Synthesis and crystal
structures of Pd3Pb2Te2 and Pd3AgSe
F. Laufek1, A. Vymazalová1, M. Drábek1, J. Drahokoupil2, Chareev D.A.3, Kristavchuk A.V. 3
1Czech Geological Survey, Geologická 6, 152 00 Praha 5
2Institute of Physics of the AS CR, v.v.i., Na Slovance 2, 182 21 Praha 8
3Institute of Experimental Mineralogy RAS, Chernogolovka,
Russia
frantisek.laufek@geology.cz
This
presentation is a part of systematic research on crystal structures, phase
relations and selected physical properties of phases from Pd-Pb-Te and Pd-Ag-Se
ternary systems. These systems comprise many platinum-group minerals or phases,
which can be found in various ore deposits as potential new minerals.
Consequently, phases from these systems are of interest in mineralogy and geology
of ore deposits.
The ternary compounds Pd3Pb2Te2 and Pd3AgSe were synthesised from elements by conventional solid-state reactions. Stoichiometric amounts of individual elements were sealed in evacuated silica glass tubes and resultant mixtures were heated at selected temperatures. Samples with Pd3Pb2Te2 and Pd3AgSe were heated at 400°C and 350°C, respectively. After long-term annealing, the samples were quenched in a cold-water bath. All attempts to prepare single crystals of studied phases suitable for single-crystal analysis failed, the crystal structure determinations of Pd3Pb2Te2 and Pd3AgSe were performed from conventional powder X-ray diffraction data. The structure solutions of title compounds by direct methods were accomplished using the program EXPO2004 [1]; subsequent refinements were performed with FullProf program.
Pd3Pb2Te2: Space group Pmmn, a = 8.59, b = 5.93, c =
6.31 Å, V = 322 Å3 and Z = 2. Its crystal
structure can be described as a layered
structure formed by face-shared [PdPb4Te2] octahedra
running parallel to b axis. Two independent palladium atoms are
surrounded by four lead and two tellurium atoms showing distorted octahedral
coordination with tellurium atoms in trans positions with respect to one another. Two independent
lead atoms are coordinated by six palladium atom in two different ways. The
crystal structure of Pd3Pb2Te2 shows many structural similarities to the
structure of shandite (Ni3Pb2S2, Rm) and parkerite
(Ni3Bi2S2, C2/m). The phase Pd3Pb2Te2 was described
as a new mineral pašavaite [3].
Pd3AgSe: Space group Pa, a = 8.63 Å, V = 642 Å3 and Z = 8. The silver atom is surrounded
by 12 palladium atoms, 3 selenium atoms and 1 silver atom. 12 of these atoms (9
Pd and 3 Se) form a truncated tetrahedron (Fig. 1). The other atoms (3Pd + 1
Ag) are located slightly above the centers of hexagonal faces of truncated
tetrahedron. Two neighboring truncated tetrahedra share the hexagonal faces and
thus form a basic structural unit of the Pd3AgSe structure. Similarly, as was
mentioned for the isostructural Au3CaGa compound [4], the Pd3AgSe
structure show comparable local structural motives as quasicrystals.
Nevertheless, Pd3AgSe is a conventional crystalline compound.
Therefore, it can be viewed as an approximant of quasikrystal [5].
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Caliandro, M. Camalli, C. Cuocci, C. Giacovazzo, A. Moliterni. R. Rizzi, J.
Appl. Cryst., 37, (2004), 1025
2. J.
Rodríguez-Carvajal, FullProf.2k, Laboratoire
Léon Brillouin, France, 2006.
3.
A.
Vymazalová, F. Laufek, M. Drábek, J. Haloda, T. Sidorinová, Can. Mineral., 47,
(2009), 53.
4.
Q.
Lin, J. D. Corbett, Inorg. Chem., 47, (2008), 3462.
5.
Q.
Lin, J. D. Corbett, Struc. Bonding, 133 (2009), 1.
This study was supported by the internal project of the Czech Geological Survey (Project No. 332300).
Figure 1. Coordination of Ag atoms in crystal
structure of Pd3AgSe. Note the truncated
tetrahedron
formed by Pd and Se atoms. .