A new strontium nickel polyphosphide, SrNi 2 P 4 , was synthesized from elements and structurally characterized by single-crystal X-ray diffraction. It crystallizes in the orthorhombic space group Fddd (No. 70), with Z = 8. The crystal structure is that of a clathrate type, composed of Ni 8 P 16 , 14-faced polyhedral cages that encapsulate Sr atoms. Together with the previously reported but unrecognized clathrate VII, BaNi 2 P 4 , and another previously reported clathrate, BaCu 2 P 4 , which is isostructural to SrNi 2 P 4 , a family of transition metal−phosphorus clathrates is represented. The crystal structures of each of the discussed transition metal-based clathrates are composed of unique polyhedra containing square faces. These structural fragments were predicted to be unstable for the conventional clathrates based on Si, Ge, and Sn. In this work, we report the crystal and electronic structures, chemical bonding, as well as the thermoelectric properties of this novel class of unconventional clathrates.
■ INTRODUCTIONGas hydrates, also known as clathrates, are a fascinating class of compounds with a crystal structure composed of a tetrahedral water framework encapsulating guest atoms and molecules inside large polyhedral cages. 1 Inorganic clathrates have similar crystal structures, comprised of covalently bound tetrahedral frameworks of heavier elements. 2−4 The frameworks of the majority of inorganic clathrates are formed from group 14 elements, Si, Ge, or Sn, which are known as tetrels. Guest cations or anions can be encapsulated inside those cages (Figure 1 top), providing atomic vibrations that are essentially independent of the surrounding framework, making clathrates promising thermoelectric materials.Inorganic clathrates crystallize into six structure types, which can be described as a tiling of space using several types of polyhedra. For known tetrel clathrates, the polyhedra are composed of pentagonal and hexagonal faces (Figure 1 top). 2−4 The crystal structure of the most common type I clathrate is composed of pentagonal dodecahedra and tetrakaidecahedra (Figures 1a, b).The stability of known and hypothetical tetrel clathrates was scrutinized by means of theoretical calculations, which predicted the lowest stability for clathrate structure types composed mainly of tetrel atoms with local coordinations that deviate furthest from a regular tetrahedral coordination. 6 The highest distortion of this local coordination occurs for tetrel elements occupying vertices of the square faces of polyhedral cages. It was proposed that clathrates formed by polyhedra with square faces should be unstable, and indeed, no such tetrel clathrates have been reported. [2][3][4]6 The energy landscape and stability of clathrates can be significantly modified by diverging from tetrel elements. Several groups have recently shown that type I clathrate frameworks can be formed from a combination of late transition metals, Zn, Cd, Cu, and Au, along with a pnicogen, a group 15 element: P, As, or Sb. 7−11 In this work, we discuss...