Plumboagardite, a new mineral of the mixite group from an occurrence in the Southern Black Forest, Germany

Authors: Walenta, Kurt; Theye, Thomas

Source: Neues Jahrbuch für Mineralogie - Abhandlungen, Volume 181, Number 3, June 2005 , pp. 219-222(4)

Publisher: E. Schweizerbart'sche Verlagsbuchhandlung

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Abstract:

Plumboagardite occurs among the secondary minerals of the mine Aitern Süd in the Southern Black Forest, Baden-Württemberg, Germany, in association with quartz, fluorite, chrysocolla and limonite.

It forms spherulitic aggregates of radial fibrous structure on chrysocolla composed of acicular crystals elongated [0001] and reaching 0,05 mm in length. Colour green, streak greenish, lustre vitreous, no distinct cleavage, hardness 3, density (calc.) 3.741g/cm3. Optical properties: nomega 1.726 (5), nepsi 1.805 (5), uniaxial (+).

Unit-cell dimensions of the hexagonal mineral: a 13.77(2), c 5.94 (1), Z = 2, space group P63/m. Strongest lines of the powder pattern: 12.01 (10) 1010, 4.51 (6) 2130, 1121, 3.60 (8), 2131, 2.98 (6) 4040, 2241, 0002, 2.49 (7) 3251, 3142. Chemical composition (wt.%): PbO 8.99, La2O3 1.91, Nd2O3 1.17, Ce2O3 0.96, Sm2O3 0.20, Pr2O3 0.19, Gd2O3 0,17, Dy2O3 0.10, Y2O3 0.96, CaO 1.44, CuO 40.49, Fe2O3 1.54, As2O5 29.74, P2O5 0.30, SiO2 1.46, H2O (by difference) 10.38, total 100.00%. The empirical formula – based on 12 O + 6 OH structural anions – is: [Pb0.44(La0.13Y0.09Nd0.08Ce0.06Pr0.01Sm0.01Gd0.01Dy0.01)SigmaREE = 0.40Ca0.28]Sigma = 1.12(Cu5.59Fe0.21)Sigma = 5.80(As2.84Si0.27P0.05)Sigma = 3.16O12(OH)6 · 3.33H2O simplified (Pb,REE,Ca)Cu6(AsO4)3(OH)6 · 3H2O. The mineral is easily soluble in dilute HCl and HNO3.
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