CONSTITUTION OF THE GAMMA-ALUMINA PHASE IN CHEMICALLY PRODUCED MULLITE PRECURSORS

被引:35
作者
SCHNEIDER, H [1 ]
VOLL, D [1 ]
SARUHAN, B [1 ]
SCHMUCKER, M [1 ]
SCHALLER, T [1 ]
SEBALD, A [1 ]
机构
[1] UNIV BAYREUTH,BAVARIAN INST GEOSCI,D-95440 BAYREUTH,GERMANY
关键词
D O I
10.1016/0955-2219(94)90022-1
中图分类号
TQ174 [陶瓷工业]; TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
The temperature development of type II mullite precursor powders have been studied in the temperature range of 150-degrees-C (as-received) and 1150-degrees-C X-ray diffraction (XRD) measurements, infrared (IR) and Si-29 and Al-27 nuclear magnetic resonance (NMR) spectroscopy and analytical transmission electron microscopy (ATEM) have been performed on the heat-treated precursors. The investigations had the aim of contributing to the frequently discussed question, whether Si is incorporated into the gamma-alumina spinel being formed as a transient phase in type II mullite precursors. The as-received precursors consist of relatively large sperical particles (less-than-or-equal-to 0.5 mum) of non-crytalline SiO2 and of much finer-grained agglomerates of pseudo-boehmite crystals (gamma-AlO(OH), almost-equal-to 20 nm), which are embedded in a SiO2 matrix. Above almost-equal-to 350-degrees-C, pseudo-boehmite transforms to spinel type alumina (gamma-Al2O3). During this transformation, all Si existing in the SiO2 matrix of the pseudo-boehmite agglomerates is incorporated into gamma-Al2O3 corresponding to a SiO2 content of almost-equal-to 12 mole% at 500-degrees-C Up to 750-degrees-C, the SiO2 content of the gamma-alumina remains constant but above this temperature it gradually rises and reaches a maximum amount of almost-equal-to 18 mole% at 1150-degrees-C A marginal decomposition of the spherical non-crystalline SiO2 particles may be the sources to provide diffusion of Si species into the gamma-alumina during a temperature increase above 750-degrees-C It is most likely that Si species diffuse into the gamma-alumina crystals along the crystallite boundaries. The diffusion process and Si incorporation are facilitated with the temperature increase.
引用
收藏
页码:441 / 448
页数:8
相关论文
共 26 条
[1]   THE KAOLINITE-MULLITE REACTION SERIES .1. A SURVEY OF OUTSTANDING PROBLEMS [J].
BRINDLEY, GW ;
NAKAHIRA, M .
JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1959, 42 (07) :311-314
[2]   THE KAOLINITE-MULLITE REACTION SERIES .2. METAKAOLIN [J].
BRINDLEY, GW ;
NAKAHIRA, M .
JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1959, 42 (07) :314-318
[3]   OUTSTANDING PROBLEMS IN THE KAOLINITE-MULLITE REACTION SEQUENCE INVESTIGATED BY SI-29 AND AL-27 SOLID-STATE NUCLEAR MAGNETIC-RESONANCE .2. HIGH-TEMPERATURE TRANSFORMATIONS OF METAKAOLINITE [J].
BROWN, IWM ;
MACKENZIE, KJD ;
BOWDEN, ME ;
MEINHOLD, RH .
JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1985, 68 (06) :298-301
[4]   SPECTROSCOPIC INVESTIGATIONS OF KAOLINITE-MULLITE REACTION SEQUENCE [J].
BULENS, M ;
LEONARD, A ;
DELMON, B .
JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1978, 61 (1-2) :81-84
[5]   RE-EXAMINATION OF KAOLINITE-TO-MULLITE REACTION SERIES [J].
CHAKRABORTY, AK ;
GHOSH, DK .
JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1978, 61 (3-4) :170-173
[7]  
ENGELHARDT G, 1987, HIGH RESOLUTION SOLI, P143
[8]  
Farmer V. C., 1974, INFRARED SPECTRA MIN
[9]  
GRIMSHAW RW, 1945, BRIT CERAM T, V44, P76
[10]  
HOFFMAN DW, 1984, J AM CERAM SOC, V67, P468, DOI 10.1111/j.1151-2916.1984.tb19636.x