Spectroscopic investigations of delaminated and intercalated phyllosilicates (Record no. 2997414)

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control field https://directory.doabooks.org/handle/20.500.12854/59832
005 - DATE AND TIME OF LATEST TRANSACTION
control field 20220714175344.0
020 ## - INTERNATIONAL STANDARD BOOK NUMBER
International Standard Book Number KSP/1000003440
020 ## - INTERNATIONAL STANDARD BOOK NUMBER
International Standard Book Number 3937300589
024 7# - OTHER STANDARD IDENTIFIER
Standard number or code 10.5445/KSP/1000003440
Terms of availability doi
041 0# - LANGUAGE CODE
Language code of text/sound track or separate title English
042 ## - AUTHENTICATION CODE
Authentication code dc
100 1# - MAIN ENTRY--PERSONAL NAME
Personal name Friedrich, Frank
Relator code auth
9 (RLIN) 528415
245 10 - TITLE STATEMENT
Title Spectroscopic investigations of delaminated and intercalated phyllosilicates
260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT)
Name of publisher, distributor, etc KIT Scientific Publishing
Date of publication, distribution, etc 2005
300 ## - PHYSICAL DESCRIPTION
Extent 1 electronic resource (VIII, 150 p. p.)
506 0# - RESTRICTIONS ON ACCESS NOTE
Terms governing access Open Access
Source of term star
Standardized terminology for access restriction Unrestricted online access
520 ## - SUMMARY, ETC.
Summary, etc The characteristic feature of phyllosilicates like muscovite (KAl2[Si3AlO10(OH)2] is their layered structure. Due to the resulting anisotropic optical and electrical properties this mineral is an important raw material in paint industries and polymer composites.Crucial for many of these properties is on one hand a high aspect ratio of the stacks, which will be enhanced by delamination of the mineral. On the other hand the exchange of the interlayer cations like potassium changes the chemical properties of the muscovite, its refraction behaviour and surface properties. But these interlayer cations are difficult to access and are not exchangeable under normal conditions.Thus a process for the intercalation of cations like Cu2+, Mg2+ or Zn2+ from super saturated nitrate solutions in autoclaves was developed to reveal a chemically modified mica phase.The extensive modification of the muscovite structure, due to the intercalation is monitored by X-ray diffractometry and several spectroscopic methods. The XRD results strongly suggest the formation of an intercalated irregular mixed-layer phase. This is proven by far infrared spectroscopy which show the simultaneous occurrence of both K+ and Cu2+ in the interlayer region, strongly increasing the interlayer space.1Investigations in the mid infrared region using diffuse reflectance spectroscopy (DRIFT) suggest a further migration of the intercalated cations deep into the ditrigonal holes of the tetrahedral sheet and their fixation within these holes close to the OH groups.
540 ## - TERMS GOVERNING USE AND REPRODUCTION NOTE
Terms governing use and reproduction All rights reserved
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546 ## - LANGUAGE NOTE
Language note English
653 ## - INDEX TERM--UNCONTROLLED
Uncontrolled term Spektroskopie
653 ## - INDEX TERM--UNCONTROLLED
Uncontrolled term Interkalation
653 ## - INDEX TERM--UNCONTROLLED
Uncontrolled term Phyllosilicate
653 ## - INDEX TERM--UNCONTROLLED
Uncontrolled term Delamination
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Host name www.oapen.org
Uniform Resource Identifier <a href="https://www.ksp.kit.edu/3937300589">https://www.ksp.kit.edu/3937300589</a>
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Host name www.oapen.org
Uniform Resource Identifier <a href="https://directory.doabooks.org/handle/20.500.12854/59832">https://directory.doabooks.org/handle/20.500.12854/59832</a>
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Public note DOAB: description of the publication
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