Huttonite

Huttonite is a thorium nesosilicate mineral with the chemical formula ThSiO4 and which crystallizes in the monoclinic system. It is dimorphous with tetragonal thorite, and isostructual with monazite. An uncommon mineral, huttonite forms transparent or translucent cream–colored crystals. It was first identified in samples of beach sands from the West Coast region of New Zealand by the mineralogist Colin Osborne Hutton (1910–1971).[4] Owing to its rarity, huttonite is not an industrially useful mineral.

Huttonite
Unit cell of huttonite
General
CategorySilicate mineral
Formula
(repeating unit)		ThSiO4
Strunz classification9.AD.35
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupP21/n
Unit cella = 6.77 Å, b = 6.96 Å
c = 6.49 Å; β = 104.99°; Z = 4
Identification
Formula mass324.12 g/mol
ColorColorless, cream, pale yellow
Crystal habitPrismatic, flattened; typically as anhedral grains
CleavageDistinct along [001], indistinct along [100]
FractureConchoidal
Mohs scale hardness4.5
LusterAdamantine
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity7.1
Optical propertiesBiaxial (+)
Refractive indexnα = 1.898, nβ = 1.900, nγ = 1.922
Birefringenceδ = 0.0240
2V angle25°
Dispersionr < v (moderate)
Ultraviolet fluorescenceDull white (under shortwave)
Other characteristics Radioactive
References[1][2][3]

Occurrence

Huttonite was first described in 1950 from beach sand and fluvio-glacial deposits in South Westland, New Zealand, where it was found as anhedral grains of no more than 0.2 mm maximum dimension. It is most prevalent in the sand at Gillespie's Beach, near Fox Glacier,[4][5] which is the type location, where it is accompanied by scheelite, cassiterite, zircon, uranothorite, ilmenite and gold. It was found at a further six nearby locations in less plentiful amounts.[6] Huttonite was extracted from the sands by first fractionating in iodomethane and then electromagnetically. Pure samples were subsequently obtained by handpicking huttonite grains under a microscope. This was accomplished either in the presence of short wave (2540 Å) fluorescent light, where the dull white fluorescence distinguishes it from scheelite (fluoresces blue) and zircon (fluoresces yellow), or by first boiling the impure sample in hydrochloric acid to induce an oxide surface on scheelite and permitting handpicking under visible light.[6]

Hutton suggested the huttonite contained in the beach sand and fluvio-glacial deposits originated from Otago schists or pegmatitic veins in the Southern Alps.[6]

In addition to New Zealand, huttonite has been found in granitic pegmatites of Bogatynia, Poland,[7] where it associated with cheralite, thorogummite, and ningyoite; and in nepheline syenites of Brevik, Norway.[8]

Physical properties

Huttonite typically occurs as anhedral grains with no external crystal faces. It is usually colorless but also appears in colors; such as cream and pale yellow. It has a white streak. It has a hardness of 4.5 and exhibits distinct cleavage parallel to the c-axis [001] and an indistinct cleavage along the a-axis [100].

Structure

Huttonite is a thorium nesosilicate with the chemical formula ThSiO4. It is composed (by weight) of 71.59% thorium, 19.74% oxygen, and 8.67% silicon. Huttonite is found very close to its ideal stoichiometric composition, with impurities contributing less than 7% mole fraction. The most significant impurities to be observed are UO2 and P2O5.[9]

Atomic environment along a SiO4–ThO5 chain (parallel to the c axis)

Huttonite crystallizes in the monoclinic system with space group P21/n. The unit cell contains four ThSiO4 units, and has dimensions a = 6.784 ± 0.002Å, b = 6.974 ± 0.003Å, c = 6.500 ± 0.003Å, and inter–axis angle β = 104.92 ± 0.03o. The structure is that of a nesosilicate — discrete SiO42− tetrahedra coordinating thorium ions. Each thorium has coordination number nine. Axially, four oxygen atoms, representing the edges of two SiO4 monomers on opposite sides of the thorium atom, form a (–SiO4–Th–) chain parallel to the c axis. Equatorially, five nearly planar oxygen atoms representing vertices of distinct silicate tetrahedra coordinate each thorium. The lengths of the axial Th–O bonds are 2.43 Å, 2.51 Å, 2.52 Å, 2.81 Å, and of the equatorial bonds, 2.40 Å, 2.41 Å, 2.41 Å, 2.50 Å, and 2.58 Å. The Si–O bonds are nearly equal, with lengths 1.58 Å, 1.62 Å, 1.63 Å, and 1.64 Å.[10]

Huttonite is isostructural with monazite. Substitution of the rare-earth elements and phosphorus of monazite with thorium and silicon of huttonite can occur to generates a solid solution. At the huttonite end-member, continuous rare-earth substitution of thorium of up to 20% by weight has been observed. Thorium substitution in monazite has been observed up to 27% by weight. Substitution of PO4 for SiO4 also occurs associated with the introduction of fluoride, hydroxide, and metal ions.[11]

Huttonite is dimorphic with thorite. Thorite crystallizes in a higher symmetry and lower density tetragonal form in which the thorium atoms coordinate to one less oxygen atom in an octahedral arrangement. Thorite is stable at lower temperatures than huttonite; at 1 atmosphere, the thorite–huttonite phase transition occurs between 1210 and 1225 °C. With increasing pressure the transition temperature increases. This relatively high transition temperature is thought to explain the relative rarity of huttonite on the Earth's crust.[12] Unlike thorite, huttonite is not affected by metamictization.

References
  1. Anthony, John W.; Richard A. Bideaux; Kenneth W. Bladh; Monte C. Nichols (1995). Handbook of Mineralogy: Silica, Silicates (PDF). Tucson, Arizona: Mineral Data Publishing. ISBN 978-0-9622097-1-0.
  2. "Huttonite Mineral Data". WebMineral.com. Retrieved 2008-12-13.
  3. Mindat.org
  4. Pabst, A. (1950). "Monoclinic Thorium Silicate". Nature. 166 (4212): 157. Bibcode:1950Natur.166..157P. doi:10.1038/166157a0. PMID 15439198.
  5. Pabst, A.; C. Osborne Hutton (1951). "Huttonite, a new monoclinic thorium silicate" (PDF). Am. Mineral. 36: 60–69.
  6. Hutton, C. Osborne (1951). "Occurrence, optical properties and chemical composition of huttonite" (PDF). Am. Mineral. 36 (1): 66–69.
  7. Kucha, H (1980). "Continuity in the monazite–huttonite series". Mineralogical Magazine. 43 (332): 1031–1034. Bibcode:1980MinM...43.1031K. doi:10.1180/minmag.1980.043.332.12.
  8. Meldrum, A., Boatner, L.A., Zinkle, S.J., Wang, S.-X., Wang, L.-M., and Ewing, R.C. (1999). "Effects of dose rate and temperature on the crystalline–to–metamict transformation in the ABO4 orthosilicates". Canadian Mineralogist. 37: 207–221.CS1 maint: multiple names: authors list (link)
  9. Förster H. J., Harlov D. E., Milke R., H.-J.; Harlov, D. E.; Milke, R. (2000). "Composition and Th –U –total Pb ages of huttonite and thorite from Gillespie's Beach,. South Island, New Zealand". The Canadian Mineralogist. 38 (3): 675–684. CiteSeerX 10.1.1.579.7465. doi:10.2113/gscanmin.38.3.675.CS1 maint: multiple names: authors list (link)
  10. Taylor, Mark; Ewing, R. C. (1978). "The Crystal Structures of the ThSiO4 Polymorphs: Huttonite and Thorite". Acta Crystallogr. B. 34 (4): 1074–1079. doi:10.1107/S0567740878004951.
  11. Kucha, Henryk (1980). "Continuity in the monazite–huttonite series". Mineralogical Magazine. 43 (332): 1031–1034. Bibcode:1980MinM...43.1031K. doi:10.1180/minmag.1980.043.332.12.
  12. Speer, J. A. (1980). "The actinide orthosilicates". Reviews in Mineralogy and Geochemistry. 5 (1): 113–135.
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