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Gibbsite
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{{short description|Form of aluminium hydroxide, mineral}} {{Infobox mineral | name = Gibbsite | boxwidth = | boxbgcolor = | image = Gibbsite-fiu14a.jpg | imagesize = | alt = | caption = Gibbsite | category = [[Hydroxide minerals]] | formula = Al(OH)<sub>3</sub> | IMAsymbol = Gbb<ref>{{Cite journal|last=Warr|first=L.N.|date=2021|title=IMA–CNMNC approved mineral symbols|journal=Mineralogical Magazine|volume=85|issue=3|pages=291–320|doi=10.1180/mgm.2021.43|bibcode=2021MinM...85..291W|s2cid=235729616|doi-access=free}}</ref> | molweight = | strunz = 4.FE.10 | dana = | system = [[Monoclinic]] | class = Prismatic (2/m) <br/><small>(same [[H-M symbol]])</small> | symmetry = ''P2''<sub>1</sub>/n | unit cell = | color = | colour = | habit = | twinning = | cleavage = | fracture = | tenacity = | mohs = 2.5–3 | luster = | streak = | diaphaneity = | gravity = 2.35 | density = | polish = | opticalprop = | refractive = | birefringence = | pleochroism = | 2V = | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | prop1 = | prop1text = | references = }} [[Image:Gibbsite-crystal-3D-balls.png|thumb|right|[[Ball-and-stick model]] of the part of the [[crystal structure]] of gibbsite]] <!-- [[File:Gibbsite-270400.jpg|thumb|upright|An unusual specimen of Gibbsite from [[Linwu County]], [[Hunan Province]], China. Size: 9.1 x 4.6 x 4.4 cm.]] --> '''Gibbsite''', Al(OH)<sub>3</sub>, is one of the mineral forms of [[aluminium hydroxide]]. It is often designated as γ-Al(OH)<sub>3</sub><ref name=":0" />{{rp| 2}} (but sometimes as α-Al(OH)<sub>3</sub><ref>N.N. Greenwood and A. Earnshaw, "Chemistry of Elements", 2nd edition, Butterworth and Heinemann, 1997</ref>). It is also sometimes called '''hydrargillite''' (or '''hydrargyllite'''). Gibbsite is an important ore of [[aluminium]] in that it is one of three main [[phase (matter)|phases]] that make up the rock [[bauxite]]. Gibbsite has three named structural [[polymorphism (materials science)|polymorphs]] or [[polytype]]s: '''bayerite''' (designated often as α-Al(OH)<sub>3</sub>,<ref name=":0" />{{rp| 2}} but sometimes as β-Al(OH)<sub>3</sub>){{Citation needed|date=October 2020}}, ''[[doyleite]]'', and '''nordstrandite'''. Gibbsite can be [[monoclinic]] or [[Triclinic crystal system|triclinic]], while bayerite is monoclinic.<ref name=":0">{{Cite book|last1=Wefers|first1=Karl|url=http://worldcat.org/oclc/894928306|title=Oxides and hydroxides of aluminum|last2=Misra|first2=Chanakya|date=1987|publisher=Alcoa Research Laboratories|oclc=894928306}}</ref>{{rp| 13}} Doyleite and nordstrandite are triclinic forms.<ref name=":0" />{{rp|13}}
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