Microorganisms play a vital role in soil by decomposing organic matter, producing oxygen, and fixing nitrogen, which are essential for plant growth and soil fertility.

While microorganisms play a crucial role in nutrient cycling, soil structure improvement, and plant disease suppression, greenhouse gas production is a negative impact associated with certain microbial activities.

Decomposition is the process by which microorganisms break down organic matter into simpler compounds, releasing nutrients back into the soil.

Nitrogen-fixing bacteria, such as Rhizobium and Azotobacter, are responsible for converting atmospheric nitrogen into a form that can be utilized by plants.

Ammonification is the process by which microorganisms convert organic nitrogen into ammonia, which is then further converted into nitrate and nitrite through nitrification.

The A horizon, also known as the topsoil, is the most fertile layer of soil and contains the highest concentration of organic matter, nutrients, and microbial activity.

Denitrification is the process by which microorganisms convert nitrate into nitrogen gas, which is released into the atmosphere.

Temperature, moisture, and pH are key factors that influence microbial activity in soil, while gravity does not directly affect microbial processes.

Mycorrhizae are symbiotic associations between certain fungi and plant roots, where the fungus helps the plant absorb nutrients from the soil in exchange for carbohydrates.

Fungi, particularly white-rot fungi, are the primary decomposers of cellulose, a major component of plant cell walls, in soil.

Mineralization is the process by which microorganisms convert organic phosphorus into inorganic forms, making it available for plant uptake.

The B horizon, also known as the subsoil, is typically the most compacted layer of soil and contains the highest concentration of clay and minerals.

Mineralization is the process by which microorganisms convert organic sulfur into inorganic forms, making it available for plant uptake.

Fungi, particularly brown-rot fungi, are the primary decomposers of lignin, a complex organic compound found in plant cell walls.

Mineralization is the process by which microorganisms convert organic potassium into inorganic forms, making it available for plant uptake.