Nitrogen
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It has been suggested that Nitrogen compounds be merged into this article. (Discuss) Proposed since September 2025. |
Liquid nitrogen (N2 at below −196 °C) | |||||||||||||||||||||||||||||||||
| Nitrogen | |||||||||||||||||||||||||||||||||
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| Allotropes | see § Allotropes | ||||||||||||||||||||||||||||||||
| Appearance | colorless gas, liquid or solid | ||||||||||||||||||||||||||||||||
| Standard atomic weight Ar°(N) | |||||||||||||||||||||||||||||||||
| Nitrogen in the periodic table | |||||||||||||||||||||||||||||||||
| Atomic number (Z) | 7 | ||||||||||||||||||||||||||||||||
| Group | group 15 (pnictogens) | ||||||||||||||||||||||||||||||||
| Period | period 2 | ||||||||||||||||||||||||||||||||
| Block | p-block | ||||||||||||||||||||||||||||||||
| Electron configuration | [He] 2s2 2p3 | ||||||||||||||||||||||||||||||||
| Electrons per shell | 2, 5 | ||||||||||||||||||||||||||||||||
| Physical properties | |||||||||||||||||||||||||||||||||
| Phase at STP | gas | ||||||||||||||||||||||||||||||||
| Melting point | (N2) 63.23[3] K (−209.92 °C, −345.86 °F) | ||||||||||||||||||||||||||||||||
| Boiling point | (N2) 77.355 K (−195.795 °C, −320.431 °F) | ||||||||||||||||||||||||||||||||
| Density (at STP) | 1.2506 g/L[4] at 0 °C, 1013 mbar | ||||||||||||||||||||||||||||||||
| when liquid (at b.p.) | 0.808 g/cm3 | ||||||||||||||||||||||||||||||||
| Triple point | 63.151 K, 12.52 kPa | ||||||||||||||||||||||||||||||||
| Critical point | 126.21 K, 3.39 MPa | ||||||||||||||||||||||||||||||||
| Heat of fusion | (N2) 0.72 kJ/mol | ||||||||||||||||||||||||||||||||
| Heat of vaporisation | (N2) 5.57 kJ/mol | ||||||||||||||||||||||||||||||||
| Molar heat capacity | (N2) 29.124 J/(mol·K) | ||||||||||||||||||||||||||||||||
Vapour pressure
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| Atomic properties | |||||||||||||||||||||||||||||||||
| Oxidation states | common: −3, +3, +5 −2,[5] −1,[5] 0,[6] +1,[5] +2,[5] +4[5] | ||||||||||||||||||||||||||||||||
| Electronegativity | Pauling scale: 3.04 | ||||||||||||||||||||||||||||||||
| Ionisation energies |
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| Covalent radius | 71±1 pm | ||||||||||||||||||||||||||||||||
| Van der Waals radius | 155 pm | ||||||||||||||||||||||||||||||||
| Other properties | |||||||||||||||||||||||||||||||||
| Natural occurrence | primordial | ||||||||||||||||||||||||||||||||
| Crystal structure | hexagonal (hP4) | ||||||||||||||||||||||||||||||||
| Lattice constants | a = 411.6 pm c = 673.4 pm (at t.p.)[7] | ||||||||||||||||||||||||||||||||
| Thermal conductivity | 25.83×10−3 W/(m⋅K) | ||||||||||||||||||||||||||||||||
| Magnetic ordering | diamagnetic | ||||||||||||||||||||||||||||||||
| Speed of sound | 353 m/s (gas, at 27 °C) | ||||||||||||||||||||||||||||||||
| CAS Number | 17778-88-0 7727-37-9 (N2) | ||||||||||||||||||||||||||||||||
| History | |||||||||||||||||||||||||||||||||
| Naming | from French nitre (“saltpetre”) + -gène ("forming") | ||||||||||||||||||||||||||||||||
| Discovery | Daniel Rutherford (1772) | ||||||||||||||||||||||||||||||||
| Named by | Jean-Antoine Chaptal (1790) | ||||||||||||||||||||||||||||||||
| Isotopes of nitrogen | |||||||||||||||||||||||||||||||||
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Nitrogen is a chemical element; it has symbol N and atomic number 7. Nitrogen is a nonmetal and the lightest member of group 15 of the periodic table, often called the pnictogens. It is a common element in the universe, estimated at seventh in total abundance in the Milky Way and the Solar System. At standard temperature and pressure, two atoms of the element bond to form N2, a colourless and odourless diatomic gas. N2 forms about 78% of Earth's atmosphere, making it the most abundant chemical species in air. Because of the volatility of nitrogen compounds, nitrogen is relatively rare in the solid parts of the Earth.
It was first discovered and isolated by Scottish physician Daniel Rutherford in 1772 and independently by Carl Wilhelm Scheele and Henry Cavendish at about the same time. The name nitrogène was suggested by French chemist Jean-Antoine-Claude Chaptal in 1790 when it was found that nitrogen was present in nitric acid and nitrates. Antoine Lavoisier suggested instead the name azote, from the Ancient Greek: ἀζωτικός "no life", as it is an asphyxiant gas; this name is used in a number of languages, and appears in the English names of some nitrogen compounds such as hydrazine, azides and azo compounds.
Elemental nitrogen is usually produced from air by pressure swing adsorption technology. About 2/3 of commercially produced elemental nitrogen is used as an inert (oxygen-free) gas for commercial uses such as food packaging, and much of the rest is used as liquid nitrogen in cryogenic applications. Many industrially important compounds, such as ammonia, nitric acid, organic nitrates (propellants and explosives), and cyanides, contain nitrogen. The extremely strong triple bond in elemental nitrogen (N≡N), the second strongest bond in any diatomic molecule after carbon monoxide (CO),[9] dominates nitrogen chemistry. This causes difficulty for both organisms and industry in converting N2 into useful compounds, but at the same time it means that burning, exploding, or decomposing nitrogen compounds to form nitrogen gas releases large amounts of often useful energy. Synthetically produced ammonia and nitrates are key industrial fertilisers, and fertiliser nitrates are key pollutants in the eutrophication of water systems. Apart from its use in fertilisers and energy stores, nitrogen is a constituent of organic compounds as diverse as aramids used in high-strength fabric and cyanoacrylate used in superglue.
Nitrogen occurs in all organisms, primarily in amino acids (and thus proteins), in the nucleic acids (DNA and RNA) and in the energy transfer molecule adenosine triphosphate. The human body contains about 3% nitrogen by mass, the fourth most abundant element in the body after oxygen, carbon, and hydrogen. The nitrogen cycle describes the movement of the element from the air, into the biosphere and organic compounds, then back into the atmosphere. Nitrogen is a constituent of every major pharmacological drug class, including antibiotics. Many drugs are mimics or prodrugs of natural nitrogen-containing signal molecules: for example, the organic nitrates nitroglycerin and nitroprusside control blood pressure by metabolising into nitric oxide. Many notable nitrogen-containing drugs, such as the natural caffeine and morphine or the synthetic amphetamines, act on receptors of animal neurotransmitters.
History
[edit]
Nitrogen compounds have a very long history, ammonium chloride having been known to Herodotus. They were well known by the Middle Ages. Alchemists knew nitric acid as aqua fortis (strong water), as well as other nitrogen compounds such as ammonium salts and nitrate salts. The mixture of nitric and hydrochloric acids was known as aqua regia (royal water), celebrated for its ability to dissolve gold, the king of metals.[10]
The discovery of nitrogen is attributed to the Scottish physician Daniel Rutherford in 1772, who called it noxious air.[11][12] Though he did not recognise it as an entirely different chemical substance, he clearly distinguished it from Joseph Black's "fixed air", or carbon dioxide.[13] The fact that there was a component of air that does not support combustion was clear to Rutherford, although he was not aware that it was an element. Nitrogen was also studied at about the same time by Carl Wilhelm Scheele,[14] Henry Cavendish,[15] and Joseph Priestley,[16] who referred to it as burnt air or phlogisticated air. French chemist Antoine Lavoisier referred to nitrogen gas as "mephitic air" or azote, from the Greek word άζωτικός (azotikos), "no life", because it is asphyxiant.[17][18] In an atmosphere of pure nitrogen, animals died and flames were extinguished. Though Lavoisier's name was not accepted in English since it was pointed out that all gases but oxygen are either asphyxiant or outright toxic, it is used in many languages (French, Italian, Portuguese, Polish, Russian, Albanian, Turkish, etc.; the German Stickstoff similarly refers to the same characteristic, viz. ersticken "to choke or suffocate") and still remains in English in the common names of many nitrogen compounds, such as hydrazine and compounds of the azide ion. Finally, it led to the name "pnictogens" for the group headed by nitrogen, from the Greek πνίγειν "to choke".[10]
The English word nitrogen (1794) entered the language from the French nitrogène, coined in 1790 by French chemist Jean-Antoine Chaptal (1756–1832),[19] from the French nitre (potassium nitrate, also called saltpetre) and the French suffix -gène, "producing", from the Greek -γενής (-genes, "begotten"). Chaptal's meaning was that nitrogen is the essential part of nitric acid, which in turn was produced from nitre. In earlier times, nitre had been confused with Egyptian "natron" (sodium carbonate) – called νίτρον (nitron) in Greek – which, despite the name, contained no nitrate.[20]
The earliest military, industrial, and agricultural applications of nitrogen compounds used saltpetre (sodium nitrate or potassium nitrate), most notably in gunpowder, and later as fertiliser. In 1910, Lord Rayleigh discovered that an electrical discharge in nitrogen gas produced "active nitrogen", a monatomic allotrope of nitrogen.[21] The "whirling cloud of brilliant yellow light" produced by his apparatus reacted with mercury to produce explosive mercury nitride.[22]
For a long time, sources of nitrogen compounds were limited. Natural sources originated either from biology or deposits of nitrates produced by atmospheric reactions. Nitrogen fixation by industrial processes like the Frank–Caro process (1895–1899) and Haber–Bosch process (1908–1913) eased this shortage of nitrogen compounds, to the extent that half of global food production now relies on synthetic nitrogen fertilisers.[23] At the same time, use of the Ostwald process (1902) to produce nitrates from industrial nitrogen fixation allowed the large-scale industrial production of nitrates as feedstock in the manufacture of explosives in the World Wars of the 20th century.[24][25]
Properties
[edit]Atomic
[edit]
A nitrogen atom has seven electrons. In the ground state, they are arranged in the electron configuration 1s2
2s2
2p1
x2p1
y2p1
z. It, therefore, has five valence electrons in the 2s and 2p orbitals, three of which (the p-electrons) are unpaired. It has one of the highest electronegativities among the elements (3.04 on the Pauling scale), exceeded only by chlorine (3.16), oxygen (3.44), and fluorine (3.98). (The light noble gases, helium, neon, and argon, would presumably also be more electronegative, and in fact are on the Allen scale.)[26] Following periodic trends, its single-bond covalent radius of 71 pm is smaller than those of boron (84 pm) and carbon (76 pm), while it is larger than those of oxygen (66 pm) and fluorine (57 pm). The nitride anion, N3−, is much larger at 146 pm, similar to that of the oxide (O2−: 140 pm) and fluoride (F−: 133 pm) anions.[26] The first three ionisation energies of nitrogen are 1.402, 2.856, and 4.577 MJ·mol−1, and the sum of the fourth and fifth is 16.920 MJ·mol−1. Due to these very high figures, nitrogen has no simple cationic chemistry.[27]
The lack of radial nodes in the 2p subshell is directly responsible for many of the anomalous properties of the first row of the p-block, especially in nitrogen, oxygen, and fluorine. The 2p subshell is very small and has a very similar radius to the 2s shell, facilitating orbital hybridisation. It also results in very large electrostatic forces of attraction between the nucleus and the valence electrons in the 2s and 2p shells, resulting in very high electronegativities. Hypervalency is almost unknown in the 2p elements for the same reason, because the high electronegativity makes it difficult for a small nitrogen atom to be a central atom in an electron-rich three-center four-electron bond since it would tend to attract the electrons strongly to itself. Thus, despite nitrogen's position at the head of group 15 in the periodic table, its chemistry shows huge differences from that of its heavier congeners phosphorus, arsenic, antimony, and bismuth.[28]
Nitrogen may be usefully compared to its horizontal neighbours' carbon and oxygen as well as its vertical neighbours in the pnictogen column, phosphorus, arsenic, antimony, and bismuth. Although each period 2 element from lithium to oxygen shows some similarities to the period 3 element in the next group (from magnesium to chlorine; these are known as diagonal relationships), their degree drops off abruptly past the boron–silicon pair. The similarities of nitrogen to sulfur are mostly limited to sulfur nitride ring compounds when both elements are the only ones present.[29]
Nitrogen does not share the proclivity of carbon for catenation. Like carbon, nitrogen tends to form ionic or metallic compounds with metals. Nitrogen forms an extensive series of nitrides with carbon, including those with chain-, graphitic-, and fullerenic-like structures.[30]
It resembles oxygen with its high electronegativity and concomitant capability for hydrogen bonding and the ability to form coordination complexes by donating its lone pairs of electrons. There are some parallels between the chemistry of ammonia NH3 and water H2O. For example, the capacity of both compounds to be protonated to give NH4+ and H3O+ or deprotonated to give NH2− and OH−, with all of these able to be isolated in solid compounds.[31]
Nitrogen shares with both its horizontal neighbours a preference for forming multiple bonds, typically with carbon, oxygen, or other nitrogen atoms, through pπ–pπ interactions.[29] Thus, for example, nitrogen occurs as diatomic molecules and therefore has very much lower melting (−210 °C) and boiling points (−196 °C) than the rest of its group, as the N2 molecules are only held together by weak van der Waals interactions and there are very few electrons available to create significant instantaneous dipoles. This is not possible for its vertical neighbours; thus, the nitrogen oxides, nitrites, nitrates, nitro-, nitroso-, azo-, and diazo-compounds, azides, cyanates, thiocyanates, and imino-derivatives find no echo with phosphorus, arsenic, antimony, or bismuth. By the same token, however, the complexity of the phosphorus oxoacids finds no echo with nitrogen.[29] Setting aside their differences, nitrogen and phosphorus form an extensive series of compounds with one another; these have chain, ring, and cage structures.[32]
Table of thermal and physical properties of nitrogen (N2) at atmospheric pressure:[33][34]
| Temperature (K) | Density (kg m−3) | Specific heat (kJ kg−1 °C−1) | Dynamic viscosity (kg m−1 s−1) | Kinematic viscosity (m2 s−1) | Thermal conductivity (W m−1 °C−1) | Thermal diffusivity (m2 s−1) | Prandtl number |
| 100 | 3.4388 | 1.07 | 6.88×10−6 | 2.00×10−6 | 0.00958 | 2.60×10−6 | 0.768 |
| 150 | 2.2594 | 1.05 | 1.01×10−5 | 4.45×10−6 | 0.0139 | 5.86×10−6 | 0.759 |
| 200 | 1.7108 | 1.0429 | 1.29×10−5 | 7.57×10−6 | 0.01824 | 1.02×10−5 | 0.747 |
| 300 | 1.1421 | 1.0408 | 1.78×10−5 | 1.56×10−5 | 0.0262 | 2.20×10−5 | 0.713 |
| 400 | 0.8538 | 1.0459 | 2.20×10−5 | 2.57×10−5 | 0.03335 | 3.73×10−5 | 0.691 |
| 500 | 0.6824 | 1.0555 | 2.57×10−5 | 3.77×10−5 | 0.03984 | 5.53×10−5 | 0.684 |
| 600 | 0.5687 | 1.0756 | 2.91×10−5 | 5.12×10−5 | 0.0458 | 7.49×10−5 | 0.686 |
| 700 | 0.4934 | 1.0969 | 3.21×10−5 | 6.67×10−5 | 0.05123 | 9.47×10−5 | 0.691 |
| 800 | 0.4277 | 1.1225 | 3.48×10−5 | 8.15×10−5 | 0.05609 | 1.17×10−4 | 0.7 |
| 900 | 0.3796 | 1.1464 | 3.75×10−5 | 9.11×10−5 | 0.0607 | 1.39×10−4 | 0.711 |
| 1000 | 0.3412 | 1.1677 | 4.00×10−5 | 1.19×10−4 | 0.06475 | 1.63×10−4 | 0.724 |
| 1100 | 0.3108 | 1.1857 | 4.23×10−5 | 1.36×10−4 | 0.0685 | 1.86×10−4 | 0.736 |
| 1200 | 0.2851 | 1.2037 | 4.45×10−5 | 1.56×10−4 | 0.07184 | 2.09×10−4 | 0.748 |
| 1300 | 0.2591 | 1.219 | 4.66×10−5 | 1.80×10−4 | 0.081 | 2.56×10−4 | 0.701 |
Isotopes
[edit]
Nitrogen has two stable isotopes: 14N and 15N. The first is much more common, making up 99.634% of natural nitrogen, and the second (which is slightly heavier) makes up the remaining 0.366%. This leads to an atomic weight of around 14.007 u.[26] Both of these stable isotopes are produced in the CNO cycle in stars, but 14N is more common as its proton capture is the rate-limiting step. 14N is one of the five stable odd–odd nuclides (a nuclide having an odd number of protons and neutrons); the other four are 2H, 6Li, 10B, and 180mTa.[35]
The relative abundance of 14N and 15N is practically constant in the atmosphere but can vary elsewhere, due to natural isotopic fractionation from biological redox reactions and the evaporation of natural ammonia or nitric acid.[1] Biologically mediated reactions (e.g., assimilation, nitrification, and denitrification) strongly control nitrogen dynamics in the soil. These reactions typically result in 15N enrichment of the substrate and depletion of the product.[36]
The heavy isotope 15N was first discovered by S. M. Naudé in 1929, and soon after heavy isotopes of the neighbouring elements oxygen and carbon were discovered.[37] It presents one of the lowest thermal neutron capture cross-sections of all isotopes.[38] It is frequently used in nuclear magnetic resonance (NMR) spectroscopy to determine the structures of nitrogen-containing molecules, due to its fractional nuclear spin of one-half, which offers advantages for NMR such as narrower line width. 14N, though also theoretically usable, has an integer nuclear spin of one and thus has a quadrupole moment that leads to wider and less useful spectra.[26] 15N NMR nevertheless has complications not encountered in the more common 1H and 13C NMR spectroscopy. The low natural abundance of 15N (0.36%) significantly reduces sensitivity, a problem which is only exacerbated by its low gyromagnetic ratio, (only 10.14% that of 1H). As a result, the signal-to-noise ratio for 1H is about 300 times as much as that for 15N at the same magnetic field strength.[39] This may be somewhat alleviated by isotopic enrichment of 15N by chemical exchange or fractional distillation. 15N-enriched compounds have the advantage that under standard conditions, they do not undergo chemical exchange of their nitrogen atoms with atmospheric nitrogen, unlike compounds with labelled hydrogen, carbon, and oxygen isotopes that must be kept away from the atmosphere.[26] The 15N:14N ratio is commonly used in stable isotope analysis in the fields of geochemistry, hydrology, paleoclimatology and paleoceanography, where it is called δ15N.[40]
Of the thirteen other isotopes produced synthetically, ranging from 9N to 23N, 13N has a half-life of ten minutes and the remaining isotopes have half-lives less than eight seconds.[41][42] Given the half-life difference, 13N is the most important nitrogen radioisotope, being relatively long-lived enough to use in positron emission tomography (PET), although its half-life is still short and thus it must be produced at the venue of the PET, for example in a cyclotron via proton bombardment of 16O producing 13N and an alpha particle.[43]
The radioisotope 16N is the dominant radionuclide in the coolant of pressurised water reactors or boiling water reactors during normal operation. It is produced from 16O (in water) via an (n,p) reaction, in which the 16O atom captures a neutron and expels a proton. It has a short half-life of about 7.1 s,[42] but its decay back to 16O produces high-energy gamma radiation (5 to 7 MeV).[42][44] Because of this, access to the primary coolant piping in a pressurised water reactor must be restricted during reactor power operation.[44] It is a sensitive and immediate indicator of leaks from the primary coolant system to the secondary steam cycle and is the primary means of detection for such leaks.[44]
Allotropes
[edit]
Atomic nitrogen, also known as active nitrogen, is highly reactive, being a triradical with three unpaired electrons. Free nitrogen atoms easily react with most elements to form nitrides, and even when two free nitrogen atoms collide to produce an excited N2 molecule, they may release so much energy on collision with even such stable molecules as carbon dioxide and water to cause homolytic fission into radicals such as CO and O or OH and H. Atomic nitrogen is prepared by passing an electric discharge through nitrogen gas at 0.1–2 mmHg, which produces atomic nitrogen along with a peach-yellow emission that fades slowly as an afterglow for several minutes even after the discharge terminates.[29]
Given the great reactivity of atomic nitrogen, elemental nitrogen usually occurs as molecular N2, dinitrogen. This molecule is a colourless, odourless, and tasteless diamagnetic gas at standard conditions: it melts at −210 °C and boils at −196 °C.[29] Dinitrogen is mostly unreactive at room temperature, but it will nevertheless react with lithium metal and some transition metal complexes. This is due to its bonding, which is unique among the diatomic elements at standard conditions in that it has an N≡N triple bond. Triple bonds have short bond lengths (in this case, 109.76 pm) and high dissociation energies (in this case, 945.41 kJ/mol), and are thus very strong, explaining dinitrogen's low level of chemical reactivity.[29][45]
Other nitrogen oligomers and polymers may be possible. If they could be synthesised, they may have potential applications as materials with a very high energy density, that could be used as powerful propellants or explosives.[46] Under extremely high pressures (1.1 million atm) and high temperatures (2000 K), as produced in a diamond anvil cell, nitrogen polymerises into the single-bonded cubic gauche crystal structure. This structure is similar to that of diamond, and both have extremely strong covalent bonds, resulting in its nickname "nitrogen diamond".[47]

At atmospheric pressure, molecular nitrogen condenses (liquefies) at 77 K (−195.79 °C) and freezes at 63 K (−210.01 °C)[48] into the beta hexagonal close-packed crystal allotropic form. Below 35.4 K (−237.6 °C) nitrogen assumes the cubic crystal allotropic form (called the alpha phase).[49] Liquid nitrogen, a colourless fluid resembling water in appearance, but with 80.8% of the density (the density of liquid nitrogen at its boiling point is 0.808 g/mL), is a common cryogen.[50] Solid nitrogen has many crystalline modifications. It forms a significant dynamic surface coverage on Pluto[51] and outer moons of the Solar System such as Triton.[52] Even at the low temperatures of solid nitrogen it is fairly volatile and can sublime to form an atmosphere, or condense back into nitrogen frost. It is very weak and flows in the form of glaciers, and on Triton geysers of nitrogen gas come from the polar ice cap region.[53]
Beyond dinitrogen (N2), chemists have long sought to synthesize and stabilize other neutral nitrogen allotropes, which are typically much less stable and often exist only fleetingly or under extreme conditions. Cyclic hexazine (N6), a hypothetical ring-like molecule analogous to benzene, has not been synthesized as a neutral species, though negatively charged variants have been produced under extreme conditions; its instability is attributed to the repulsion of lone pairs on nitrogen atoms. Hexanitrogen (N6), a neutral, linear chain of six nitrogen atoms with alternating double and single bonds, which is stable only at cryogenic temperatures and represents the first stable neutral nitrogen allotrope beyond dinitrogen.[54][55][56][57] Octaazacubane (N8), a hypothetical cubane-like cluster of eight nitrogen atoms, is predicted to be highly energetic and potentially useful as an explosive or rocket fuel, though it remains unsynthesized to date.[55] Tetranitrogen (N4) and trinitrogen (N3, the azide radical) are also known, but these are either extremely unstable or exist only as short-lived intermediates.[55] Among the several different phases of solid nitrogen, an N8 molecular allotrope has been detected[58] as well as several different three-dimensional lattices and amorphous forms.[54]
Chemistry and compounds
[edit]Dinitrogen complexes
[edit]
The first example of a dinitrogen complex to be discovered was [Ru(NH3)5(N2)]2+ (see figure at right), and soon many other such complexes were discovered. These complexes, in which a nitrogen molecule donates at least one lone pair of electrons to a central metal cation, illustrate how N2 might bind to the metal(s) in nitrogenase and the catalyst for the Haber process: these processes involving dinitrogen activation are vitally important in biology and in the production of fertilisers.[59][60]
Dinitrogen is able to coordinate to metals in five different ways. The more well-characterised ways are the end-on M←N≡N (η1) and M←N≡N→M (μ, bis-η1), in which the lone pairs on the nitrogen atoms are donated to the metal cation. The less well-characterised ways involve dinitrogen donating electron pairs from the triple bond, either as a bridging ligand to two metal cations (μ, bis-η2) or to just one (η2). The fifth and unique method involves triple-coordination as a bridging ligand, donating all three electron pairs from the triple bond (μ3-N2). A few complexes feature multiple N2 ligands and some feature N2 bonded in multiple ways. Since N2 is isoelectronic with carbon monoxide (CO) and acetylene (C2H2), the bonding in dinitrogen complexes is closely allied to that in carbonyl compounds, although N2 is a weaker σ-donor and π-acceptor than CO. Theoretical studies show that σ donation is a more important factor allowing the formation of the M–N bond than π back-donation, which mostly only weakens the N–N bond, and end-on (η1) donation is more readily accomplished than side-on (η2) donation.[29]
Today, dinitrogen complexes are known for almost all the transition metals, accounting for several hundred compounds. They are normally prepared by three methods:[29]
- Replacing labile ligands such as H2O, H−, or CO directly by nitrogen: these are often reversible reactions that proceed at mild conditions.
- Reducing metal complexes in the presence of a suitable co-ligand in excess under nitrogen gas. A common choice includes replacing chloride ligands with dimethylphenylphosphine (PMe2Ph) to make up for the smaller number of nitrogen ligands attached to the original chlorine ligands.
- Converting a ligand with N–N bonds, such as hydrazine or azide, directly into a dinitrogen ligand.
Occasionally the N≡N bond may be formed directly within a metal complex, for example by directly reacting coordinated ammonia (NH3) with nitrous acid (HNO2), but this is not generally applicable. Most dinitrogen complexes have colours within the range white-yellow-orange-red-brown; a few exceptions are known, such as the blue [{Ti(η5-C5H5)2}2-(N2)].[29]
Nitrides, azides, and nitrido complexes
[edit]Nitrogen bonds to almost all the elements in the periodic table except the first two noble gases, helium and neon, and some of the very short-lived elements after bismuth, creating an immense variety of binary compounds with varying properties and applications.[29] Many binary compounds are known: with the exception of the nitrogen hydrides, oxides, and fluorides, these are typically called nitrides. Many stoichiometric phases are usually present for most elements (e.g. MnN, Mn6N5, Mn3N2, Mn2N, Mn4N, and MnxN for 9.2 < x < 25.3). They may be classified as "salt-like" (mostly ionic), covalent, "diamond-like", and metallic (or interstitial), although this classification has limitations generally stemming from the continuity of bonding types instead of the discrete and separate types that it implies. They are normally prepared by directly reacting a metal with nitrogen or ammonia (sometimes after heating), or by thermal decomposition of metal amides:[61]
- 3 Ca + N2 → Ca3N2
- 3 Mg + 2 NH3 → Mg3N2 + 3 H2 (at 900 °C)
- 3 Zn(NH2)2 → Zn3N2 + 4 NH3
Many variants on these processes are possible. The most ionic of these nitrides are those of the alkali metals and alkaline earth metals, Li3N (Na, K, Rb, and Cs do not form stable nitrides for steric reasons) and M3N2 (M = Be, Mg, Ca Sr, Ba). These can formally be thought of as salts of the N3− anion, although charge separation is not actually complete even for these highly electropositive elements. However, the alkali metal azides NaN3 and KN3, featuring the linear N−
3 anion, are well-known, as are Sr(N3)2 and Ba(N3)2. Azides of the B-subgroup metals (those in groups 11 through 16) are much less ionic, have more complicated structures, and detonate readily when shocked.[61]

Many covalent binary nitrides are known. Examples include cyanogen ((CN)2), triphosphorus pentanitride (P3N5), disulfur dinitride (S2N2), and tetrasulfur tetranitride (S4N4). The essentially covalent silicon nitride (Si3N4) and germanium nitride (Ge3N4) are also known: silicon nitride, in particular, would make a promising ceramic if not for the difficulty of working with and sintering it. In particular, the group 13 nitrides, most of which are promising semiconductors, are isoelectronic with graphite, diamond, and silicon carbide and have similar structures: their bonding changes from covalent to partially ionic to metallic as the group is descended. In particular, since the B–N unit is isoelectronic to C–C, and carbon is essentially intermediate in size between boron and nitrogen, much of organic chemistry finds an echo in boron–nitrogen chemistry, such as in borazine ("inorganic benzene"). Nevertheless, the analogy is not exact due to the ease of nucleophilic attack at boron due to its deficiency in electrons, which is not possible in a wholly carbon-containing ring.[61]
The largest category of nitrides are the interstitial nitrides of formulae MN, M2N, and M4N (although variable composition is perfectly possible), where the small nitrogen atoms are positioned in the gaps in a metallic cubic or hexagonal close-packed lattice. They are opaque, very hard, and chemically inert, melting only at very high temperatures (generally over 2500 °C). They have a metallic lustre and conduct electricity as do metals. They hydrolyse only very slowly to give ammonia or nitrogen.[61]
The nitride anion (N3−) is the strongest π donor known among ligands (the second-strongest is O2−). Nitrido complexes are generally made by the thermal decomposition of azides or by deprotonating ammonia, and they usually involve a terminal {≡N}3− group. The linear azide anion (N−
3), being isoelectronic with nitrous oxide, carbon dioxide, and cyanate, forms many coordination complexes. Further catenation is rare, although N4−
4 (isoelectronic with carbonate and nitrate) is known.[61]
Hydrides
[edit]
Industrially, ammonia (NH3) is the most important compound of nitrogen and is prepared in larger amounts than any other compound because it contributes significantly to the nutritional needs of terrestrial organisms by serving as a precursor to food and fertilisers. It is a colourless alkaline gas with a characteristic pungent smell. The presence of hydrogen bonding has very significant effects on ammonia, conferring on it its high melting (−78 °C) and boiling (−33 °C) points. As a liquid, it is a very good solvent with a high heat of vaporisation (enabling it to be used in vacuum flasks), that also has a low viscosity and electrical conductivity and high dielectric constant, and is less dense than water. However, the hydrogen bonding in NH3 is weaker than that in H2O due to the lower electronegativity of nitrogen compared to oxygen and the presence of only one lone pair in NH3 rather than two in H2O. It is a weak base in aqueous solution (pKb 4.74); its conjugate acid is ammonium, NH+
4. It can also act as an extremely weak acid, losing a proton to produce the amide anion, NH−
2. It thus undergoes self-dissociation, similar to water, to produce ammonium and amide. Ammonia burns in air or oxygen, though not readily, to produce nitrogen gas; it burns in fluorine with a greenish-yellow flame to give nitrogen trifluoride. Reactions with the other nonmetals are very complex and tend to lead to a mixture of products. Ammonia reacts on heating with metals to give nitrides.[63]
Many other binary nitrogen hydrides are known, but the most important are hydrazine (N2H4) and hydrogen azide (HN3). Although it is not a nitrogen hydride, hydroxylamine (NH2OH) is similar in properties and structure to ammonia and hydrazine as well. Hydrazine is a fuming, colourless liquid that smells similar to ammonia. Its physical properties are very similar to those of water (melting point 2.0 °C, boiling point 113.5 °C, density 1.00 g/cm3). Despite it being an endothermic compound, it is kinetically stable. It burns quickly and completely in air very exothermically to give nitrogen and water vapour. It is a very useful and versatile reducing agent and is a weaker base than ammonia.[64] It is also commonly used as a rocket fuel.[65]
Hydrazine is generally made by reaction of ammonia with alkaline sodium hypochlorite in the presence of gelatin or glue:[64]
- NH3 + OCl− → NH2Cl + OH−
- NH2Cl + NH3 → N
2H+
5 + Cl− (slow) - N
2H+
5 + OH− → N2H4 + H2O (fast)
(The attacks by hydroxide and ammonia may be reversed, thus passing through the intermediate NHCl− instead.) The reason for adding gelatin is that it removes metal ions such as Cu2+ that catalyses the destruction of hydrazine by reaction with monochloramine (NH2Cl) to produce ammonium chloride and nitrogen.[64]
Hydrogen azide (HN3) was first produced in 1890 by the oxidation of aqueous hydrazine by nitrous acid. It is very explosive and even dilute solutions can be dangerous. It has a disagreeable and irritating smell and is a potentially lethal (but not cumulative) poison. It may be considered the conjugate acid of the azide anion, and is similarly analogous to the hydrohalic acids.[64]
Halides and oxohalides
[edit]All four simple nitrogen trihalides are known. A few mixed halides and hydrohalides are known, but are mostly unstable; examples include NClF2, NCl2F, NBrF2, NF2H, NFH2, NCl2H, and NClH2.[66]
Nitrogen trifluoride (NF3, first prepared in 1928) is a colourless and odourless gas that is thermodynamically stable, and most readily produced by the electrolysis of molten ammonium fluoride dissolved in anhydrous hydrogen fluoride. Like carbon tetrafluoride, it is not at all reactive and is stable in water or dilute aqueous acids or alkalis. Only when heated does it act as a fluorinating agent, and it reacts with copper, arsenic, antimony, and bismuth on contact at high temperatures to give tetrafluorohydrazine (N2F4). The cations NF+
4 and N
2F+
3 are also known (the latter from reacting tetrafluorohydrazine with strong fluoride-acceptors such as arsenic pentafluoride), as is ONF3, which has aroused interest due to the short N–O distance implying partial double bonding and the highly polar and long N–F bond. Tetrafluorohydrazine, unlike hydrazine itself, can dissociate at room temperature and above to give the radical NF2•. Fluorine azide (FN3) is very explosive and thermally unstable. Dinitrogen difluoride (N2F2) exists as thermally interconvertible cis and trans isomers, and was first found as a product of the thermal decomposition of FN3.[66]
Nitrogen trichloride (NCl3) is a dense, volatile, and explosive liquid whose physical properties are similar to those of carbon tetrachloride, although one difference is that NCl3 is easily hydrolysed by water while CCl4 is not. It was first synthesised in 1811 by Pierre Louis Dulong, who lost three fingers and an eye to its explosive tendencies. As a dilute gas it is less dangerous and is thus used industrially to bleach and sterilise flour. Nitrogen tribromide (NBr3), first prepared in 1975, is a deep red, temperature-sensitive, volatile solid that is explosive even at −100 °C. Nitrogen triiodide (NI3) is still more unstable and was only prepared in 1990. Its adduct with ammonia, which was known earlier, is very shock-sensitive: it can be set off by the touch of a feather, shifting air currents, or even alpha particles.[66][67] For this reason, small amounts of nitrogen triiodide are sometimes synthesised as a demonstration to high school chemistry students or as an act of "chemical magic".[68] Chlorine azide (ClN3) and bromine azide (BrN3) are extremely sensitive and explosive.[69][70]
Two series of nitrogen oxohalides are known: the nitrosyl halides (XNO) and the nitryl halides (XNO2). The first is very reactive gases that can be made by directly halogenating nitrous oxide. Nitrosyl fluoride (NOF) is colourless and a vigorous fluorinating agent. Nitrosyl chloride (NOCl) behaves in much the same way and has often been used as an ionising solvent. Nitrosyl bromide (NOBr) is red. The reactions of the nitryl halides are mostly similar: nitryl fluoride (FNO2) and nitryl chloride (ClNO2) are likewise reactive gases and vigorous halogenating agents.[66]
Oxides
[edit]
2 converts to colourless dinitrogen tetroxide (N
2O
4) at low temperatures, and reverts to NO
2 at higher temperatures.
Nitrogen forms nine molecular oxides, some of which were the first gases to be identified: N2O (nitrous oxide), NO (nitric oxide), N2O3 (dinitrogen trioxide), NO2 (nitrogen dioxide), N2O4 (dinitrogen tetroxide), N2O5 (dinitrogen pentoxide), N4O (nitrosylazide),[71] and N(NO2)3 (trinitramide).[72] All are thermally unstable towards decomposition to their elements. One other possible oxide that has not yet been synthesised is oxatetrazole (N4O), an aromatic ring.[71]
Nitrous oxide (N2O), better known as laughing gas, is made by thermal decomposition of molten ammonium nitrate at 250 °C. This is a redox reaction and thus nitric oxide and nitrogen are also produced as byproducts. It is mostly used as a propellant and aerating agent for sprayed canned whipped cream, and was formerly commonly used as an anaesthetic. Despite appearances, it cannot be considered to be the anhydride of hyponitrous acid (H2N2O2) because that acid is not produced by the dissolution of nitrous oxide in water. It is rather unreactive (not reacting with the halogens, the alkali metals, or ozone at room temperature, although reactivity increases upon heating) and has the unsymmetrical structure N–N–O (N≡N+O−↔−N=N+=O): above 600 °C it dissociates by breaking the weaker N–O bond.[71] Nitric oxide (NO) is the simplest stable molecule with an odd number of electrons. In mammals, including humans, it is an important cellular signalling molecule involved in many physiological and pathological processes.[73] It is formed by catalytic oxidation of ammonia. It is a colourless paramagnetic gas that, being thermodynamically unstable, decomposes to nitrogen and oxygen gas at 1100–1200 °C. Its bonding is similar to that in nitrogen, but one extra electron is added to a π* antibonding orbital and thus the bond order has been reduced to approximately 2.5; hence dimerisation to O=N–N=O is unfavourable except below the boiling point (where the cis isomer is more stable) because it does not actually increase the total bond order and because the unpaired electron is delocalised across the NO molecule, granting it stability. There is also evidence for the asymmetric red dimer O=N–O=N when nitric oxide is condensed with polar molecules. It reacts with oxygen to give brown nitrogen dioxide and with halogens to give nitrosyl halides. It also reacts with transition metal compounds to give nitrosyl complexes, most of which are deeply coloured.[71]
Blue dinitrogen trioxide (N2O3) is only available as a solid because it rapidly dissociates above its melting point to give nitric oxide, nitrogen dioxide (NO2), and dinitrogen tetroxide (N2O4). The latter two compounds are somewhat difficult to study individually because of the equilibrium between them, although sometimes dinitrogen tetroxide can react by heterolytic fission to nitrosonium and nitrate in a medium with high dielectric constant. Nitrogen dioxide is an acrid, corrosive brown gas. Both compounds may be easily prepared by decomposing a dry metal nitrate. Both react with water to form nitric acid. Dinitrogen tetroxide is very useful for the preparation of anhydrous metal nitrates and nitrato complexes, and it became the storable oxidiser of choice for many rockets in both the United States and USSR by the late 1950s. This is because it is a hypergolic propellant in combination with a hydrazine-based rocket fuel and can be easily stored since it is liquid at room temperature.[71]
The thermally unstable and very reactive dinitrogen pentoxide (N2O5) is the anhydride of nitric acid, and can be made from it by dehydration with phosphorus pentoxide. It is of interest for the preparation of explosives.[74] It is a deliquescent, colourless crystalline solid that is sensitive to light. In the solid state it is ionic with structure [NO2]+[NO3]−; as a gas and in solution it is molecular O2N–O–NO2. Hydration to nitric acid comes readily, as does analogous reaction with hydrogen peroxide giving peroxonitric acid (HOONO2). It is a violent oxidising agent. Gaseous dinitrogen pentoxide decomposes as follows:[71]
- N2O5 ⇌ NO2 + NO3 → NO2 + O2 + NO
- N2O5 + NO ⇌ 3 NO2
Oxoacids, oxoanions, and oxoacid salts
[edit]Many nitrogen oxoacids are known, though most of them are unstable as pure compounds and are known only as aqueous solutions or as salts. Hyponitrous acid (H2N2O2) is a weak diprotic acid with the structure HON=NOH (pKa1 6.9, pKa2 11.6). Acidic solutions are quite stable but above pH 4 base-catalysed decomposition occurs via [HONNO]− to nitrous oxide and the hydroxide anion. Hyponitrites (involving the N
2O2−
2 anion) are stable to reducing agents and more commonly act as reducing agents themselves. They are an intermediate step in the oxidation of ammonia to nitrite, which occurs in the nitrogen cycle. Hyponitrite can act as a bridging or chelating bidentate ligand.[75]
Nitrous acid (HNO2) is not known as a pure compound, but is a common component in gaseous equilibria and is an important aqueous reagent: its aqueous solutions may be made from acidifying cool aqueous nitrite (NO−
2, bent) solutions, although already at room temperature disproportionation to nitrate and nitric oxide is significant. It is a weak acid with pKa 3.35 at 18 °C. They may be titrimetrically analysed by their oxidation to nitrate by permanganate. They are readily reduced to nitrous oxide and nitric oxide by sulfur dioxide, to hyponitrous acid with tin(II), and to ammonia with hydrogen sulfide. Salts of hydrazinium N
2H+
5 react with nitrous acid to produce azides which further react to give nitrous oxide and nitrogen. Sodium nitrite is mildly toxic in concentrations above 100 mg/kg, but small amounts are often used to cure meat and as a preservative to avoid bacterial spoilage. It is also used to synthesise hydroxylamine and to diazotise primary aromatic amines as follows:[75]
- ArNH2 + HNO2 → [ArNN]Cl + 2 H2O
Nitrite is also a common ligand that can coordinate in five ways. The most common are nitro (bonded from the nitrogen) and nitrito (bonded from an oxygen). Nitro-nitrito isomerism is common, where the nitrito form is usually less stable.[75]

Nitric acid (HNO3) is by far the most important and the most stable of the nitrogen oxoacids. It is one of the three most used acids (the other two being sulfuric acid and hydrochloric acid) and was first discovered by alchemists in the 13th century. It is made by the catalytic oxidation of ammonia to nitric oxide, which is oxidised to nitrogen dioxide, and then dissolved in water to give concentrated nitric acid. In the United States of America, over seven million tonnes of nitric acid are produced every year, most of which is used for nitrate production for fertilisers and explosives, among other uses. Anhydrous nitric acid may be made by distilling concentrated nitric acid with phosphorus pentoxide at low pressure in glass apparatus in the dark. It can only be made in the solid state, because upon melting it spontaneously decomposes to nitrogen dioxide, and liquid nitric acid undergoes self-ionisation to a larger extent than any other covalent liquid as follows:[75]
- 2 HNO3 ⇌ H
2NO+
3 + NO−
3 ⇌ H2O + [NO2]+ + [NO3]−
Two hydrates, HNO3·H2O and HNO3·3H2O, are known that can be crystallised. It is a strong acid and concentrated solutions are strong oxidising agents, though gold, platinum, rhodium, and iridium are immune to attack. A 3:1 mixture of concentrated hydrochloric acid and nitric acid, called aqua regia, is still stronger and successfully dissolves gold and platinum, because free chlorine and nitrosyl chloride are formed and chloride anions can form strong complexes. In concentrated sulfuric acid, nitric acid is protonated to form nitronium, which can act as an electrophile for aromatic nitration:[75]
- HNO3 + 2 H2SO4 ⇌ NO+
2 + H3O+ + 2 HSO−
4
The thermal stabilities of nitrates (involving the trigonal planar NO−
3 anion) depends on the basicity of the metal, and so do the products of decomposition (thermolysis), which can vary between the nitrite (for example, sodium), the oxide (potassium and lead), or even the metal itself (silver) depending on their relative stabilities. Nitrate is also a common ligand with many modes of coordination.[75]
Finally, although orthonitric acid (H3NO4), which would be analogous to orthophosphoric acid, does not exist, the tetrahedral orthonitrate anion NO3−
4 is known in its sodium and potassium salts:[75]
These white crystalline salts are very sensitive to water vapour and carbon dioxide in the air:[75]
- Na3NO4 + H2O + CO2 → NaNO3 + NaOH + NaHCO3
Despite its limited chemistry, the orthonitrate anion is interesting from a structural point of view due to its regular tetrahedral shape and the short N–O bond lengths, implying significant polar character to the bonding.[75]
Organic nitrogen compounds
[edit]Nitrogen is one of the most important elements in organic chemistry. Many organic functional groups involve a carbon–nitrogen bond, such as amides (RCONR2), amines (R3N), imines (RC(=NR)R), imides (RCO)2NR, azides (RN3), azo compounds (RN2R), cyanates (ROCN), isocyanates (RNCO), nitrates (RONO2), nitriles (RCN), isonitriles (RNC), nitrites (RONO), nitro compounds (RNO2), nitroso compounds (RNO), oximes (RC(=NOH)R), and pyridine derivatives. C–N bonds are strongly polarised towards nitrogen. In these compounds, nitrogen is usually trivalent (though it can be tetravalent in quaternary ammonium salts, R4N+), with a lone pair that can confer basicity on the compound by being coordinated to a proton. This may be offset by other factors: for example, amides are not basic because the lone pair is delocalised into a double bond (though they may act as bases at very low pH, being protonated at the oxygen), and pyrrole is not basic because the lone pair is delocalised as part of an aromatic ring.[76] The amount of nitrogen in a chemical substance can be determined by the Kjeldahl method.[77] In particular, nitrogen is an essential component of nucleic acids, amino acids and thus proteins, and the energy-carrying molecule adenosine triphosphate and is thus vital to all life on Earth.[76]
Occurrence
[edit]
Nitrogen is the most common pure element in the earth, making up 78.1% of the volume of the atmosphere[10] (75.5% by mass), around 3.89 million gigatonnes (3.89×1018 kg). Despite this, it is not very abundant in Earth's crust, making up somewhere around 19 parts per million of this, on par with niobium, gallium, and lithium. (This represents 300,000 to a million gigatonnes of nitrogen, depending on the mass of the crust.[78]) The only important nitrogen minerals are nitre (potassium nitrate, saltpetre) and soda nitre (sodium nitrate, Chilean saltpetre). However, these have not been an important source of nitrates since the 1920s, when the industrial synthesis of ammonia and nitric acid became common.[79]
Nitrogen compounds constantly interchange between the atmosphere and living organisms. Nitrogen must first be processed, or "fixed", into a plant-usable form, usually ammonia. Some nitrogen fixation is done by lightning strikes producing the nitrogen oxides, but most is done by diazotrophic bacteria through enzymes known as nitrogenases (although today industrial nitrogen fixation to ammonia is also significant). When the ammonia is taken up by plants, it is used to synthesise proteins. These plants are then digested by animals who use the nitrogen compounds to synthesise their proteins and excrete nitrogen-bearing waste. Finally, these organisms die and decompose, undergoing bacterial and environmental oxidation and denitrification, returning free dinitrogen to the atmosphere. Industrial nitrogen fixation by the Haber process is mostly used as fertiliser, although excess nitrogen–bearing waste, when leached, leads to eutrophication of freshwater and the creation of marine dead zones, as nitrogen-driven bacterial growth depletes water oxygen to the point that all higher organisms die. Furthermore, nitrous oxide, which is produced during denitrification, attacks the atmospheric ozone layer.[79]
Many saltwater fish manufacture large amounts of trimethylamine oxide to protect them from the high osmotic effects of their environment; conversion of this compound to dimethylamine is responsible for the early odour in unfresh saltwater fish.[80] In animals, free radical nitric oxide (derived from an amino acid), serves as an important regulatory molecule for circulation.[81]
Nitric oxide's rapid reaction with water in animals results in the production of its metabolite nitrite. Animal metabolism of nitrogen in proteins, in general, results in the excretion of urea, while animal metabolism of nucleic acids results in the excretion of urea and uric acid. The characteristic odour of animal flesh decay is caused by the creation of long-chain, nitrogen-containing amines, such as putrescine and cadaverine, which are breakdown products of the amino acids ornithine and lysine, respectively, in decaying proteins.[82]
Production
[edit]Nitrogen gas is an industrial gas produced by the fractional distillation of liquid air, or by mechanical means using gaseous air (pressurised reverse osmosis membrane or pressure swing adsorption). Nitrogen gas generators using membranes or pressure swing adsorption (PSA) are typically more cost and energy efficient than bulk-delivered nitrogen.[83] Commercial nitrogen is often a byproduct of air-processing for industrial concentration of oxygen for steelmaking and other purposes. When supplied compressed in cylinders it is often called OFN (oxygen-free nitrogen).[84] Commercial-grade nitrogen already contains at most 20 ppm oxygen, and specially purified grades containing at most 2 ppm oxygen and 10 ppm argon are also available.[85]
In a chemical laboratory, it is prepared by treating an aqueous solution of ammonium chloride with sodium nitrite.[86]
- NH4Cl + NaNO2 → N2 + NaCl + 2 H2O
Small amounts of the impurities NO and HNO3 are also formed in this reaction. The impurities can be removed by passing the gas through aqueous sulfuric acid containing potassium dichromate.[86]
It can also be obtained by the thermal decomposition of ammonium dichromate.[87]
- 3(NH4)2Cr2O7 → 2N2 + 9H2O + 3Cr2O3 + 2NH3 + 32O2
Very pure nitrogen can be prepared by the thermal decomposition of barium azide or sodium azide.[88]
- 2 NaN3 → 2 Na + 3 N2
Applications
[edit]The applications of nitrogen compounds are naturally extremely widely varied due to the huge size of this class: hence, only applications of pure nitrogen itself will be considered here. Two-thirds (2/3) of nitrogen produced by industry is sold as gas and the remaining one-third (1/3) as a liquid.
Gas
[edit]The gas is mostly used as a low reactivity safe atmosphere wherever the oxygen in the air would pose a fire, explosion, or oxidising hazard. Some examples include:[85]
- As a modified atmosphere, pure or mixed with carbon dioxide, to nitrogenate and preserve the freshness of packaged or bulk foods (by delaying rancidity and other forms of oxidative damage). Pure nitrogen as food additive is labelled in the European Union with the E number E941.[89]
- In incandescent light bulbs as an inexpensive alternative to argon.[90]
- In fire suppression systems for Information technology (IT) equipment.[85]
- In the manufacture of stainless steel.[91]
- In the case-hardening of steel by nitriding.[92]
- In some aircraft fuel systems to reduce fire hazard (see inerting system).
- To inflate race car and aircraft tires,[93] reducing the problems of inconsistent expansion and contraction caused by moisture and oxygen in natural air.[85]
Nitrogen is commonly used during sample preparation in chemical analysis. It is used to concentrate and reduce the volume of liquid samples. Directing a pressurised stream of nitrogen gas perpendicular to the surface of the liquid causes the solvent to evaporate while leaving the solute(s) and un-evaporated solvent behind.[94]
Nitrogen can be used as a replacement, or in combination with, carbon dioxide to pressurise kegs of some beers, particularly stouts and British ales, due to the smaller bubbles it produces, which makes the dispensed beer smoother and headier.[95] A pressure-sensitive nitrogen capsule known commonly as a "widget" allows nitrogen-charged beers to be packaged in cans and bottles.[96][97] Nitrogen tanks are also replacing carbon dioxide as the main power source for paintball guns. Nitrogen must be kept at a higher pressure than CO2, making N2 tanks heavier and more expensive.[98]
Equipment
[edit]Some construction equipment uses pressurised nitrogen gas to help hydraulic system to provide extra power to devices such as hydraulic hammer. Nitrogen gas, formed from the decomposition of sodium azide, is used for the inflation of airbags.[99]
Execution
[edit]As nitrogen is an asphyxiant gas in itself, some jurisdictions have considered asphyxiation by inhalation of pure nitrogen as a means of capital punishment (as a substitute for lethal injection).[100][101][102] In January 2024, Kenneth Eugene Smith became the first person executed by nitrogen asphyxiation.[103]
Liquid
[edit]Liquid nitrogen is a cryogenic liquid which looks like water. When insulated in proper containers such as dewar flasks, it can be transported and stored with a low rate of evaporative loss.[104]

Like dry ice, the main use of liquid nitrogen is for cooling to low temperatures. It is used in the cryopreservation of biological materials such as blood and reproductive cells (sperm and eggs). It is used in cryotherapy to remove cysts and warts on the skin by freezing them.[105] It is used in laboratory cold traps, and in cryopumps to obtain lower pressures in vacuum pumped systems. It is used to cool heat-sensitive electronics such as infrared detectors and X-ray detectors. Other uses include freeze-grinding and machining materials that are soft or rubbery at room temperature, shrink-fitting and assembling engineering components, and more generally to attain very low temperatures where necessary. Because of its low cost, liquid nitrogen is often used for cooling even when such low temperatures are not strictly necessary, such as refrigeration of food, freeze-branding livestock, freezing pipes to halt flow when valves are not present, and consolidating unstable soil by freezing whenever excavation is going on underneath.[85]
Safety
[edit]Gas
[edit]Although nitrogen is non-toxic, when released into an enclosed space it can displace oxygen, and therefore presents an asphyxiation hazard. This may happen with few warning symptoms, since the human carotid body is a relatively poor and slow low-oxygen (hypoxia) sensing system.[106] An example occurred shortly before the launch of the first Space Shuttle mission on March 19, 1981, when two technicians died from asphyxiation after they walked into a space located in the Space Shuttle's mobile launcher platform that was pressurised with pure nitrogen as a precaution against fire.[107]
When inhaled at high partial pressures (more than about 4 bar, encountered at depths below about 30 m in scuba diving), nitrogen is an anaesthetic agent, causing nitrogen narcosis, a temporary state of mental impairment similar to nitrous oxide intoxication.[108][109]
Nitrogen dissolves in the blood and body fats. Rapid decompression (as when divers ascend too quickly or astronauts decompress too quickly from cabin pressure to spacesuit pressure) can lead to a potentially fatal condition called decompression sickness (formerly known as caisson sickness or the bends), when nitrogen bubbles form in the bloodstream, nerves, joints, and other sensitive or vital areas.[110][111] Bubbles from other "inert" gases (gases other than carbon dioxide and oxygen) cause the same effects, so replacement of nitrogen in breathing gases may prevent nitrogen narcosis, but does not prevent decompression sickness.[112]
Liquid
[edit]As a cryogenic liquid, liquid nitrogen can be dangerous by causing cold burns on contact, although the Leidenfrost effect provides protection for very short exposure (about one second).[113] Ingestion of liquid nitrogen can cause severe internal damage. For example, in 2012, a young woman in England had to have her stomach removed after ingesting a cocktail made with liquid nitrogen.[114]
Because the liquid-to-gas expansion ratio of nitrogen is 1:694 at 20 °C, a tremendous amount of force can be generated if liquid nitrogen is rapidly vaporised in an enclosed space. In an incident on January 12, 2006, at Texas A&M University, the pressure-relief devices of a tank of liquid nitrogen were malfunctioning and later sealed. As a result of the subsequent pressure buildup, the tank failed catastrophically. The force of the explosion was sufficient to propel the tank through the ceiling immediately above it, shatter a reinforced concrete beam immediately below it, and blow the walls of the laboratory 0.1–0.2 m off their foundations.[115]
Liquid nitrogen readily evaporates to form gaseous nitrogen, and hence the precautions associated with gaseous nitrogen also apply to liquid nitrogen.[116][117][118] For example, oxygen sensors are sometimes used as a safety precaution when working with liquid nitrogen to alert workers of gas spills into a confined space.[119]
Vessels containing liquid nitrogen can condense oxygen from air. The liquid in such a vessel becomes increasingly enriched in oxygen (boiling point −183 °C, higher than that of nitrogen) as the nitrogen evaporates, and can cause violent oxidation of organic material.[120]
Oxygen deficiency monitors
[edit]Oxygen sensors are used to measure oxygen levels in confined spaces and any place where nitrogen gas or liquid are stored or used. In the event of a nitrogen leak, and a decrease in oxygen to a pre-set alarm level, an oxygen deficiency monitor can be programmed to set off audible and visual alarms. Most commonly, the oxygen range to alert personnel is when oxygen levels drop below 19.5%. In the U.S., OSHA specifies that a hazardous atmosphere may include one where the oxygen concentration is below 19.5% or above 23.5%.[121]
See also
[edit]References
[edit]- ^ a b "Standard Atomic Weights: Nitrogen". CIAAW. 2009.
- ^ Prohaska, Thomas; Irrgeher, Johanna; Benefield, Jacqueline; Böhlke, John K.; Chesson, Lesley A.; Coplen, Tyler B.; Ding, Tiping; Dunn, Philip J. H.; Gröning, Manfred; Holden, Norman E.; Meijer, Harro A. J. (2022-05-04). "Standard atomic weights of the elements 2021 (IUPAC Technical Report)". Pure and Applied Chemistry. doi:10.1515/pac-2019-0603. ISSN 1365-3075.
- ^ Lide, David R. (1990–1991). CRC Handbook of Physics and Chemistry (71st ed.). Boca Raton, Ann Arbor, Boston: CRC Press, inc. pp. 4-22 (one page).
- ^ "Gases - Density". The Engineering Toolbox. Retrieved 27 January 2019.
- ^ a b c d e Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. p. 28. doi:10.1016/C2009-0-30414-6. ISBN 978-0-08-037941-8.
- ^ Tetrazoles contain a pair of double-bonded nitrogen atoms with oxidation state 0 in the ring. A Synthesis of the parent 1H-tetrazole, CH2N4 (two atoms N(0)) is given in Henry, Ronald A.; Finnegan, William G. (1954). "An Improved Procedure for the Deamination of 5-Aminotetrazole". Journal of the American Chemical Society. 76 (1): 290–291. Bibcode:1954JAChS..76..290H. doi:10.1021/ja01630a086. ISSN 0002-7863.
- ^ Arblaster, John W. (2018). Selected Values of the Crystallographic Properties of Elements. Materials Park, Ohio: ASM International. ISBN 978-1-62708-155-9.
- ^ Kondev, F. G.; Wang, M.; Huang, W. J.; Naimi, S.; Audi, G. (2021). "The NUBASE2020 evaluation of nuclear properties" (PDF). Chinese Physics C. 45 (3) 030001. doi:10.1088/1674-1137/abddae.
- ^ Common Bond Energies (D) and Bond Lengths (r) Archived 2010-05-15 at the Wayback Machine. wiredchemist.com
- ^ a b c Greenwood and Earnshaw, pp. 406–07
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Bibliography
[edit]- Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. doi:10.1016/C2009-0-30414-6. ISBN 978-0-08-037941-8.
External links
[edit]- Etymology of Nitrogen
- Nitrogen at The Periodic Table of Videos (University of Nottingham)
- Nitrogen podcast from the Royal Society of Chemistry's Chemistry World
Nitrogen
View on GrokipediaHistory
Discovery and isolation
Nitrogen was first isolated in 1772 by Scottish physician Daniel Rutherford during his doctoral research at the University of Edinburgh. Rutherford conducted experiments in which he confined a mouse in a sealed container of air until it suffocated, then removed the carbon dioxide (referred to as "fixed air") produced by respiration using an alkali solution, such as limewater. The remaining gas, which he termed "mephitic air" or "noxious air," extinguished flames and was lethal to small animals, leading him to conclude it was a distinct component of the atmosphere saturated with phlogiston, separate from oxygen and carbon dioxide.[4][5] Rutherford's isolation occurred amid a flurry of contemporaneous investigations into the composition of air during the late 18th century. Swedish chemist Carl Wilhelm Scheele independently produced a similar gas in 1772 by heating ammonium nitrate and other nitrates, though he did not fully characterize it as an element. English chemist Joseph Priestley also isolated the gas around the same time through combustion experiments, calling it "phlogisticated air," and further studied its properties by reacting it with metals to form oxides. In 1781, Henry Cavendish confirmed nitrogen's inert nature by sparking mixtures of air and oxygen over water, producing nitric acid and quantifying the proportions of atmospheric gases. Rutherford received primary credit for the discovery due to the publication of his dissertation, De aere fixo dicto aut mephitico, in 1772.[5][4]Etymology and nomenclature
The element nitrogen was first isolated in 1772 by Scottish physician Daniel Rutherford, who referred to it as "mephitic air" or "noxious air," terms reflecting its inability to support combustion or respiration, akin to earlier descriptions of "phlogisticated air" by chemists like Joseph Priestley and Henry Cavendish.[6] These early names highlighted its asphyxiating properties rather than its chemical identity.[7] In 1789, French chemist Antoine Lavoisier proposed the name azote for the gas, derived from the Greek prefix a- (meaning "without" or "not") and zōē (meaning "life"), emphasizing its role in causing suffocation by displacing oxygen.[6] This term gained traction in France and influenced names in several languages. The following year, in 1790, French chemist Jean-Antoine Chaptal coined nitrogène, which became the basis for the English "nitrogen" adopted around 1794; Chaptal's name was suggested upon recognizing the element's presence in nitric acid and nitrates.[7][6] The etymology of "nitrogen" traces to the French nitrogène, combining nitre (from Latin nitrum, referring to saltpeter or potassium nitrate) with the suffix -gène (from Greek -genēs, meaning "producing" or "begetting").[7] Thus, it literally means "nitre-forming" or "soda-producing," alluding to nitrogen's role in forming nitre compounds essential for gunpowder and fertilizers. The root nitron itself originates from ancient Greek, likely borrowed from Semitic languages denoting natural soda or salt deposits.[8] Alternative names persist in various languages, often reflecting either the azote tradition or asphyxiation. In French, Italian (azoto), Russian (azot), and Polish (azot), the term derives from Lavoisier's azote, underscoring its lifeless quality.[6] German Stickstoff, introduced by Swiss physician Christoph Girtanner in 1791, combines stick- (from ersticken, "to suffocate" or "choke") with Stoff ("substance"), directly referencing its toxic effects in pure form.[6] Similarly, Dutch stikstof follows this suffocation motif. In contrast, languages like Spanish (nitrógeno), Portuguese (nitrogênio), and Swedish (kväve, from kväva, "to choke") blend or adapt these roots.[6] In modern chemical nomenclature, nitrogen is designated by the IUPAC-approved name "nitrogen" and atomic symbol N, reflecting its position as element 7 in the periodic table.[6] The symbol N is universally used, derived straightforwardly from the English and Latin nitrogenium, ensuring consistency across scientific literature. Historical proposals like alcaligène (emphasizing alkali production) were abandoned in favor of these standardized terms.[6]Properties
Physical and atomic properties
Nitrogen is a chemical element with atomic number 7 and chemical symbol N.[1] It is a nonmetal in group 15 (pnictogens) of the periodic table, with an atomic weight ranging from 14.00643 to 14.00728 due to isotopic variation.[9] The electron configuration of the nitrogen atom is [He] 2s² 2p³, featuring three unpaired electrons in the 2p orbitals that contribute to its reactivity in bonding.[1] On the Pauling scale, nitrogen has an electronegativity of 3.04, reflecting its strong tendency to attract electrons in chemical bonds.[10] The first ionization energy is 14.5341 eV (equivalent to 1402.3 kJ/mol), indicating the energy required to remove one electron from a neutral atom in the gas phase.[11] At standard temperature and pressure, elemental nitrogen exists as a diatomic molecule (N₂), formed by a strong triple bond between two nitrogen atoms, which imparts high stability and low reactivity under ambient conditions.[12] N₂ is a colorless, odorless, and tasteless gas that is noncombustible and nontoxic, comprising about 78% of Earth's atmosphere by volume.[12] Its density at standard temperature and pressure (0°C, 1 atm) is 1.2506 g/L (or 1.2506 kg/m³).[13] Nitrogen liquefies and solidifies at very low temperatures, characteristic of its weak intermolecular forces despite the molecular triple bond. The following table summarizes key phase transition points for N₂:| Property | Value | Reference |
|---|---|---|
| Melting point | 63.3 K (-209.85°C) | Streng (1971) via NIST |
| Boiling point | 77.34 K (-195.81°C) | Jacobsen et al. (1986) via NIST |
| Triple point (T) | 63.14 K (-210.01°C) | Jacobsen et al. (1986) via NIST |
| Triple point (P) | 0.1252 bar | Jacobsen et al. (1986) via NIST |
| Critical temperature | 126.19 K (-146.96°C) | Jacobsen et al. (1986) via NIST |
| Critical pressure | 33.978 bar | Jacobsen et al. (1986) via NIST |
| Critical density | 11.18 mol/L | Jacobsen et al. (1986) via NIST |
Isotopes
Nitrogen has two stable isotopes: nitrogen-14 (¹⁴N) and nitrogen-15 (¹⁵N). Nitrogen-14 is the predominant isotope, accounting for 99.634% of naturally occurring nitrogen, while nitrogen-15 constitutes 0.366%. These abundances were precisely determined through mass spectrometry measurements of atmospheric nitrogen, establishing a standard ratio of ¹⁴N/¹⁵N at 272.0 ± 0.3.[16] Both isotopes are non-radioactive and indefinitely stable, with nitrogen-14 having a nuclear spin of 1 and nitrogen-15 a spin of 1/2, the latter enabling its use in nuclear magnetic resonance (NMR) spectroscopy for structural analysis in organic and biochemical studies.[17] Nitrogen-15 is particularly valuable as a tracer in environmental and biological research due to its stable nature and slight mass difference from nitrogen-14, which leads to isotopic fractionation in processes like nitrogen fixation and denitrification. In biogeochemical cycles, variations in the ¹⁵N/¹⁴N ratio (expressed as δ¹⁵N) help trace nutrient sources, with atmospheric nitrogen serving as the reference standard at 0‰ and terrestrial materials ranging from -20‰ to +30‰. For instance, fertilizers typically show δ¹⁵N values near 0‰, while animal manure ranges from +10‰ to +25‰, aiding in pollution source identification.[18] In addition to its stable isotopes, nitrogen has 15 known radioactive isotopes, spanning mass numbers from ¹⁰N to ²⁵N, along with one observed nuclear isomer. These isotopes are short-lived, with the longest half-life belonging to nitrogen-13 (¹³N) at 9.965 minutes, which undergoes 100% positron emission (β⁺) decay to carbon-13 (¹³C), making it suitable for positron emission tomography (PET) imaging in medical diagnostics. Other notable radioactive isotopes include nitrogen-12 (¹²N), with a half-life of 11 milliseconds and primarily β⁺ decay (98%) to carbon-12, and nitrogen-16 (¹⁶N), with a 7.13-second half-life and β⁻ decay (nearly 100%) to oxygen-16, the latter produced in nuclear reactors for coolant flow monitoring due to its high-energy gamma emission.[17] Nitrogen-17 decays primarily by β⁻ emission to oxygen-17 (branching ratio ≈99%) with a 4.173-second half-life, with a small branch (≈1%) for β⁻ decay accompanied by neutron emission to oxygen-16.[19] These isotopes are artificially produced and play roles in nuclear physics research and radiopharmaceutical applications, but their rapid decay limits natural occurrence.[20]| Isotope | Stability | Natural Abundance (%) | Half-Life | Decay Mode | Key Applications/Notes |
|---|---|---|---|---|---|
| ¹⁴N | Stable | 99.634 | - | - | Most common; basis for atomic mass of N (14.0067 u) |
| ¹⁵N | Stable | 0.366 | - | - | NMR spectroscopy; isotopic tracer in biology and ecology |
| ¹²N | Radioactive | - | 11 ms | β⁺ (98%) | Short-lived; nuclear research |
| ¹³N | Radioactive | - | 9.965 min | β⁺ (100%) | PET imaging in medicine |
| ¹⁶N | Radioactive | - | 7.13 s | β⁻ (~100%) | Reactor monitoring; gamma emitter |
| ¹⁷N | Radioactive | - | 4.173 s | β⁻ (≈99%), β⁻-n (≈1%) | Nuclear studies |
Allotropes
Nitrogen exists primarily as the diatomic molecule N₂ under standard conditions, which constitutes about 78% of Earth's atmosphere and is the most stable allotrope, characterized by a strong triple bond with a bond dissociation energy of 945 kJ/mol.[21] Atomic nitrogen, also known as monatomic or "active" nitrogen, is a highly reactive allotrope produced by electrical discharges in N₂ gas, first observed in 1910 by Lord Rayleigh as a glowing yellow afterglow known as the Lewis-Rayleigh afterglow.[22] This form consists of nitrogen atoms in the ground state (^4S) or excited states, with three unpaired electrons making it a triradical that rapidly recombines to N₂, releasing energy as light and heat; it is transient and not stable at ambient conditions.[23] Beyond diatomic and atomic forms, nitrogen forms various polynitrogen molecules, often unstable and requiring low temperatures or isolation techniques for observation. The azide radical N₃• is a short-lived species observed spectroscopically, while N₄ has been identified but not fully structurally characterized.[24] In 2025, researchers synthesized neutral hexanitrogen (N₆) via gas-phase reaction of chlorine or bromine with silver azide at room temperature, trapping it in an argon matrix at 10 K or as films in liquid nitrogen at 77 K; this linear molecule features four double bonds and one central single bond, exhibiting a high dissociation barrier but poor thermal stability, decomposing explosively to N₂ and potentially serving as a high-energy-density material.[25] Polymeric nitrogen allotropes, consisting of extended networks of single-bonded nitrogen atoms, are synthesized under extreme high-pressure conditions and represent promising energy storage materials due to their potential to release large amounts of energy upon decomposition to N₂. Cubic gauche nitrogen (cg-N), first synthesized in 2004 at pressures above 110 GPa and temperatures around 2000 K, features a diamond-like three-dimensional structure with sp³ hybridization and is metastable upon decompression to ambient pressure.[26] Other forms include black phosphorus-like nitrogen (bp-N), achieved by laser heating N₂ at 140 GPa, which adopts a layered puckered structure similar to black phosphorus and exhibits semiconducting properties.[27] Layered polymeric nitrogen (LP-N) and post-layered variants like PLP-N form at pressures between 100–240 GPa, displaying two-dimensional sheets or hexagonal layers with varying stability up to room temperature under pressure.[28] These polymeric phases are typically accessed using diamond anvil cells and confirmed via X-ray diffraction, highlighting nitrogen's ability to mimic carbon's allotropy under compression.[29]Chemistry
Reactivity and bonding
Nitrogen exists primarily as the diatomic molecule N₂, characterized by a strong triple bond (N≡N) with a bond dissociation energy of 941 kJ/mol, which renders it highly stable and contributes to its low chemical reactivity under ambient conditions.[30] This triple bond arises from the overlap of one σ orbital (from sp hybridization) and two π orbitals (from unhybridized p orbitals), allowing each nitrogen atom to achieve an octet configuration while sharing six electrons.[31] The high bond energy—nearly twice that of the O=O double bond in O₂ (498 kJ/mol)—stems from nitrogen's small atomic size and effective orbital overlap, making bond cleavage endothermic and kinetically unfavorable without activation.[31] Due to this stability, N₂ exhibits minimal reactivity at room temperature, interacting only with highly electropositive metals such as lithium to form nitrides like Li₃N, or with certain biological enzymes in nitrogen-fixing bacteria that employ metal cofactors to weaken the bond.[32] Enhanced reactivity occurs under extreme conditions, including high temperatures (e.g., above 1000°C for combination with oxygen to yield NO), high pressures, or catalysis; the industrial Haber-Bosch process, for instance, uses iron-based catalysts at 200–300 atm and 400–500°C to facilitate N₂ + 3H₂ → 2NH₃.[31] In contrast, atomic nitrogen or activated N₂ species, such as those generated in electrical discharges, display high reactivity, forming azides or inserting into C–H bonds.[32] In bonding, nitrogen's five valence electrons enable versatile hybridization (sp, sp², sp³) and multiple bond formation, favoring π-bonding with second-period elements like carbon and oxygen due to similar orbital sizes and energies.[31] Common motifs include triple bonds in cyanides (e.g., H–C≡N), double bonds in imines (R₂C=NR), and single bonds in amines (R–NH₂), with catenation allowing chains like hydrazine (H₂N–NH₂).[31] Nitrogen's electronegativity (3.04 on the Pauling scale) promotes polar covalent bonds, where it often acts as a Lewis base via its lone pair, as in ammonia coordinating to metal centers.[31] Nitrogen spans oxidation states from −3 (e.g., in NH₃ and N³⁻ nitrides) to +5 (e.g., in NO₃⁻ and HNO₃), reflecting its ability to gain three electrons for reduction or lose five for oxidation, which underpins its redox versatility in compounds.[31] Intermediate states include +2 in NO (with a formal double bond and unpaired electron, making it paramagnetic) and +4 in NO₂ (dimerizing to N₂O₄ via N–N single bond).[31] This range facilitates reactions like the oxidation of NH₃ to HNO₃ in the Ostwald process, where nitrogen cycles through multiple states.[31]Inorganic compounds
Inorganic nitrogen compounds encompass a diverse array of species reflecting nitrogen's variable oxidation states from −3 to +5, enabling it to form stable bonds with metals, nonmetals, hydrogen, and oxygen. These compounds are pivotal in industrial processes, agriculture, and environmental chemistry, with ammonia and nitric acid ranking among the most produced chemicals globally.[33][34][31] Nitrides represent compounds where nitrogen adopts the −3 oxidation state, typically forming with alkali and alkaline earth metals. Lithium nitride (Li₃N) is synthesized by direct reaction of lithium metal with dinitrogen at ambient temperature, yielding a solid that reacts vigorously with water to produce ammonia and lithium hydroxide.[2][31] Transition metal nitrides, such as titanium nitride (TiN), exhibit high hardness and melting points, often prepared by heating metals in ammonia or nitrogen atmospheres, and find applications in coatings and ceramics due to their refractory properties.[2] Hydrides of nitrogen, primarily ammonia (NH₃) and hydrazine (N₂H₄), are key binary compounds with hydrogen. Ammonia, the most abundant inorganic nitrogen compound industrially, is produced via the Haber-Bosch process, which combines dinitrogen and dihydrogen at 200–300 atm and 400–500°C over an iron catalyst, achieving equilibrium yields optimized by Le Châtelier's principle.[2][31] It acts as a weak base in aqueous solution, forming the ammonium ion (NH₄⁺) with pK_a ≈ 9.25, and serves as a precursor for fertilizers and explosives. Hydrazine, prepared by oxidation of ammonia with sodium hypochlorite, is a high-energy liquid used in rocket propulsion, combusting exothermically with oxygen (ΔH = −622 kJ/mol) to yield dinitrogen and water.[2][31][34][35] Nitrogen oxides constitute a series of gaseous compounds with oxidation states ranging from +1 to +5, many of which play roles in atmospheric and biological processes. Nitrous oxide (N₂O), or laughing gas, is generated by thermal decomposition of ammonium nitrate at 170–200°C and serves as an anesthetic due to its inertness under physiological conditions, though it contributes to stratospheric ozone depletion.[2][31] Nitric oxide (NO), an odd-electron radical formed in combustion or by reduction of nitric acid with copper, acts as a signaling molecule in mammals for vasodilation and neurotransmission, while reacting with dioxygen to form nitrogen dioxide (NO₂).[2][31][34] NO₂, a toxic brown gas that dimerizes to N₂O₄ at lower temperatures, is a key pollutant from engine exhausts, oxidizing to nitrogen pentoxide (N₂O₅) in air, which hydrolyzes to nitric acid.[31] Oxoacids and their anions, such as nitric acid (HNO₃) and nitrous acid (HNO₂), exemplify nitrogen in higher oxidation states. Nitric acid, produced industrially by the Ostwald process—oxidizing ammonia to NO over platinum, then to NO₂, followed by absorption in water—is a strong, fuming acid used in nitrate fertilizer production and explosives like ammonium nitrate.[33][31] It exhibits +5 oxidation state and acts as a powerful oxidizer, decomposing metals to release NO or NO₂ depending on concentration. Nitrite ions (NO₂⁻) from nitrous acid serve as preservatives in food, while nitrate ions (NO₃⁻) are essential in fertilizers but can cause eutrophication in waterways.[2][34][36] Nitrogen halides, though less stable than fluorides, include nitrogen trifluoride (NF₃), synthesized from ammonia and fluorine over copper catalyst, which is thermodynamically stable and used in plasma etching due to its +3 oxidation state.[34][31] Nitrogen trichloride (NCl₃), formed from ammonia and chlorine, is highly explosive and decomposes to dinitrogen and chlorine. Azides, containing the N₃⁻ ion, are energetic materials; sodium azide (NaN₃) is prepared by reacting sodium amide with nitrous oxide and detonates to release dinitrogen, powering automobile airbags.[2][34] These compounds highlight nitrogen's versatility, though many require careful handling due to reactivity.[34]Organic nitrogen compounds
Organic nitrogen compounds are a diverse class of substances in which nitrogen atoms are covalently bonded to carbon atoms, forming part of the molecular backbone or functional groups. These compounds play crucial roles in organic synthesis, pharmaceuticals, dyes, and biological systems, with nitrogen's ability to form up to four bonds enabling a wide range of structures and reactivities.[37] They are classified based on the functional group involving nitrogen, including amines, amides, nitriles, nitro compounds, imines, and nitrogen-containing heterocycles, among others.[38] Amines are derivatives of ammonia (NH₃) where one or more hydrogen atoms are replaced by organic substituents such as alkyl or aryl groups. They are categorized as primary (R-NH₂), secondary (R₂NH), or tertiary (R₃N), with quaternary ammonium salts (R₄N⁺X⁻) formed by further alkylation. Amines exhibit basicity due to the lone pair on nitrogen, which accepts a proton, and their boiling points increase with hydrogen bonding capability—primary and secondary amines form hydrogen bonds, while tertiary ones do not. Common examples include methylamine (CH₃NH₂), used in chemical synthesis, and aniline (C₆H₅NH₂), a precursor for dyes and pharmaceuticals; they often have a fishy odor and are synthesized industrially from alcohols and ammonia.[38] Amides feature a nitrogen atom bonded to a carbonyl group (R-C(O)-NR₂), resulting from the condensation of carboxylic acids and amines, releasing water. This functional group is planar due to resonance between the nitrogen lone pair and the carbonyl π-bond, reducing basicity compared to amines and imparting stability. Primary amides (R-C(O)NH₂) like acetamide are soluble in water via hydrogen bonding, while secondary and tertiary amides appear in peptides and synthetic polymers. Amides are key in biochemistry as peptide bonds in proteins and in materials like nylon, formed from diamines and dicarboxylic acids.[38][39] Nitriles, or cyanides (R-C≡N), contain a carbon-nitrogen triple bond, making them versatile intermediates in organic synthesis for converting to carboxylic acids, esters, or amines via hydrolysis or reduction. The cyano group is electron-withdrawing, influencing reactivity in adjacent positions, and nitriles are typically liquids or low-melting solids with high dipole moments. Acetonitrile (CH₃CN) serves as a common solvent, while adiponitrile is used in nylon production; they are prepared from halides and cyanide ions or dehydration of amides.[40] Nitro compounds (R-NO₂) consist of a nitro group attached to carbon, often via electrophilic aromatic substitution on arenes or direct nitration of alkanes. The nitro group is strongly electron-withdrawing, activating ortho/para positions for further electrophilic attack in aromatics and stabilizing carbanions in aliphatic cases. Nitrobenzene (C₆H₅NO₂) is a major industrial compound, reduced to aniline for dyes and drugs, while nitromethane (CH₃NO₂) acts as a solvent and explosive precursor; these compounds are typically pale yellow liquids or solids with high boiling points.[41] Imines (R₂C=NR') arise from condensation of carbonyl compounds with primary amines, featuring a C=N double bond that imparts rigidity and is key in Schiff bases for coordination chemistry. They are less stable than carbonyls and hydrolyze under acidic or basic conditions, with examples like benzaldimine used in synthetic routes to heterocycles.[39] Nitrogen-containing heterocyclic compounds integrate nitrogen into ring structures, such as five- or six-membered rings, exhibiting aromaticity and unique reactivities. Pyrrole (five-membered, NH in ring) contributes to porphyrins in heme, while pyridine (six-membered, N replacing CH) behaves like benzene but with basic nitrogen for nucleophilic substitutions. These are foundational in alkaloids, vitamins (e.g., nicotine), and pharmaceuticals, with synthesis often involving cyclization reactions.[38][37] Other notable classes include azo compounds (R-N=N-R), valued for dyes due to visible light absorption, and hydrazines (R-NH-NH₂), used in rocket fuels and as reducing agents. Overall, the reactivity of organic nitrogen compounds stems from nitrogen's electronegativity and lone pair, enabling applications across chemistry and biology.[39][42]Occurrence
In the universe and Earth's crust
Nitrogen is among the most abundant elements in the universe, ranking sixth overall by atomic number fraction, with a cosmic abundance of approximately $ 7.5 \times 10^{-5} $ atoms relative to hydrogen (or ). This places it at roughly 0.007% of the total number of atoms in the cosmos, behind hydrogen, helium, oxygen, carbon, and neon. The element is primarily synthesized through the carbon-nitrogen-oxygen (CNO) cycle, a proton-capture process occurring in the cores of main-sequence stars more massive than about 1.3 solar masses, where carbon acts as a catalyst to fuse hydrogen into helium, producing nitrogen as a byproduct.[43][44] In the interstellar medium, nitrogen exists predominantly as molecular N₂, with detections confirmed via ultraviolet spectroscopy, though atomic and ionic forms are also present in diffuse regions. Its distribution reflects stellar nucleosynthesis over cosmic time, with higher abundances observed in metal-rich environments due to contributions from asymptotic giant branch (AGB) stars and supernovae. Observations of distant galaxies indicate that nitrogen enrichment correlates with star formation history, serving as a tracer for galactic chemical evolution.[45] In contrast to its cosmic prevalence, nitrogen is scarce in Earth's crust, comprising only about 83 ppm by weight in the upper continental crust and around 50–74 ppm in the bulk crust. This low concentration arises because nitrogen is volatile and largely partitioned into the atmosphere and hydrosphere during planetary differentiation, with minimal incorporation into silicate minerals. It occurs mainly as nitrate minerals (e.g., in evaporites), ammonium ions adsorbed onto clays or substituted in micas and feldspars, and trace nitrides in meteoritic materials, though organic-bound forms dominate in sedimentary rocks. Subduction and metamorphic processes can release crustal nitrogen back to the mantle or atmosphere, influencing the global nitrogen cycle.[46][47]In the atmosphere
Nitrogen constitutes approximately 78% of Earth's atmosphere by volume in dry air, making it the most abundant gas and a primary component influencing overall atmospheric pressure and density. This dominance arises from the stability of its diatomic form, N₂, which accounts for nearly all atmospheric nitrogen due to the molecule's strong triple bond, rendering it chemically inert under typical conditions.[48][49][50] The presence of N₂ serves a critical role in maintaining atmospheric balance by diluting oxygen concentrations to about 21%, which prevents uncontrolled combustion and rapid burning at the Earth's surface. Without this buffering effect, the higher oxygen levels would accelerate fire propagation and oxidation processes, potentially altering ecosystems and climate dynamics. N₂'s inertness also contributes to the long-term stability of the atmosphere, as it resists reaction with other gases except under high-energy conditions like lightning or in the upper atmosphere.[51][48] While N₂ overwhelmingly predominates, trace reactive nitrogen compounds exist in the atmosphere at concentrations below 0.01%, including nitric oxide (NO), nitrogen dioxide (NO₂), nitrous oxide (N₂O), and ammonia (NH₃). These species originate from natural sources such as soil emissions, wildfires, and microbial activity, as well as human activities like fossil fuel combustion and agriculture. They participate in key atmospheric processes, including the formation of tropospheric ozone, aerosol production, and nutrient deposition to ecosystems, though their low abundances limit direct impacts on bulk atmospheric composition.[52][53]In living organisms
Nitrogen is an essential constituent of all known living organisms, where it ranks as the fourth most abundant element in cellular biomass after carbon, hydrogen, and oxygen.[54] It occurs primarily in organic forms integrated into vital biomolecules, and its abundance varies by organism type and environmental conditions. In the terrestrial biosphere, the total nitrogen reservoir associated with living systems is estimated at around 135 Gt, though much of this is cycled through non-living organic matter; live plant biomass alone holds approximately 5% of this pool, or about 6.75 Gt of nitrogen. In plants, nitrogen constitutes 1–5% of the total dry matter, making it the most abundant mineral nutrient after carbon, hydrogen, and oxygen.[55] This proportion is highest in metabolically active tissues like leaves, where it supports photosynthesis and growth, and lower in woody parts. Healthy above-ground plant tissues often contain 3–4% nitrogen by dry weight, reflecting its concentration in chlorophyll and enzymes.[56] Leguminous plants can achieve higher levels through symbiotic nitrogen fixation, enhancing overall biomass nitrogen content. In animals, nitrogen typically accounts for about 3% of total body mass, as seen in humans, where it is concentrated in muscle proteins and other tissues.[57] On a dry weight basis, this rises to roughly 7–12%, depending on the species and tissue type, due to the exclusion of water. Microbial biomass, including bacteria and fungi, exhibits even higher nitrogen concentrations, often 10–14% of dry weight, driven by their protein-rich composition. For example, in the bacterium Escherichia coli, nitrogen comprises approximately 12% of dry biomass under standard growth conditions.[58] Globally, vegetation dominates the nitrogen inventory in living organisms, while microbial communities contribute substantially in soils (up to several Gt N in aggregate) and marine environments.Biological role
Nitrogen fixation
Biological nitrogen fixation (BNF) is the microbial process that converts atmospheric dinitrogen (N₂) into bioavailable forms, primarily ammonia (NH₃), which plants and other organisms can assimilate for growth.[59] This process is essential for maintaining global nitrogen cycles, as it provides the primary natural input of fixed nitrogen, estimated at approximately 128 teragrams (Tg) of nitrogen per year in natural terrestrial ecosystems and 60 Tg in agricultural systems.[60] Without BNF, ecosystems would lack sufficient nitrogen for protein synthesis and other vital functions, leading to severe limitations in primary productivity.[61] The core mechanism of BNF is catalyzed by the nitrogenase enzyme complex, a metalloenzyme consisting of the Fe protein (also called nitrogenase reductase) and the MoFe protein, encoded by nif genes.[62] Nitrogenase reduces N₂ to NH₃ using electrons from ferredoxin or flavodoxin and requires 16 ATP molecules per N₂ molecule fixed, making it highly energy-intensive.[59] The enzyme is extremely sensitive to oxygen, which inactivates it; thus, diazotrophs (nitrogen-fixing microorganisms) employ protective strategies such as spatial separation in heterocysts (in cyanobacteria like Anabaena), rapid respiration in free-living bacteria like Azotobacter, or isolation within plant root nodules in symbiotic associations.[59] Alternative nitrogenases containing vanadium (V-nitrogenase) or iron only (Fe-nitrogenase) exist but are less efficient and active under specific metal-limited conditions.[59] Genetic regulation of BNF ensures expression only under nitrogen-limiting conditions to conserve energy. In free-living diazotrophs like Azotobacter vinelandii, the enhancer-binding protein NifA activates transcription of nif genes via σ⁵⁴-dependent promoters, while the inhibitory protein NifL, a flavoprotein, senses redox status and ammonium levels to repress NifA activity.[62] In symbiotic systems, such as Rhizobium with legumes, oxygen sensing occurs via the FixL/FixJ two-component system, where low oxygen activates NifA to initiate nodule-specific nif gene expression.[62] These regulatory cascades integrate signals from nitrogen availability, oxygen, and plant host factors to coordinate fixation.[62] BNF occurs through three main types: free-living, associative, and symbiotic. Free-living diazotrophs, including aerobic Azotobacter and anaerobic Clostridium, fix nitrogen in soil, contributing 20–30 kg N ha⁻¹ yr⁻¹, though rates vary widely (3–51 kg N ha⁻¹ per crop).[59] Associative symbiosis involves endophytic bacteria like Azospirillum in cereal roots, providing modest inputs (up to 82% of plant nitrogen derived from air in some maize studies).[60] Symbiotic fixation is most efficient, particularly in legumes where Rhizobium or Bradyrhizobium form nodules on roots, fixing 20–300 kg N ha⁻¹ yr⁻¹; for example, soybeans globally fix about 24.8 Tg N annually, representing 70% of legume contributions.[59] Other symbioses include Frankia with actinorhizal plants and cyanobacteria like Nostoc in lichens or Azolla in rice paddies (20–146 kg N ha⁻¹).[60] In agriculture, BNF supports sustainable practices by reducing reliance on synthetic fertilizers; grain legumes alone provide 35.5 Tg N globally per year, enhancing soil fertility for subsequent crops through residual nitrogen (30–50 kg N ha⁻¹ leaked to soil).[63] Ecologically, BNF drives primary production in diverse habitats, including inland and coastal waters where it fixes 40 Tg N yr⁻¹, accounting for 15% of total global marine and terrestrial fixation.[61] Efforts to engineer BNF into non-leguminous cereals, such as through microbial inoculation or genetic transfer of nif genes, aim to boost yields while minimizing environmental impacts like eutrophication from fertilizer runoff.[60]Role in biomolecules
Nitrogen is an essential element in numerous biomolecules, forming the structural backbone of key macromolecules that underpin cellular function, growth, and heredity in all living organisms. It constitutes a critical component of amino acids, nucleic acids, and other vital compounds, enabling the synthesis of proteins, genetic material, and energy carriers. Without biologically available nitrogen, these molecules could not form, limiting the development and maintenance of life.[64][49] In proteins, nitrogen is integral to the amino group (-NH₂) present in every amino acid, the fundamental building blocks of these macromolecules. Proteins, which can comprise up to 55% of a prokaryote's dry weight, serve diverse roles as enzymes catalyzing metabolic reactions, structural components like collagen, and signaling molecules such as hormones. The incorporation of nitrogen into amino acids occurs through assimilation processes where ammonia (NH₃) or nitrate is converted into glutamine or glutamate, precursors for all other amino acids. This nitrogen-dependent synthesis is vital for protein folding and function, directly influencing organismal physiology and adaptation.[65][66] Nucleic acids, including DNA and RNA, rely on nitrogenous bases—purines (adenine, guanine) and pyrimidines (cytosine, thymine, uracil)—which contain multiple nitrogen atoms within their heterocyclic rings. These bases, accounting for about 23% of prokaryotic dry weight in nucleotide forms, enable the storage, replication, and expression of genetic information. Nitrogen's presence in these structures facilitates base pairing and hydrogen bonding, essential for the double-helix stability of DNA and the functional versatility of RNA in processes like transcription and translation. The synthesis of these bases begins with nitrogen-rich precursors like aspartate and glutamine, highlighting nitrogen's irreplaceable role in heredity.[64][66][65] Beyond proteins and nucleic acids, nitrogen features in other biomolecules such as chlorophyll, where it forms the porphyrin ring central to photosynthesis, allowing plants and algae to convert light energy into chemical energy. It is also a key element in ATP (adenosine triphosphate), the primary energy currency of cells, and in amino sugars like chitin, which provide structural support in fungal cell walls and arthropod exoskeletons. These roles underscore nitrogen's versatility in supporting energy metabolism, photosynthesis, and extracellular matrices across ecosystems.[64][65]The nitrogen cycle
The nitrogen cycle is a biogeochemical process through which nitrogen is converted among its multiple chemical forms—including dinitrogen gas (N₂), ammonia (NH₃), ammonium (NH₄⁺), nitrite (NO₂⁻), nitrate (NO₃⁻), and organic nitrogen compounds—as it circulates among the atmosphere, terrestrial and aquatic ecosystems, and living organisms.[64] This cycle is fundamental to sustaining life on Earth, as nitrogen is an essential element in amino acids, proteins, nucleic acids, and other biomolecules required for growth and reproduction.[67] Microorganisms, particularly bacteria and archaea, drive most transformations, while abiotic processes like lightning contribute smaller amounts.[64] The cycle begins with nitrogen fixation, the conversion of atmospheric N₂ into biologically available ammonia (NH₃) or ammonium (NH₄⁺). This energy-intensive process requires 16 ATP molecules and eight electrons per N₂ molecule and is primarily biological, performed by diazotrophic prokaryotes such as symbiotic bacteria (Rhizobium spp. in legume root nodules) and free-living bacteria (Azotobacter spp.).[64] Abiotic fixation occurs via lightning or industrial processes like the Haber-Bosch method, but biological fixation accounts for the majority of natural inputs, estimated at around 100–200 teragrams of nitrogen per year globally.[67] Once fixed, ammonia is rapidly assimilated by plants and microbes into organic forms, such as amino acids, through nitrogen assimilation.[64] Organic nitrogen from dead organisms, waste, or plant residues is then mineralized back into ammonium via ammonification (or mineralization), a decomposition process carried out by diverse heterotrophic bacteria and fungi that break down proteins and other nitrogenous compounds.[64] In aerobic soils and waters, ammonium is oxidized to nitrate in a two-step nitrification process: first to nitrite by ammonia-oxidizing bacteria (Nitrosomonas spp.) or archaea (Nitrosopumilus maritimus), and then to nitrate by nitrite-oxidizing bacteria (Nitrospira spp.).[64] This autotrophic process supports plant uptake of nitrate as a primary nitrogen source.[67] Under anaerobic conditions, such as waterlogged soils or sediments, nitrate is reduced back to N₂ through denitrification, a respiratory process performed by facultative anaerobes like Pseudomonas and Paracoccus spp., which use nitrate as an electron acceptor instead of oxygen.[64] This step releases dinitrogen gas (N₂) and nitrous oxide (N₂O), a potent greenhouse gas, closing the cycle by returning nitrogen to the atmosphere.[67] An additional anaerobic pathway, anaerobic ammonium oxidation (anammox), directly converts ammonium and nitrite to N₂ using specialized bacteria from the phylum Planctomycetes (Candidatus Brocadia anammoxidans), contributing significantly to nitrogen loss in marine and freshwater systems—up to 50% of oceanic N₂ production in some oxygen minimum zones.[64] These interconnected processes maintain a dynamic balance in the reactive nitrogen pool, with global fluxes dominated by microbial activity; for instance, biological fixation vastly exceeds abiotic sources by a factor of 10 or more.[67] Human activities, including fertilizer production and fossil fuel combustion, have doubled reactive nitrogen inputs since the mid-20th century, accelerating the cycle and leading to imbalances such as excess nitrate in ecosystems.[64]Production
Industrial processes
The primary industrial production of nitrogen gas (N₂) occurs through the separation of air, which consists of approximately 78% nitrogen by volume. This is achieved via three main processes: cryogenic distillation, pressure swing adsorption (PSA), and membrane permeation, each suited to different scales and purity requirements. Cryogenic methods dominate large-scale production, while PSA and membrane techniques enable on-site generation for medium to small volumes. These processes supply nitrogen for applications in chemicals, food preservation, electronics, and metallurgy, primarily from air separation units (ASUs).[68] Cryogenic air separation, the most established method, involves compressing atmospheric air to 5–10 bar, cooling it to remove impurities like water vapor and carbon dioxide via refrigeration and molecular sieves, and then liquefying it at around -196°C using the Joule-Thomson effect and expansion turbines. The liquefied air enters a double distillation column where nitrogen, with its lower boiling point (-196°C), vaporizes and rises to the top, while oxygen (-183°C) and other components remain liquid or distill separately; argon can be extracted as a byproduct in advanced setups. This process, pioneered in the late 19th century and commercialized in the early 20th, achieves ultra-high purity levels of 99.999% or greater and is energy-efficient for large plants producing thousands of tons per day, though it requires significant capital investment and is less viable for small-scale operations.[69][70] Pressure swing adsorption (PSA) provides a non-cryogenic alternative by passing compressed air (typically 7–10 bar) through beds of carbon molecular sieves or zeolites that preferentially adsorb oxygen and water vapor, allowing nitrogen to pass through. The process cycles between high-pressure adsorption (where oxygen is captured) and low-pressure desorption (purging the adsorbent with a portion of the product nitrogen), often using two or more beds in parallel for continuous operation. Developed in the mid-20th century and refined since the 1980s, PSA systems yield nitrogen purities of 95–99.999%, with recoveries around 70–90%, and are cost-effective for medium-scale on-site production (up to 100 tons per day) due to lower energy use (about 0.3–0.5 kWh/Nm³) compared to cryogenic methods, though they consume more air per unit of nitrogen.[71][72] Membrane separation, another non-cryogenic technique, employs bundles of hollow polymeric fibers (e.g., polyimide or polysulfone) that selectively permeate faster-diffusing gases like oxygen and carbon dioxide through their walls under pressure (8–15 bar), retaining slower-permeating nitrogen on the high-pressure side. The process, commercialized in the 1980s, requires pre-treatment of air to remove oil and particulates, and a single-stage setup typically produces nitrogen at 95–99.5% purity with 40–50% recovery, while multi-stage configurations can exceed 99%. It is compact, modular, and ideal for small-scale, portable applications (e.g., 1–50 Nm³/h) with low maintenance, but purity is generally lower than cryogenic or PSA methods, limiting its use in high-precision industries. Advances in membrane materials continue to improve selectivity and durability.[68] In addition to direct N₂ production, the Haber-Bosch process indirectly utilizes nitrogen by reacting it with hydrogen to form ammonia (NH₃) on an iron-based catalyst at 200–300 bar and 400–500°C, accounting for over 90% of global fixed-nitrogen output (approximately 185 million tons of ammonia annually as of 2023).[73] Nitrogen for this process is sourced from air separation, primarily cryogenic ASUs integrated with ammonia plants to supply high-purity N₂. This method revolutionized agriculture but is energy-intensive, consuming about 1–2% of global energy.[68]Laboratory preparation
In the laboratory, nitrogen gas (N₂) is commonly prepared by the thermal decomposition of ammonium nitrite (NH₄NO₂), which is generated in situ from an equimolar mixture of ammonium chloride (NH₄Cl) and sodium nitrite (NaNO₂) to avoid handling the unstable pure compound.[74] The reaction proceeds as follows:Applications
Agricultural and fertilizer uses
Nitrogen is an essential macronutrient for plant growth, forming the building blocks of amino acids, proteins, nucleic acids, and chlorophyll, which are critical for photosynthesis and overall crop productivity.[79] In agriculture, nitrogen fertilizers address soil deficiencies caused by intensive cropping, enabling higher yields and supporting global food security.[80] Without supplemental nitrogen, natural soil supplies would limit crop production to levels insufficient for the world's population.[81] The widespread use of nitrogen fertilizers began with the Haber-Bosch process, invented in 1909 by Fritz Haber and Carl Bosch, which synthesizes ammonia from atmospheric nitrogen and hydrogen (primarily from natural gas) under high pressure and temperature using an iron catalyst.[81] This industrial method scaled up during World War I for explosives and post-war for fertilizers, increasing global nitrogen application from 1.3 million metric tons in 1930 to about 80 million metric tons by 1988, a roughly 60-fold rise. As of 2022, global nitrogen fertilizer consumption had reached approximately 109 million metric tons of nutrient.[80][82] In the United States, synthetic nitrogen fertilizers transformed corn production, with usage stabilizing around 10-12 million metric tons annually since the 1970s, primarily as anhydrous ammonia, urea, and urea-ammonium nitrate (UAN) solutions.[81] Nitrogen fertilizers are categorized by their chemical form, each suited to specific soil types, crops, and application timings to minimize losses from leaching, volatilization, or denitrification.[83] The table below summarizes common types, their nitrogen content, and agricultural applications:| Fertilizer Type | Nitrogen Content (%) | Key Uses and Characteristics |
|---|---|---|
| Anhydrous Ammonia | 82 | Injected into soil for fall plowdown in corn on medium- to heavy-textured soils; high efficiency but requires specialized equipment to avoid volatilization.[83] |
| Urea | 46 | Surface-applied or incorporated for top-dressing wheat and pastures in late winter; converts to ammonium via hydrolysis, but prone to ammonia loss if not incorporated above 50°F (10°C).[83] |
| Ammonium Nitrate | 34 | Top-dressing for wheat or spring plowdown for corn; provides both ammonium and nitrate forms for quick availability, though it poses explosion risks if mishandled.[83] |
| Urea-Ammonium Nitrate (UAN) Solutions | 28-32 | Sidedressing for corn via irrigation or spray; versatile liquid form for banded application, reducing overall usage rates.[83] |
| Ammonium Sulfate | 21 | Fall plowdown or top-dressing for sulfur-deficient soils in pastures and wheat; acidifies soil slightly and resists volatilization on neutral to alkaline soils.[83] |
| Calcium Nitrate | 15.5 | Supplemental for high-pH or calcium-deficient soils in vegetables and fruits; nitrate form minimizes acidification but increases leaching risk on sandy soils.[83] |
