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n-HEXANE CONVERSION IN Ir/KLTL ZEOLITE
15
by aqueous ion exchange or simply washed with water to aged. A Si(111) double-crystal monochromator was used,
lower the K+ content; alternatively, some samples were with a resolution of 1E/E = 2 ꢁ 10ꢄ4. Higher harmonics
impregnated with KNO3 to increase the K+ content. The were rejected by detuning the monochromator by 20%.
several procedures were as follows:
EXAFS Data Analysis (11)
(A) KLTL zeolite (130 g) was ion exchanged with 1 liter
of 1.5 M NH4NO3 at 60ꢃC for 2 h. The zeolite was filtered,
Phase shift and backscattering amplitude data were
obtained from EXAFS spectra of suitable reference
compounds. Pt foil was used as a reference for Ir–Ir
absorber–backscatterer pairs. Na2Pt(OH)6 was used for Ir–
O absorber–backscatterer pairs. The crystallographic data
and details of the preparation of the reference files are
summarized elsewhere (11). The transferability of phase
shifts and backscattering amplitudes has been shown theo-
retically (23, 24) and experimentally (12, 25–27). Standard
procedures (27) were used to extract the EXAFS (chi) func-
tion from the raw data. Normalization of the EXAFS data
was performed by dividing the absorption intensity by the
height of the background absorption at 50 eV beyond the
absorption edge. The main EXAFS contributions were iso-
lated by Fourier filtering of the final EXAFS function (ex-
tracted EXAFS data), with k3 weighting (k is the wave vec-
tor) and phase and amplitude correction by using the Pt foil
reference (Table 1). Data analysis was performed on the fil-
tered data. Best-fit parameters were obtained by fitting with
the Koningsberger difference file technique (28). Low-Z
and high-Z contributions were fitted on both r space (r is
the radial distance from absorbing atom to backscattering
atom) and k space, with both k1 and k3 weighting so as not to
overemphasize either the low-Z or high-Z backscatterers.
Details of the fitting procedures are given elsewhere (27).
washed, and calcined at 540ꢃC for 3 h.
(B) KLTL zeolite (50 g) was washed six times with 500 ml
of hot water (pH 8.0); the resultant sample was calcined at
400ꢃC for 3 h.
(C) KLTL zeolite (100 g) was washed three times with
500 ml of hot water (pH 9.0) and calcined at 400ꢃC for 3 h.
(D) KLTL zeolite (15 g) was added to a solution of 0.78 g
KNO3 in 11 ml of water, dried, and calcined at 400ꢃC for 3 h.
(E) KNO3 (1.5 g) was dissolved in 11 ml of water and
added to KLTL zeolite (15 g), which was then dried and
calcined at 400ꢃC for 3 h.
(F) KNO3 (2.5 g) was dissolved in 11 ml of water and
added to 15 g of zeolite, which was dried and calcined at
400ꢃC for 3 h.
Each of these samples was dried, crushed into a fine pow-
der, and brought in contact with [Ir(NH3)5Cl]Cl2 (Johnson
Matthey) in water by the incipient wetness method. For ex-
ample, 2.0 g of [Ir(NH3)5Cl]Cl2 dissolved in 40 ml of water
at 70ꢃC was added to 50.0 g of zeolite. After the addition
of a few drops of HNO3, the pH of the [Ir(NH3)5Cl]Cl2
solution was adjusted to 7 by addition of NH4OH. The so-
lution was filtered and added dropwise to the zeolite. The
resultant slurry was allowed to stand at room temperature
for 3 h, and the sample was dried at 120ꢃC overnight. The
crystallites of zeolite were held together without a binder.
Chemisorption Measurements
Elemental Analysis
H2 chemisorption was carried out with an RXM-100 cata-
lyst testing and characterization apparatus (Advanced Sci-
entific Design, Inc.). The Ir/KLTL zeolites were reduced
at either 300 or 500ꢃC for 1 h and then evacuated at pres-
sures <10ꢄ6 Torr for 2 h at the reduction temperature. The
The zeolites were analyzed for Ir by Schwartzkopf Micro-
analytical Laboratories, Woodside, NY, and for Al and K
by the analytical division of Amoco Oil Co. by inductively
coupled plasma analysis.
TABLE 1
Extended X-Ray Absorption Fine Structure Spectroscopy
Parameters Used for Isolation of Main EXAFS Data
in Fourier Filteringa
In preparation for EXAFS spectroscopy, the catalysts
were treated for 1 h at 300ꢃC in flowing H2 (99.999 + %,
formed by electrolysis of water in a Balston generator).
Traps containing Cu2O and 4A zeolite were used to re-
move traces of oxygen and water, respectively. The cata-
lysts were pressed into self-supporting wafers and loaded
into a cell in the absence of air. EXAFS measurements were
done at Beamline X-11A at the National Synchrotron Light
Source, Brookhaven National Laboratory, Upton, NY. The
synchrotron energy was maintained at 2.5 GeV, and the ring
current was at least 110 mA. Two scans were done for each
sample at the Ir LIII edge (11215 eV), with the sample at
near liquid nitrogen temperature, and the scans were aver-
K : Al atomic ratio
ꢄ1
˚
˚
in zeolite
1k (A
)
1r (A)
p
0.34
0.95
1.34
1.56
3.59–14.55
3.48–13.96
3.62–13.60
3.70–13.60
1.74–3.47
1.42–3.52
1.70–3.38
1.67–3.40
13
15
12
12
a
Notation: 1k, range used for forward Fourier transform; 1r,
range used for isolation of main data; p, number of free parame-
ters from Nyquist theorem, p = (21k1r)/ꢀ + 1. Spectral isolation
was carried out on k3-weighted Fourier transform, with phase and
amplitude correction using Pt foil reference.