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Ammonium

From Wikipedia, the free encyclopedia
This article is about the ammonium ion. For its neutral conjugate base, seeammonia.
This article is about the molecular ion. For the ancient city, seeSiwa Oasis.
Ammonium
2-D skeletal version of the ammonium ion
Ball-and-stick model of the ammonium cation
Space-filling model of the ammonium cation
Names
IUPAC name
Ammonium ion
Systematic IUPAC name
Azanium[1]
Identifiers
3D model (JSmol)
ChEBI
ChemSpider
84
KEGG
MeSHD000644
UNII
  • InChI=1S/H3N/h1H3/p+1
    Key: QGZKDVFQNNGYKY-UHFFFAOYSA-O
  • InChI=1/H3N/h1H3/p+1
    Key: QGZKDVFQNNGYKY-IKLDFBCSAZ
  • [NH4+]
Properties
[NH4]+
Molar mass18.039 g·mol−1
Acidity (pKa)9.25
Conjugate baseAmmonia
Structure
Tetrahedral
Related compounds
Othercations
Related compounds
Ammonium radical •NH4
Except where otherwise noted, data are given for materials in theirstandard state (at 25 °C [77 °F], 100 kPa).
Chemical compound

Ammonium is a modified form ofammonia that has an extra hydrogen atom. It is a positively charged (cationic)molecular ion with thechemical formulaNH+4 or[NH4]+. It is formed by theaddition of a proton (a hydrogen nucleus) to ammonia (NH3). Ammonium is also a general name for positively charged (protonated) substitutedamines andquaternary ammonium cations ([NR4]+), where one or morehydrogenatoms are replaced byorganic or other groups (indicated by R). Not only is ammonium a source ofnitrogen and a keymetabolite for many living organisms, but it is an integral part of the globalnitrogen cycle.[2] As such, human impact in recent years could have an effect on the biological communities that depend on it.

Acid–base properties

[edit]
Fumes fromhydrochloric acid and ammonia forming a white cloud ofammonium chloride

The ammonium ion is generated when ammonia, a weak base, reacts withBrønsted acids (proton donors):

H+ + NH3 → [NH4]+

The ammonium ion is mildly acidic, reacting with Brønsted bases to return to the uncharged ammonia molecule:

[NH4]+ + B → HB + NH3

Thus, the treatment of concentrated solutions of ammonium salts with a strong base gives ammonia. When ammonia is dissolved in water, a tiny amount of it converts to ammonium ions:

H2O + NH3 ⇌ OH + [NH4]+

The degree to which ammonia forms the ammonium ion depends on thepH of the solution. If the pH is low, the equilibrium shifts to the right: more ammonia molecules are converted into ammonium ions. If the pH is high (the concentration ofhydrogen ions is low andhydroxide ions is high), the equilibrium shifts to the left: thehydroxide ion abstracts a proton from the ammonium ion, generating ammonia.

Formation of ammonium compounds can also occur in thevapor phase; for example, when ammonia vapor comes in contact with hydrogen chloride vapor, a white cloud of ammonium chloride forms, which eventually settles out as asolid in a thin white layer on surfaces.

Salts and characteristic reactions

[edit]
Formation of ammonium

Ammonium cation is found in a variety ofsalts such asammonium carbonate,ammonium chloride, andammonium nitrate. Most simple ammonium salts are verysoluble in water. An exception isammonium hexachloroplatinate, the formation of which was once used as a test for ammonium. The ammonium salts of nitrate and especiallyperchlorate are highly explosive, in these cases, ammonium is the reducing agent.

In an unusual process, ammonium radicals (NH4) form anamalgam. Such species are prepared by the addition of sodium amalgam to a solution of ammonium chloride.[3] This amalgam eventually decomposes to release ammonia and hydrogen.[4]

To find whether the ammonium ion is present in the salt, first, the salt is heated in presence ofalkali hydroxide releasing a gas with a characteristic smell, which isammonia.

[NH4]+ + OH → NH3 + H2O

To further confirm ammonia, it is passed through a glass rod dipped in anHCl solution (hydrochloric acid), creating white dense fumes ofammonium chloride.

NH3 + HCl → [NH4]Cl

Ammonia or ammonium ion when added toNessler's reagent gives a brown color precipitate known as the iodide of Million's base in basic medium.

Ammonium ion when added tochloroplatinic acid gives a yellow precipitate ofammonium hexachloroplatinate(IV).

H2[PtCl6] + [NH4]+ → [NH4]2[PtCl6](s) + 2 H+

Ammonium ion when added tosodium cobaltinitrite gives a yellow precipitate of ammonium cobaltinitrite.

Na3[Co(NO2)6] + 3 [NH4]+ → [NH4]3[Co(NO2)6](s) + 3 Na+

Ammonium ion gives a white precipitate of ammonium bitartrate when added topotassium bitartrate.

KC4H5O6 + [NH4]+ → [NH4]C4H5O6(s) + K+

Structure and bonding

[edit]

Thelone electron pair on thenitrogen atom (N) in ammonia, represented as a line above the N, forms acoordinate bond with aproton (H+). After that, all fourN−H bonds are equivalent, being polarcovalent bonds. The ion has atetrahedral structure and isisoelectronic withmethane and theborohydride anion. In terms of size, the ammonium cation (rionic = 148 pm), it is intermediate in size between potassium (144 pm) and rubidium ions (152 pm) when in an octahedral environment.[5]

Thevibrational spectrum consists of two main sets of absorptions, νN-H and δHNH. These bands are found near 3300 and 1400 cm-1.[6]

Organic ions

[edit]
See also:Amine

The hydrogen atoms in the ammonium ion can be substituted with analkyl group or some other organic group to form asubstituted ammonium ion (IUPAC nomenclature:aminium ion). Depending on the number of organic groups, the ammonium cation is called aprimary,secondary,tertiary, orquaternary. Except the quaternary ammonium cations, the organic ammonium cations are weak acids.

An example of a reaction forming an ammonium ion is that betweendimethylamine,(CH3)2NH, and an acid to give thedimethylammonium cation,[(CH3)2NH2]+:

Quaternary ammonium cations have four organic groups attached to the nitrogen atom, they lack a hydrogen atom bonded to the nitrogen atom. These cations, such as thetetra-n-butylammonium cation, are sometimes used to replace sodium or potassium ions to increase thesolubility of the associated anion in organicsolvents. Primary, secondary, and tertiary ammonium salts serve the same function but are lesslipophilic. They are also used asphase-transfer catalysts andsurfactants.

An unusual class of organic ammonium salts is derivatives of amineradical cations,[•NR3]+ such astris(4-bromophenyl)ammoniumyl hexachloroantimonate.

Biology

[edit]
Main article:Excretion
Ammonium exists as a result of ammonification anddecomposers. Ammonium is eventually nitrified, where it contributes to the flow ofnitrogen through the ecosystem. Human impacts are not shown here, but can impact the globalnitrogen cycle.

Becausenitrogen often limits netprimary production due to its use inenzymes that mediate the biochemical reactions that are necessary for life, ammonium is utilized by some microbes and plants.[7] For example, energy is released by theoxidation of ammonium in a process known asnitrification, which producesnitrate andnitrite.[8] This process is a form ofautotrophy that is common amongstNitrosomonas,Nitrobacter,Nitrosolobus, andNitrosospira, amongst others.[8]

The amount of ammonium in soil that is available fornitrification by microbes varies depending on environmental conditions.[9][10] For example, ammonium is deposited as a waste product from some animals, although it is converted intourea in mammals, sharks, and amphibians, and intouric acid in birds, reptiles, and terrestrial snails.[11] Its availability in soils is also influenced bymineralization, which makes more ammonium available from organicnitrogen sources, andimmobilization, which sequesters ammonium into organicnitrogen sources, both of which are mitigated by biological factors.[8]

Conversely,nitrate andnitrite can be reduced to ammonium as a way for living organisms to accessnitrogen for growth in a process known as assimilatory nitrate reduction.[12] Once assimilated, it can be incorporated intoproteins andDNA.[13]

Ammonium can accumulate in soils wherenitrification is slow or inhibited, which is common in hypoxic soils.[14] For example, ammonium mobilization is one of the key factors for thesymbiotic association between plants and fungi, calledmycorrhizae.[15] However, plants that consistently utilize ammonium as anitrogen source often must invest into more extensive root systems due to ammonium's limited mobility in soils compared to othernitrogen sources.[16][17]

Human impact

[edit]

Ammonium deposition from the atmosphere has increased in recent years due to volatilization from livestock waste and increased fertilizer use.[18] Because netprimary production is often limited bynitrogen, increased ammonium levels could impact the biological communities that rely on it. For example, increasingnitrogen content has been shown to increase plant growth, but aggravate soil phosphorus levels, which can impact microbial communities.[19]

Metal

[edit]

The ammonium cation has very similar properties to the heavieralkali metal cations and is often considered a close equivalent.[20][21][22] Neutral ammonium is expected to behave as ametal ([NH4]+ ions in a sea ofelectrons) at very high pressures, such as insidegiant planets such asUranus andNeptune.[21][22]

Under normal conditions, ammonium does not exist as a pure metal but does as anamalgam (NH4 alloy withmercury).[23]

See also

[edit]

References

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  1. ^International Union of Pure and Applied Chemistry (2005).Nomenclature of Inorganic Chemistry (IUPAC Recommendations 2005). Cambridge (UK):RSCIUPAC.ISBN 0-85404-438-8. pp. 71,105,314.Electronic version.
  2. ^Schlesinger, William H.; Bernhardt, Emily S. (2020-01-01), Schlesinger, William H.; Bernhardt, Emily S. (eds.),"Chapter 12 - The Global Cycles of Nitrogen, Phosphorus and Potassium",Biogeochemistry (Fourth Edition), Academic Press, pp. 483–508,doi:10.1016/b978-0-12-814608-8.00012-8,ISBN 978-0-12-814608-8, retrieved2024-03-08{{citation}}: CS1 maint: work parameter with ISBN (link)
  3. ^"Pseudo-binary compounds". Archived fromthe original on 2020-07-27. Retrieved2007-10-12.
  4. ^"Ammonium Salts".VIAS Encyclopedia.
  5. ^Shannon, R. D. (1976). "Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides".Acta Crystallographica Section A.32 (5):751–767.doi:10.1107/S0567739476001551.
  6. ^Meeron, Emmanuel (1957). "Mayer's Treatment of Ionic Solutions".The Journal of Chemical Physics.26 (4):804–806.doi:10.1063/1.1743411.
  7. ^Schlesinger, William H.; Bernhardt, Emily S. (2020-01-01), Schlesinger, William H.; Bernhardt, Emily S. (eds.),"Chapter 12 - The Global Cycles of Nitrogen, Phosphorus and Potassium",Biogeochemistry (Fourth Edition), Academic Press, pp. 483–508,doi:10.1016/b978-0-12-814608-8.00012-8,ISBN 978-0-12-814608-8, retrieved2024-03-08{{citation}}: CS1 maint: work parameter with ISBN (link)
  8. ^abcRosswall, T. (1982)."Microbiological regulation of the biogeochemical nitrogen cycle / Regulación microbiana del ciclo bíogeoquímico del nitrógeno".Plant and Soil.67 (1/3):15–34.doi:10.1007/BF02182752.ISSN 0032-079X.JSTOR 42934020.
  9. ^Barsdate, Robert J.; Alexander, Vera (January 1975)."The Nitrogen Balance of Arctic Tundra: Pathways, Rates, and Environmental Implications".Journal of Environmental Quality.4 (1):111–117.Bibcode:1975JEnvQ...4..111B.doi:10.2134/jeq1975.00472425000400010025x.ISSN 0047-2425.
  10. ^Nadelhoffer, Knute J.; Aber, John D.; Melillo, Jerry M. (1984-10-01)."Seasonal patterns of ammonium and nitrate uptake in nine temperate forest ecosystems".Plant and Soil.80 (3):321–335.Bibcode:1984PlSoi..80..321N.doi:10.1007/BF02140039.ISSN 1573-5036.
  11. ^Campbell, Neil A.; Reece, Jane B. (2002).Biology. Internet Archive. San Francisco : Benjamin Cummings.ISBN 978-0-8053-6624-2.{{cite book}}: CS1 maint: publisher location (link)
  12. ^Tiedje, J. M.; Sørensen, J.; Chang, Y.-Y. L. (1981)."Assimilatory and Dissimilatory Nitrate Reduction: Perspectives and Methodology for Simultaneous Measurement of Several Nitrogen Cycle Processes".Ecological Bulletins (33):331–342.ISSN 0346-6868.JSTOR 45128674.
  13. ^Llácer, José L; Fita, Ignacio; Rubio, Vicente (2008-12-01)."Arginine and nitrogen storage".Current Opinion in Structural Biology. Catalysis and regulation / Proteins.18 (6):673–681.doi:10.1016/j.sbi.2008.11.002.hdl:10261/111022.ISSN 0959-440X.PMID 19013524.
  14. ^Wang, Lixin; Macko, Stephen A. (March 2011)."Constrained preferences in nitrogen uptake across plant species and environments".Plant, Cell & Environment.34 (3):525–534.Bibcode:2011PCEnv..34..525W.doi:10.1111/j.1365-3040.2010.02260.x.ISSN 0140-7791.PMID 21118424.
  15. ^Hodge, Angela; Storer, Kate (2015-01-01)."Arbuscular mycorrhiza and nitrogen: implications for individual plants through to ecosystems".Plant and Soil.386 (1):1–19.Bibcode:2015PlSoi.386....1H.doi:10.1007/s11104-014-2162-1.ISSN 1573-5036.
  16. ^Raven, John A.; Linda, Bernd Wollenweber; Handley, L. (May 1992)."Ammonia and ammonium fluxes between photolithotrophs and the environment in relation to the global nitrogen cycle".New Phytologist.121 (1):5–18.Bibcode:1992NewPh.121....5R.doi:10.1111/j.1469-8137.1992.tb01087.x.ISSN 0028-646X.
  17. ^Bloom, A. J.; Jackson, L. E.; Smart, D. R. (March 1993)."Root growth as a function of ammonium and nitrate in the root zone".Plant, Cell & Environment.16 (2):199–206.Bibcode:1993PCEnv..16..199B.doi:10.1111/j.1365-3040.1993.tb00861.x.ISSN 0140-7791.
  18. ^Ackerman, Daniel; Millet, Dylan B.; Chen, Xin (January 2019)."Global Estimates of Inorganic Nitrogen Deposition Across Four Decades".Global Biogeochemical Cycles.33 (1):100–107.Bibcode:2019GBioC..33..100A.doi:10.1029/2018GB005990.ISSN 0886-6236.
  19. ^Dong, Junfu; Cui, Xiaoyong; Niu, Haishan; Zhang, Jing; Zhu, Chuanlu; Li, Linfeng; Pang, Zhe; Wang, Shiping (2022-06-20)."Effects of Nitrogen Addition on Plant Properties and Microbiomes Under High Phosphorus Addition Level in the Alpine Steppe".Frontiers in Plant Science.13.doi:10.3389/fpls.2022.894365.ISSN 1664-462X.PMC 9251499.PMID 35795351.
  20. ^Holleman, Arnold Frederik; Wiberg, Egon (2001), Wiberg, Nils (ed.),Inorganic Chemistry, translated by Eagleson, Mary; Brewer, William, San Diego/Berlin: Academic Press/De Gruyter,ISBN 0-12-352651-5
  21. ^abStevenson, D. J. (November 20, 1975). "Does metallic ammonium exist?".Nature.258 (5532):222–223.Bibcode:1975Natur.258..222S.doi:10.1038/258222a0.S2CID 4199721.
  22. ^abBernal, M. J. M.; Massey, H. S. W. (February 3, 1954)."Metallic Ammonium".Monthly Notices of the Royal Astronomical Society.114 (2):172–179.Bibcode:1954MNRAS.114..172B.doi:10.1093/mnras/114.2.172.
  23. ^Reedy, J.H. (October 1, 1929). "Lecture demonstration of ammonium amalgam".Journal of Chemical Education.6 (10): 1767.Bibcode:1929JChEd...6.1767R.doi:10.1021/ed006p1767.
Ammonium salts
Inorganic salts
monatomic anions
oxyanions
other anions
Organic salts
Molecules
Diatomic








Triatomic
Four
atoms
Five
atoms
Six
atoms
Seven
atoms
Eight
atoms
Nine
atoms
Ten
atoms
or more
Deuterated
molecules
Unconfirmed
Related
Nitrogen species
Hydrides
Organic
Oxides
Halides
Oxidation states
−3,−2,−1, 0,+1,+2,+3,+4,+5 (a stronglyacidic oxide)
National
Other
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