Plants are surrounded by the nitrogen (N) in our atmosphere.
Every acre of the earth’s surface is covered by thousands of
pounds of this essential nutrient, but because atmospheric gaseous
nitrogen is present as almost inert nitrogen (N2) molecules, this
nitrogen is not directly available to the plants that need it to
grow, develop and reproduce. Healthy plants often contain 3-4% nitrogen in their above-ground
tissues. These are much higher concentrations than those of any
other nutrient except carbon, hydrogen and oxygen, nutrients not
of soil fertility management concern in most situations. Nitrogen
is an important component of many important structural, genetic
and metabolic compounds in plant cells. It is a major component of
chlorophyll, the compound by which plants use sunlight energy to
produce sugars from water and carbon dioxide (i.e.
photosynthesis). It is also a major component of amino acids, the
building blocks of proteins. Some proteins act as structural units
in plant cells while others act as enzymes, making possible many
of the biochemical reactions on which life is based. Nitrogen is a
component of energy-transfer compounds, such as ATP (adenosine tri
phosphate) which allow cells to conserve and use the energy
released in metabolism. Finally, nitrogen is a significant
component of nucleic acids such as DNA, the genetic material that
allows cells (and eventually whole plants) to grow and
reproduce.
Soil Nitrogen
Soil nitrogen exists in three general forms - organic nitrogen
compounds, ammonium (NH4+) ions, and nitrate (NO3-) ions. At any
given time, 95-99% of the potentially available nitrogen in the
soil is in organic forms, either in plant and animal residues, in
the relatively stable soil organic matter or in living soil
organisms, mainly microbes such as bacteria. This nitrogen is not
directly available to plants, but some can be converted to
available forms by microorganisms. A very small amount of organic
nitrogen may exist in soluble organic compounds, such as urea,
that may be slightly available to plants. The majority of
plant-available nitrogen is in the inorganic (sometimes called
mineral nitrogen) NH4+and NO3-forms. Ammonium ions bind to the
soil’s negatively-charged cation exchange complex and behave much
like other cations in the soil. Nitrate ions do not bind to the
soil solids because they carry negative charges, but exist
dissolved in the soil water, or precipitated as soluble salts
under dry conditions. Some NH4+and NO3- may also exist in the
crystal structure of certain soil minerals, and may be quite
available; however, such nitrogen is important in only a few
soils.