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Pb2(AsO2OH)Cl2, a new phase from the Lavrion ancient slags, Greece: occurrence and characterization

Published online by Cambridge University Press:  05 July 2018

O. I. Siidra*
Affiliation:
Department of Crystallography, Geological faculty, Saint Petersburg State University, University emb. 7/9, St Petersburg, 199034, Russia
N. V. Chukanov
Affiliation:
Institute of Problems of Chemical Physics, Chernogolovka, Moscow 142432, Russia
I. V. Pekov
Affiliation:
Faculty of Geology, Moscow State University, Vorob’evy Gory, GSP-2, Moscow 119992, Russia
S. V. Krivovichev
Affiliation:
Department of Crystallography, Geological faculty, Saint Petersburg State University, University emb. 7/9, St Petersburg, 199034, Russia
A. Magganas
Affiliation:
Department of Mineralogy and Petrology, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupolis 15784, Athens, Greece
A. Katerinopoulos
Affiliation:
Department of Mineralogy and Petrology, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupolis 15784, Athens, Greece
P. Voudouris
Affiliation:
Department of Mineralogy and Petrology, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupolis 15784, Athens, Greece

Abstract

Transparent prismatic crystals of Pb2(AsO2OH)Cl2 were collected in black metallurgical slag on the coast in the Punta Zeza area, 3 km south of the town of Lavrion, Greece. Analyses by energy-dispersive X-ray spectrometry (EDS) provided the following chemical composition: PbO 73.04, As2O3 15.97, Cl 11.42, O=Cl –2.58, total 97.85 wt.%. The empirical formula calculated on the basis of As = 1 is HxPb2.03(AsO3)1.00Cl1.995 (x = 0.96). The infrared spectrum of Pb2(AsO2OH)Cl2 has characteristic AsO33– bands at 707 and 594 cm–1, O–H stretching vibrations at 3310 and 2900 cm–1 and a band at 1107 cm–1 which is assigned to As–O–H bending vibrations. The structure, which is monoclinic P21/m, a = 6.4235(8), b = 5.5399(7), c = 9.321(1) Å, β = 90.767(2)°, V = 331.67(7) Å3, R1 = 0.035, is identical to that of synthetic Pb2(AsO2OH)Cl2 and contains two symmetrically unique Pb sites and one As site. The crystal structure is based on [Pb2AsO2OH]2+ double chains interconnected via weak Pb–Cl bonds to produce a three-dimensional framework which is closely related to that of Pb oxysalt minerals containing [O2Pb3]2+ chains of oxocentred [OPb4]6+ tetrahedra including mendipite, damaraite, rickturnerite and plumboselite.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2016

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