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Background on Nitrogen

The Formation of Reactive Nitrogen:

Nitrogen makes up 78% of the Earth's atmosphere, but this form of nitrogen (N2) is inert. All other species of nitrogen are called reactive forms of nitrogen. Reactive nitrogen in the environment is the type of nitrogen that causes impacts to environmental and human health; N2 is generally considered to be inert and therefore does not react with the environment in the same ways. Examples of reactive nitrogen include the greenhouse gas nitrous oxide (N2O), nitrogen oxides (NOx), ammonia (NH3), nitrate (NO3-), and nitrite (NO2-) (Galloway et al. 2008).

Reactive nitrogen is created from inert nitrogen through both natural processes (green arrows in the figure below) and human activites (blue arrows the figure below). Human activities that create reactive nitrogen are the creation of synthetic fertilizer through the Haber-Bosch process and the burning of fossil fuels. The primary natural process that creates reactive nitrogen is nitrogen fixation by microbes. The intense heat of lightning also can create reactive nitrogen by splitting the triple bond of N2.

(Figure credit for both the above and the below images to Andrew Greene)

The human creation of reactive nitrogen (all N species except N2) by food and energy production has profound beneficial and detrimental impacts on people and the environment (Leach et al. 2012). Agricultural uses, including both food production and consumption, contribute the most reactive nitrogen to the environment. The main beneficial impact of the agricultural use of reactive nitrogen comes from the food produced by nitrogen fertilizer and human-enhanced biological nitrogen fixation. These two processes provide the N to sustain about half of the world's population (Erisman et al. 2008). The detrimental impacts result because a large fraction of the N used in food and biofuel, biofuel profuction, and all of the N used in non-biofuel (i.e. non-agricultural) energy production are lost to the environment. Of the N used to produce food, about 80% is lost to the environment before consumption, and the remainder is lost after consumption as human waste. As a result of these processes, humans have substsantially altered the global nitrogen cycle. Rockstrom et al.(2009) identified the nitrogen cycle as one of the three planetary systems for which humans have exceeded the safe operating space. Human inputs of reactive nitrogen are 7x greater than inputs from natural sources (Vitousek et al. 2013, Fowler et al. 2013).


Once lost to the environment, this nitrogen moves through the Earth's atmosphere, forests, grasslands and waters, causing a cascade of environmental changes that negatively impact both people and ecosystems. These changes include smog, acid rain, forest dieback, coastal 'dead zones', biodiversity loss, stratospheric ozone depletion, and an enhanced greenhouse effect (Galloway et al. 2003).








How does excess reactive nitrogen impact the environment?

Smog and Haze:

Near the surface of the Earth, NOx (nitrogen oxides) reacts with intense sunlight to create smog and tropospheric ozone. Ozone is beneficial in the stratosphere, but at the surface of the Earth, ozone is dangerous and hazadous to human health. Tropospheric ozone can lead to increases in heart and lung disease; in Europe, increases in NOx in the atmosphere and other air pollutants have lead to decreases in life expectancy for at least 50% of the population (Sutton et al. 2011). In addition to being hazardous to human health, tropospheric ozone reduces plant productivity, negatively affecting crops and forests (Galloway et al. 2003). 

Photo: photo credit and copyright to Craig Nagy under a Creative Commons license.


Forest Die-Back: