Editing Nitrogen cycle (section)

=== Nitrification ===
{{Main|Nitrification}}
The conversion of ammonium to nitrate is performed primarily by soil-living bacteria and other nitrifying bacteria. In the primary stage of nitrification, the oxidation of ammonium ({{chem2|NH4+}}) is performed by bacteria such as the ''[[Nitrosomonas]]'' species, which converts ammonia to [[nitrites]] ({{chem2|NO2-}}). Other bacterial species such as ''[[Nitrobacter]]'', are responsible for the oxidation of the nitrites ({{chem2|NO2-}}) into [[nitrates]] ({{chem2|NO3-}}). It is important for the [[ammonia]] ({{chem2|NH3}}) to be converted to nitrates or nitrites because ammonia gas is toxic to plants.

Due to their very high [[solubility]] and because soils are highly unable to retain [[anions]], nitrates can enter [[groundwater]]. Elevated nitrate in groundwater is a concern for drinking water use because nitrate can interfere with blood-oxygen levels in infants and cause [[methemoglobinemia]] or blue-baby syndrome.<ref name="Vitousek 1997" /> Where groundwater recharges stream flow, nitrate-enriched groundwater can contribute to [[eutrophication]], a process that leads to high algal population and growth, especially blue-green algal populations. While not directly toxic to fish life, like ammonia, nitrate can have indirect effects on fish if it contributes to this eutrophication. Nitrogen has contributed to severe eutrophication problems in some water bodies. Since 2006, the application of nitrogen [[fertilizer]] has been increasingly controlled in Britain and the United States. This is occurring along the same lines as control of phosphorus fertilizer, restriction of which is normally considered essential to the recovery of eutrophied waterbodies.