Human activities
have had several effects on the current nitrogen cycle.
One such intervention has been the
addition of large amounts of nitric
oxide (NO) to the atmosphere resulting from the burning of fossil fuels.
This nitric oxide combines with oxygen to form nitrogen dioxide (NO2),
which in turn reacts with water vapor to form nitric acid (HNO3). Droplets of nitric acid dissolved
in rain or snow are components of acid deposition, which along with other air
pollutants can cause damage to both
terrestrial and aquatic ecosystems, corrode metals, and damage structures.
A second intervention is the release of
nitrous oxide (N2O), a greenhouse
gas, and results primarily from agricultural activities including inorganic
nitrogen fertilizer application and livestock wastes.
Third, agricultural runoff and the discharge of municipal
sewage add nitrogen compounds to aquatic ecosystems. This excess nitrogen stimulates
rapid growth of photosynthesizing algae (eutrophication). As these algae die,
their decomposition robs the water of dissolved oxygen, which in turn causes
other aquatic organisms, including many fishes, to die of suffocation.
Fourth, nitrates from fertilizer can
also leach through the soil and contaminate groundwater. Nitrate-contaminated
groundwater is dangerous, particularly for infants and children.
Glossary
:
Fossil fuels: All of these fuels were formed from the remains of
plants and animals that lived millions of years.
Fossil: A remnant or trace of an
organism of a past geologic age, such as a skeleton or leaf imprint, embedded
and preserved in the earth's crust.
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