The earth's atmosphere is made up of about 78% nitrogen, making it the largest pool of this gas. Nitrogen is essential for many biological processes. It is in all amino acids, proteins and nucleic acids. As you will see in a later chapter, these compounds are needed to build tissues, transport substances around the body and control what happens in living organisms. In plants, much of the nitrogen is used in chlorophyll molecules which are needed for photosynthesis and growth.
So, if nitrogen is so essential for life, how does it go from being a gas in the atmosphere to being part of living organisms such as plants and animals? The problem with nitrogen is that it is an 'inert' gas, which means that it is unavailable to living organisms in its gaseous form. This is because of the strong triple bond between its atoms that makes it difficult to break. Something needs to happen to the nitrogen gas to change it into a form that it can be used. And at some later stage, these new compounds must be converted back into nitrogen gas so that the amount of nitrogen in the atmosphere stays the same. This process of changing nitrogen into different forms is called the nitrogen cycle (Figure 1).
- Definition 1: The nitrogen cycle
The nitrogen cycle is a biogeochemical cycle that describes how nitrogen and nitrogen-containing compounds are changed in nature.
Very broadly, the nitrogen cycle is made up of the following processes:
- Nitrogen fixation - The process of converting inert nitrogen gas into more useable nitrogen compounds such as ammonia.
- Nitrification - The conversion of ammonia into nitrites and then into nitrates, which can be absorbed and used by plants.
- Denitrification - The conversion of nitrates back into nitrogen gas in the atmosphere.
We are going to look at each of these processes in more detail.
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