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Lesson 32 Mineral Cycling - Alaska Geobotany Center

Lesson 32 Mineral Cycling - Alaska Geobotany Center

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Another gaseous cycle: the nitrogen cycle<br />

5<br />

N 2<br />

1<br />

4<br />

7<br />

6<br />

Nitrogen<br />

fixation<br />

3<br />

2<br />

1. Nitrogen is taken up from the soil by plants in<br />

theformofNH 4 + or NO 3 - , where it is used to<br />

form organic compounds (amino acids,<br />

proteins, nucleic acids).<br />

2. It returns to the soil via litter, which is<br />

decomposed to form ammonia. This process<br />

of decomposition is also called nitrogen<br />

mineralization.<br />

3,4. The ammonia is oxidized in a two step<br />

nitrification process to form nitrates<br />

(NO 3 - ),which are an available form of N for<br />

plant uptake.<br />

5. NO 3 - -N can also be converted back to the<br />

gaseous NO, N 2 O, and N 2 , through the<br />

process of denitrification. The atmospheric<br />

store of N is about 1 million times larger than<br />

the total N in living organisms.<br />

6. Nitrogen-fixation transforms atmospheric<br />

N 2 into ammonia (NH 3 ) , which is also an<br />

available form of N for plant uptake.<br />

7. NO 3 - is also easily leached from the soil.<br />

Courtesy of Michael Pidwirny and Jim Deacon web sites<br />

http://helios.bto.ed.ac.uk/bto/microbes/nitrogen.htm<br />

http://www.physicalgeography.net/fundamentals/9s.html

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