高岭石粘土中伴生矿物对其作为补充胶凝材料的理化特性的影响

IF 3.9 3区 工程技术 Q2 CONSTRUCTION & BUILDING TECHNOLOGY
Mehnaz Dhar, Shashank Bishnoi
{"title":"高岭石粘土中伴生矿物对其作为补充胶凝材料的理化特性的影响","authors":"Mehnaz Dhar,&nbsp;Shashank Bishnoi","doi":"10.1617/s11527-025-02790-y","DOIUrl":null,"url":null,"abstract":"<div><p>Clays in their natural state are complex and often occur as mixtures of clay and non-clay minerals. Medium-grade kaolinite clays that are feasible for supplementary cementitious material (SCM) applications contain various associated minerals that can affect their behavior. This study explores how associated minerals viz., iron, illite and quartz impact the physical and chemical properties both raw and after calcination at 600 °C, 700 °C, 800 °C, 900 °C, and 1000 °C using thermal analysis, XRD, FTIR and pozzolanic reactivity techniques. The results show that associated minerals influence the crystallinity, specific surface area and water demand of kaolinite clays. Iron rich kaolinite clays are found to be highly disordered and show higher specific surface area and water demand than quartz rich clays. The effect of associated minerals on the formation temperature of metakaolin was also observed as iron rich kaolinite showed conversion at lower temperatures when compared to quartz rich kaolinite. The catalytic role of iron in the metakaolin formation is confirmed by its interaction with the kaolinite structure in model iron rich clay system using EPR technique. The optimal calcination temperature of kaolinite varies depending on the associated minerals and a positive effect of illite impurities on the pozzolanic reactivity of low-grade kaolinite clay has been observed.</p></div>","PeriodicalId":691,"journal":{"name":"Materials and Structures","volume":"58 8","pages":""},"PeriodicalIF":3.9000,"publicationDate":"2025-09-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The impact of associated minerals in kaolinite clays on their physico-chemical characteristics for use as supplementary cementitious material\",\"authors\":\"Mehnaz Dhar,&nbsp;Shashank Bishnoi\",\"doi\":\"10.1617/s11527-025-02790-y\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Clays in their natural state are complex and often occur as mixtures of clay and non-clay minerals. Medium-grade kaolinite clays that are feasible for supplementary cementitious material (SCM) applications contain various associated minerals that can affect their behavior. This study explores how associated minerals viz., iron, illite and quartz impact the physical and chemical properties both raw and after calcination at 600 °C, 700 °C, 800 °C, 900 °C, and 1000 °C using thermal analysis, XRD, FTIR and pozzolanic reactivity techniques. The results show that associated minerals influence the crystallinity, specific surface area and water demand of kaolinite clays. Iron rich kaolinite clays are found to be highly disordered and show higher specific surface area and water demand than quartz rich clays. The effect of associated minerals on the formation temperature of metakaolin was also observed as iron rich kaolinite showed conversion at lower temperatures when compared to quartz rich kaolinite. The catalytic role of iron in the metakaolin formation is confirmed by its interaction with the kaolinite structure in model iron rich clay system using EPR technique. The optimal calcination temperature of kaolinite varies depending on the associated minerals and a positive effect of illite impurities on the pozzolanic reactivity of low-grade kaolinite clay has been observed.</p></div>\",\"PeriodicalId\":691,\"journal\":{\"name\":\"Materials and Structures\",\"volume\":\"58 8\",\"pages\":\"\"},\"PeriodicalIF\":3.9000,\"publicationDate\":\"2025-09-29\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Materials and Structures\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://link.springer.com/article/10.1617/s11527-025-02790-y\",\"RegionNum\":3,\"RegionCategory\":\"工程技术\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"CONSTRUCTION & BUILDING TECHNOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Materials and Structures","FirstCategoryId":"5","ListUrlMain":"https://link.springer.com/article/10.1617/s11527-025-02790-y","RegionNum":3,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"CONSTRUCTION & BUILDING TECHNOLOGY","Score":null,"Total":0}
引用次数: 0

摘要

粘土在自然状态下是复杂的,通常是粘土和非粘土矿物的混合物。中等品位的高岭石粘土是可行的补充胶凝材料(SCM)的应用含有各种伴生矿物,可以影响其行为。本研究利用热分析、XRD、FTIR和火山灰反应技术,探讨了伴生矿物(即铁、伊利石和石英)在600°C、700°C、800°C、900°C和1000°C煅烧后对原料和物理化学性能的影响。结果表明,伴生矿物影响高岭石粘土的结晶度、比表面积和需水量。富铁高岭石粘土具有高度的无序性,比表面积和需水量均高于富石英粘土。伴生矿物对偏高岭土形成温度的影响也被观察到,富铁高岭土比富石英高岭土在更低的温度下发生转化。利用EPR技术,通过铁与模型富铁粘土体系中高岭石结构的相互作用,证实了铁在偏高岭土形成过程中的催化作用。高岭石的最佳煅烧温度随伴生矿物的不同而不同,并且观察到伊利石杂质对低品位高岭石粘土的火山灰反应性有积极影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The impact of associated minerals in kaolinite clays on their physico-chemical characteristics for use as supplementary cementitious material

Clays in their natural state are complex and often occur as mixtures of clay and non-clay minerals. Medium-grade kaolinite clays that are feasible for supplementary cementitious material (SCM) applications contain various associated minerals that can affect their behavior. This study explores how associated minerals viz., iron, illite and quartz impact the physical and chemical properties both raw and after calcination at 600 °C, 700 °C, 800 °C, 900 °C, and 1000 °C using thermal analysis, XRD, FTIR and pozzolanic reactivity techniques. The results show that associated minerals influence the crystallinity, specific surface area and water demand of kaolinite clays. Iron rich kaolinite clays are found to be highly disordered and show higher specific surface area and water demand than quartz rich clays. The effect of associated minerals on the formation temperature of metakaolin was also observed as iron rich kaolinite showed conversion at lower temperatures when compared to quartz rich kaolinite. The catalytic role of iron in the metakaolin formation is confirmed by its interaction with the kaolinite structure in model iron rich clay system using EPR technique. The optimal calcination temperature of kaolinite varies depending on the associated minerals and a positive effect of illite impurities on the pozzolanic reactivity of low-grade kaolinite clay has been observed.

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
Materials and Structures
Materials and Structures 工程技术-材料科学:综合
CiteScore
6.40
自引率
7.90%
发文量
222
审稿时长
5.9 months
期刊介绍: Materials and Structures, the flagship publication of the International Union of Laboratories and Experts in Construction Materials, Systems and Structures (RILEM), provides a unique international and interdisciplinary forum for new research findings on the performance of construction materials. A leader in cutting-edge research, the journal is dedicated to the publication of high quality papers examining the fundamental properties of building materials, their characterization and processing techniques, modeling, standardization of test methods, and the application of research results in building and civil engineering. Materials and Structures also publishes comprehensive reports prepared by the RILEM’s technical committees.
×
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:604180095
Book学术官方微信