By Arieh Singer, Emilio Galan
The purpose of this comprehenvise publication is to present the most important effects completed within the learn of the clay minerals palygorskite and sepiolite. Palygorskite and sepiolite have chanced on to be helpful in a big number of commercial and scientific functions. consequently, examine on those clays has been intensified over the last twenty years, and important advances of their characterization were made. The e-book comprises contributions from uncommon scientists within the field.Comprehensive remedy of palygorskite and sepioliteCutting-edge developments in commercial minerals and applicationsWritten through exclusive scientists within the box
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Additional resources for Developments in Palygorskite-Sepiolite Research
Thus, consideration of structural parameters, which generally involve averaging, is probably more fruitful than direct comparisons of individual distances and angles. , 2002). Both minerals have palygorskite-like Si tetrahedral frameworks, and both contain Na, Mn, and Ti, but tuperssuatsiaite is Fe rich. The octahedral backbone in raite (Figure 2) consists of a continuous strip of Mn octahedra (Mn1, Mn2) along the  direction with appendages of Na octahedra (Na1) on either side of the strip to form the octahedral part of the polysome.
25, 405–410. , 2002. The structure of Mnrich tuperssuatsiaite: a palygorskite-related mineral. Am. Mineral. 87, 1458–1463. , 1997. Textural transition and genetic relationship between precursor stevensite and sepiolite in lacustrine sediments (Jbel Rhssoul, Morocco). Clays Clay Miner. 45, 378–389.
2002. Formation of sepiolite-palygorskite and related minerals from solution. Clays Clay Miner. 50, 736–745. , 1971. Precipitation of deep-sea palygorskite and sepiolite. Earth Planet. Sci. Lett. 11, 324–332. , 1940. The structural scheme of attapulgite. Am. Mineral. 25, 405–410. , 2002. The structure of Mnrich tuperssuatsiaite: a palygorskite-related mineral. Am. Mineral. 87, 1458–1463. , 1997. Textural transition and genetic relationship between precursor stevensite and sepiolite in lacustrine sediments (Jbel Rhssoul, Morocco).