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{{Infobox mineral
[[Image:Mineraly.sk - hauerit.jpg|right|thumb|250px|A sample of Hauerite]]
| name = Hauerite
'''Hauerite''' is a [[manganese]] [[sulfide]] mineral with the [[chemical formula]] [[manganese|Mn]][[sulfur|S]]<sub>2</sub>. It forms reddish brown or black octahedral [[crystal]]s and it is usually found associated with the sulfides of other transition metals such as [[rambergite]].
| boxwidth =
| boxbgcolor =
| image = Hauerite-mun05-64a.jpg
| imagesize = 260px
| alt =
| caption =
| category = [[Sulfide mineral]], [[pyrite group]]
| formula = MnS<sub>2</sub>
| IMAsymbol = Hr<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 = 119.07 g/mol
| strunz = 2.EB.05a
| dana =
| system = [[Cubic crystal system|Cubic]]
| class = Diploidal (m{{overline|3}}) <br/>[[H–M symbol]]: (2/m {{overline|3}})
| symmetry = ''Pa''{{overline|3}}
| unit cell = a = 6.107&nbsp;Å; Z&nbsp;=&nbsp;4
| color = Reddish brown or brownish black
| colour =
| habit = Octahedral crystals and globular aggregates
| twinning =
| cleavage = {100} Perfect, {010} Perfect, Perfect on {001}
| fracture = Uneven to subconchoidal
| tenacity = Brittle
| mohs = 4
| luster = Metallic-adamantine
| streak = Reddish brown
| diaphaneity = Opaque to subtranslucent
| gravity = 3.463
| density =
| polish =
| opticalprop = Isotropic
| refractive = n = 2.69
| birefringence =
| pleochroism =
| 2V =
| dispersion =
| extinction =
| length fast/slow =
| fluorescence =
| absorption =
| melt =
| fusibility =
| diagnostic =
| solubility =
| impurities =
| alteration =
| other =
| prop1 =
| prop1text =
| references = <ref name=HBM>{{cite web |last1=Anthony |first1=John W. |last2=Bideaux |first2=Richard A. |last3=Bladh |first3=Kenneth W. |last4=Nichols |first4=Monte C. |title=Hauerite |url=http://www.handbookofmineralogy.org/pdfs/hauerite.pdf |website=Handbook of Mineralogy |publisher=Mineral Data Publishing |access-date=1 August 2022 |date=2005}}</ref><ref name=Webmin>{{Cite web|last1=Barthelmy|first1=David|year=2014|url=http://www.webmineral.com/data/Hauerite.shtml|access-date=1 August 2022|title = Hauerite Mineral Data|website=Webmineral.com}}</ref><ref name=Mindat>{{mindat|id=1831|title=Hauerite|access-date=1 August 2022}}</ref>
}}


'''Hauerite''' is a [[manganese]] [[sulfide]] mineral with the [[chemical formula]] [[manganese|Mn]][[sulfur|S]]<sub>2</sub>. It forms reddish brown or black octahedral [[crystal]]s with the [[pyrite]] structure and it is usually found associated with the sulfides of other transition metals such as [[rambergite]]. It occurs in low temperature, sulfur rich environments associated with [[solfatara]]s and salt deposits in association with [[native sulfur]], [[realgar]], [[gypsum]] and [[calcite]].<ref name=HBM/>
It was discovered in [[Austria]] in 1846 and named after the Austrian geologists, Joseph Ritter von Hauer (1778–1863) and Franz Ritter von Hauer (1822–1899).<ref>http://www.handbookofmineralogy.org/pdfs/hauerite.pdf Handbook of Mineralogy</ref><ref>http://www.webmineral.com/data/Hauerite.shtml Webmineral</ref><ref>http://www.mindat.org/min-1831.html mindat</ref>

It was discovered in [[Austro-Hungarian Monarchy]] in Kalinka (now [[Vígľašská Huta-Kalinka]] village) sulfur deposit near Detva in what is now [[Slovakia]] in 1846 and named after the Austrian geologists, [[Joseph Ritter von Hauer]] (1778–1863) and [[Franz Ritter von Hauer]] (1822–1899).<ref name=HBM/><ref name=Mindat/>

It is found in Texas, US; the Ural Mountains of Russia, and Sicily, Italy.<ref>{{Cite book |last= |first= |title=Rocks and Minerals |publisher=[[DK publishers]] |year=2012 |isbn=978-1-4093-8659-9 |editor-last=Star |editor-first=Fleur}}</ref>

Under high pressure conditions (P>11 GPa), Hauerite undergoes a large collapse in unit cell volume (22%) driven by a spin-state transition.<ref>[http://www.pnas.org/content/111/14/5106.abstract Kimber, S.A.J., et al., ''Giant pressure-induced volume collapse in the pyrite mineral MnS<sub>2</sub>,'' PNAS, April 8, 2014, vol. 111, no. 14, pp. 5106–5110]</ref>


==References==
==References==
{{Reflist}}
{{Reflist}}


{{Commons}}

{{Manganese minerals}}
{{Manganese minerals}}


[[Category:Manganese minerals]]
[[Category:Manganese minerals]]
[[Category:Sulfide minerals]]
[[Category:Pyrite group]]
[[Category:Pyrite group]]
[[Category:Cubic minerals]]
{{sulfide-mineral-stub}}
[[Category:Minerals in space group 205]]
[[Category:Minerals described in 1846]]


{{sulfide-mineral-stub}}
[[ca:Hauerita]]
[[it:Hauerite]]
[[nl:Haueriet]]
[[sk:Hauerit]]

Latest revision as of 21:55, 10 January 2024

Hauerite
General
CategorySulfide mineral, pyrite group
Formula
(repeating unit)
MnS2
IMA symbolHr[1]
Strunz classification2.EB.05a
Crystal systemCubic
Crystal classDiploidal (m3)
H–M symbol: (2/m 3)
Space groupPa3
Unit cella = 6.107 Å; Z = 4
Identification
Formula mass119.07 g/mol
ColorReddish brown or brownish black
Crystal habitOctahedral crystals and globular aggregates
Cleavage{100} Perfect, {010} Perfect, Perfect on {001}
FractureUneven to subconchoidal
TenacityBrittle
Mohs scale hardness4
LusterMetallic-adamantine
StreakReddish brown
DiaphaneityOpaque to subtranslucent
Specific gravity3.463
Optical propertiesIsotropic
Refractive indexn = 2.69
References[2][3][4]

Hauerite is a manganese sulfide mineral with the chemical formula MnS2. It forms reddish brown or black octahedral crystals with the pyrite structure and it is usually found associated with the sulfides of other transition metals such as rambergite. It occurs in low temperature, sulfur rich environments associated with solfataras and salt deposits in association with native sulfur, realgar, gypsum and calcite.[2]

It was discovered in Austro-Hungarian Monarchy in Kalinka (now Vígľašská Huta-Kalinka village) sulfur deposit near Detva in what is now Slovakia in 1846 and named after the Austrian geologists, Joseph Ritter von Hauer (1778–1863) and Franz Ritter von Hauer (1822–1899).[2][4]

It is found in Texas, US; the Ural Mountains of Russia, and Sicily, Italy.[5]

Under high pressure conditions (P>11 GPa), Hauerite undergoes a large collapse in unit cell volume (22%) driven by a spin-state transition.[6]

References[edit]

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ a b c Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C. (2005). "Hauerite" (PDF). Handbook of Mineralogy. Mineral Data Publishing. Retrieved 1 August 2022.
  3. ^ Barthelmy, David (2014). "Hauerite Mineral Data". Webmineral.com. Retrieved 1 August 2022.
  4. ^ a b Hauerite, Mindat.org, retrieved 1 August 2022
  5. ^ Star, Fleur, ed. (2012). Rocks and Minerals. DK publishers. ISBN 978-1-4093-8659-9.
  6. ^ Kimber, S.A.J., et al., Giant pressure-induced volume collapse in the pyrite mineral MnS2, PNAS, April 8, 2014, vol. 111, no. 14, pp. 5106–5110