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Inorganic materials aluminosilicates

Two alternative explanations have been suggested which are both quite speculative. First, portions of mineral surfaces of intermediate polarity (e.g., siloxane regions, -Si-O-Si-) may permit some exchange of polar water and nonpolar organic sorbates (Hundal et al., 2001). Such surfaces occur in minerals like the faces of aluminosilicates. However, amorphous solids like silica (-Si-OH) and alumina (-A1-OH) have very hydrophilic exteriors when these inorganic materials are suspended in water. Yet these amorphous materials still clearly show sorption of apolar substances (e.g., Mills and Biggar, 1969a Schwarzenbach and Westall, 1981 Estes et al., 1988 Szecsody and Bales, 1989 Farrell et al., 1999). [Pg.410]

Organic and polymeric semiconductive materials also show a strong ER effect. They are generally electronic conductive materials with a rr-conjugated bond structure. It is believed that they have better dispersing ability compared to inorganic materials. However, the ER effect of organic and polymeric ER fluids is relatively weak compared to that of aluminosilicate materials. [Pg.657]

FIGURE 2.94 MAS NMR spectra of titanoaluminosilicate ETAS-10 with different Al/Ti ratios (curves 1-5). (Adapted from Rocha and Anderson, Eur. J. Inorg. Chem., 801, 2000) and aluminosilicate zeolite ZK-5 (curve 6) at Si/Al = 2.2 and from J. Mol. Struct., 441, Nakata, S., Tanaka, Y., Asaoka, S., and Nakamura, M., Recent advances in applications of multinuclear solid-state NMR to heterogeneous catalysis and inorganic materials, 267-281,1998, Copyright 1998, with permission from Elsevier.)... [Pg.447]

K-T. Lee and P.B. Aswath, Kinetics of the hexacelsian to celsian transformation in barium aluminosilicates doped with CaO, International Joumed of Inorganic Materials, 3,687 (2001). [Pg.88]

To illustrate the relationship between the two areas we will consider in detail the effect of coordinative unsaturation or underbonding at O in aluminosilicates on their structures, stabilities and properties, using examples from both inorganic chemistry and mineralogy. We use traditional methods of quantum chemistry in order to calculate the properties of such compounds. Similar relationships could be drawm between the bulk and surface structural properties of Fe (oxy)hydroxide) minerals and analog inorganic materials, but we will focus only upon the aluminosilicates, for which the structural and NMR data is most definitive. [Pg.166]

ILs can also be covalently immobilized on inorganic materials of silica, mesoporous silicates, aluminosilicate, and alumina. For that three ways are known (Scheme 10). The first method is the co-condensation of a trialkoxysdylalkyl onium salt and triethoxysilane (Scheme 10-A) [37-39]. The second one is the immobilization by the reaction between surface hydroxyl groups of the solid and the alkoxysilyl group (Scheme 10-B) [40,41]. For the last one (Scheme 10-C), the inorganic materials modified with alkyl halide (usually propylchloride) are used [42-46] on them, corresponding amine, phosphine, or pyridine can be immobilized and quaternized. For the preparation of imidazolium-based immobilized IL, imidazole is fixed on the modified support in the presence of alkali compounds, followed by quaternization with alkyl halides. [Pg.282]

Sealosafe A family of processes for encapsulating inorganic and organic wastes in a cementitious material suitable for landfill. The product, known as Stablex, is made from a cement and an aluminosilicate and may incorporate pulverized fly ash. Developed by C. Chappell in the United Kingdom in the 1970s and now operated in a number of countries. Offered by the Stablex Corporation, Radnor, PA. The environmental acceptability of the product has since been criticized. [Pg.239]


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Aluminosilicate

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