Aluminium chloride, also known asaluminium trichloride, is aninorganic compound with the formulaAlCl3. It forms ahexahydrate with the formula[Al(H2O)6]Cl3, containing sixwater molecules of hydration. Both the anhydrous form and the hexahydrate are colourless crystals, but samples are often contaminated withiron(III) chloride, giving them a yellow colour.
The anhydrous form is commercially important. It has a low melting and boiling point. It is mainly produced and consumed in the production of aluminium, but large amounts are also used in other areas of the chemical industry.[8] The compound is often cited as aLewis acid. It is aninorganic compound thatreversibly changes from apolymer to amonomer at mild temperature.
AlCl3 adopts three structures, depending on thetemperature and thestate (solid, liquid, gas). SolidAlCl3 has a sheet-like layered structure with cubic close-packed chloride ions. In this framework, the Al centres exhibitoctahedral coordination geometry.[9]Yttrium(III) chloride adopts the same structure, as do a range of other compounds. When aluminium trichloride is in its melted state, it exists as thedimer (Al2Cl6point group D2h), withtetracoordinate aluminium. This change in structure is related to the lower density of the liquid phase (1.78 g/cm3) versus solid aluminium trichloride (2.48 g/cm3).Al2Cl6 dimers are also found in thevapour phase. At higher temperatures, theAl2Cl6 dimersdissociate intotrigonal planarAlCl3monomer (point group D3h), which is structurally analogous toBF3. The meltconductselectricity poorly,[10] unlike moreionichalides such assodium chloride.
The hexahydrate consists ofoctahedral[Al(H2O)6]3+cation centers and chlorideanions (Cl−) ascounterions.Hydrogen bonds link the cation and anions.[11]The hydrated form of aluminium chloride has an octahedral molecular geometry, with the central aluminium ion surrounded by sixwater ligand molecules. Being coordinatively saturated, the hydrate is of little value as acatalyst inFriedel-Crafts alkylation and related reactions.
Thealkylation reaction is more widely used than theacylation reaction, although its practice is more technically demanding. For both reactions, the aluminium chloride, as well as other materials and the equipment, should be dry, although a trace of moisture is necessary for the reaction to proceed.[13] Detailed procedures are available for alkylation[14] and acylation[15][16] of arenes.
A general problem with the Friedel-Crafts reaction is that the aluminium chloride catalyst sometimes is required in fullstoichiometric quantities, because itcomplexes strongly with the products. This complication always generates a large amount ofcorrosive waste. For these and similar reasons, the use of aluminium chloride has rarely been displaced byzeolites.[8]
Anhydrous aluminium chloride ishygroscopic, having a very pronounced affinity for water. It fumes in moist air and hisses when mixed with liquid water as theCl− ligands are displaced withH2O molecules to form the hexahydrate[Al(H2O)6]Cl3. The anhydrous phase cannot be regained on heating the hexahydrate. Instead HCl is lost leaving aluminium hydroxide or alumina (aluminium oxide):
Aluminium chloride is manufactured on a large scale by theexothermic reaction ofaluminium metal with chlorine orhydrogen chloride at temperatures between 650 and 750 °C (1,202 and 1,382 °F).[10]
In the US in 1993, approximately 21,000 tons were produced, not counting the amounts consumed in the production of aluminium.[8]
Hydrated aluminium trichloride is prepared by dissolving aluminium oxides inhydrochloric acid. Metallic aluminium also readily dissolves in hydrochloric acid ─ releasing hydrogen gas and generating considerable heat. Heating this solid does not produce anhydrous aluminium trichloride, the hexahydrate decomposes toaluminium hydroxide when heated:
[Al(H2O)6]Cl3 → Al(OH)3 + 3 HCl + 3 H2O
Aluminium also forms a lowerchloride,aluminium(I) chloride (AlCl), but this is very unstable and only known in the vapour phase.[10]
Anhydrous aluminium chloride is not found as a mineral. The hexahydrate, however, is known as the rare mineral chloraluminite.[26] A more complex, basic and hydrated aluminium chloride mineral iscadwaladerite.[27][26]
Aluminium chlorides were known in the 18th century as muriate of alumina, marine alum, argillaceous marine salt,[28] muriated clay.[29] It was first chemically studied in the 1830s.[30]
^abcaluminium chloride in Linstrom, Peter J.; Mallard, William G. (eds.);NIST Chemistry WebBook, NIST Standard Reference Database Number 69, National Institute of Standards and Technology, Gaithersburg (MD)
^Wells AF (1984).Structural Inorganic Chemistry.Oxford, United Kingdom.: Oxford Press.ISBN0198553706.In contrast,AlBr3 has a more molecular structure, with theAl3+ centers occupying adjacent tetrahedral holes of the close-packed framework ofBr− ions.
^Andress KR, Carpenter C (1934). "Kristallhydrate II. Die Struktur von Chromchlorid- und Aluminiumchloridhexahydrat".Zeitschrift für Kristallographie – Crystalline Materials.87.doi:10.1524/zkri.1934.87.1.446.S2CID263857074.
^abcOlah GA, ed. (1963).Friedel-Crafts and Related Reactions. Vol. 1. New York City: Interscience.
^Nenitzescu CD, Cantuniari IP (1933). "Durch Aluminiumchlorid Katalysierte Reaktion, VI. Mitteil.: Die Umlagerung des Cyclohexans in Metyl-cyclopentan".Berichte der Deutschen Chemischen Gesellschaft (A and B Series).66 (8):1097–1100.doi:10.1002/cber.19330660817.ISSN1099-0682.
^Galatsis P (1999). "Aluminum Chloride". In Reich HJ, Rigby JH (eds.).Acidic and Basic Reagents. Handbook of Reagents for Organic Synthesis.New York City:Wiley. pp. 12–15.ISBN978-0-471-97925-8.
^Buchner B, Lockhart Jr LB (1951). "Phenyldichlorophosphine".Organic Syntheses.31: 88.doi:10.15227/orgsyn.031.0088.
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^Nawrocki S, Cha J (September 2019). "The etiology, diagnosis, and management of hyperhidrosis: A comprehensive review: Therapeutic options".Journal of the American Academy of Dermatology.81 (3):669–680.doi:10.1016/j.jaad.2018.11.066.PMID30710603.
^Mather WW (1835)."Chloride of Aluminium and its Analysis". In Silliman B (ed.).The American Journal of Science. Vol. 27. Kline Geology Laboratory, Yale University. pp. 241–253 (249).