Brandãoite, [BeAl2(PO4)2(OH)2(H2O)4](H2O), a new Be–Al phosphate mineral from the João Firmino mine, Pomarolli farm region, Divino das Laranjeiras County, Minas Gerais State, Brazil: description and crystal structure. (29th June 2018)

• Record Type: Journal Article
• Authors: Menezes Filho, Luiz A. D.; Chaves, Mário L. S. C.; Cooper, Mark A.; Ball, Neil A.; Abdu, Yassir A.; Sharpe, Ryan; Day, Maxwell C.; Hawthorne, Frank C.
• Is Part Of: Mineralogical magazine. Volume 83:Number 2(2019)
• Page Start: 261
• Page End: 267
• Publication Date: 2018-06-29
• Subjects: brandãoite, -- new mineral, -- chemical analysis, -- beryllium phosphate, -- crystal structure, -- infrared spectrum, -- Minas Gerais State, -- Brazil; Mineralogy -- Periodicals; Mineralogy -- Great Britain -- Periodicals; 549.05
• DOI: 10.1180/mgm.2018.121
• Languages: English
• ISSNs: 0026-461X

Abstract

Abstract: Brandãoite, [BeAl2 (PO4 )2 (OH)2 (H2 O)4 ](H2 O), is a new Be–Al phosphate mineral from the João Firmino mine, Pomarolli farm region, Divino das Laranjeiras County, Minas Gerais State, Brazil, where it occurs in an albite pocket with other secondary phosphates, including beryllonite, atencioite and zanazziite, in a granitic pegmatite. It occurs as colourless acicular crystals <10 µm wide and <100 µm long that form compact radiating spherical aggregates up to 1.0–1.5 mm across. It is colourless and transparent in single crystals and white in aggregates, has a white streak and a vitreous lustre, is brittle and has conchoidal fracture. Mohs hardness is 6, and the calculated density is 2.353 g/cm 3 . Brandãoite is biaxial (+), α = 1.544, β = 1.552 and γ = 1.568, all ± 0.002; 2Vobs = 69.7(10)° and 2Vcalc = 71.2°. No pleochroism was observed. Brandãoite is triclinic, space group P $\bar{1}$, a = 6.100(4), b = 8.616(4), c = 10.261(5) Å, α = 93.191(11), β = 95.120(11), γ = 96.863(11)°, V = 532.1(8) Å 3 and Z = 2. Chemical analysis of a 4 µm wide needle-shaped crystal by electron microprobe and secondary-ion mass spectrometry gave P2 O5 = 28.42, Al2 O3 = 20.15, BeO = 4.85, H2 O = 21.47 and sum = 74.89 wt.%. The empirical formula, normalised on the basis of 15 anions pfu with (OH) = 2 and (H2 O) = 5 apfu (from the crystal structure) is Be0.98 Al1.99 P2.02 H12 O15 . The crystal structure was solved by direct methods and refined to an R 1 index of 7.0%. There are two P sites occupied by P 5+, two Al sites occupied by octahedrally coordinated Al 3+, and one Be site occupied by tetrahedrally coordinated Be 2+ . There are fifteen anions, two of which are (OH) groups and five of which are (H2 O) groups. The simplified ideal formula is thus [BeAl2 (PO4 )2 (OH)2 (H2 O)4 ](H2 O) with Z = 2. Beryllium and P tetrahedra share corners to form a four-membered ring. Aluminium octahedra share a common vertex to form an [Al2 φ11 ] dimer, and these dimers are cross-linked by P tetrahedra to form a complex slab of polyhedra parallel to (001). These slabs are cross-linked by BeO2 (OH)(H2 O) tetrahedra, with interstitial (H2 O) groups in channels that extend along [100].