microorganisms produce plant growth hormones like auxins, gibberellins, and cytokinins, which promote root growth, shoot elongation, and overall plant development.
  • Disease Suppression: Beneficial microbes can suppress plant diseases by competing with pathogens, producing antibiotics, or inducing systemic resistance in plants.
  • Improved Nutrient Uptake: Mycorrhizal fungi, in particular, form symbiotic relationships with plant roots, extending the root system and increasing the surface area for nutrient and water absorption. This is especially important for phosphorus uptake.

In summary, the combined activities of microorganisms in the soil significantly enhance its fertility by improving nutrient availability, soil structure, and plant health, ultimately leading to increased crop yields and sustainable agriculture.

Related Articles