Bible Encyclopedias
Carbon

Compounds

Three oxides of carbon are known, namely, carbon suboxide, C,02, carbon monoxide, CO, and carbon dioxide, C02. Carbon suboxide, C302, is formed by the action of phosphorus pentoxide on ethyl malonate (0. Diels and B. Wolf, Ber., 1906, 39, p. 689), CH2(000C2H5)2 =2C 2 H 4 +2H 2 0+C 3 0 2. At ordinary temperatures it is a colourless gas, possessing a penetrating and suffocating smell. It liquefies at 7° C. It is an exceedingly reactive compound, combining with water to form malonic acid, with hydrogen chloride to form malonyl chloride, and with ammonia to form malonamide. When kept for some time in sealed tubes it changes to a yellowish liquid, from which a yellow flocculent substance gradually separates, and finally it suddenly solidifies to a dark red mass, which appears to be a polymeric form. Its vapour density agrees with the molecular formula C302, and this formula is also confirmed by exploding the gas with oxygen and measuring the amount of carbon dioxide produced (see Ketenes).

Carbon monoxide, CO, is found to some extent in volcanic gases. It was first prepared in 1776 by J. M. F. Lassone (Mem. Acad. Paris) by heating zinc oxide with carbon, and was for some time considered to be identical with hydrogen. Cruikshank concluded that it was an oxide of carbon, a fact which was confirmed by Clement and J. B. Desormes (Ann. Chim. Phys., 1801, 38, p. 285). It may be prepared by passing carbon dioxide over red-hot carbon, or red-hot iron; by heating carbonates (magnesite, chalk, &c.) with zinc dust or iron; or by heating many metallic oxides with carbon. It may also be prepared by heating formic and oxalic acids (or their salts) with concentrated sulphuric acid (in the case of oxalic acid, an equal volume of carbon dioxide is produced); and by heating potassium ferrocyanide with a large excess of concentrated sulphuric acid, K 4 Fe(CN) 6 -i-6H2S04+6H20=2K2S04+FeS04+3(NH4)2S04+6C0. It is a colourless, odourless gas of specific gravity 0.967 (air = I). It is one of the most difficultly liquefiable gases, its critical temperature being - 139'5° C., and its critical pressure 35'5 atmos. The liquid boils at - 190° C., and solidifies at - 21 I ° C. (L. P. Cailletet, Comptes rendus, 1884, 99, p. 706). It is only very slightly soluble in water. It burns with a characteristic pale blue flame to form carbon dioxide. It is very poisonous, uniting with the haemoglobin of the blood to form carbonyl-haemoglobin. It is a powerful reducing agent, especially at high temperatures. It is rapidly absorbed by an ammoniacal or acid (hydrochloric acid) solution of cuprous chloride. It unites directly with chlorine, forming carbonyl chloride or phosgene (see below), and with nickel and iron to form nickel and iron carbonyls (see Nickel and IxoN). It also combines directly with potassium hydride to form potassium formate (see Formic Acid). The volume composition of carbon monoxide is established by exploding a mixture of the gas with oxygen, two volumes of the gas combining with one volume of oxygen to form two volumes of carbon dioxide. This fact, coupled with the determination of the vapour density of the gas, establishes the molecular formula CO.

Carbon dioxide, C02, is a gas first distinguished from air by van Helmont (1577-1644), who observed that it was formed in fermentation processes and during combustion, and gave to it the name gas sylvestre. J. Black (Edin. Phys. and Lit. Essays, 1755) showed that it was a constituent of the carbonated alkalis and called it "fixed air." T. 0. Bergman, in 1774, pointed out its acid character, and A. L. Lavoisier (1781-1788) first proved it to be an oxide of carbon by burning carbon in the oxygen obtained from the decomposition of mercuric oxide. It is a regular constituent of the atmosphere, and is found in many spring waters and in volcanic gases; it also occurs in the uncombined condition at the Grotto del Cane (Naples) and in the Poison Valley (Java). It is a constituent of the minerals cerussite, malachite, azurite, spathic iron ore, calamine, strontianite, witherite, calcite aragonite, limestone, &c. It may be prepared by burning carbon in excess of air or oxygen, by the direct decomposition of many carbonates by heat, and by the decomposition of carbonates with mineral acids, M2C03+2HC1=2MCl-FH 2 O+CO 2. It is also formed in ordinary fermentation processes, in the combustion of all carbon compounds (oil, gas, candles, coal, &c.), and in the process of respiration.

It is a colourless gas, possessing a faint pungent smell and a slightly acid taste. It does not burn, and does not support ordinary combustion, but the alkali metals and magnesium, if strongly heated, will continue to burn in the gas with formation of oxides and liberation of carbon. Its specific gravity is 1.529 (air = I). It is readily condensed, passing into the liquid condition at o° C. under a pressure of 35 atmospheres. Its critical temperature is 31.35° C., and its critical pressure is 72.9 atmos. The liquid boils at - 78.2° C. (1 atmo.), and by rapid evaporation can be made to solidify to a snow-white solid which melts at - 65° C. (see Liquid Gases). Carbon dioxide is moderately soluble in water, its coefficient of solubility at o° C. being 1.7977 (R. Bunsen). It is still more soluble in alcohol. The solution of the gas in water shows a faintly acid reaction and is supposed to contain carbonic acid, H2C03. The gas is rapidly absorbed by solutions of the caustic alkalis, with the production of alkaline carbonates (q.v.), and it combines readily with potassium hydride to form potassium formate. It unites directly with ammonia gas to form ammonium carbamate, NH 2 00ONH 4. It may be readily recognized by the white precipitate which it forms when passed through lime or baryta water. Carbon dioxide dissociates, when strongly heated, into carbon monoxide and oxygen, the reaction being a balanced action; the extent of dissociation for varying temperatures and pressures has been calculated by H. Le Chatelier (Zeit. Phys. Chem., 1888, 2, p. 782; see H. Sainte-Claire Deville, Comptes rendus, 1863, 56, p. 195 et seq.). The volume composition of carbon dioxide is determined by burning carbon in oxygen, when it is found that the volume of carbon dioxide formed is the same as that of the oxygen required for its production, hence carbon dioxide contains its own volume of oxygen. Carbon dioxide finds industrial application in the preparation of soda by the Solvay process, in the sugar industry, in the manufacture of mineral waters, and in the artificial production of ice.

Carbonyl chloride (phosgene), COC1 2, was first obtained by John Davy (Phil. Trans., 1812, 40, p. 220). It may be prepared by the direct union of carbon monoxide and chlorine in sunlight (Th. Wilm and G. Wischin, Ann., 1868, 14, p. 150); by the action of phosphorus pentoxide on carbon tetrachloride at 200-210° C. (G. Gusta y son, Ber., 1872, 5, P. 30), 4CC14-+P4010 =2C02+4P0Cl3 20001 2; by the oxidation of chloroform with chromic acid mixture (A. Emmerling acid B. Lengyel, Ber., 1869, 2, P. 54), 4CHC13+302= 40001 2 +2H 2 O+2C1 2 i or most conveniently by heating carbon tetrachloride with fuming sulphuric acid (H. Erdmann, Ber., 1893, 26, p. 1 993), 2S03-FCC14=S205C12+COC12.

It is a colourless gas, possessing an unpleasant pungent smell. Its vapour density is 3.46 (air = I). It may be condensed to a liquid, which boils at 8° C. It is readily soluble in benzene, glacial acetic acid, and in many hydrocarbons. Water decomposes it violently, with formation of carbon dioxide and hydrochloric acid. It reacts with alcohol to form chlorcarbonic ester and ultimately diethyl carbonate (see Carbonates), and with ammonia it yields urea. It is employed commercially in the production of colouring matters (see Benzophenone), and for various synthetic processes.

Carbon oxysulphide, COS, was first prepared by C. Than in 1867 (Ann. Suppl., 5, p. 236) by passing carbon monoxide and sulphur vapour through a tube at a moderate heat. It is also formed by the action of sulphuretted hydrogen on the isocyanic esters, 2CONC 2 H 5 +H 2 S=COS+CO(NHC 2 H 5) 2, by the action of concentrated sulphuric acid on the isothiocyanic esters, Rncs H 2 O = Cos Rnh 2, Or Of Dilute Sulphuric Acid On The Thiocyanates. In The Latter Reaction Various Other Compounds, Such As Carbon Dioxide, Carbon Bisulphide And Hydrocyanic Acid, Are Produced. They Are Removed By Passing The Vapours In Succession Through Concentrated Solutions Of The Caustic Alkalis, Concentrated Sulphuric Acid, And Triethyl Phosphine; The Residual Gas Is Then Purified By Liquefaction (W. Hempel, Zeit. Angew. Chemie, 1901, 14, P. 865). It Is Also Formed When Sulphur Trioxide Reacts With Carbon Bisulphide At 100° C., Cs2 3S03 =Cos 4So 2, And By The Decomposition Of Ethyl Potassium Thiocarbonate With Hydrochloric Acid, Co(0C2115)Sk Hc1= Cos Kc1 C 2 H 5 Oh. It Is A Colourless, Odourless Gas, Which Burns With A Blue Flame And Is Decomposed By Heat. Its Vapour Density Is 2.1046 (Air= I). The Liquefied Gas Boils At 47° C. Under Atmospheric Pressure. It Is Soluble In Water; The Aqueous Solution Gradually Decomposes On Standing, Forming Carbon Dioxide And Sulphuretted Hydrogen. It Is Easily Soluble In Solutions Of The Caustic Alkalis, Provided They Are Not Too Concentrated, Forming Solutions Of Alkaline Carbonates And Sulphides, Cos 4Kho = K2C03 K 2 S 2H20.