Codex @codex  0

The atmospheric gas mixture, principally nitrogen and oxygen near the Earth's surface, with variable water vapour and smaller amounts of other components. Gas relative density comparisons conventionally specify dry air as the reference.

“Carbonic oxide” means carbon monoxide, $\mathrm{CO}$: a combustible, reducing, colourless gas distinct from carbon dioxide. Several preparations remove part of the oxygen from a carbon–oxygen compound or prevent complete oxidation of carbon.

Passing carbon dioxide over sufficiently hot carbon givesHigh temperature favours substantial conversion. The reaction is important in furnaces, but gas emerging from such a process need not be pure carbon monoxide; residual carbon dioxide and other gases must be considered. Incomplete combustion of carbonaceous fuel is another source, with the ideal net balance $2\mathrm{C}+{\mathrm{O}}_2\to 2\mathrm{CO}$. It is a source principle rather than a selective method guaranteeing a pure sample.

For a historical laboratory preparation, formic acid can be dehydrated by a suitable strongly dehydrating medium:Oxalic acid under an appropriate dehydrating treatment yields a mixture:An alkaline absorption stage removes much of the carbon dioxide, while carbon monoxide passes on. A generator, droplet trap, purifier and collecting vessel illustrate why preparation and purification are separate operations. The gas is only slightly soluble in water, so collection over water is possible in principle. Concentrated sulfuric acid acting on carbonaceous material can also give mixed carbon oxides and sulfur dioxide; that route requires additional purification and should not be presented as clean CO evolution without by-products.

The relative density of carbon monoxide against dry air is approximately $28.01/28.97\simeq 0.967$. It has no reliable warning odour. It burns with a blue flame when supplied with suitable oxygen:A CO sample itself does not ordinarily support combustion of a taper. Nor does it immediately give the usual limewater test of carbon dioxide; oxidation of the CO first gives a gas that does. This distinguishes fuel behaviour from the property of supporting combustion of another material.

Its reducing power is illustrated byand by reduction of suitable iron oxides in metallurgy. The products reflect transfer of oxygen from the oxide to carbon monoxide. Its ability to bind metal centres is also chemically important. In biological exposure, binding to haemoglobin and other effects disrupt oxygen delivery and use; it is a serious poison, not merely an innocuous replacement of atmospheric oxygen. This modern explanation must not turn an historical gas-preparation answer into a proposed exposure experiment.^[ref][ref]

Ammonia is the volatile nitrogen–hydrogen chemical compound ${\mathrm{NH}}_3$, obtained historically from ammoniacal salts and from the decomposition of nitrogen-containing organic matter. Sources include the decay of animal and vegetable material, the conversion of urea in stale urine, and the destructive distillation of coal, bones or horn. In gasworks, much of the Ammonia was captured in the aqueous ammoniacal liquor during cooling and washing of crude coal gas. These sources do not mean that nitrogen-free constituents of coal spontaneously produce nitrogen.

An ammonium salt releases Ammonia when heated with a suitable chemical base. For ammonium chloride and slaked lime,The ionic principle is ${\mathrm{NH}}_4^{+}+{\mathrm{OH}}^{-}\to {\mathrm{NH}}_3+{\mathrm{H}}_2\mathrm{O}$. A generating vessel supplies a drying stage and then an inverted dry collecting vessel in which the lighter Ammonia displaces air. It is unsuitable for ordinary collection over water because it dissolves so readily. Quicklime can serve as a drying agent; a strongly acidic drying material would instead consume the Ammonia.

Ammonia is a colourless gas with a penetrating, irritating odour. Its approximate relative density against air is $17.03/28.97\simeq 0.59$. It is readily liquefied under suitable cooling or pressure, and its dissolution in water releases heat. It is toxic and corrosive at sufficient exposure; direct smelling is not an analytical requirement.^[ref]

The aqueous chemical equilibriumexplains the alkaline reaction and the change of moist red litmus to blue. The historical name “ammonium hydroxide” for the solution should not imply that every dissolved molecule has become a discrete molecule of ${\mathrm{NH}}_4\mathrm{OH}$. With hydrochloric acid, Ammonia forms ammonium chloride:The familiar white cloud where the gases meet consists of fine solid salt particles, rather than liquid water alone. In solution, Ammonia also acts as a ligand; an excess can produce a deep-blue copper–ammine coordination complex from suitable copper(II) solutions. Although Ammonia does not readily sustain an ordinary flame in air, it is not intrinsically incapable of combustion; sufficiently favourable mixtures burn.

Take dry air as unity, and compare each gas at the same temperature and pressure. In the ideal gas approximation, $\rho =pM/(RT)$, so the relative density isHere $M$ is molar mass. The following values use modern approximate molar masses; rounding and historical atomic weight conventions can shift the last figures.

“Olefiant gas” is confirmed as a historical synonym of Ethylene in the NIST Chemistry WebBook, SRD 69. In this gas list, “carbonic acid” means carbon dioxide, not an isolated vapour of aqueous ${\mathrm{H}}_2{\mathrm{CO}}_3$. “Alcohol” and “ether” refer to ethanol and diethyl ether, rather than their entire modern chemical classes.^[ref]

The order is therefore Ammonia, then carbon monoxide and Ethylene nearly tied, then air, then carbon dioxide and nitrous oxide nearly tied, then ethanol vapour, then diethyl ether vapour. Nearly equal molar masses do not imply equal chemical behaviour.

If instead molecular hydrogen is chosen as unity, divide each molar mass by about $2.016\mathrm{g}\mathrm{mo}{\mathrm{l}}^{-1}$ and state that convention. In the older nominal ${\mathrm{H}}_2=2$ approximation, the corresponding values are about $22,14,22,14.5,8.5,14,23,37$ in the source order. These are a different reference scale, not different substances.

The vapour comparisons are not comparisons of the liquid densities. Pure ethanol and diethyl ether must be considered at conditions where they remain gaseous, or by a low-pressure gas approximation. Their liquids can be lighter than water while their vapours are heavier than air.

Examples heavier than water are Mercury, glycerol and concentrated sulfuric acid; examples lighter than water are ethanol and diethyl ether. “Heavier” here means greater mass for the same volume, rather than greater total mass in arbitrarily sized samples.

Representative room-temperature relative densities, with water as unity, are

These are illustrative values, not exact constants independent of temperature or composition. Dilution changes the density of sulfuric acid, glycerol and ethanol solutions.^[ref][ref]

A distinction from simply observing a floating layer is essential: ethanol is miscible with water, so it mixes rather than remaining as a permanent upper layer. Diethyl ether has limited water solubility and can form an upper layer. More broadly, gases are also fluids, but the natural comparison intended here is between liquids; air at ordinary conditions is much less dense than liquid water.