- Phosgenite
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Phosgenite
Crystal of phosgenite from the Monteponi Mine, Iglesias, Sardinia, Italy (size: 3.0 x 3.0 x 2.5 cm)General Category Carbonate minerals Chemical formula (PbCl)2CO3 Strunz classification 05.BE.20 Crystal symmetry Tetragonal (4/m 2/m 2/m) ditetragonal dipyramidal Unit cell a = 8.16Å, c = 8.883(6) Å; Z = 4 Identification Color Pale yellow to yellowish brown, pale brown, smoky brown, smoky violet; colorless, pale rose, gray, yellowish gray, pale green Crystal habit Short prismatic crystals, granular, massive Crystal system Tetragonal Cleavage Distinct on {001} and {110}, indistinct on {100} Fracture Conchoidal Tenacity Sectile, flexible perpendicular to {001} Mohs scale hardness 2 – 3 Luster Adamantine Streak White Diaphaneity Transparent to translucent Specific gravity 6.12 – 6.15 Optical properties Uniaxial (+); anomalously biaxial if strained Refractive index nω = 2.118 nε = 2.145 Birefringence δ = 0.027 Pleochroism Weakly pleochroic with O - reddish and E - greenish in thick sections. Ultraviolet fluorescence Fluoresces yellow under LW and SW UV Solubility Soluble in dilute nitric acid with effervescence, decomposes slowly in cold water References [1][2][3] Phosgenite is a rare mineral consisting of lead chlorocarbonate, (PbCl)2CO3. The tetragonal crystals are prismatic or tabular in habit: they are usually colorless and transparent, and have a brilliant adamantine lustre. Sometimes the crystals have a curious helical twist about the tetrad or principal axis. The hardness is 3 and the specific gravity 6.3. The mineral is rather sectile, and consequently was earlier known as corneous lead.
Name and occurrence
The name phosgenite was given by August Breithaupt in 1820, from phosgene, carbon oxychloride, because the mineral contains the elements carbon, oxygen and chlorine.
It was found associated with anglesite and matlockite in cavities within altered galena in a lead mine at Cromford, near Matlock: hence its common name cromfordite.[4] Crystals are also found in galena at Monteponi near Iglesias in Sardinia, and near Dundas in Tasmania. It has also been reported from Laurium, Greece; Tarnowitz, Poland; the Altai district, Siberia; the Touissit mine, near Oujda, Morocco; Sidi Amor ben Salem, Tunisia; Tsumeb, Namibia; Broken Hill, New South Wales; and Boleo, near Santa Rosalia, Baja California. In the US it has been reported from the Terrible mine, Custer County, Colorado; the Stevenson-Bennett mine, Organ Mountains, Dona Ana County, New Mexico; and the Mammoth mine, Tiger, Pinal County, Arizona.[1]
Crystals of phosgenite, and also of the corresponding bromine compound PbBr2CO3, have been prepared artificially.
References
- ^ a b Handbook of Mineralogy
- ^ Mindat.org
- ^ Webmineral data
- ^ "Phosgenite and Matlockite in Derbyshire (Part 1). T. Bridges, M.E. Smith. Journal of the Russell Society Volume 1, No. 2, p7-14, 1983 Retrieved on 2011-01-11
- This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press.
Categories:- Lead minerals
- Halide minerals
- Carbonate minerals
- Tetragonal minerals
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