Slow Magnetic Relaxations in Cobalt(II) Tetranitrate Complexes. Studies of Magnetic Anisotropy by Inelastic Neutron Scattering and High-Frequency and High-Field EPR Spectroscopy

Lei Chen, Hui Hui Cui, Shelby E. Stavretis, Seth C. Hunter, Yi Quan Zhang, Xue Tai Chen, Yi Chen Sun, Zhenxing Wang, You Song, Andrey A. Podlesnyak, Zhong Wen Ouyang, Zi Ling Xue

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Abstract

Three mononuclear cobalt(II) tetranitrate complexes (A)2[Co(NO3)4] with different countercations, Ph4P+ (1), MePh3P+ (2), and Ph4As+ (3), have been synthesized and studied by X-ray single-crystal diffraction, magnetic measurements, inelastic neutron scattering (INS), high-frequency and high-field EPR (HF-EPR) spectroscopy, and theoretical calculations. The X-ray diffraction studies reveal that the structure of the tetranitrate cobalt anion varies with the countercation. 1 and 2 exhibit highly irregular seven-coordinate geometries, while the central Co(II) ion of 3 is in a distorted-dodecahedral configuration. The sole magnetic transition observed in the INS spectroscopy of 1-3 corresponds to the zero-field splitting (2(D2 + 3E2)1/2) from 22.5(2) cm-1 in 1 to 26.6(3) cm-1 in 2 and 11.1(5) cm-1 in 3. The positive sign of the D value, and hence the easy-plane magnetic anisotropy, was demonstrated for 1 by INS studies under magnetic fields and HF-EPR spectroscopy. The combined analyses of INS and HF-EPR data yield the D values as +10.90(3), +12.74(3), and +4.50(3) cm-1 for 1-3, respectively. Frequency- and temperature-dependent alternating-current magnetic susceptibility measurements reveal the slow magnetization relaxation in 1 and 2 at an applied dc field of 600 Oe, which is a characteristic of field-induced single-molecule magnets (SMMs). The electronic structures and the origin of magnetic anisotropy of 1-3 were revealed by calculations at the CASPT2/NEVPT2 level.

Original languageEnglish
Pages (from-to)12603-12617
Number of pages15
JournalInorganic Chemistry
Volume55
Issue number24
DOIs
StatePublished - Dec 19 2016

Funding

We are grateful for financial support from the National Basic Research Program of China (No. 2013CB922102 to X.-T.C. and Y.S.), the Natural Science Grant of China (No. 21471078 to X.-T.C.), the Natural Science Foundation of Jiangsu Province of China (BK20151542), and the U.S. National Science Foundation (CHE-1362548 and CHE-1633870 to Z.-L.X.). Acknowledgment is also made to the donors of the American Chemical Society Petroleum Research Fund for partial support of this research.

FundersFunder number
Natural Science Grant of China21471078
U.S. National Science FoundationCHE-1633870, CHE-1362548
National Science Foundation1633870, 1362548
American Chemical Society Petroleum Research Fund
Natural Science Foundation of Jiangsu ProvinceBK20151542
National Basic Research Program of China (973 Program)2013CB922102

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