粘土-方解石混合物:烧结和相形成

Mohamed Ali Hajjaji, S. Kacim
{"title":"粘土-方解石混合物:烧结和相形成","authors":"Mohamed Ali Hajjaji, S. Kacim","doi":"10.1179/096797804225012701","DOIUrl":null,"url":null,"abstract":"Abstract Clay - calcite mixes containing up to 20 wt-% calcite were fired at temperatures ranging from 800 to 1075 ° C and investigated by means of X-ray diffraction and scanning electron microscopy as well as by measuring some common ceramic properties. It was found that for < 10 wt-% calcite additions the sintering process is controlled by viscous flow, whereas at greater levels of addition sintering proceeds mainly by diffusion. Moreover, a metastable phase identified as grossular developed and disappeared at the expense of anorthite. The absence of wollastonite is also discussed. Attempts to predict phase formation on the basis of the CaOSiO2-Al2O3 phase diagram show that predictions hold only for the mixtures richest in calcite.","PeriodicalId":350675,"journal":{"name":"British Ceramic Transactions","volume":"29 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2004-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"23","resultStr":"{\"title\":\"Clay - calcite mixes: sintering and phase formation\",\"authors\":\"Mohamed Ali Hajjaji, S. Kacim\",\"doi\":\"10.1179/096797804225012701\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract Clay - calcite mixes containing up to 20 wt-% calcite were fired at temperatures ranging from 800 to 1075 ° C and investigated by means of X-ray diffraction and scanning electron microscopy as well as by measuring some common ceramic properties. It was found that for < 10 wt-% calcite additions the sintering process is controlled by viscous flow, whereas at greater levels of addition sintering proceeds mainly by diffusion. Moreover, a metastable phase identified as grossular developed and disappeared at the expense of anorthite. The absence of wollastonite is also discussed. Attempts to predict phase formation on the basis of the CaOSiO2-Al2O3 phase diagram show that predictions hold only for the mixtures richest in calcite.\",\"PeriodicalId\":350675,\"journal\":{\"name\":\"British Ceramic Transactions\",\"volume\":\"29 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2004-02-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"23\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"British Ceramic Transactions\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1179/096797804225012701\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"British Ceramic Transactions","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1179/096797804225012701","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 23

摘要

摘要:在800 ~ 1075℃的温度范围内烧制了方解石含量高达20%的粘土-方解石混合物,并通过x射线衍射和扫描电子显微镜以及测量一些常见的陶瓷性能进行了研究。研究发现,当方解石添加量< 10 wt-%时,烧结过程受粘性流动控制,而当方解石添加量较大时,烧结主要通过扩散进行。此外,以钙长石为代价,一个被确定为粗晶的亚稳相发育并消失。还讨论了硅灰石的缺乏。根据cao - al2o3相图预测相形成的尝试表明,预测只适用于方解石含量最丰富的混合物。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Clay - calcite mixes: sintering and phase formation
Abstract Clay - calcite mixes containing up to 20 wt-% calcite were fired at temperatures ranging from 800 to 1075 ° C and investigated by means of X-ray diffraction and scanning electron microscopy as well as by measuring some common ceramic properties. It was found that for < 10 wt-% calcite additions the sintering process is controlled by viscous flow, whereas at greater levels of addition sintering proceeds mainly by diffusion. Moreover, a metastable phase identified as grossular developed and disappeared at the expense of anorthite. The absence of wollastonite is also discussed. Attempts to predict phase formation on the basis of the CaOSiO2-Al2O3 phase diagram show that predictions hold only for the mixtures richest in calcite.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
CiteScore
0.10
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信