2011
DOI: 10.1016/b978-0-444-53607-5.00002-5
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Advances in the Crystal Chemistry of Sepiolite and Palygorskite

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Cited by 59 publications
(31 citation statements)
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“…As the octahedral sheet is discontinuous at each inversion of tetrahedra, oxygen atoms in the octahedra at the edge of the ribbons are coordinated to cations on the ribbon side only, and coordination and charge balance are completed along the channel by protons, coordinated water and a small number of exchangeable cations. Also, a variable amount of zeolitic water is contained in channels (Bradley, 1940;Alvarez, 1984;Krekeler and Guggenheim, 2008;Álvarez et al, 2011;Guggenheim and Krekeler, 2011;Suárez and García-Romero, 2011).…”
Section: Palygorskite and Sepiolitementioning
confidence: 99%
“…As the octahedral sheet is discontinuous at each inversion of tetrahedra, oxygen atoms in the octahedra at the edge of the ribbons are coordinated to cations on the ribbon side only, and coordination and charge balance are completed along the channel by protons, coordinated water and a small number of exchangeable cations. Also, a variable amount of zeolitic water is contained in channels (Bradley, 1940;Alvarez, 1984;Krekeler and Guggenheim, 2008;Álvarez et al, 2011;Guggenheim and Krekeler, 2011;Suárez and García-Romero, 2011).…”
Section: Palygorskite and Sepiolitementioning
confidence: 99%
“…The structural formula of sepiolite is Si 12 O 30 Mg 8 (OH) 4 (OH 2 ) 4 .nH 2 O (Brauner and Preisinger, 1956), where the four possible octahedral positions are occupied by Mg. Although sepiolite is an almost pure magnesian clay mineral, the existence of structural substitutions of Mg in the octahedral sheet by Al and Fe has been reported (García-Romero and Suárez, 2010;Suárez and García-Romero, 2011).…”
Section: Introductionmentioning
confidence: 95%
“…Few years later Van Olphen finally succeeded in producing a stable blue pigment, resembling Maya blue, by mixing and heating indigo with either palygorskite or sepiolite, both being fibrous clays with a tunnel structure [22]. Palygorskite is a magnesium aluminium phyllosilicate with ideal composition Si 8 O 20 (Al 2 Mg 2 ) (OH) 2 (OH 2 ) 4 •4H 2 O. Zeolite-like channels running along the fibres are filled by weakly bound, non-structural (zeolitic) water, while magnesium and aluminium cations complete their coordination with tightly bound water molecules (structural water) [23]. In sepiolite, a complex magnesium silicate (Si 12 O 30 Mg 8 (OH) 4 (OH 2 ) 4 (H 2 O) 8 ), the structure defines channels of 10.6 × 3.7 Å dimensions, wider with respect to palygorskite (6.4 × 3.7 Å) [24].…”
Section: Introductionmentioning
confidence: 99%