Abstract

AbstractReVIIO2(PO4) and (ReVII2O5)Sio2[Sit2O(PO4)6] were obtained from Re2O7 and P4O10 in sealed silica tubes (250 ≤ ϑ ≤ 400 °C). The crystal structures were solved and refined from X‐ray single crystal data (ReVIIO2(PO4): C2/c, Z = 24, a = 14.403(1) Å, b = 8.414(1) Å, c = 20.647(3) Å, β = 93.165(8)°, T = 123 K, 10352 ind. refl., 218 variables, 24 atoms in asymmetric unit, R1 = 0.041, wR2 = 0.106; (ReVII2O5)Sio2[Sit2O(PO4)6]: P$\bar{1}$, Z = 1, a = 7.8589(3) Å, b = 7.8609(3) Å, c = 10.8311(4) Å, α = 85.312(2)°, β = 73.078(2)°, γ = 60.075(2)°, T = 298 K, 2551 ind. reflections, 174 variables, 22 atoms in asymmetric unit, R1 = 0.078, wR2 = 0.208). The complex crystal structure of ReO2(PO4) can be derived from the ReO3 structure type. The crystal structure of the silicophosphate consists of distorted [Re2O11] dioctahedra (1.69 Å ≤ d(Re–O) ≤ 2.08 Å), [SiIVO6] octahedra, and [Sit2O(PO4)6]12– heteropolyanions. In ReO2(PO4) monomeric perrhenyl ions (ReO2)3+ (∠(Ot,Re, Ot) ≈ 101.5°) are formed. The silicophosphate (Re2O5)Sio2[Sit2O(PO4)6] contains dinuclear (Re2O5)4+ cations. 31P‐MAS‐NMR studies on ReO2(PO4) are in accordance with three independent sites of phosphorus. The results of 31P‐ and 29Si‐MAS‐NMR studies on (Re2O5)Sio2[Sit2O(PO4)6] are in agreement with three crystallographically independent sites for phosphorus and two sites for silicon.

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