posted on 2020-08-19, 15:44authored byVinicius Martins, Jun Xu, Xiaoling Wang, Kuizhi Chen, Ivan Hung, Zhehong Gan, Christel Gervais, Christian Bonhomme, Shijia Jiang, Anmin Zheng, Bryan E. G. Lucier, Yining Huang
The
spectroscopic study of oxygen, a vital element in materials,
physical, and life sciences, is of tremendous fundamental and practical
importance. 17O solid-state NMR (SSNMR) spectroscopy has
evolved into an ideal site-specific characterization tool, furnishing
valuable information on the local geometric and bonding environments
about chemically distinct and, in some favorable cases, crystallographically
inequivalent oxygen sites. However, 17O is a challenging
nucleus to study via SSNMR, as it suffers from low sensitivity and
resolution, owing to the quadrupolar interaction and low 17O natural abundance. Herein, we report a significant advance in 17O SSNMR spectroscopy. 17O isotopic enrichment
and the use of an ultrahigh 35.2 T magnetic field have unlocked the
identification of many inequivalent carboxylate oxygen sites in the
as-made and activated phases of the metal–organic framework
(MOF) α-Mg3(HCOO)6. The subtle 17O spectral differences between the as-made and activated phases yield
detailed information about host–guest interactions, including
insight into nonconventional O···H–C hydrogen
bonding. Such weak interactions often play key roles in the applications
of MOFs, such as gas adsorption and biomedicine, and are usually difficult
to study via other characterization routes. The power of performing 17O SSNMR experiments at an ultrahigh magnetic field of 35.2
T for MOF characterization is further demonstrated by examining activation
of the MIL-53(Al) MOF. The sensitivity and resolution enhanced at
35.2 T allows partially and fully activated MIL-53(Al) to be unambiguously
distinguished and also permits several oxygen environments in the
partially activated phase to be tentatively identified. This demonstration
of the very high resolution of 17O SSNMR recorded at the
highest magnetic field accessible to chemists to date illustrates
how a broad variety of scientists can now study oxygen-containing
materials and obtain previously inaccessible fine structural information.