Conversion of ammonia or ammonia compounds into nitrates or nitrites by microorganisms in the soil.
Nitrification is a key process in the nitrogen cycle, where certain bacteria convert ammonium (NH₄⁺) into nitrate (NO₃⁻) through a two-step biochemical process. This transformation is essential for soil fertility, as plants can readily absorb nitrate.
Steps of Nitrification:
-
Ammonium Oxidation (Nitritation):
- Ammonium (NH₄⁺) is converted into nitrite (NO₂⁻) by ammonia-oxidizing bacteria (AOB) or archaea (e.g., Nitrosomonas).
- Reaction:
-
Nitrite Oxidation (Nitratation):
- Nitrite (NO₂⁻) is further oxidized to nitrate (NO₃⁻) by nitrite-oxidizing bacteria (NOB) (e.g., Nitrobacter).
- Reaction:
Importance of Nitrification:
- Soil Fertility: Nitrate produced is a crucial nutrient for plant growth.
- Ecosystem Health: Supports the nitrogen cycle, essential for life on Earth.
- Water Quality Concerns: Excessive nitrification (often due to fertilizers) can lead to nitrate leaching into water bodies, causing eutrophication.
Factors Affecting Nitrification:
- Oxygen Levels: Nitrification is aerobic and requires oxygen.
- Soil pH: Optimal at neutral to slightly alkaline pH.
- Temperature: Thrives in moderate temperatures (20–30°C).
- Organic Matter: Provides ammonium for the process.
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