Page:Encyclopædia Britannica, Ninth Edition, v. 14.djvu/721

 L I T L I T 097 present ; A Survey of London and England s State, 1643 ; Relation of the Siege of Newcastle, 1645. His poetical remains, collected by James Maidment, were published at Edinburgh in 1803. LITHIUM, one of the rarer metallic elements, intermediate in its character between sodium and barium. It was discovered in 1817 by Arfvedson in the course of an analysis of petalite in Berzelius s laboratory. He recognized the presence in this mineral of a new kind of alkali, which his master subsequently named &quot; lithia,&quot; to denote its mineral origin. Lithia, though widely dis seminated throughout the mineral world traces of it being found in almost all alkaliferous silicates, in the soils derived from these, and in many mineral waters nowhere occurs in any abundance, except in the immense masses of lithia-mica (lepidolite) known to exist in Bohemia. Of other lithia-minerals (all rare) we may name petalite and spodumene (both silicates of alumina and alkalies) and triphylline, a mixed phosphate of ferrous, manganous, and lithium oxides. Only lepidolite comes into consideration as a raw material for the preparation of lithia and its salts. But the extraction from it of pure lithia in any form is difficult. The first step is the disintegration of the finely powdered mineral, which may be effected by means of vitriol and hydrofluoric acid (or vitriol and fluor spar) ; the silicon goes off as gaseous fluoride, the bases remain as sulphates. Or else we may mix the mineral intimately with quicklime, and by very intense heating of the mixture produce a more highly basic silicate, which is readily disintegrate by acids. In either case it is easy to unite all the bases (A1 2 O 3, Fe 2 O 3 , CaO, MgO, Li 2 0, K 2 0, Na.,O) into a solution of chlorides or sulphates. From it we precipitate successively and remove by filtra tion (1) the bases not alkalies or Li by means of excess of milk of lime, and (2) the lime introduced by operation (1) by means of carbonate of ammonia. There results a mixed solution of potash, soda, lithia, and ammonia salt, from which the last-named component is easily removed by evaporation to dryness and ignition. For these very tedious operations Troost has substituted an elegant process which, though admittedly imperfect in the analytic sense, lends itself admirably to manufacturing purposes. He mixes ten parts of the finely powdered mineral with ten parts of carbonate of baryta, five parts of sulphate of baryta, and three parts of sulphate of potash, and melts down the mixture in a power ful wind-furnace. There results a mass which separates spontaneously into a lower layer forming a transparent glass, and an upper one consisting of the sulphates of barium, potassium (sodium), and lithium, the latter representing about three-fourths of the lithia contained in the mineral. By treatment with water the sulphate of baryta is easily removed as an insoluble residue ; the mixed alkaline sulphates are converted into chlorides by decomposition with chloride of barium, and from the dry mixed chlorides approximately pure chloride of lithium is obtained by lixiviation with ether- alcohol, which solvent dissolves only very small proportions of the other chlorides. To purify the crude chloride it is dissolved in water and, by doable decomposition with carbonate of soda, converted into a precipitate of carbonate of lithia, Li 2 CO 3, which must be washed with small instalments of water, as it is very appreciably soluble in water. This carbonate of lithia is still contaminated with soda. To purify it fully dissolve it in water with the help of carbonic acid, filter, and evaporate slowly on a water-bath ; the added carbonic acid goes off, and pure carbonate of lithia separates out in crystalline crusts (Troost). One litre of pure water dissolves 12 grammes; 1 litre of water kept saturated with carbonic acid dissolves 5 2 5 grammes of the carbonate. The dry salt fuses at a red heat, but before doing so loses part of its carbonic acid, which, after cooling, it shows no tendency to take up again from the atmosphere. Perfectly acid-free lithia, Li 2 O, can be obtained by heating a mixture of the carbonate and pure charcoal in a platinum crucible, or by heating the nitrate for a long time in a silver one. If the preparation, ultimately, of the hydrate Li. 2 OH 2 O = 2LiOH is contemplated, the latter operation may be very materially shortened by addition of metallic copper, which reduces the nitric acid. The anhydrous oxide, when treated with water, dissolves without much evolution of heat as hydrate, LiOH, which, by evaporation (in silver) is easily obtained in the solid form. It melts at a dull red heat, but at even higher temperatures loses no water. It dissolves in water (far less abundantly than soda), with formation of a strongly alkaline solution, which neutralizes all acids, with formation of salts. Like baryta, it refuses to form acid sulphates or carbonates (the bodies HLiS0 4 and HLiC0 3 exist only in solution), and forms insoluble or almost insoluble salts with carbonic and phosphoric acids (formulae Li 2 CO 3 and Li 3 P0 4 ); and, last not least, it is not reducible to metal by charcoal at any temperature. Add to this that the highly deliquescent chloride LiCl, when dehydrated by heating, always loses part of its chlorine as HC1, and we feel tempted to conclude that in the case of lithium, as in that of barium or magnesium, two equivalents are united into one atom ti = Li =14. But the specific heat of the metal demands the lesser number. 1 Metallic Lithium, although long before known to exist, was suc cessfully prepared for the first time in 1855, by Bunsen. He obtained it by fusing the pure chloride in a porcelain crucible, and decomposing the fused salt by a battery of four or six; &quot;Bunsens, using a rod of retort charcoal as a positive and a knitting wire as a negative pole. The metal separates out in about pea-sized globules, which stick to the wire, and, thanks to the protecting action of the fused chloride, can be lifted out and col lected without reoxidation, under rock-oil. Lithium is a silver- white metal, of only 58 specific gravity (it floats on rock-oil), somewhat softer than lead, and like it susceptible of being pressed into wire. It tarnishes in air, though far less readily than sodium. AYhen thrown upon water it gradually dissolves as hydrate, with evolution of hydrogen, but without fusing. The metal melts at 180 C., and at a somewhat higher temperature takes fire and burns into oxide with a brilliant white flame. Hence the characteristic intensely red colour which a colourless gas flame assumes when a lithium salt is volatilized in it must be a property of something else than the metal itself; perhaps it is the hydroxide LiOH that emits it. The red lithium flame forms a spectrum consisting chiefly of one brilliant red and a somewhat faint orange line. Lithia-salt solutions behave to general reagents pretty much like those of potash or soda, from which, however, they differ in the following points : (1) concentrated solutions are precipitated by carbonate of potash or soda ; (2) even dilute solutions when mixed with phosphate of soda and caustic soda, in the heat more readily, give precipitates of the phosphate l 4 Li 3, soluble in 2530 parts of plain, and in 3900 parts of ammonia water, more largely _in solutions of ammonia salts ; (3) unlike potassium salts, they give no precipitate with chloride of platinum. (W. D. ) LITHOGRAPHY. The principle upon which the art of lithography is based is very simple the antagonistic qualities of grease and water. An unctuous composition is made to adhere to a peculiar kind of limestone ; the parts thus covered acquire the power of receiving printing ink ; the other parts are prevented from receiving it by the interposition of a film of water ; and then by pressing paper strongly upon the stone impressions are obtained. There are two distinct branches in lithography drawing and printing. Those practising the first are known as lithographic draughtsmen or writers, the second as litho graphic printers. The art of lithography was discovered by Alois Senef elder, a native of Prague, born 6th November 1771. His father, Peter Senefelder, was one of the performers of 1 Lithia oxide and carbonate were long supposed to exert a charac teristically powerful corrosive action on platinum vessels used for their fusion. This, according to Troost, holds only for such preparations as are contaminated with rubidia or crcsia. The pure lithia com pounds, even the oxide (and hydrate ?). do not attack platinum. XIV. 88