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Soil nitrogen conversion processes
The three main sources of nitrogen, used in agriculture are urea, ammonium and nitrate. The biological oxidation of ammonia to nitrate is known as nitrification. This process consists of various steps, as demonstrated in Figure 1, and is mediated by autotrophic, obligately aerobic bacteria. In waterlogged soils the oxidation of NH4+ is thus restricted. Urea is decomposed by the enzyme urease or chemically hydrolyzed into ammonia and CO2. In the ammonification step, ammonia is converted by ammonium-oxidizing bacteria into ammonium. In a next step, ammonium is converted by nitrifying bacteria into nitrate (nitrification).
The nitrogen conversion rate depends on the conditions, present in the soil for nitrifying bacteria. Nitrification of NH4+ to NO3- preferably occurs under the following conditions:
The three main sources of nitrogen, used in agriculture are urea, ammonium and nitrate. The biological oxidation of ammonia to nitrate is known as nitrification. This process consists of various steps, as demonstrated in Figure 1, and is mediated by autotrophic, obligately aerobic bacteria. In waterlogged soils the oxidation of NH4+ is thus restricted. Urea is decomposed by the enzyme urease or chemically hydrolyzed into ammonia and CO2. In the ammonification step, ammonia is converted by ammonium-oxidizing bacteria into ammonium. In a next step, ammonium is converted by nitrifying bacteria into nitrate (nitrification).
The nitrogen conversion rate depends on the conditions, present in the soil for nitrifying bacteria. Nitrification of NH4+ to NO3- preferably occurs under the following conditions:
- In the presence of nitrifying bacteria.
- Soil temperature > 20 °C.
- Soil pH 5,5 - 7,5.
- Sufficiently available soil moisture and oxygen.