Argentite: Difference between revisions
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[[Image:Argentite-unit-cell-3D-balls.png|thumb|The unit cell of '''argentite''']] |
[[Image:Argentite-unit-cell-3D-balls.png|thumb|The unit cell of '''argentite''']] |
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In [[mineral]]ogy, '''Argentite''' is [[Cubic crystal system|cubic]] [[silver sulfide]] (Ag<sub>2</sub>S), which can only exist at temperatures above 173 |
In [[mineral]]ogy, '''Argentite''' is [[Cubic crystal system|cubic]] [[silver sulfide]] (Ag<sub>2</sub>S), which can only exist at temperatures above 173 °C,<ref>[http://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Argentit Mineralienatlas Lexikon - Argentit (in German)]</ref> 177 °C<ref>[http://www.mindat.org/min-326.html] Argentite mindat.org:mineral information and data.</ref> or 179 °C.<ref>[http://www.webmineral.com/data/Argentite.shtml Argentite on Webmineral]</ref> When it cools to ordinary temperatures it turns into its [[monoclinic]] [[Polymorphism (materials science)|polymorph]], [[acanthite]].<ref>[http://www.mindat.org/min-326.html] Argentite mindat.org:mineral information and data.</ref><ref>[http://www.webmineral.com/data/Argentite.shtml Argentite on Webmineral]</ref> Argentite belongs to the [[galena]] group. |
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The name "argentite" sometimes also refers to [[pseudomorph]]s of argentite: specimens of acanthite which still display some of the outward signs of the cubic crystal form, even though their actual crystal structure is monoclinic due to the lower temperature.<ref>[http://www.mindat.org/min-326.html] Argentite mindat.org:mineral information and data.</ref><ref>[http://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Argentit Mineralienatlas Lexikon - Argentit (in German)]</ref> This form of acanthite is occasionally found as uneven [[cube]]s and [[octahedron|octahedra]], but more often as dendritic or earthy masses, with a blackish lead-grey color and metallic lustre{{sfn|Spencer|1911}} |
The name "argentite" sometimes also refers to [[pseudomorph]]s of argentite: specimens of acanthite which still display some of the outward signs of the cubic crystal form, even though their actual crystal structure is monoclinic due to the lower temperature.<ref>[http://www.mindat.org/min-326.html] Argentite mindat.org:mineral information and data.</ref><ref>[http://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Argentit Mineralienatlas Lexikon - Argentit (in German)]</ref> This form of acanthite is occasionally found as uneven [[cube]]s and [[octahedron|octahedra]], but more often as dendritic or earthy masses, with a blackish lead-grey color and metallic lustre{{sfn|Spencer|1911}} |
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Revision as of 18:56, 17 July 2014
In mineralogy, Argentite is cubic silver sulfide (Ag2S), which can only exist at temperatures above 173 °C,[1] 177 °C[2] or 179 °C.[3] When it cools to ordinary temperatures it turns into its monoclinic polymorph, acanthite.[4][5] Argentite belongs to the galena group.
The name "argentite" sometimes also refers to pseudomorphs of argentite: specimens of acanthite which still display some of the outward signs of the cubic crystal form, even though their actual crystal structure is monoclinic due to the lower temperature.[6][7] This form of acanthite is occasionally found as uneven cubes and octahedra, but more often as dendritic or earthy masses, with a blackish lead-grey color and metallic lustre[8]
cleavage, which is so prominent a feature in galena, here present only in traces. The mineral is perfectly sectile and has a shining streak; hardness 2.5, specific gravity 7.2-7.4. It occurs in mineral veins, and when found in large masses, as in is Mexico and in the Comstock Lode in Nevada, it forms an important ore of silver. The mineral was mentioned 1529 by G. Agricola, but the name argentite (from the Lat. argentum, silver) was not used till 1845 and is due to W. Haidinger. Old names for the species are Glaserz, silver-glance and vitreous silver. A related Cu-rich mineral occurring i.e. in Jalpa, Zacatecas, Mexico, is known as jalpaite.[8]
Rejection by the International Mineralogical Association
The International Mineralogical Association has decided to reject argentite as a proper mineral,[9] possibly due to its instability in normal air temperatures.[citation needed][10] Some people, including some past editors of this page, thus refer to it as a "discredited mineral species".[11]
External links
References
- ^ Mineralienatlas Lexikon - Argentit (in German)
- ^ [1] Argentite mindat.org:mineral information and data.
- ^ Argentite on Webmineral
- ^ [2] Argentite mindat.org:mineral information and data.
- ^ Argentite on Webmineral
- ^ [3] Argentite mindat.org:mineral information and data.
- ^ Mineralienatlas Lexikon - Argentit (in German)
- ^ a b Spencer 1911.
- ^ Argentite on Webmineral
- ^ Unsourced claim in a previous version of this page
- ^ Please browse the Wikipedia history of this page and its talk page to see who made this claim
(Note: Some references are repeated above to protect them against damage by an ill-conceived bot which compresses merged reference tags into a non-editable form).
- Attribution
- This article incorporates text from a publication now in the public domain: Spencer, Leonard James (1911). "Argentite". In Chisholm, Hugh (ed.). Encyclopædia Britannica (11th ed.). Cambridge University Press.
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