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46923-AC5
Determining the Effect of Local Structure on Acidity in High Surface Area Oxides
Luis J. Smith, Clark University
The overall goal of this research is to understand how the
local variations in the structure of layered niobates affects the surface
properties of the material. In
this particular study our focus is on the surface acid sites present in the
nanosheet versions of these materials that are produced upon exfoliation. To examine these local changes, 93Nb
solid-state NMR has been used to measure both the electric field gradient (EFG)
and the chemical shift anisotropy (CSA) at the niobium sites. As both effects are sensitive to the
local bonding of the niobium, they can serve as guides to small changes in
local structure and symmetry.
Building from our previous work[1] on the triple-perovskite
layered Dion-Jacobson phase, KCa2Nb3O10, it
was clear that there are two different NMR environments in these layered
materials: a niobium site at the interface between layers and a niobium
environment in the center of the layer.
To understand the effects of the alkaline earth cation on the local
structure, strontium-containing Dion-Jacobson phases were studied with
potassium or rubidium as the alkali cation. While the interface and interior niobium sites in the
calcium containing forms had quadrupolar coupling (CQ) values for
the EFG typical of pervoskite niobates (20 – 30 MHz), the two different
niobium environments in the strontium-containing materials had couplings that
ranged from 45 – 93 MHz. The
large values indicate that a substantial amount of strain must be present at
the niobium sites due in part to the increased size of the strontium atom and
is consistent with the observed increase in the lattice parameters of the
niobate layers. Initial
calculations of the EFG in the RbSr2Nb3O10
sample using periodic density functional theory methods point to the source of
the strain coming from a possible tilting of the niobate octahedra as has been
suggested from Raman spectroscopy.[2]
To understand the effect of cation replacement, the
pre-exfoliated acid-exchanged forms of the KSr2Nb3O10
and RbSr2Nb3O10 samples were also examined
using solid-state NMR methods.
From x-ray powder diffraction studies, the acid-exchanged materials were
identical and observed to both be tetragonal with identical lattice constants
even though the parent compounds were either tetragonal (RbSr2Nb3O10)
or orthorhombic (KSr2Nb3O10). 93Nb NMR studies however
revealed that the two acid-exchanged compounds had different environments for
the niobium sites with the interior niobium position demonstrating drastic
differences in strain. Both the symmetry
and magnitude of the EFG at these positions were significantly different. In both cases, the local structure of
the interior niobium site was more similar to environment observed in the
parent compounds than to each other.
Both niobium sites in the acid-exchanged forms show a reduction in the
EFG demonstrating that the effect of the proton on bonding does translate
throughout the layer.
Nevertheless, the changes are not sufficient to erase the influence of
the parent compound. Our studies
of the nanosheets derived from these acid forms will thus need to examine the
materials from numerous parent compounds to understand the subtle differences
that could alter the surface acidity.
In the summer of 2008, Professor Sarah Pilkenton from
Framingham State College was supported to conduct research associated with the
synthesis and analysis of the surface acidity of the nanosheet materials that
can be produced from the layered niobates. Her research resulted in an improved exfoliation method for
the production of nanosheets. The
progress was promising and we plan to continue the collaboration to further
study the surface of the materials.
Her summer work has also helped to jump start a research project at her
institution on exfoliation methods that will include undergraduate students.
[1] X. Wang, L. J. Smith, J. Mol. Catal. A, 281, 214-218 (2008).
[2] J. A. Kurzman, M. J. Geselbracht, Mater. Res. Soc.
Symp. Proc. 988, 0988-QQ08-06
(2007).
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