Nitrogen Cycle
Definition
The nitrogen cycle is the continuous movement of nitrogen through the atmosphere, soil, and living organisms, cycling through fixation, ammonification, nitrification, assimilation, and denitrification. Each step is driven by different groups of bacteria, converting nitrogen between forms plants can and cannot use.
Why It Matters
Nitrogen is the macronutrient plants need in the greatest quantity, but it exists in the atmosphere in a form plants can't use directly. The nitrogen cycle is what makes nitrogen usable in the first place, and understanding it explains both fertility and nitrogen loss in soil.
How It Works
Nitrogen fixation converts atmospheric N₂ into ammonia. Ammonification breaks down organic nitrogen from decomposing matter into ammonium. Nitrification converts ammonium into nitrate, the form plants absorb most readily. Assimilation is plants taking up that nitrate. Denitrification, occurring mainly in low-oxygen conditions, converts nitrate back into atmospheric nitrogen gas, completing the cycle.
Benefits of a Healthy Nitrogen Cycle
- Sustained natural soil fertility
- Reduced need for synthetic nitrogen inputs
- Lower nitrogen loss to leaching or the atmosphere
- Better long-term nutrient cycling balance
How to Support a Healthy Nitrogen Cycle
Working with the cycle beats bypassing it with a single synthetic form.
Feed the Whole Cycle With Organic Matter
Worm castings and compost supply organic nitrogen and the diverse bacteria that carry it through ammonification and nitrification naturally.
Avoid Waterlogged, Compacted Soil
Anaerobic conditions drive denitrification, converting valuable plant-available nitrogen back into gas that's lost to the atmosphere.
Plant Legume Cover Crops
Legumes contribute directly to nitrogen fixation, adding new nitrogen into the cycle beyond what's already cycling through the system.
Support Diverse Soil Biology Generally
Each stage of the cycle depends on different bacteria. A biologically diverse soil supports the full cycle rather than just one stage of it.
Sources: University of Minnesota Extension
The Five Stages of the Nitrogen Cycle
Each stage transforms nitrogen into a different chemical form, driven by a different group of bacteria.
| Converts | Driven By | |
|---|---|---|
| 1. Fixation | Atmospheric N₂ → Ammonia (NH₃) | Rhizobium (symbiotic) and free-living bacteria |
| 2. Ammonification | Organic nitrogen → Ammonium (NH₄⁺) | Decomposer bacteria and fungi |
| 3. Nitrification | Ammonium → Nitrite → Nitrate (NO₃⁻) | Nitrifying bacteria (requires oxygen) |
| 4. Assimilation | Nitrate/ammonium → Plant tissue | Plant root uptake |
| 5. Denitrification | Nitrate → Atmospheric N₂ gas | Denitrifying bacteria (low-oxygen conditions) |
Common Mistakes to Avoid
The nitrogen cycle is often reduced to just "fixation" or ignored entirely in favor of synthetic fertilizer.
Sources: University of Minnesota Extension, Iowa State University Extension, Ohio State University Extension, University of Minnesota Extension (compaction)
Frequently Asked Questions
What is the nitrogen cycle? +
What are the main steps of the nitrogen cycle? +
What is ammonification? +
What is nitrification? +
What is denitrification and why does it matter? +
How can I minimize nitrogen loss from my soil? +
How do worm castings interact with the nitrogen cycle? +
How does nitrogen fixation fit into the nitrogen cycle? +
Worm castings introduce a diverse population of nitrogen-cycling bacteria, supporting the natural cycle rather than bypassing it with a single synthetic nitrogen form.









