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FLUORINE (symbol F, atomic weight 19)

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Originally appearing in Volume V10, Page 578 of the 1911 Encyclopedia Britannica.
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FLUORINE (See also:symbol F, atomic See also:weight 19) , a chemical See also:element of the halogen See also:group. It is never found in the uncombined See also:condition, but in See also:combination with See also:calcium as fluor-spar CaF2 it is widely distributed; it is also found in See also:cryolite Na3AlF6, in fluor-See also:apatite, CaF2.3Ca3P2O8, and in See also:minute traces in See also:sea-See also:water, in some See also:mineral springs, and as a constituent of the See also:enamel of the See also:teeth. It was first isolated by H. See also:Moissan in 1886 by the See also:electrolysis of pure anhydrous hydrofluoric See also:acid containing dissolved See also:potassium fluoride. The U-shaped electrolytic See also:vessel and the electrodes are made of an alloy of See also:platinum-See also:iridium, the limbs of the See also:tube being closed by stoppers made of fluor-spar, and fitted with two lateral exit tubes for carrying off the gases evolved. Whilst the. electrolysis is proceeding, the apparatus is kept at a See also:constant temperature of – 23° C. by means of liquid methyl chloride. The fluorine, which is liberated as a See also:gas at the anode, is passed through a well cooled platinum vessel, in See also:order to See also:free it from any acid fumes that may be carried over, and finally through two platinum tubes containing See also:sodium fluoride to remove the last traces of hydrofluoric acid; it is then collected in a platinum tube closed with fluor-spar plates. B. Brauner (Jour. Chem. See also:Soc., 1894, 65, p. 393) obtained fluorine by See also:heating potassium fluorplumbate 3KF•HF•PbF4.

At 200° C. this See also:

salt decomposes, giving off hydrofluoric acid, and between 230–250° C. fluorine is liberated. Fluorine is a See also:pale greenish-yellow gas with a very See also:sharp See also:smell; its specific gravity is 1.265 (H. Moissan); it has been liquefied, the liquid also being of a yellow See also:colour and boiling at -187° C. It is the most active of all the chemical elements; in contact with See also:hydrogen combination takes See also:place between the two gases with explosive violence, even in the dark, and at as See also:low a temperature as -21o° C.; finely divided See also:carbon See also:burns in the gas, forming carbon tetrafluoride; water is decomposed even at See also:ordinary temperatures, with the formation of hydrofluoric acid and " ozonised " See also:oxygen; See also:iodine, See also:sulphur and See also:phosphorus melt and then inflame in the gas; it liberates See also:chlorine from chlorides, and combines with most metals instantaneously to See also:form fluorides; it does not, however, combine with oxygen. Organic compounds are rapidly attacked by the gas. Only one See also:compound of hydrogen and fluorine is known, namely hydrofluoric acid, HF or H2F2, which was first obtained by C. See also:Scheele in 1771 by decomposing fluor-spar with concentrated sulphuric acid, a method still used for the commercial preparation of the aqueous See also:solution of the acid, the mixture being distilled from leaden retorts and the acid stored in leaden or See also:gutta-percha bottles. The perfectly anhydrous acid is a very volatile colour-less liquid and is best obtained, according to G. See also:Gore (Phil. Trans., 1869, p. 173) by decomposing the See also:double fluoride of hydrogen and potassium, at a red See also:heat in a platinum See also:retort fitted with a platinum See also:condenser surrounded by a freezing mixture, and having a platinum See also:receiver luted on. It can also be prepared in the anhydrous condition by passing a current of hydrogen over dry See also:silver fluoride.

The pure acid thus obtained is a most dangerous substance to handle, its vapour even when highly diluted with See also:

air having an exceedingly injurious See also:action on the See also:respiratory See also:organs, whilst inhalation of the pure vapour is followed by See also:death. The anhydrous acid boils at 19°.5 C. (H. Moissan), and on cooling, sets to a solid See also:mass at -102°•5 C., which melts at–92°•3 C. (K. Olszewski, Monats. See also:fur Chemie, 1886, 7, p. 371). Potassium and sodium readily dissolve in the anhydrous acid with See also:evolution of hydrogen and formation of fluorides. The aqueous solution is strongly acid to See also:litmus and dissolves most metals directly. Its most important See also:property is that it rapidly attacks See also:glass, reacting with the See also:silica of the glass to form gaseous See also:silicon fluoride, and consequently it is used for See also:etching. T. E.

See also:

Thorpe (Jour. Chem. Soc., 1889, 55, p. 163) determined the vapour See also:density of hydrofluoric acid at different temperatures, and showed that there is no approach to a definite value below about 88° C. where it reaches the value 10.29 corresponding to the molecular See also:formula HF; at temperatures below 88° C. the value increases rapidly, showing that the See also:molecule is more complex in its structure. (For references see J. N. Friend, The Theory of See also:Valency (1909), p. III.) The aqueous solution behaves on concentration similarly to the other halogen -acids; E. Deussen (Zeit. anorg. Chem., 1905, 44, pp. 300, 408; 1906, 49, p. 297) found the solution of constant boiling point to contain 43.2% HF and to See also:boil at IIo° (75o mm.).

The salts of hydrofluoric acid are known as fluorides and are easily obtained by the action of the acid on metals or their oxides, hydroxides or See also:

carbonates. The fluorides of the See also:alkali metals, of silver, and of most of the heavy metals are soluble in water; those of the alkaline earths are insoluble. A characteristic property of the alkaline fluorides is their See also:power of combining with a molecule of hydrofluoric acid and with the fluorides of the more electro-negative elements to form double fluorides, a behaviour not shown by other metallic halides. Fluorides can be readily detected by their power of etching glass when warmed with sulphuric acid; or by warming them in a glass tube with concentrated sulphuric acid and holding a moistened glass See also:rod in the mouth of the tube, the water apparently gelatinizes owing to the decomposition of the silicon fluoride formed. The atomic weight of fluorine has been determined by the See also:con-version of calcium, sodium and potassium fluorides into the corresponding sulphates. J. See also:Berzelius, by converting silver fluoride into silver chloride, obtained the value 19.44, and by analysing calcium fluoride the value 19.16; the more See also:recent See also:work of H. Moissan gives the value 19.05. See H. Moissan, Le Fluor et ses composes (See also:Paris, 1900). FLUOR-SPAR, native calcium fluoride (CaF2), known also as FLUORITE or simply FLUOR. In See also:France it is called fluorine, whilst the See also:term fluor is applied to the element (F).

All these terms, from the See also:

Lat. fluere, " to flow," recall the fact that the spar is useful as a See also:flux in certain metallurgical operations. (Cf. its Ger. name Flussspat or Fluss.) Fluor-spar crystallizes in the cubic See also:system, commonly in cubes, either alone or combined with the See also:octahedron, rhombic See also:dodecahedron, four-faced See also:cube, &c. The four-faced cube has been called-the fluoroid. In fig. 1, a is the cube (See also:loo), d the rhombic dodecahedron (11o), and f the four-faced cube (310). Fig. 2 shows a characteristic twin of interpenetrant cubes. The crystals are sometimes polysynthetic, a large octahedron, e.g., being built up of small cubes. The faces are often etched or corroded. Cleavage is nearly always perfect, parallel to the octahedron. Fluor-spar has a hardness of 4, so that it is scratched by a See also:knife, though not so readily as See also:calcite. Its specific gravity is about 3.2.

The colour is very variable, and often beautiful, but the mineral is too soft for See also:

personal decoration, though it forms a handsome material for vases, &c. In some fluor-spar the colour is disposed in bands, regularly following the See also:contour of the crystal. As the colour is usually expelled, or much altered, by heat, it is believed to be due to an organic pigment, and the presence of See also:hydrocarbons has been detected in many specimens by G. Wyrouboff, and other observers. H. W. See also:Morse (Prot. Amer. Acad., 1906, p. 587)obtained carbon monoxide and dioxide, hydrogen and See also:nitrogen and small quantities of oxygen from Weardale specimens by heating. He concluded that the gases are due to the decomposition of an organic colouring See also:matter, which has, however, no connexion with the See also:fluorescence or thermo-luminescence of the mineral. Certain crystals from See also:Cumberland are beautifully fluorescent, appearing See also:purple with a bluish See also:internal haziness by reflected See also:light, and greenish by transmitted light.

Fluor-spar, though cubic, sometimes exhibits weak double See also:

refraction, probably due to internal tension. Many kinds of fluor-spar are thermo-luminescent, i.e. they glow on exposure to a moderate heat, and the name of chlorophane has been given to a variety which exhibits a See also:green glow. The mineral also phosphoresces under the See also:Rontgen rays. Cavities containing liquid occasionally occur in crystals of fluor-spar, notably in the greasy green cubes of Weardale in See also:Durham. A dark See also:violet fluor-spar from WSlsendorf in See also:Bavaria, evolves an odour of See also:ozone when struck, and has been called antozonite. Ozone is also emitted by a violet fluor-spar from Quincie, dep. See also:Rhone, France. In both cases the spar evolves free fluorine, which ozonizes the air. Fluor-spar is largely employed by the metallurgist, especially in See also:lead-smelting, and in the See also:production of ferro-silicon and ferro-See also:manganese. It is also used in See also:iron and See also:brass foundries, and has been found useful as a flux for certain See also:gold-ores and in the reduction of See also:aluminium. It is used as a source of hydrofluoric acid, which it evolves when heated with sulphuric acid. The mineral is also used in the production of See also:opal glass and enamel See also:ware.

In consequence of its low refractive and dispersive power, colourless pellucid fluor-spar is valuable in the construction of apochromatic lenses, but this variety is rare. The dark violet fluor-spar of See also:

Derbyshire, known locally as " See also:Blue See also:John," is prized for ornamental purposes. It occurs almost exclusively at See also:Tray Cliff, near See also:Castleton. The dark purple spar, called by the workmen " See also:bull See also:beef," may be changed, by heat, to a See also:rich amethystine tint. Being very brittle, the spar is rather difficult to work on the See also:lathe, and is often toughened by means of See also:resin. F. Corsi, the eminent See also:Italian See also:antiquary, held that fluor-spar was the material of the famous murrhine vases. Fluor-spar is a mineral of very wide See also:distribution. Some of the finest crystals occur in the lead-See also:veins of the Carboniferous See also:Limestone See also:series in the See also:north of See also:England, especially at Weardale, Allendale and See also:Alston See also:Moor. It is also found in the lead and See also:copper-mines of See also:Cornwall and S. See also:Devon, notably near See also:Liskeard, where See also:fine crystals have been found, with faces of the six-faced octahedron replacing the corners of the cube. In Cornwall fluor-spar is known to the miners as " cann." Fine yellow fluor-spar occurs in some of the Saxon mines, and beautiful See also:rose-red octahedra are found in the See also:Alps, near Goschenen.

Many localities in the See also:

United States yield fluor-spar, and it is worked commercially in a few places, notably at Rosiclare in See also:southern See also:Illinois.

End of Article: FLUORINE (symbol F, atomic weight 19)

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