Mejillonesite, a new acid sodium, magnesium phosphate mineral, from Mejillones, Antofagasta, Chile


Autoria(s): Atencio, Daniel; Chukanov, Nikita V.; Nestola, Fabrizio; Witzke, Thomas; Coutinho, Jose Moacyr Vianna; Zadov, Aleksandr E.; Contreira Filho, Reynaldo R.; Faerber, Gunnar
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

23/08/2013

23/08/2013

2012

Resumo

Mejillonesite, ideally NaMg(2)(PO(3)OH)(PO(4))(OH)center dot H(5)O(2), is a new mineral approved by the CNMNC (IMA 2010-068). It occurs as isolated crystal aggregates in thin zones in fine-grained opal-zeolite aggregate on the north slope of Cerro Mejillones, Antofagasta, Chile. Closely associated minerals are bobierrite, opal, clinoptilolite-Na, clinoptilolite-K, and gypsum. Mejillonesite forms orthorhombic, prismatic, and elongated thick tabular crystals up to 6 mm long, usually intergrown in radiating aggregates. The dominant form is pinacoid {100}. Prisms {hk0}, {h0l}, and {0kl} are also observed. The crystals are colorless, their streak is white, and the luster is vitreous. The mineral is transparent. It is non-fluorescent under ultraviolet light. Mohs' hardness is 4, tenacity is brittle. Cleavage is perfect on {100}, good on {010} and {001}, and fracture is stepped. The measured density is 2.36(1) g/cm(3); the calculated density is 2.367 g/cm(3). Mejillonesite is biaxial (-), alpha= 1.507(2), beta= 1.531(2), gamma= 1.531(2), 2V(meas) = 15(10)degrees, 2V(calc) = 0 degrees (589 nm). Orientation is X= a, Z= elongation direction. The mineral is non-pleochroic. Dispersion is r> v, medium. The IR spectrum contains characteristic bands of the Zundel cation (H(5)O(2)(+), or H(+)center dot 2H(2)O) and the groups P-OH and OH(-). The chemical composition is (by EDS, H(2)O by the Alimarin method, wt%): Na(2)O 9.19, MgO 26.82, P(2)O(5) 46.87, H(2)O 19, total 101.88. The empirical formula, based on 11 oxygen atoms, is Na(0.93)Mg(2.08)(PO(3)OH)(1.00) (PO(4)) (OH)(0.86) .0.95H(5)O(2) The strongest eight X-ray powder-diffraction lines [d in angstrom(I)(hkl)] are: 8.095(100)(200), 6.846(9) (210), 6.470(8)(111), 3.317(5)(302), 2.959(5)(132), 2.706(12)(113), 2.157(19)(333), and 2.153(9) (622). The crystal structure was solved on a single crystal (R = 0.055) and gave the following data: orthorhombic, Pbca, a = 16.295(1), b = 13.009(2), c = 8.434(1) angstrom, V= 1787.9(4) angstrom(3), Z = 8. The crystal structure of mejillonesite is based on a sheet (parallel to the b-c plane) formed by two types of MgO(6) octahedra, isolated tetrahedra PO(4) and PO(3)OH whose apical vertices have different orientation with respect to the sheet. The sheets are connected by interlayer, 5-coordinated sodium ions, proton hydration complexes, and hydroxyl groups. The structure of mejillonesite is related to that of angarfite, NaFe(5)(3+)(PO(4))(4)(OH)(4).4H(2)O and bakhchisaraitsevite, Na(2)Mg(5)(PO(4))(4)center dot 7H(2)O.

Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)

FAPESP (Fundacao de Amparo a Pesquisa do Estado de Sao Paulo)

Russian Foundation for Basic Research [11-05-00407-a]

Russian Foundation for Basic Research

Identificador

AMERICAN MINERALOGIST, CHANTILLY, v. 97, n. 1, supl. 1, Part 4, pp. 19-25, JAN, 2012

0003-004X

http://www.producao.usp.br/handle/BDPI/32694

10.2138/am.2012.3867

http://dx.doi.org/10.2138/am.2012.3867

Idioma(s)

eng

Publicador

MINERALOGICAL SOC AMER

CHANTILLY

Relação

AMERICAN MINERALOGIST

Direitos

restrictedAccess

Copyright MINERALOGICAL SOC AMER

Palavras-Chave #MEJILLONESITE #NEW MINERAL #CHILE #PHOSPHATE #WATER CLUSTERS #RUSSIA #PROTON #BOND #GEOCHEMISTRY & GEOPHYSICS #MINERALOGY
Tipo

article

original article

publishedVersion