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Effect of Sintering Atmosphere on the a/p-Transformation of Si_3N_4

机译:烧结气氛对Si_3N_4 a / p转变的影响

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Effect of carbon and CO gas atmosphere on a-SiAlON generation in the surface of a β-Si_3N_4 ceramics was investigated. Silicon nitride ceramics having the composition, Si_3N_4 92-Y_2O_3 5-Al_2O_3 3 (mass%), was sintered at 1750℃ for 2h. in four sagger conditions under a N_2 pressure of 0.1-100 MPa. The four conditions were in a carbon sagger with carbon powder-bed, in a carbon sagger without powder-bed, in a BN sagger without powder-bed and in a BN sagger with Si_3N_4/BN mixed powder-bed. The 100% β-Si_3N_4 ceramics, which were sintered in the BN sagger with Si_3N_4/BN mixed powder-bed, were heated under the N_2 pressure of 0.1-100 MPa in the same four sagger. The crystal phases of the ceramics were influenced by the N_2 pressure and the sagger conditions. A SiC thin layer was formed in the surface of the β-Si_3N_4 ceramics when the 100% β-Si_3N_4 ceramics were heated at 1750℃ for 2h. in a carbon powder under a N_2 pressure of 0.1 MPa. In the inner part of the ceramics under the SiC lay er, α-SiAlON and melilite (Si_3N_4 ·Y_2O_3) were generated. These were observed to a depth of 60-70μm from the surface after peeling the SiC layer. The a-SiAlON and melilite are thought to be generated by the following mechanism,: The SiC layer excludes the liquid phase including Y and Al, which are in the grAlN boundary of the β-Si_3N_4, from the layer. Then, the liquid phase concentrates between the SiC layer and the β-Si_3N_4 bulk, and Y and Al in the liquid phase react with β-Si_3N_4, and α-SiA10N and melilite are formed.
机译:研究了碳和CO气体气氛对β-Si_3N_4陶瓷表面a-SiAlON生成的影响。将具有Si_3N_4 92-Y_2O_3 5-Al_2O_3 3(质量%)的组成的氮化硅陶瓷在1750℃下烧结2h。在N-100压力为0.1-100 MPa的四个苛刻条件下。这四个条件分别是:带有碳粉床的碳刀,没有粉床的碳刀,没有粉床的BN刀和带有Si_3N_4 / BN混合粉床的BN刀。将在100N的Si_3N_4 / BN混合粉末床的BN晶格中烧结的100%β-Si_3N_4陶瓷在相同的4晶格中在0.1-100 MPa的N_2压力下加热。陶瓷的晶相受N_2压力和摇动条件的影响。当将100%β-Si_3N_4陶瓷在1750℃下加热2h时,在β-Si_3N_4陶瓷的表面形成SiC薄层。在N压力为0.1 MPa的碳粉中加入碳。在SiC层下的陶瓷内部,生成了α-SiAlON和硅沸石(Si_3N_4·Y_2O_3)。在剥离SiC层之后,从表面观察到深度为60-70μm。认为a-SiAlON和陨石是通过以下机理生成的:SiC层从该层中排除了包括Y和Al的液相,其中Y和Al在β-Si_3N_4的grAlN边界内。然后,液相集中在SiC层和β-Si_3N_4块之间,并且液相中的Y和Al与β-Si_3N_4反应,并形成α-SiA10N和沸石。

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