of the rhombic system, which are identical in their crystalline form with anhydrite, and generally occur as transparent and semi-transparent masses of tabular crystals having a high specific gravity, namely 4·45, for which reason this salt bears the name of heavy spar or barytes . Analogous to it is celestine , SrSO 4 , which is, however, more rarely met with. Heavy spar frequently forms the gangue separated on dressing metallic ores from the vein stuff; this mineral is the source of all other barium compounds; for the carbonate, although more easily transformed into the other compounds (because acids act directly on it, evolving carbonic anhydride), is a comparatively rare mineral (BaCO 3 forms the mineral witherite ; SrCO 3 , strontianite ; both are rare, the latter is found at Etna). The treatment of barium sulphate is rendered difficult from the fact that it is insoluble both in water and acids, and has therefore to be treated by a method of reduction. Like sodium sulphate and calcium sulphate, heavy spar when heated with charcoal parts with its oxygen and forms barium sulphide, BaS. For this purpose a pasty mixture of powdered heavy spar, charcoal, and tar is subjected to the action of a strong heat, when BaSO 4 + 4C = BaS + 4CO. The residue is then treated with water, in which the barium sulphide is soluble. When boiled with hydrochloric acid, barium chloride, BaCl 2 , is obtained in solution, and the sulphur is disengaged as gaseous sulphuretted hydrogen, BaS + 2HCl = BaCl 2 + H 2 S. In this manner barium sulphate is converted into barium chloride, and the latter by double decomposition with strong nitric acid or nitre gives the less soluble barium nitrate, Ba(NO 3 ) 2 , or with sodium carbonate a precipitate of barium carbonate, BaCO 3 . Both these salts are able to give barium oxide , or baryta , BaO, and the hydroxide, Ba(HO) 2 , which differs from lime by its
Table of Contents
CHAPTER XIV THE VALENCY AND SPECIFIC HEAT OF THE METALS. MAGNESIUM. CALCIUM, STRONTIUM, BARIUM, AND BERYLLIUM
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