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dc.contributor.authorKaraismailoğlu, Meltem
dc.contributor.authorKutlu, Sena Zeynep
dc.contributor.authorDemir, T. U.
dc.date.accessioned2021-01-08T21:51:31Z
dc.date.available2021-01-08T21:51:31Z
dc.date.issued2020
dc.identifier.isbn9781536168136
dc.identifier.urihttps://hdl.handle.net/20.500.12846/324
dc.description.abstractHalloysite is a natural clay mineral that belongs to the kaolin group. Its chemical formula is Al2(OH)4Si2O5.nH2O. When n is equal to 2, it is hydrated, and when n is equal to 0, the halloysite is dehydrated. Generally, halloysite has a tubular structure; however, as a result of different deposits and crystallization conditions, this mineral can consist of spheroidal and plate-like particles. Its main deposits are in the United States, China, New Zealand, Mexico, Brazil, and Turkey where halloysite is formed by weathering or hydrothermal alteration of pumice, ultramafic, and volcanic rocks. Halloysite can be used in various fields due to its characteristic features. Primarily, this mineral is an ideal nanofiller for polymer composites. It is also utilized in the manufacture of ceramic wares and encapsulation of drugs in the pharmaceutical industry. Moreover, its higher specific surface area makes halloysite a good candidate for catalyst support. © 2020 Nova Science Publishers, Inc. All rights reserved.en_US
dc.language.isoengen_US
dc.publisherNova Science Publishers, Inc.en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectClay mineralen_US
dc.subjectHalloysiteen_US
dc.subjectKaoliniteen_US
dc.subjectOccurrenceen_US
dc.titleA general approach to halloysite clay mineralen_US
dc.typebookParten_US
dc.relation.journalHalloysite: Structure, Occurrence and Applicationsen_US
dc.relation.publicationcategoryKitap Bölümü - Uluslararasıen_US
dc.contributor.departmentTAÜ, Fen Fakültesi, Enerji Bilimi ve Teknolojileri Bölümüen_US
dc.contributor.institutionauthorKaraismailoğlu, Meltem
dc.identifier.startpage1en_US
dc.identifier.endpage15en_US


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