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See also: paraffin See also: hydrocarbons
.
It occurs as a constituent of the " fire-See also: damp " of See also: coal-mines, in the gases evolved from volcanoes, and in the gases which arise in marshy districts (due to the decomposition of See also: vegetable See also: matter under the See also: surface of See also: water)
.
It is found associated with petroleum and also in human intestinal gases
.
It is a product of the destructive See also: distillation of complex organic matter (See also: wood, coal, bituminous shale, &c.), forming in this way from 3o to 40% of ordinary See also: illuminating
See also: gas
.
It may be, synthetically obtained by passing a mixture of the vapour of See also: carbon bisulphide with sulphuretted hydrogen over red-hot copper (M
.
Berthelot, Comptes rendus, 1856, 43, p
.
236), CS2 + 2H2S + 8Cu = 4Cu2S + See also: CH4; by passing a mixture of hydrogen and carbon monoxide over reduced nickel at 200—250° C., or hydrogen and carbon dioxide at 230—300° C
.
(P
.
See also: Sabatier and J
.
B
.
Senderens, Comptes rendus, 1902, 134, pp
.
514, 689); by the decomposition of aluminium See also: carbide with water [H
.
See also: Moissan, Bull
.
See also: Soc
.
Chim., 1894, (3) II, p
.
1012]; and by See also: heating phosphonium iodide with carbon bisulphide in a sealed See also: tube to 120-140 C
.
(H
.
Jahn, Ber., 1880, 13, p
.
127)
.
It is also obtained by the reduction of many methyl compounds with nascent hydrogen; thus methyl iodide dissolved in methyl See also: alcohol readily yields methane when acted on by the See also: zinc-copper couple (J
.
H
.
Gladstone and A
.
Tribe, Jour
.
Chem
.
Soc., 1884, 45, p . 156) or by the aluminium- mercury couple . It may be obtained in an indirect manner from methyl iodide by conversion of this compound into zinc methyl, or into magnesium methyl iodide (formed by theSee also: action of magnesium on methyl iodide dissolved in anhydrous See also: ether), and decomposing these latter substances with water (E
.
See also: Frankland, 1856; V
.
Grignard, 1900),
Zn(See also: CH3)2+See also: H2O=2CH4+ZnO; 2CH3MgI +H2O=2CH4+MgI2+ MgO
.
In the laboratory it is usually prepared by J
.
B
.
A
.
See also: Dumas' method (See also: Ann., 1840, 33, p
.
181), which consists in heating an-hydrous sodium acetate with soda lime, CH3CO2Na + NaOH= Na2CO3 + CH4
.
The product obtained by this method is not pure, containing generally more or less See also: ethylene and hydrogen
.
Methane is a colourless gas of specific gravity 0.559 (air = I)
.
It may be condensed to a colourless liquid at -155° to -16o° C. under atmospheric pressure (S . Wroblewsky, Comptes rendus, 1884, 99, p . 136) . It boils at -162° C. and freezes at -186°C . Its critical temperature is -99.5° C . (J .See also: Dewar)
.
The gas is almost insoluble in water, but is slightly soluble in alcohol
.
It decomposes into its constituents when passed through a red-hot tube, small quantities of other hydrocarbons (ethane, ethylene, See also: acetylene, See also: benzene, &c.) being formed at the same See also: time
.
It burns with a pale flame, and when mixed with air or See also: oxygen forms a highly explosive mixture
.
W
.
A
.
See also: Bone (Jour
.
Chem
.
Soc., 1902, 81, p
.
535; 1903, 83, p
.
1074) has shown that in the oxidation of methane by oxygen at 450—500° C. formaldehyde (or possibly methyl alcohol) is formed as an intermediate product, and is ultimately oxidized to carbon dioxide
.
Methane is an exceedingly See also: stable gas, being unaffected by the action of chromic acid, nitric acid, or a mixture of nitric and sulphuric acids
.
Chlorine and bromine, however, react with methane, gradually replacing hydrogen and forming chlor- and brom- substitution products
.
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