Nitrogen Cycle Worksheets
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Nitrogen Cycle Worksheets
Investigation: nutrients near the station
After heavy rain, Aisha and Callum investigate a patch of land beside a busy train station. Run-off from nearby fields enters a stream. They test nitrogen compounds upstream and downstream.
Sample site
Nitrate concentration (mg/L)
Upstream of fields
2.1
Downstream of fields
12.6
Trace the nitrogen
Use this simplified cycle to help with Questions 1–3. Arrows show the direction nitrogen moves.
Atmospheric N₂ → nitrogen fixation → ammonia / ammonium in soil
Ammonia / ammonium → nitrification → nitrite → nitrate
Nitrate → assimilation into plants → animals; dead matter and waste → ammonification → ammonia / ammonium
Nitrate → denitrification → atmospheric N₂
Lightning can also fix some atmospheric nitrogen, forming compounds that reach soil in rain.
Nitrogen-fixing bacteria may live freely in soil or in root nodules of leguminous plants.
- N₂ is too reactive to remain in the atmosphere.
- The triple bond in N₂ is very strong, so plants cannot convert it into usable nitrogen compounds.
- Plants only absorb nitrogen through their leaves.
- Nitrogen gas contains no nitrogen atoms.
- Nitrogen fixation
- Nitrification
- Assimilation
- Ammonification
- Denitrification
- Plants take up inorganic nitrogen and incorporate it into organic molecules.
- Decomposers convert organic nitrogen in waste or dead matter to ammonia / ammonium.
- Nitrate is reduced to nitrogen gas, often in low-oxygen conditions.
- Atmospheric N₂ is converted to ammonia or ammonium.
- Ammonia / ammonium is oxidised to nitrite, then nitrate.
- High nitrate availability and low oxygen
- Low nitrate availability and bright light
- High oxygen and very dry soil
- No decomposers and low temperature
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