4.1 Article

The Phosphidosilicates SrSi7P10 and BaSi7P10

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WILEY-V C H VERLAG GMBH
DOI: 10.1002/zaac.202000296

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Phosphidosilicates; Alkaline earth; Supertetrahedra; Semiconductors; Bandgap

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  1. Deutsche Forschungsgemeinschaft (DFG)

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The new phosphidosilicates SrSi7P10 and BaSi7P10 were synthesized and their crystal structures determined. They exhibit a new triclinic structure type with vertex sharing SiP4 tetrahedra and alkaline earth cations residing in cuboctahedral voids. Both compounds are classified as semiconductors with small indirect bandgaps of 1.1 eV.
The new phosphidosilicates SrSi7P10 and BaSi7P10 were synthesized by solid-state reactions, and their crystal structures determined by single-crystal X-ray diffraction [P1, Z = 1, SrSi7P10: a = 6.1521(1) angstrom, b = 8.0420(2) angstrom, c = 8.1374(2) angstrom, alpha = 106.854(1)degrees, beta = 99.020(1)degrees, gamma = 105.190(1)degrees; BaSi7P10: a = 6.1537(1) angstrom, b = 8.0423(2) angstrom, c = 8.1401(2) angstrom, alpha = 106.863(1)degrees, beta = 99.050(1)degrees, gamma = 105.188(1)degrees]. The compounds crystallize in a new triclinic structure type with vertex sharing SiP4 tetrahedra, which assemble a non-centrosymmetric diamond-like network of T2 supertetrahedra. The alkaline earth cations reside in cuboctahedral voids. P-31 solid-state MAS-NMR spectra confirm the crystal structure. SrSi7P10 and BaSi7P10 exhibit the lowest charged SiP network in phosphidosilicates so far. Full-potential DFT calculations classify both compounds as semiconductors with small indirect bandgaps of 1.1 eV.

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