By Arieh Singer, Emilio Galan

ISBN-10: 0444536078

ISBN-13: 9780444536075

The purpose of this comprehenvise ebook is to present the most important effects accomplished within the examine of the clay minerals palygorskite and sepiolite. Palygorskite and sepiolite have came across to be important in a major number of business and clinical functions. consequently, learn on those clays has been intensified over the last 20 years, and important advances of their characterization were made. The e-book includes contributions from unusual scientists within the field.Comprehensive remedy of palygorskite and sepioliteCutting-edge developments in commercial minerals and applicationsWritten by means of uncommon scientists within the box

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Extra resources for Developments in Palygorskite-Sepiolite Research

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S. Krekeler{ *Department of Earth and Environmental Sciences, University of Illinois at Chicago, Chicago, Illinois, USA { Department of Geology, Miami University Hamilton, Hamilton, Ohio, USA 1. g. the biopyriboles, Zoltai, 1981), their affinities to the (layer) phyllosilicates are a valuable asset in comparative crystal chemistry. Bailey (1980), and to a much lesser extent Guggenheim and Eggleton (1988), made comparisons of palygorskite and sepiolite to ideal phyllosilicates or modulated phyllosilicates, respectively.

TEM of palygorskite–sepiolite group minerals for microtexture study is challenging owing to the high H2O content and the small crystallite size of most of these minerals, which make imaging and acquisition of selected area electron diffraction (SAED) data in the [100] direction difficult. 7 s) image capture by a charge-coupled device, beam damage of the sample is common. TEM data must be acquired with very low illumination. 1. Polysome-Width Disorder and the Transformation of Palygorskite to Smectite Variation in the width of polysomes can commonly be observed from heavily streaked SAED patterns.

1997) projected down the [001] direction in (A) and down [100] direction in (B). 55 per cell, signified in the label as a box). Part (B) better illustrates the discontinuous nature of the octahedral sheet because Na2 resides in the centre of the channel, and it is poorly linked to the octahedral ribbons via a site that contains mostly vacancies and some Ti. topology of the tetrahedral connectivity is sufficiently different that this mineral is not considered in detail here. Kalifersite is believed to be composed of two polysomes: a palygorskite- and a sepiolite-like polysome.

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Developments in Palygorskite-Sepiolite Research by Arieh Singer, Emilio Galan


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