Witzkeite: A new rare nitrate-sulphate mineral from a guano deposit at Punta de Lobos, Chile


Autoria(s): Nestola, Fabrizio; Camara, Fernando; Chukanov, Nikita V.; Atencio, Daniel; Coutinho, Jose Moacyr Vianna; Contreira Filho, Reynaldo R.; Faerber, Gunnar
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

06/11/2013

06/11/2013

2012

Resumo

Witzkeite, ideally Na4K4Ca(NO3)(2)(SO4)(4)center dot 2H(2)O, is a new mineral found in the oxidation zone of the guano mining field at Punta de Lobos, Tarapaca region, Chile. It occurs as colorless, tabular crystals up to 140 mu m in length, associated with dittmanite and nitratine. Witzkeite is colorless and transparent, with a white streak and a vitreous luster. It is brittle, with Molts hardness 2 and distinct cleavage on {001}. Measured density is 2.40(2) g/cm(3), calculated density is 2.403 g/cm(3). Witzkeite is biaxial (-) with refractive indexes alpha = 1.470(5), beta = 1.495(5), gamma = 1.510(5), measured 2V = 50-70 degrees. The empirical composition is (electron microprobe, mean of five analyses, H2O, CO2, and N2O5 by gas chromatography; wt%): Na2O 12.83, K2O 22.64, CaO 7.57, FeO 0.44, SO3 39.96, N2O5 12.7, H2O 4.5, total 100.64; CO2 was not detected. The chemical formula, calculated based on 24 O, is: Na3.40K3.95Ca1.11Fe0.05(NO3)(1.93)(SO4)(4.10)(H4.10O1.81). Witzkeite is monoclinic, space group C2/c, with unit-cell parameters: a = 24.902(2), b = 5.3323(4), c = 17.246(1) angstrom, beta = 94.281(7)degrees, V = 2283.6(3) angstrom(3) (Z = 4). The crystal structure was solved using single-crystal X-ray diffraction data and refined to R-1(F) = 0.043. Witzkeite belongs to a new structure type and is noteworthy for the very rare simultaneous presence of sulfate and nitrate groups. The eight strongest X-ray powder-diffraction lines [d in angstrom (I in %) (h k l)] are: 12.38 (100) (2 0 0), 4.13 (19) (6 0 0), 3.10 (24) (8 0 0), 2.99 (7) ((8) over bar 02), 2.85 (6) (8 02), 2.69 (9) ((7) over bar 1 3), 2.48 (12) (10 0 0), and 2.07 (54) (12 0 0). The IR spectrum of witzkeite was collected in the range 390-4000 cm(-1). The spectrum shows the typical bands of SO42- ions (1192, 1154, 1116, 1101, 1084, 993, 634, and 617 cm(-1)) and of NO3- ions (1385, 1354, 830, 716, and 2775 cm(-1)). Moreover, a complex pattern of bands related to H2O is visible (bands at 3565, 3419, 3260, 2405, 2110, 1638, and 499 cm(-1)). The IR spectrum is discussed in detail.

University of Padova

University of Padova

Russian Foundation for Basic Research [11-05-00407-a, 11-05-00397-a]

Russian Foundation for Basic Research

FAPESP (Fundacao de Amparo Pesquisa do Estado de Sao Paulo) [2009/09125-5]

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

Identificador

AMERICAN MINERALOGIST, CHANTILLY, v. 97, n. 10, supl. 1, Part 4, pp. 1783-1787, OCT, 2012

0003-004X

http://www.producao.usp.br/handle/BDPI/42093

10.2138/am.2012.4109

http://dx.doi.org/10.2138/am.2012.4109

Idioma(s)

eng

Publicador

MINERALOGICAL SOC AMER

CHANTILLY

Relação

AMERICAN MINERALOGIST

Direitos

restrictedAccess

Copyright MINERALOGICAL SOC AMER

Palavras-Chave #WITZKEITE #NEW MINERAL #GUANO #CRYSTAL STRUCTURE #SULFATE #NITRATE #IR SPECTROSCOPY #GEOCHEMISTRY & GEOPHYSICS #MINERALOGY
Tipo

article

original article

publishedVersion