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    Sr<sub>2</sub>Te<sub>4</sub>V<sub>2</sub>O<sub>13</sub>Cl<sub>2</sub>, a Layered Structure Forming a Canted Antiferromagnetic Ground State

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    The 2D oxychloride, Sr2Te4V2O13Cl2, was synthesized by high-temperature solid-state synthesis in a closed silica ampule with low internal pressure of inert atmosphere. The crystal structure, determined by single-crystal diffraction, can be described with the orthorhombic space group, Pca21 (No. 29), with the pseudo-tetragonal unit cell, a = b = 8.802(1) Å and c = 19.221(2) Å. Cl, as well as Sr and Te, forms layers similar to that of Cu in SrCu2(BO3)2 (“SrCuBO”), one of the 11 Archimedean lattices. V(IV) shows the classical square pyramidal coordination, containing one short V–O distance, indicative of a vanadyl ion; furthermore, a relatively short V–V interatomic distance of 3.927(1) Å is found across a superexchange path V–O–V with an angle of 173.9(2)°. Initial magnetic investigations suggest that the compound is a canted antiferromagnet with a slightly negative Curie–Weiss constant of θCW = −5.5 K and an effective magnetic moment of μeff = 1.71 μB V–1. A significant second-order-like entropy release in the specific heat capacity measurement is observed in the same temperature range as a magnetic anomaly, as measured by magnetic susceptibility. This suggests a long-range ordering of magnetic spins below 3 K. Further magnetic data, in combination with the noncentrosymmetric atomic lattice, indicate that the ground state is a canted antiferromagnet
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