J. Am. Ceram. Soc., 81 [8] 2188–90 (1998)
A New, Low-Temperature Polymorph of O
-SiAlON
Mark E. Bowden, Glen C. Barris, and Ian W. M. Brown
Industrial Research Limited, Lower Hutt, New Zealand
David A. Jefferson
Department of Chemistry, University of Cambridge, Cambridge CB2 1EW, United Kingdom
A new phase in the Si-Al-O-N system has been identified,
following syntheses based on the nitridation of silicon/clay
mixtures at low temperatures (<1350°C). The structure of
the new phase was determined using a combination of dif-
fraction and high-resolution imaging techniques, and this
new phase possessed the same sheet structure as O
-SiAlON
(Si2−xAlxO1+xN2−x) but with a different stacking arrange-
ment. It is considered to be a low-temperature polymorph
of O
-SiAlON and transforms to conventional O
-SiAlON
at temperatures greater than 1350°C.
copy (HREM) utilized a 200 keV instrument (Model 200CX,
JEOL, Tokyo, Japan) equipped with a high-resolution (Cs ס
0.41 mm) pole piece. Simulated HREM images were calculated
with the EMS software system,5 using values of 0.5 mrad for
beam divergence and 100 Å for focal spread.
III. Results and Discussion
The first indications of the formation of a new phase arose
when the XRD patterns of reacted mixtures could not be
matched to any known compounds. The unmatched XRD
peaks were particularly apparent in samples reacted at tempera-
tures <1300°C, which is a temperature considerably lower than
those normally used for solid-state syntheses of OЈ-SiAlON
(e.g., 1800°C6). The ability to prepare SiAlON phases at low
temperature was a consequence of the synthesis method used
and, in particular, the use of clay and silicon as reactants.
Adding small amounts of iron (1.5% as Fe2O3) improved the
reaction rate, as has been observed for the nitridation of silicon
to Si3N4.7 The results obtained here do not show whether the
iron or other impurities derived from the clay have any role in
stabilizing the new phase, in a manner similar to the additional
cations used to stabilize ␣-SiAlON. However, we do note that
the level of impurities in the present material is considerably
lower than that required to stabilize ␣-SiAlON.
The composition of the new phase approximated that of
OЈ-SiAlON, as reacted mixtures with this composition pro-
duced the highest yields. In addition, the new phase trans-
formed to OЈ-SiAlON at 1350°C without a significant weight
change and without the appearance or disappearance of sec-
ondary phases. All these factors have led us to believe that the
low-temperature conditions used here permitted the synthesis
of a new, low-temperature polymorph of OЈ-SiAlON.
Although the crystallites prepared were too small for single-
crystal analysis, the structure was solved by using a combina-
tion of HREM and selected-area electron diffraction. Electron
diffraction patterns taken from different zone axes suggested an
orthorhombic unit cell, and preliminary structural coordinates
were proposed on the basis of the HREM images. Simulation
of these images and the XRD pattern confirmed the proposed
structure, which was subsequently refined from the observed
XRD data using the Rietveld technique. Some small discrep-
ancies between the observed and calculated XRD patterns re-
mained after the refinement; these discrepancies were ascribed
to the presence of planar defects in the specimen (this point will
be discussed later in the paper). However, the overall agree-
ment (Bragg factor (R) of 5.37%, goodness of fit is 10.3) was
sufficient to give us considerable confidence in the validity of
the model. Structural coordinates that resulted from these re-
finements are given in Table I, and tabulated XRD pattern data
are provided in Table II.
I. Introduction
HE Si-Al-O-N system has become the subject of widespread
T
research since the initial discovery1,2 that aluminum and
oxygen can be substituted into the Si3N4 lattice. One reason for
the intensity of the research effort is the many different
SiAlON phases that can be prepared, each of which presents
different physical properties. The Si-Al-O-N phase diagram
was explored in the early history of SiAlON research, and by
the time Jack performed his review in 1976,3 all the presently
known phases had been discovered. In this communication, we
describe the structure of the first new SiAlON to be found since
that times: a low-temperature polymorph of OЈ-SiAlON
(Si2−xAlxO1+xN2−x).4
II. Experimental Procedure
Mixtures of clay (light kaolin, BDH Chemicals Pty., Ltd.,
Poole, U.K.), silicon (grade 4D, Permascand AB, Ljungaverk,
Sweden), and silica (Superfine Quartz, Commercial Minerals
Ltd., Auckland, New Zealand) were blended for 20 h in a ball
mill using Si3N4 media and hexane solvent. Major impurities
(>0.05%) in this clay are 0.75% K2O, 0.45% Fe2O3, 0.35%
MgO, 0.21% P2O5, and 0.14% Na2O. The stoichiometry for
each mixture was calculated according to the following reac-
tion scheme, illustrated for the x ס
0.2 OЈ-SiAlON composition:
0.1Si2Al2O5(OH)4 + 1.35Si + 0.25SiO2 + 0.9N2
→ Si1.8Al0.2O1.2N1.8 ם
0.2H2O
After drying, the powder was lightly pressed (8 MPa) into disks
15 mm in diameter and heated under flowing H2 (10%) in N2
for 8 h at 1270°C.
X-ray diffractometry (XRD) was performed using a system
(Model PW1700, Philips Research Laboratories, Eindhoven,
The Netherlands) with a post-diffraction graphite monochro-
mator and CoK␣ radiation. High-resolution electron micros-
The structure is best described by comparing it with OЈ-
SiAlON,6 and projections of both structures are shown in Fig.
1. For simplicity, we will consider the x ס
0 composition
(Si2N2O), although the actual specimen that was examined
contained 10 mol% of aluminum and oxygen, substituted on
T. Ekstro¨m—contributing editor
Manuscript No. 190375. Received February 16, 1998; approved April 27, 1998.
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