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Other sources of fluoride ion

Fluorides are used as anticarie agents in toothpastes since they reduce decay by increasing the strength of teeth. Sodinm fluoride, NaF, is the most commonly used fluoride. However, the literature mentions several other sources of fluoride ions such as potassium fluoride, lithium fluoride, aluminum fluoride, zinc flnoride, sodium monofluorophosphate, acidic phosphate fluoride, ammonium fluoride, titanium tetrafluoride, and amine flnoride. [Pg.488]

The carbanions formed by scission of a C-Si bond with TASF can also be oxygenated. Benzylic trimethylsilyl groups can be converted to hydroxyl groups in 20-95% yield by reaction with TASF(Me) in the presence of oxygen and Trimethyl Phosphite (eq 17). No other source of fluoride ion was found that could replace TASF. [Pg.466]

The proton exchange membrane can be a source of fluoride ions as well [143]. Hydroxyl radicals, formed via crossover gases or reactions of hydrogen peroxide with Fenton-active contaminants (e.g., Fe +), could attack the backbone of Nafion, causing the release of fluoride anions these anions in turn promote corrosion of the fuel cell plates and catalyst, and release transition metals into the fuel cell [143]. Transition metal ions, such as Fe, then catalyze the formation of radicals within the Nafion membrane, resulting in a further release of fluoride anions. On the other hand, transition metal ions also can cause decreased membrane and ionomer conductivity in catalyst layers, as discussed in section 2.4 of this chapter. [Pg.75]

In an attempt to produce TS-1 at low cost, alternative, cheaper sources of Ti and Si and other bases such as binary mixtures of (tetrabutylammonium and tetraethylammonium hydroxides), (tetrabutylphosphonium and tetraethylpho-sphonium hydroxides), (tetrapropylammonium bromide and ammonia, water, hexanediamine, n-butylamine, diethylamine, ethylenediamine, or triethanolamine) in place of TPAOH have been used (284—294). TS-1 was synthesized in the presence of fluoride ions but the material thus formed contained extraframework Ti species (295-297). [Pg.166]

Hydrothermal synthesis of microporous compounds in the presence of fluoride source refers to the hydrothermal or solvothermal crystallization of aluminosilicate zeolites or microporous aluminophosphate such as AlP04-n series in the presence of a fluoride source. The successful introduction of fluoride ion into the hydrothermal or solvothermal synthesis of microporous materials paves the way for the introduction of other complex-ion or chelation agent s to the hydrothermal crystallization of microporous compounds. [Pg.161]

The main source of fluoride in ground water is fluoride-bearing rocks such as fluorospar, fluorite, eiyolite, fluorapatite and hydroxylapatite [12]. The flouride content in ground water is a function of several faetors including hydrogeological environment, solubility of fluoride minerals in water, velocity of flowing water, pH, temperature as well as coneentrations of other species such as calcium and bicarbonate ions in water [13,14]. [Pg.115]

It has been shown4l that the reaction of [ReMe(CO)s] with Ph3CPP6 or Et20 HPF6 in dichloromethane produces the complex, [(CO)5Re((i-F)Re(CO)s][PF6]. The source of the bridging fluoride ligand is the PF6 ion. Other examples of fluoride abstraction from the normally inert PFg" and BF4 ions,42-45 as well as examples of facile PFe hydrolysis, are found in the literature. [Pg.47]

In the case of molten salts, the functional electrolytes are generally oxides or halides. As examples of the use of oxides, mention may be made of the electrowinning processes for aluminum, tantalum, molybdenum, tungsten, and some of the rare earth metals. The appropriate oxides, dissolved in halide melts, act as the sources of the respective metals intended to be deposited cathodically. Halides are used as functional electrolytes for almost all other metals. In principle, all halides can be used, but in practice only fluorides and chlorides are used. Bromides and iodides are thermally unstable and are relatively expensive. Fluorides are ideally suited because of their stability and low volatility, their drawbacks pertain to the difficulty in obtaining them in forms free from oxygenated ions, and to their poor solubility in water. It is a truism that aqueous solubility makes the post-electrolysis separation of the electrodeposit from the electrolyte easy because the electrolyte can be leached away. The drawback associated with fluorides due to their poor solubility can, to a large extent, be overcome by using double fluorides instead of simple fluorides. Chlorides are widely used in electrodeposition because they are readily available in a pure form and... [Pg.697]

These rod-shaped ligands share a sterically efficient terminal N-donor and their divalent Co chemistry is well established. They will be discussed here only with selected examples. [Co (NCMe)6](TFPB)2 (TFPB- = tetrakis(3,5-bis(trifhioromethyl)phenyl)borate)) has been synthesized and characterized in the solid state along with a number of other divalent transition metal analogs.357 As a result of the extremely poor coordinating ability of the anion and facile loss of MeCN ligands from the cation, the salt is an excellent source of naked Co2+ ions. Thermolysis up to 100 °C leads to the loss of one MeCN and formation of a r -bound nitrile, whereas above 130 °C decomposition occurs with loss of MeCN and abstraction of fluoride from the anion to form CoF2. [Pg.38]

Fluoride is a natural component of most types of soil, in which it is mainly bound in complexes and not readily leached. The major source of free fluoride ion in soil is the weathering and dissolution of fluoride rich rock that depends on the natural solubility of the fluoride compound in question, pH, and the presence of other minerals and compounds and of water. The major parameters that control fluoride fixation in soil through adsorption, anion exchange, precipitation, formation of mixed solids and complexes are aluminium, calcium, iron, pH, organic matter and clay [19,20]. [Pg.491]

Tris(dimethylam1no)sulfonium difluorotrimethylsilicate is a source of soluble organic fluoride ion of high anionic reactivity. Fluoride ion from this salt and other tris(dialkylamino)sulfonium difluorotrimethyl si 11 cates has... [Pg.223]

Various oligomers of fluorinated alkenes and cycloalkenes have been prepared by fluoride ion induced oligomerisation of various monomers (Sect. 5.3), and the chemistry of these systems provides some unique reactions. The oligomers of special interest here may be described as of types (95) or (96) (Scheme 59), i. e. systems with either four (95) or three (96) perfluoro-alkyl or -cycloalkyl groups attached to the double bond, whereas systems with two perfluoroalkyl groups attached, i. e. (97) and (98), have a chemistry more similar to fluorinated alkenes that may be derived from other sources. [Pg.27]


See other pages where Other sources of fluoride ion is mentioned: [Pg.82]    [Pg.340]    [Pg.49]    [Pg.741]    [Pg.82]    [Pg.340]    [Pg.49]    [Pg.741]    [Pg.303]    [Pg.202]    [Pg.93]    [Pg.303]    [Pg.1005]    [Pg.109]    [Pg.249]    [Pg.43]    [Pg.17]    [Pg.114]    [Pg.28]    [Pg.162]    [Pg.163]    [Pg.164]    [Pg.538]    [Pg.598]    [Pg.24]    [Pg.323]    [Pg.61]    [Pg.546]    [Pg.168]    [Pg.3]    [Pg.23]    [Pg.323]    [Pg.244]    [Pg.223]    [Pg.61]    [Pg.25]    [Pg.236]    [Pg.4]    [Pg.42]    [Pg.1214]    [Pg.20]   


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Fluoride ion

Fluoride source

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