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Factsheet: Nitrogen

What is Nitrogen?

Nitrogen is a naturally occurring chemical element, with the symbol N. In its gas form (N2), nitrogen makes up about 80% of the Earth's atmosphere. In other forms it is one of the most important nutrients for plant growth. It is also found in amino acids that make up proteins, in nucleic acids (that make up DNA) and in many other organic and inorganic compounds.

 Nitrogen cycle

This figure shows a schematic representation of the flow of nitrogen through the environment.  Bacteria are a key aspect of the cycle, providing different forms of nitrogen compounds that can be utilised by higher organisms. Source: Wikipedia.

 

Nitrogen occurs as several forms in the environment:

Nitrogen gas (N2)

As a gas, nitrogen is relatively inactive but can be converted to other more reactive forms by certain bacteria through a process called fixation.

Nitrate-Nitrogen (NO3-N)

Nitrate-nitrogen is the concentration of nitrogen present in the form of the nitrate ion. Nitrate is a water soluble molecule made up of nitrogen and oxygen with the chemical formula NO3. It is a very important plant nutrient but because it is highly water soluble, it leaches through soils and into groundwater very easily, particularly after heavy rainfall.

It is one of the most common contaminants of rivers, streams and groundwater in rural and urban areas. Sources of nitrate include excessive application of inorganic fertiliser, animal and human waste. Nitrogen fixation and soil cultivation can also cause nitrate leaching if poorly managed. On grazed pastures, animal urine patches can be a major source of nitrate leaching.

Once in groundwater, nitrate can persist for many years and travel long distances. Under some conditions, where aquifers contain decaying organic material that consumes available oxygen dissolved in the water, nitrate can be converted to nitrogen gas in a process called “denitrification”. This has been shown to occur on a local scale in many parts of New Zealand, and it can explain why some wells have very low nitrate concentrations when other wells nearby have much higher concentrations. However, it is unclear that denitrification plays a major role in removing nitrate from groundwater on a regional scale.

Where groundwater emerges as springs, it can be an important source of contamination in streams and lakes. In fact, transport via groundwater is probably the main pathway by which nitrogen is carried from agricultural land into surface water bodies.

In drinking water, high nitrate concentrations can be harmful to humans and livestock. The New Zealand Ministry of Health (2018) has set a Maximum Acceptable Value (MAV) for nitrate (as the nitrate ion) in drinking water of 50 milligrams per litre (mg/L) to prevent against short-term health risk to bottle-fed babies. When expressed as nitrate nitrogen, the units used in LAWA, the MAV is equivalent to 11.3 mg/L.

Nitrite-Nitrogen (NO2-N)

Nitrite-nitrogen is the concentration of nitrogen present in the form of the nitrite ion. Nitrite is a water soluble molecule with the chemical formula NO2. Concentrations of nitrite are normally low compared to nitrate and ammoniacal nitrogen. However, too much nitrite can be toxic. In drinking water, it can be harmful to humans and livestock.

Ammoniacal nitrogen (NH4-N)

Ammoniacal nitrogen (NH4-N), also often called ‘ammonium’, is the concentration of nitrogen present as either ammonia (NH3) or ammonium (NH4).  These ammoniacal forms can be transformed to other forms of nitrogen and are very important plant fertilisers but are generally less mobile in the soil than nitrate. Ammoniacal forms of nitrogen enter waterways primarily through point source discharges, such as raw sewage or dairy shed effluent. It is toxic to aquatic life at high concentrations.

Ammonia (NH3)

Ammonia (NH3) is a gas that reacts to form the ammonium ion (NH4) when it is dissolved in water. The balance between ammonia and ammonium in water depends on the pH and temperature of the water.  Ammonia is highly toxic to aquatic life.

Total Nitrogen (TN)

Total Nitrogen is the sum of all organic and inorganic forms of nitrogen that are found in a water sample (i.e., nitrate-nitrogen (NO3-N), nitrite-nitrogen (NO2-N), ammoniacal-nitrogen (NH4-N) and organic nitrogen such as amino acids or plant tissue).

In New Zealand, total nitrogen is measured (on unfiltered water) by two different methods used by different regional councils and other agencies doing regular water testing:

One method is called TN-A where total nitrogen is measured by a procedure called “direct persulphate digestion”. The other method is called TN-K, which involves summing the separate measurements of organic nitrogen compounds, ammoniacal nitrogen (NH4-N, NH3) and oxidised nitrogen (NO3-N, NO2-N) to estimate total nitrogen.

Scientists recently found out that total nitrogen water quality measurements vary significantly, depending on the turbidity of the river water and the methodology used. Total nitrogen laboratory results were slightly higher when the TN-K method was used and lower with the TN-A method (an average of 8% less) in very turbid rivers (that is a river with Total Suspended Solids > 10 mg/L).

These new findings raise the question which method should be used by councils and whether councils may need to change the way they currently calculate total nitrogen, adjusting their methods to either TN-K or TN-A. To date, however, there is no clear answer to the question which method is ‘best practice’. Moreover, a change in methodology can cause difficulties when calculating long-term trends in turbid waters (such as flooded rivers or shallow wind-disturbed lakes prone to sediment re-suspension). We therefore recommend that until further research has been done on this subject, existing TN methods within regions should be continued to maintain sampling continuity for trend calculations.

Why is too much nitrogen a problem?

Nitrogen is an effective fertiliser and essential plant nutrient, but increased concentrations in water can cause negative environmental effects. Excess nitrogen can contribute to rapid growth of aquatic weeds and algae in rivers, streams, lakes, estuaries and the ocean. Commonly, this can result in plant or algal blooms. As the plants then die and the excess organic material decomposes, oxygen in the surrounding water is used up and in severe cases this reduction of oxygen poses a threat to aquatic life. Nitrogen itself can also become toxic to aquatic life at high concentrations, particularly under certain temperature and pH conditions. This can cause direct harm to fish and macroinvertebrates.

In drinking water, the nitrate form of nitrogen can be toxic to humans and other animals at high concentrations (see the discussion on nitrate above).

Where does nitrogen come from?

The most common sources are leaching and run-off from agriculture, wastewater treatment plants, fertilised lawns, leaky septic systems, and industrial discharges.

How to test for nitrogen?

Water samples are collected by local authorities and sent to laboratories. Each form of nitrogen requires a different chemical test.  The majority of local authorities use methods that follow the American Public Health Association (APHA) standards. Local authorities, together with the Ministry for the Environment, are currently working towards standardising sampling and testing methodologies for nutrients, including nitrogen.

Which unit is it given in?

Concentrations of nitrogen forms are reported on LAWA in grams per cubic metre (g/m3) or milligrams per litre (mg/L); note that these two units are equivalent and interchangeable.  In some literature, concentrations may be reported as parts per billion (ppb); 1 ppb = 0.001 g/m3. On LAWA, all forms of nitrogen are reported as the concentration of the nitrogen alone rather than the concentration of the entire molecule.

Where do I find more information?

ANZECC & ARMCANZ (2000). Australian and New Zealand guidelines for fresh and marine water quality. Australian and New Zealand Environment and Conservation Council and Agriculture and Resource Management Council of Australia and New Zealand.

Biggs B 2000. New Zealand Periphyton Guidelines: detecting, monitoring and managing enrichment of streams.  Prepared for Ministry for the Environment.

Davies-Colley, R.  2000. “Trigger” values for New Zealand rivers. Prepared for the Ministry for the Environment. NIWA Client Report: MfE002/22 May 2000.

Matheson F, Quinn J, Hickey C 2012. Review of the New Zealand instream plant and nutrient guidelines and development of an extended decision making framework: Phases 1 & 2 final report.  Prepared for the Ministry of Science and Innovation Envirolink Fund. 

Milne J. R, Perrie A., Robinson P.  Davies-Colley R. J. (2014). National consistency in nutrient test methods: assessing the implications of changing methods on long-term water quality datasets – Part 1.  Water Symposium, NZ Freshwater Sciences and NZ Hydrological Society joint annual conference, 24-28 November 2014, Blenheim.

Ministry of Health (2018). Drinking-water Standards for New Zealand 2005 (revised 2018). New Zealand Ministry of Health, Wellington.

Robinson P., Milne J.R., Perrie A., Davies-Colley R. J. (2014). National consistency in nutrient test methods: assessing the implications of changing methods on long-term water quality datasets – Part 2.  Water Symposium, NZ Freshwater Sciences and NZ Hydrological Society joint annual conference, 24-28 November 2014, Blenheim