The
effect of temperature on the formation of copper centers in
Cu-mordenite (Cu-MOR), obtained by solid-state ion exchange between
copper chloride and zeolite H-mordenite, was studied by combining
Density Functional Theory (DFT) simulations of the local atomic structures
of copper with the analysis of Cu K-edge XANES and EXAFS, measured
“in situ” from room temperature to 400 °C. Cu K
edge XANES and EXAFS spectra have a different level of sensitivity
regarding the detection of the angular and radial distribution of
atoms in the closest vicinity of copper. Based on this, a simultaneous
theoretical description of XANES and Fourier transforms F(R) of EXAFS in the extended range of interatomic
distances R (up to ∼6 Å) was used as
an efficient filter for selecting suitable atomic models of copper
species from the number of models given by DFT. It was revealed that,
between RT and ∼200 °C, the local structure around copper
in Cu-MOR did not change and was similar to that of bulk CuCl. By
increasing the temperature to 300 °C and then to 400 °C,
changes in both Cu K-edge XANES and EXAFS were observed, indicating
the reconstruction of the local structure of copper. At 300 °C,
copper-containing fragments, with a CuCl-like structure, decompose
to form two different types of copper centers in the vicinity of the
eight-member rings of the zeolite framework. The first type contains
one copper atom, a monomer, coordinated to three O atoms of the framework
as first neighbors and an O, an Al, and two Si atoms as the next neighbors.
The second type contains two Cu atoms, which form a dimer, in which
each Cu atom has two O atoms and one Cl atom as the first neighbors
and one Al and two Si atoms as the next neighbors. At 400 °C,
the Cu–Cu interaction in all the structural models, which describe
the Cu K-edge XAS spectra, led to the assumption that the formation
of dicopper centers dominated. Furthermore, the simultaneous description
of both Cu XANES and EXAFS suggested the necessity of doing the structural
analysis based on a single dicopper model of the Cu center and to
also consider linear combinations of other such models. The suitable
linear combination was found based on the three most plausible structural
models of the Cu environment containing a Cu–Cl–Cu chain,
in which each copper atom is characterized by a very similar pair
radial distribution function of the neighboring atoms. However, the
angular distributions of these neighboring atoms are different in
all three Cu centers due to the difference in the nonequivalent crystallographic
sites of the Al atoms, near which the Cu centers formed in the zeolite
framework. In Cu-MOR at 400 °C another type of Cu center, containing
a Cu–O–Cu dimer, can exist simultaneously with the above-mentioned
Cu centers with Cu–Cl–Cu dimers.