Structure and Properties of an Amorphous Metal-Organic Framework

被引:268
作者
Bennett, Thomas D. [1 ]
Goodwin, Andrew L. [2 ,3 ]
Dove, Martin T. [2 ]
Keen, David A. [4 ,5 ]
Tucker, Matthew G. [4 ]
Barney, Emma R. [4 ]
Soper, Alan K. [4 ]
Bithell, Erica G. [1 ]
Tan, Jin-Chong [1 ]
Cheetham, Anthony K. [1 ]
机构
[1] Univ Cambridge, Dept Mat Sci, Cambridge CB2 3QZ, England
[2] Univ Cambridge, Dept Earth Sci, Cambridge CB2 3EQ, England
[3] Univ Oxford, Dept Chem, Oxford OX1 3QR, England
[4] Rutherford Appleton Lab, ISIS Facil, Didcot OX11 0QX, Oxon, England
[5] Univ Oxford, Dept Phys, Clarendon Lab, Oxford OX1 3PU, England
基金
欧洲研究理事会; 英国工程与自然科学研究理事会;
关键词
EXTENDED POLYMORPHISM; CRYSTALLINE PHASES; SILICA; PRESSURE; POWDER; SI;
D O I
10.1103/PhysRevLett.104.115503
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
ZIF-4, a metal-organic framework (MOF) with a zeolitic structure, undergoes a crystal-amorphous transition on heating to 300 degrees C. The amorphous form, which we term a-ZIF, is recoverable to ambient conditions or may be converted to a dense crystalline phase of the same composition by heating to 400 degrees C. Neutron and x-ray total scattering data collected during the amorphization process are used as a basis for reverse Monte Carlo refinement of an atomistic model of the structure of a-ZIF. The structure is best understood in terms of a continuous random network analogous to that of a-SiO2. Optical microscopy, electron diffraction and nanoindentation measurements reveal a-ZIF to be an isotropic glasslike phase capable of plastic flow on its formation. Our results suggest an avenue for designing broad new families of amorphous and glasslike materials that exploit the chemical and structural diversity of MOFs.
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页数:4
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