Tarbuttite

Tarbuttite
Tarbuttite from Broken Hill mine (Kabwe mine) in Central Province, Zambia
General
CategoryPhosphate minerals
FormulaZn2(PO4)(OH)
IMA symbolTbt[1]
Strunz classification8.BB.35
Dana classification41.6.7.1
Crystal systemTriclinic
Crystal classPinacoidal (1)
(same H-M symbol)
Space groupP1
Unit cella = 5.400 Å, b = 5.654 Å
c = 6.465 Å, α = 102.51°
β = 102.46°, γ = 86.50°
Z = 2[2]
Identification
ColorWhite, colorless, yellow, red, green, or brown
Crystal habitEquant to short prismatic [001], sheaf-like aggregates, crusts, individual crystals rounded and deeply striated
CleavagePerfect on {010}
FractureIrregular, uneven
Mohs scale hardness3.5
LusterVitreous, pearly on cleavages[2]
StreakWhite
DiaphaneityTransparent, translucent
Specific gravity4.12; 4.19 (calc.)
Density4.12 g/cm3 (measured)
Optical propertiesBiaxial (−)
Refractive indexnα = 1.660
nβ = 1.705
nγ = 1.713
Birefringenceδ = 0.053
2V angle50° (measured)
DispersionWeak,[3] strong[2]
Ultraviolet fluorescenceNon-fluorescent[4]
References[3]

Tarbuttite is a rare phosphate mineral with formula Zn2(PO4)(OH). It was discovered in 1907 in what is now Zambia and named for Percy Coventry Tarbutt.

Description and habit

Tarbuttite is white, yellow, red, green, brown, or colorless; in transmitted light it is colorless.[3] Traces of copper cause green coloring, while iron hydroxides cause the other colors. Colorless crystals tend to be transparent while colored specimens have varying degrees of transparency.[5]

The mineral occurs as equant to short prismatic crystals up to 2 cm (0.79 in), in sheaf-like or saddle-shaped aggregates, or as crusts.[2] Individual crystals are commonly rounded and striated.[3]

Structure

Zinc ions are surrounded by oxygen in a nearly perfect trigonal bipyramid and phosphate groups are tetrahedral. The crystal structure consists of zig-zag chains of Zn1 polyhedra linked by phosphate groups and pairs of Zn2 polyhedra. In each unit cell are two formula units of Zn2(PO4)(OH).[6]

History

Tarbuttite was discovered in 1907 in Broken Hill mine, Northern Rhodesia, (now Kabwe, Zambia).[3][7] The mineral was described from specimens in cellular limonite in the largest hill of the group, Kopje No. 2.[8][9] In a cave discovered in Kopje No. 1 by boring a tunnel,[7] tarbuttite was also found in association with hopeite as obscure crystals and crystals smaller than 116 mm (0.0025 in)[9] and as an encrustation on some bones.[10] Several specimens of the mineral were collected by Percy Coventry Tarbutt, a director of the Broken Hill Exploration Company.[5][8] In 1907, the name tarbuttite was proposed by L.J. Spencer in the journal Nature in honor of Tarbutt.[5]

When the International Mineralogical Association was founded, tarbuttite was grandfathered as a valid mineral species.[3]

Occurrence

Tarbuttite has been found in Algeria, Angola, Australia, Canada, China, Namibia, the United States, and Zambia.[2][3]

Tarbuttite forms as secondary mineral in oxidized zinc deposits. It has been found in association with cerussite, descloizite, hemimorphite, hopeite, hydrozincite, "limonite", parahopeite, pyromorphite, scholzite, smithsonite, and vanadinite.[2]

See also

References

  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 d e f "Tarbuttite" (PDF). Handbook of Mineralogy. Mineral Data Publishing. Archived from the original (PDF) on July 15, 2012. Retrieved July 13, 2012.
  3. ^ a b c d e f g "Tarbuttite". Mindat. Retrieved July 13, 2012.
  4. ^ "Tarbuttite". Webmineral. Retrieved July 13, 2012.
  5. ^ a b c Spencer, p. 22.
  6. ^ Cocco, p. 321.
  7. ^ a b Spencer, p. 1.
  8. ^ a b Spencer, p. 2.
  9. ^ a b Spencer, p. 30.
  10. ^ Spencer, p. 31.

Bibliography

Further reading

  • Richmond, Wallace E. (December 1938). "Tarbuttite" (PDF). American Mineralogist. 23 (12). Mineralogical Society of America: 881–893.

Wikimedia Commons logo Media related to Tarbuttite at Wikimedia Commons

Content Disclaimer

Informasi ini disarikan dari Wikipedia dan disajikan kembali untuk tujuan edukasi. Konten tersedia di bawah lisensi CC BY-SA 3.0. Kami tidak bertanggung jawab atas ketidakakuratan data yang bersumber dari kontribusi publik tersebut.

  1. The information displayed on this website is sourced in part or in whole from Wikipedia and has been adapted for the purpose of restating it. We strive to provide accurate and relevant information, however:
  2. There is no guarantee of absolute accuracy. Wikipedia is an open, collaborative project that can be edited by anyone, so information is subject to change.
  3. It is not intended to constitute professional advice. The content displayed is for informational and educational purposes only. For important decisions (e.g., medical, legal, or financial), please consult a professional.
  4. Content copyright. Wikipedia is licensed under the Creative Commons Attribution-ShareAlike License (CC BY-SA). This means that content may be reused with appropriate attribution and shared under a similar license.
  5. Responsible use. Any risk arising from the use of information from this website is entirely the responsibility of the user.