5
24
M.-D. Wei et al. / Materials Research Bulletin 35 (2000) 521–530
Cu K␣ radiation (Rigaku RINT-2200VL, 30 kV, 16 mA). The specific surface areas of
catalysts, which were measured by N adsorption at liquid N temperature (BET
2
2
2
Ϫ1
method), were very small, ranging between 1.0 and 0.2 m ⅐g
.
2
.2. Catalytic activity test
The catalytic activity was measured in a fixed-bed flow reactor between 300 and
00°C. A mixture of NO (0.44%), C H (0.29%), O (4.4%) and He (balance) was fed
8
3
3
8
2
Ϫ1
Ϫ1
to 0.5 g catalyst at a rate of 30 cm ⅐min ; the space velocity was 7000 h , or the
Ϫ3
contact time (catalyst weight/gas flow rate) was 1.0 g⅐s⅐cm . The effluent gas was
analyzed by a gas chromatograph equipped with a thermal conductivity detector (Shi-
madzu GC 14B). A molecular sieve 5A column was used to separate NO, O , N , and
2
2
CO, and a Porapak N column for CO and C H . The catalytic activity at a steady state,
2
3 8
which was attained after 1 h or more on stream, was evaluated by the following
parameters:
Y Conversion of NO into N (X[N ]/%) ϭ (2[N ] /[NO] ) ϫ 100
2
2
2 out
in
Y Conversion of NO into N O (X[N O]/%) ϭ (2[N O] /[NO] ) ϫ 100
2
2
2
out
in
Y Conversion of C H into CO (X[CO ]/%) ϭ ([CO ] /3[C H ] ) ϫ 100
3
8
2
2
2 out
3 8 in
Y Conversion of C H into CO (X[CO]/%) ϭ ([CO] /3[C H ] ) ϫ 100
3
8
out
3 8 in
The total conversion of NO (X[NO]), which is a sum of X[N ] and X[N O], is also used to
2
2
discuss the NO reduction activity.
3
. Results and discussion
3
.1. Crystal structure
Double perovskites with the rock-salt sublattice have unit cells with lattice constants
of 2a or ͌2a ϫ ͌2a ϫ 2a , where a is the lattice constant of cubic perovskite of
p
p
p
p
p
the primitive ABO type (a Ϸ 0.4 nm). In the present study, four types of unit cells were
3
p
discerned, and XRD pattern of the representative sample in each type is shown in Fig.
. The appearance of superlattice lines, for example, 111, 311, and 511 lines of Fig. 2(a),
2
II
VI
evidences the rock-salt ordering of B and B cations [5]. As can be seen from Table
1
almost all oxides with A ϭ Ba, Sr, and Ca have the structure of cubic 2a type,
II II VI
2 6
II
, the unit-cell type of A B B O is almost exclusively determined by the A cation;
II
p
tetragonal ͌2a ϫ ͌2a ϫ 2a type, or orthorhombic ͌2a ϫ ͌2a ϫ 2a type,
p
p
p
p
p
p
II
IV
respectively. Exceptions to this rule are oxides with B ϭ Cu and Sr CaB O . The
2
6
former crystallizes in the tetragonal 2a -type structure, due to the Jahn–Teller distortion
p
2
ϩ
VI
of the Cu ion [7]. The structure of SrCaB O , the orthorhombic ͌2a ϫ ͌2a ϫ 2a
type, is more distorted than that of other tetragonal SrB B O oxides, because the
combination of smaller A (Sr) and larger B (Ca) gives a smaller tolerance factor or
fitness factor [8], which results in the lattice distortion. Details of the crystal structure
6
p
p
p
II VI
6
II
II