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Diffuse Pollution – The Nitrogen Cycle

Pollution Sources

There are two types of pollution sources:

Point source – this included industrial discharges; sewage treatment continuous and storm discharges; and accidental spillage from farm slurry stores; and

Diffuse sources – these as the name suggest cannot be attributed to a point or incident. Unlike point source pollution it cannot be seen and may affect both water and air.

Diffuse pollution can occur from range of activities including agriculture, forestry, mining, construction and urban actions. It is due to the day to day activities over a larger area. Diffuse pollutants from agriculture includes, silt from soil erosion, nutrient loss from fertilisers and manure and pesticides.

Nutrients may be in the form of nitrates or phosphates. Over 70% of Nitrates and 40% of Phosphates in English waters come from agriculture practices.

As illustrated earlier nitrate levels in water, especially groundwater, is on the increase. No one farmer is responsible for this as it is a cumulative affect. It is for this reason there are a number of initiative to address diffuse pollution. WAgriCo is one such initiative.

But how does the release of nitrates occur from the application of fertilisers and manures – this is explained by the ‘Nitrogen Cycle’.

The Nitrogen Cycle

The Nitrogen Cycle in soils is a very dynamic process but has great practical implications on modern agriculture and protection of nitrate pollution of watercourses and is illustrated in the diagram below.

Most plants can absorb nitrogen in both the nitrate and ammonium forms. However, ammonium-N is rapidly nitrified to nitrate-N which is the main form absorbed by agricultural crops.

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Soil organic matter is the main ‘pool’ of nitrogen in the soil but in organic form is not available for plant uptake. Organic matter may be of recent origin (organic manures, crop debris) or much older. However, in order for the organic matter to decompose it is necessary to have a population of living bacteria and other organisms in the soil, these are called the Microbial biomass. Leguminous plants have symbiotic micro-organisms (e.g. rhizobia) associated with their root systems. These micro organisms form part of the microbial biomass and ‘fix’ nitrogen gas from the atmosphere. This is termed Nitrogen fixation and is the only way that organisms can attain nitrogen directly from the atmosphere.

Key processes in the Nitrogen Cycle are:

MineralisationThis is the process of organic matter decomposition by the microbial biomass into ammonium-N.
NitrificationThis is the process of bacterial conversion of ammonium to nitrate-N. Ammonium-N that is not nitrified will be absorbed by the soil as exchangeable ammonium.

Immobilisation (‘locking up’)

To ‘feed, the living microbial biomass, nitrate is absorbed and ‘immobilised’ by bacteria. As these bacteria die so this nitrogen is mineralised - hence the nitrogen ‘cycle’.
LeachingThis is the process of downward movement of nitrate-N through the soil profile.
Ammonia volatilisationThis is the direct loss of ammonia (NH3) gas. Organic manures are the main source of ammonia volatilisation.
Denitrification

This is the process of chemical reduction of nitrate (NO3) to nitrous oxides (NOx) and nitrogen (N2). The process requires warmish soils and anaerobic (without oxygen) conditions - waterlogged soils.

In the cycle a critical process to diffuse pollution is nitrate leaching. The amount of nitrate leached from soils is influenced by many factors. The most important factors are:

  • The amount of nitrogen in the soil.  Where there is a lot of nitrate present, the leachate water will have a high concentration of nitrate which will increase the total amount of nitrate leached for a given volume of drainage water.  Nitrogen management practices are designed to minimise the concentration of nitrates in soil at any point in time, but especially before times of the year when there is a high risk of leaching.  The key principle is to match nitrogen inputs (fertiliser, organic manures) to crop growth patterns.
  • Water.  Water must drain through the soil before leaching can occur.  Hydrologically Effective Rainfall (HER) - also called excess rainfall - is the amount of water that drains through the soil.  The risk of nitrate leaching is higher in wetter areas than in dry areas.
  • The soil type.  Nitrates are more rapidly leached below rooting depth in sandy soils of low available water capacity (AWC) than other silty and clayey soils of higher AWC.  Nitrates are more easily leached on shallow soils over rock where rooting depth is limited.
  • Cropping.  Where a crop is growing on the soil (particularly over-winter), nitrates will be taken up by the crop thus reducing leaching.  Evapotranspiration, the process of transferring water from soil to atmosphere, will also reduce HER.

Further sources of information

Further useful information can be found on the following websites:

http://www.defra.gov.uk/environment/water/quality/nitrate/intro.htm

http://www.visionlearning.com/library/module_viewer.php?mid=98&l=&c3

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

  
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