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Tobermorite

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Tobermorite
Crystalline mass of tobermorite
General
CategorySilicate mineral,
Calcium silicate hydrate
Formula
(repeating unit)
Ca5Si6O16(OH)2·4H2O, or;
Ca5Si6(O,OH)18·5H2O
Strunz classification9.DG.10
Crystal systemOrthorhombic
Crystal classDisphenoidal (222)
H-M symbol: (2 2 2)
Unit cella = 11.17 Å, b = 7.38 Å
c = 22.94 Å; β = 90°; Z = 4
Identification
Formula mass702.36 g/mol
ColorPale pinkish white, white, brown
Crystal habitAs minute laths; fibrous bundles, rosettes or sheaves, radiating or plumose, fine granular, massive.
Cleavage{001} Perfect, {100} Imperfect
Mohs scale hardness2.5
LusterVitreous, silky in fibrous aggregates
StreakWhite
DiaphaneityTranslucent to translucent
Specific gravity2.423 - 2.458
Optical propertiesBiaxial (+)
Refractive indexnα = 1.570 nβ = 1.571 nγ = 1.575
Birefringenceδ = 0.005
Ultraviolet fluorescenceFluorescent, Short UV:weak white to yellow, Long UV:weak white to yellow
References[1][2][3]
Not to be confused with torbernite, a hydrated copper uranyl phosphate.

Tobermorite is a calcium silicate hydrate mineral with chemical formula: Ca5Si6O16(OH)2·4H2O or Ca5Si6(O,OH)18·5H2O.

Two structural varieties are distinguished: tobermorite-11 Å and tobermorite-14 Å. Tobermorite occurs in hydrated cement paste and can be found in nature as alteration mineral in metamorphosed limestone and in skarn. It has been reported from the Maqarin Area of north Jordan and in the Crestmore Quarry near Crestmore Heights, Riverside County, California.

Tobermorite was first described in 1880 for an occurrence in Scotland, on the Isle of Mull, around the locality of Tobermory.[2]

Use in Roman concrete

Aluminium substituted tobermorite is understood to be a key ingredient in the longevity of ancient Roman undersea concrete, as per the American Ceramic Society.[4]

Crystal structure of tobermorite: elementary unit cell

See also

References

  • American Mineralogist (1954) 39, 1038.
  • Abdul-Jaber, Q.H.; Khoury, H. (1998), "Unusual mineralisation in the Maqarin Area (North Jordan) and the occurrence of some rare minerals in the marbles and the weathered rocks", Neues Jahrb. Geol. Paläontol. Abh., vol. 208, pp. 603–629 {{citation}}: |access-date= requires |url= (help)
  • Chen, Jeffrey J.; Jeffrey J. Thomas; Hal F.W. Taylor; Hamlin M. Jennings (2004). "Solubility and structure of calcium silicate hydrate". Cement and Concrete Research. 34 (9): 1499–1519. doi:10.1016/j.cemconres.2004.04.034. ISSN 0008-8846. Retrieved 2009-02-04.
  • Coleman, Nichola J. (2011). "11 Ä tobermorite ion exchanger from recycled container glass". International Journal of Environment and Waste Management. 8 (3–4): 366–382. doi:10.1504/IJEWM.2011.042642.
  • Currie, J. (1905). "Note on some new localities for gyrolite and tobermorite". Mineralogical Magazine. 14: 93–95. doi:10.1180/minmag.1905.014.64.06.
  • Eakle, Arthur S. (1927). "Famous mineral localities: Crestmore, Riverside County, California". American Mineralogist. 12: 319–321. Retrieved 2009-11-01.
  • Kikuma, J.; Tsunashima M.; Ishikawa T.; Matsuno S.; Ogawa A.; Matsui K.; Sato M. (2009). "Hydrothermal formation of tobermorite studied by in situ X-ray diffraction under autoclave condition". Journal of Synchrotron Radiation. 16: 683–686. doi:10.1107/s0909049509022080.
  • McConnell, J.D.C. (1954). "The hydrated calcium silicates riversideite, tobermorite and plombierite". Mineralogical Magazine. 30: 293–305. doi:10.1180/minmag.1954.030.224.02.
  • Merlino, S.; Bonaccorsi E.; Armbruster T. (1999). "Tobermorites: Their real structure and order-disorder (OD) character, Sample: 9 Angstrom". American Mineralogist. 84: 1613–1621.
  • Merlino, S.; Bonaccorsi E.; Armbruster T. (2001). "The real structure of tobermorite 11A: normal and anomalous forms, OD character and polytypic modifications (Note: MDO2 - synchrotron radiation source. Locality: Bascenov, Urals, Russia)". European Journal of Mineralogy. 13: 577–590. doi:10.1127/0935-1221/2001/0013-0577.
  • Naomichi, Hara (2000). "Formation of jennite and tobermorite from amorphous silica". J. Soc. Inorg. Mater. Japan. 7 (285): 133–142. ISSN 1345-3769. Retrieved 2009-02-04.