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Neue thermische Abbauprodukte von Ln2CeMO6Cl3 (M = Nb,Ta; Ln = La–Sm) – Darstellung von strukturverwandtem (La, Tb)3,5TaO6Cl4–x
Authors:H. Weitzel  B. Behler  R. Gruehn
Abstract:Contributions on the Investigation of Inorganic Nonstoichiometric Compounds. XLV. New Thermal Decomposition Products of Ln2CeMO6Cl3 – Preparation of Structure‐related (La, Tb)3.5TaO6Cl4–x The thermal decomposition (T £ 900–1050°C) of Ln2CeMO6Cl3 (M = Nb, Ta; Ln = La, Ce, Pr, Nd, Sm) leads to the formation of two mixed‐valenced phases (Ln, Ce)3.25MO6Cl3.5–x (phase ‘‘AB”︁”︁) and (Ln, Ce)3.5MO6Cl4–x (phase ‘‘BB”︁”︁) and to the formation of chlorine according to redox‐reactions between Ce4+ and Cl. Single crystals of both phases (Ln, Ce)3.25MO6Cl3.5–x (‘‘AB”︁”︁) and (Ln, Ce)3.5MO6Cl4–x (‘‘BB”︁”︁) were obtained by chemical transport reactions using both powder of Ln2CeMO6Cl3 (phase ‘‘A”︁”︁) and powder of (Ln, Ce)3.25MO6Cl3.5–x (phase ‘‘AB”︁”︁) as starting materials and chlorine (p{Cl2; 298 K} = 1 atm) or HCl (p{HCl; 298 K} = 1 atm) as transport agent. A crystal of (La, Ce)3.25NbO6Cl3.5–x (”︁AB”︁”︁) (space group: C2/m, a = 35.288(1) Å, b = 5.418(5) Å, c = 9.522(1) Å, β = 98.95(7)°, Z = 4) was investigated by x‐ray diffraction methods, a crystal of (Pr, Ce)3.5NbO6Cl4–x (”︁BB”︁”︁) was investigated by synchrotron radiation (λ = 0.56 Å) diffraction methods. The lattice constants are a = 18.863(6) Å, b = 5.454(5) Å, c = 9.527(6) Å, β = 102.44(3)° and Z = 4. Structure determination in the space group C2/m (No. 12) let to R1 = 0.0313. Main building units are NbO6‐polyhedra with slightly distorted trigonally prismatic environment for Nb and chains of face‐sharing Cl6‐octahedra along [010]. The rare earth ions are coordinated by chlorine and oxygen atoms. These main structure features confirmed the expected relation to the starting material Ln2CeMO6Cl3 (phase ”︁A”︁”︁) and to (Ln, Ce)3.25MO6Cl3.5–x (phase ”︁AB”︁”︁).
Keywords:Rare earth oxochlorometallates(V)  nobium  tantalum  rare earth  chemical vapour transport  synchrotron radiation  crystal structure
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