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Relationship between rheological properties of slurries and pore size distribution of cast and compressed compacts of mullite

机译:浆料的流变性质与莫来石铸坯和压缩坯的孔径分布之间的关系

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Mullite slurries with varying particle size, solid fraction and dispersant content were cast, dried and subsequently compressed to obtain a series of green compacts. The relationship between the rheological properties of slurries and pore size distribution of the green compacts was examined. Slip cast bodies obtained from shear thinning slurries have larger total pore volume, which decreases considerably with increasing pressure during post-compression. The ratio of the median pore diameter of the compact to the median particle size is higher on the as-cast bodies obtained from shear thinning slurries than on those from Newtonian ones. The difference of the ratio becomes smaller with increasing post-compressive pressure. The agglomerates in the slurry affect the dried green casts and hinder the densification. The effect of agglomerates decreases considerably during subsequent mechanical compaction, yet remains at a compressive pressure as high as 196 MPa.
机译:将具有不同粒径,固形分率和分散剂含量的莫来石浆液进行浇铸,干燥并随后压制以获得一系列生坯。检查了浆料的流变性质与生坯的孔径分布之间的关系。由剪切稀浆获得的滑模坯体具有较大的总孔体积,其在后压缩期间随着压力的增加而显着减小。由剪切稀化浆料得到的铸态坯体中的压坯的中值孔径与中值粒径的比高于从牛顿型的铸态坯体。比率的差随着后压缩压力的增加而变小。浆料中的附聚物影响干燥的生坯并阻碍致密化。在随后的机械压实过程中,附聚物的作用大大降低,但仍保持在高达196 MPa的压缩压力下。

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