NITROGEN CYCLE SIMULATION

Plants live immersed in nitrogen and still go hungry for it: N₂ makes up 78% of the air, but the N≡N triple bond is so strong that almost nothing can touch it. Only bacteria carrying nitrogenase, lightning strikes and the Haber-Bosch reactor can prise it open. Step by step around the loop the ammonium and nitrate pools rise and fall: over-fertilising flushes nitrate into the water and triggers eutrophication, while denitrification sends N₂ back to the sky along with some N₂O, a potent greenhouse gas.

▸ Building the land–sky landscape…
▸ Loading the N₂ atmosphere (N≡N triple bond)
▸ Seeding nitrogen-fixing bacteria into root nodules
▸ Linking the flow: fixation → nitrification → assimilation
▸ Starting ammonification & denitrification…
▸ Ready — Online. ✅
0%
⌂ The Living World

Simulation room Nitrogen Cycle

Nitrogen Cycle
Online
N₂ · bacteria · closed loop
Nitrogen reservoirs
🟦 Reservoirs & fluxes
Atmospheric N₂—
NH₄⁺ ammonium—
NO₃⁻ nitrate—
Organic nitrogen—
Fixation rate—
Viewing—
Note
Nitrogen makes up 78% of the air, but its N₂ form has a very strong N≡N triple bond — most organisms cannot use it. Bacteria are the "workers" that convert N₂ into nitrogen plants can absorb, then close the loop and return it to the air.
—
Pick a "Scenario" (emphasize fixation / nitrification / denitrification / over-fertilize…) · click a stage or concept for details
Your browser has not enabled canvas.
Soil nitrogen forms over time NH₄⁺NO₃⁻organic
About Nitrogen Cycle

Plants live immersed in nitrogen and still go hungry for it: N₂ makes up 78% of the air, but the N≡N triple bond is so strong that almost nothing can touch it. Only bacteria carrying nitrogenase, lightning strikes and the Haber-Bosch reactor can prise it open. Step by step around the loop the ammonium and nitrate pools rise and fall: over-fertilising flushes nitrate into the water and triggers eutrophication, while denitrification sends N₂ back to the sky along with some N₂O, a potent greenhouse gas.

Related topics in Living World