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Ruige Cao

Researcher at Northeast Normal University

Publications -  25
Citations -  605

Ruige Cao is an academic researcher from Northeast Normal University. The author has contributed to research in topics: Hydrogen bond & Crystal structure. The author has an hindex of 12, co-authored 25 publications receiving 579 citations.

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Two Dawson-templated three-dimensional metal-organic frameworks based on oxalate-bridged binuclear cobalt(II)/Nickel(II) SBUs and Bpy linkers.

TL;DR: The Dawson anion P2W18O626− has been used as a noncoordinating polyoxoanion template for the construction of two metal−organic frameworks as discussed by the authors.
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Mixed-valence iron(II, III) trimesates with open frameworks modulated by solvents.

TL;DR: The mixed-valence character of the frameworks of 1 and 2 was confirmed by Mossbauer spectroscopy studies as discussed by the authors, which revealed that there are antiferromagnetic exchange interactions among the Fe atoms in these two iron trimesates.
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Organic-inorganic hybrids constructed of anderson-type polyoxoanions and oxalato-bridged dinuclear copper complexes.

TL;DR: To elucidate the electronic properties and magnetic properties of the metal ions (Cu2+ or Cu2+ and Cr3+), EPR studies and magnetic susceptibility studies have been performed, respectively and the results are consistent with the structural feature of these compounds.
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Organic-inorganic hybrids assembled by bis(undecatungstophosphate) lanthanates and dinuclear copper(II)-oxalate complexes.

TL;DR: Single-crystal X-ray diffraction studies reveal that compounds 1-5 are isomorphic and consist of one-dimensional chains, which are constructed by alternating bis(undecatungstophosphate) lanthanates [Ln(PW11O39)2](11-) and dinuclear copper(II)-oxalate complexes [Cu2(bpy)2(mu-ox)]2+.
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Influence of different site symmetries of Eu3+ centers on the luminescence properties of Anderson-based compounds

TL;DR: In this paper, a 1D chain structure built up of alternating Anderson-type polyanions [Al(OH) 6 Mo 6 O 18 ] 3− and hydrated rare-earth ions Eu 3+ was determined by singlecrystal X-ray diffraction.