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ULPHUR, a non-metallic element known from very early times, and proved to be an element by Lavoisier, in 1772. It was not definitely admitted to the list of recognized elements, however, until after the researches of Gay-Lussac and Thénard, in 1809. In the free state, it occurs native in many parts of the earth, usually in volcanic regions or in connection with gypsum and other allied rocks. Until within recent years the commercial supply has been obtained largely from Sicily, though a considerable quantity has been obtained from the Chilean Andes, and from certain parts of Mexico, China, Japan, India and the Philippine Islands. The large deposits of southern Utah are also mined, but the American supply is now obtained almost wholly from the extensive deposits in and near Calcasieu Parish, La. Four general methods have been employed for separating sulphur from the stony and earthy impurities with which it is usually associated in nature. (1) The "ore" containing it may be heated to a temperature high enough to melt the sulphur and permit it to run out at the bottom; or (2) the "ore" may be heated still more strongly, so as to cause the sulphur to volatilize and pass away in the form of vapor; or (3) the "ore" may be lixiviated with a fluid (such as carbon disulphide) in which the sulphur is soluble, the sulphur being afterward recovered by evaporating the solvent. (4) The Frasch process, specially developed in connection with the Louisiana deposits, is described below. The method by melting is almost exclusively used in extracting sulphur from the inert material with which it is associated in nature, the volatilization and solution methods being reserved for the subsequent purification of the product as first obtained by melting. When the sulphur is extracted from an "ore," the heat required for melting it and isolating it is obtained by various means. In some regions it is obtained by burning a part of the sulphur itself. This method is wasteful in sulphur, but it can be put into practice very simply, and hence its application does not call for skilled labor. In Nevada and California, and, to a more limited extent, in Italy and Sicily, the "ore" is heated by steam under a pressure of 70 pounds or more; the yield by this method being considerably greater, though the expense of treatment is also much greater.

In mining the Louisiana deposits a special method is used, which merits separate description. These vast deposits occur in the form of

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subterranean beds, having an average thickness of 125 feet, and covered by about 90 feet of soft rock (mainly gray limestone) and 375 feet of clay, sand and gravel. The deposits were first discovered in 1865, and between 1868 and 1895 many unsuccessful attempts were made to work them commercially by ordinary methods of mining. Herman Frasch, an American petroleum expert, then undertook a careful study of the subject, and worked out a method of mining the sulphur that has proved eminently successful. The entire practicability of the Frasch process was first established in 1903, in which year 35,000 tons of sulphur were brought to the surface by means of it. The essential ideas of the Frasch process are (1) the use of highly heated water to melt the sulphur as it lies in its bed, and (2) the use of compressed air to force the molten sulphur to the surface of the ground. Several concentrically-arranged steel pipes are driven into the ground, and highly superheated water is forced down into the sulphur bed through the outer ones. The sulphur is thereby melted, and as it is considerably heavier than water it collects in a subterranean pool, into which the pipe system dips. Air, compressed to a pressure of about 250 pounds to the square inch, is forced down the central pipe (which is one inch in diameter), and as this air returns to the surface of the ground through the annular space between the inner pipe and the next one to it, the melted sulphur is carried upward at the same time. When the operation is properly conducted the melted sulphur and hot water can be kept separate, so that when the sulphur reaches the surface it is only necessary to run it into bins to cool and solidify. The product that is obtained in this way is remarkably free from impurities. In fact it is not uncommonly 99.9 (and sometimes even 99.98) per cent pure, and hence it does not require further purification for technical use. For a good technical description of the Frasch process, consult Thorpe's Dictionary of Applied Chemistry,' article "Sulphur."

Iron pyrites (native yellow sulphide of iron) is utilized quite extensively as a source of sulphur in certain lines of manufacture, but the sulphur of the pyrites is rarely won in the elementary form. Almost invariably the sulphur dioxide that is obtained by roasting the pyrites is used in the preparation of sulphuric acid or other compounds, without being reduced to sulphur.

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Native crystals of sulphur are common. They belong to the orthorhombic system, and are usually pyramidal in habit, often with truncated ends. They are transparent to translucent, and are usually yellow in color, with a resinous lustre, a hardness of from 1.5 to 2.5, and a specific gravity of about 2.07.

Sulphur occurs abundantly, also, in combination with other elements, mostly as sulphides and sulphates. Many of the compounds of sulphur are valuable as ores of other elements than sulphur. Galena (sulphide of lead) and cinnabar (sulphide of mercury), for example, are valuable ores of lead and mercury, respectively.

It is difficult to give an adequate physical description of sulphur since the element is capable of existing in many allotropic forms. Six of these appear to have been prepared in a state of satisfactory purity, and others, although they have long been known, are not yet universally admitted to be true allotropic modifications of pure sulphur. A brief description of the six best-known forms follows:

1. Ordinary Rhombic Sulphur.- This is the form in which native crystalline sulphur occurs. Crystals of this variety may be prepared by dissolving ordinary sulphur in carbon disulphide, and evaporating the solvent. This variety is also obtained by melting sulphur and allowing it to cool with extreme slowness. Ordinary rhombic sulphur melts at about 240° F., and boils (under a pressure of 760 millimeters of mercury at Paris) at 832.2° F., according to the very careful experiments made by Callendar and Griffiths with the normal constant-pressure air thermometer. In the solid form rhombic sulphur has a specific gravity of from 2.03 to 2.09, and in the liquid form (just above the melting point) its specific gravity is about 1.81. It is practically a non-conductor of electricity at ordinary temperatures, although it conducts to some extent near its boiling point. When rubbed, sulphur becomes negatively electrified, and globes of sulphur were used in the place of glass in some of the earlier forms of static electrical machines. Rhombic sulphur has a coefficient of linear expansion of about 0.0000356 (Fahrenheit scale), and, when at a temperature just above the melting point, it has a specific heat of approximately 0.235. It is easily soluble in carbon disulphide, and, to a lesser extent, in benzene, chloroform, warm concentrated acetic acid and liquid sulphur dioxide.

2. Monoclinic Sulphur.- Sulphur may be obtained in the form of monoclinic crystals by melting a considerable quantity of ordinary sulphur, allowing it to cool until a crust has formed upon the surface and then piercing the crust and pouring out the still molten portion. The walls of the crucible will then be found to be covered with the monoclinic crystals. It may also be prepared in mass by melting ordinary sulphur, cooling it almost to the point of solidification, and then throwing in a single crystal of monoclinic sulphur; the whole mass then solidifying in the monoclinic form. (If a crystal of rhombic sulphur is added under these circumstances, the crystalline structure of the resulting solid mass is rhombic). Monoclinic sulphur has a specific gravity of about 1.97, melts at about 245° F., and is freely solu

ble in carbon disulphide, from which it crystal-> lizes in the rhombic form. It also dissolves in alcohol, chloroform and benzene, the crystals obtained from these solutions being partly monoclinic and partly rhombic. Monoclinic crystals may be obtained by evaporating the solution obtained by dissolving sulphur in an alcoholic solution of ammonium sulphide. Monoclinic sulphur passes slowly into the ordinary rhombic form, the transformation being facilitated by rubbing the monoclinic crystals with a glass rod. When heated, under atmospheric pressure, to 203° F., monoclinic sulphur passes at once into the ordinary rhombic form, the transformation being accompanied by a small contraction in volume, and the evolution of a certain amount of heat.

3. Soft Soluble Sulphur.-This variety of sulphur may be prepared in various ways,for example, by decomposing sodium hyposulphite (or thiosulphate) by means of a limited quantity of a mineral acid. It is a soft, amorphous substance, nearly white in color, which gradually hardens, and eventually passes (like all the other kinds) into ordinary rhombic sulphur. This form of sulphur is not (as its name indicates) entirely soluble in carbon disulphide; it consists, apparently, of a mixture of two kinds of sulphur, one of which is soluble, while the other is insoluble. When heated, it evolves sensible quantities of sulphuretted hydrogen, showing that it contains hydrogen in some form or other; but it has not been determined whether such hydrogen is essential to the existence of the sulphur in this form, or whether it is to be regarded merely as a non-essential constituent, which could be eliminated (if we knew how to eliminate it) without affecting the continued existence of the sulphur in the "soft soluble" form.

4. Plastic Insoluble Sulphur.-When ordinary sulphur is melted, it first passes into the form of a clear, yellow liquid; but as the temperature is raised, the liquid begins to thicken and darken at about 300° F., and at about 360° F. it is black and quite viscid. If the temperature is still further increased, the liquid gradually loses its viscidity, until, at about 640° F., it becomes quite fluid again, though it remains dark even at its boiling point (832.2° F.). If sulphur which has been heated almost to its boiling point is suddenly cooled by being poured in a thin stream into water, it becomes converted into a plastic mass, which may be readily kneaded with the fingers. Plastic sulphur is commonly dark brown; but Mitscherlich states that the dark color is due to impurities, and that perfectly pure plastic sulphur is citronyellow in color. Plastic sulphur soon becomes hard and yellow, the transformation taking place quickly (and with evolution of heat) at temperatures in the vicinity of 212° F. It is not soluble, as a whole, in carbon disulphide, though that reagent dissolves a portion of it.

5. Amorphous Yellow Insoluble Sulphur. - Plastic sulphur, when treated with warm carbon disulphide until all the soluble part is removed, leaves a yellow, amorphous powder as a residuum. This form appears to be stable at ordinary temperatures, but at about 212° F. it slowly passes into the ordinary rhombic crystalline form.

6. Colloidal Sulphur.-When sulphuretted

hydrogen gas is passed into a cold solution of sulphur dioxide, sulphur is liberated in still another allotropic form. If the current of sulphuretted hydrogen is continued until all the dioxide has been decomposed and the solution (after filtration) is concentrated by evaporation in a vacuum, a yellow solid is finally obtained, which is soluble in water, but which gradually passes into the form of ordinary rhombic sulphur. "Colloidal" sulphur receives its name from the fact that in its aqueous solution it is not diffusible.

Sulphur occurs in commerce in several forms. When cast into cylindrical or slightly conical sticks it is known as "roll sulphur" or "brimstone." It is very brittle under ordinary circumstances, and when reduced to powder by crushing it is sold simply as "sulphur." When sulphur vapor is suddenly cooled, the sulphur condenses in the form of a very finely divided powder, which is commercially known "flowers of sulphur," or "sublimed sulphur.» "Precipitated sulphur» is the fine powder that is thrown down upon the addition of hydrochloric acid to a solution prepared by heating sublimed sulphur with lime and water.

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Chemically, sulphur has the symbol S, and an atomic weight of 32.06 if O=16, or 31.81 if H=1. It combines directly with many of the other elements, producing binary compounds which are known as "sulphides," and which are analogous to the oxides of the corresponding elements. With hydrogen it forms hydrogen sulphide, or "sulphuretted hydrogen," which has the formula HS, and is gaseous under ordinary conditions of temperature and pressure. (See HYDROGEN). Many of the metallic sulphides occur in nature as minerals, as has been already mentioned. Many of them may also be prepared by passing a current of sulphuretted hydrogen gas through acid or alkaline solutions of various metallic salts, or by adding a soluble sulphate to such solutions. See CHEMICAL ANALYSIS.

Several oxides of sulphur are known, of which two are of great industrial importance. These are the dioxide, SO2, and the trioxide, SO3.

Sulphur dioxide, SO2, is prepared, in the laboratory, by treating sodium acid sulphite (HNASO) with concentrated sulphuric acid (H2SO4); sulphur dioxide and sodium acid sulphate being formed, as indicated by the equation HNASO, H2SO. SO2+HNaSO. + H2O. It is also prepared by heating strong sulphuric acid with metallic copper, the reaction in this case being 2H2SO. + Cu SO + CuSO, + 2H2O.

Sulphur dioxide is a colorless gas with the familiar suffocating odor of burning sulphur. It is irrespirable in the pure state, or even when largely diluted with air. Mere traces of it, when inhaled for some time, produce inflammation of the mucous surfaces of the respiratory tract and of the stomach, followed by nausea. The gas is about twice as heavy as air under the same conditions of temperature and pressure. Its specific heat at constant pressure (as compared with an equal weight of water) is about 0.154; and the ratio of its specific heat at constant pressure to its specific heat at constant volume is about 1.256. When exposed to a temperature of 18° F. under ordinary atmospheric pressure, sulphur dioxide condenses to a colorless liquid having a specific gravity of

about 1.43. The critical temperature of the gas is probably about 313° F., and the critical pressure about 79 atmospheres. When cooled to about 105° F. below zero, liquid sulphur dioxide freezes to a transparent solid. Liquid sulphur dioxide evaporates rapidly when exposed to the air, the evaporation being attended with the absorption of a very considerable quantity of heat; a temperature as low as 140° F. below zero being attainable in this manner. On account of this property, liquid sulphur dioxide has been employed to a considerable extent in machinery for the manufacture of artificial ice; though at the present time anhydrous liquid ammonia is usually preferred for this purpose. Gaseous sulphur dioxide dissolves freely in water, especially under pressure; the solution being known as sulphurous acid (q.v.).

Sulphur dioxide is prepared in large quantities, in the arts, by the simple process of burning sulphur with a proper supply of air. When obtained in this manner, the gas contains large quantities of atmospheric nitrogen, but for many industrial purposes this is of no importance. The gas is used for bleaching straw, silk and wool, and (in enormous quantities) in the manufacture of sulphuric acid (q.v.). It is likewise employed extensively in the "sulphite process" for the manufacture of paper from wood.

Sulphur dioxide and sulphuretted hydrogen readily combine with each other to form water and free sulphur, according to the equation SO2+ 2H2S 3S+ 2H2O; and it has been suggested that the deposits of sulphur that occur in volcanic districts have been formed, at least in part, by this reaction. In bleaching by means of chlorine compounds, it is found to be impossible to wash the last traces of chlorine from the bleached fabric, and hence it is customary to treat the fabric, after the bleaching is complete, with some substance (called an "antichlor") with which the free chlorine will combine, to produce compounds that can be more easily washed out. Sulphur dioxide gas is very useful for this purpose, since it combines with chlorine (in the presence of moisture) to form sulphuric and hydrochloric acids, according to the equation SO2 + 2H2O + 2C1 H2SO4 + 2HCl. The dioxide is also used as an antiseptic and disinfectant; but it is inferior to chlorine in this respect, and although it possesses germicidal powers to some extent, it is seldom used in sufficient quantities to be really effective in this application.

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Sulphur trioxide, SO, may be prepared by distilling fuming sulphuric acid, or by passing a mixture of one volume of oxygen with two of sulphur dioxide over red-hot platinized asbestos; the latter method being now used to a considerable extent in the manufacture of sulphuric acid (q.v.) by the so-called "contact process." The trioxide appears to be capable of existing in two different physical states. The white fumes that are first obtained in the course of its preparation condense into long prismatic crystals, which melt at 62° F. to a colorless, mobile. liquid, boiling at 112.8° F. Upon standing, these prismatic crystals are said to change into needle-like forms, which, when heated to about 122° F., pass directly into the gaseous state. Weber has shown that this second form is not observed unless the trioxide contains some measurable quantity of sulphuric acid, due to

the action of the trioxide itself upon moisture.
Sulphur trioxide has a powerful affinity for
water, in which it dissolves with a hissing noise
and the formation of sulphuric acid, as indi-
cated by the equation HO + SO, H2SO1.
The reaction is accompanied by the liberation
of a great deal of heat.

Sulphur combines directly with carbon, at a

red-heat, with the formation of a substance

known as "carbon disulphide" (or "carbon bi-

sulphide"), which has the chemical formula CS2.

The vapor that is thus produced may be con-

densed to a very volatile, mobile liquid, pos-

sessing a high dispersive action upon light.

Carbon disulphide freezes at about

166° F.,

boils (under a pressure of one atmosphere) at

115° F., has a specific gravity of 1.29 and a

specific heat of 0.247, and is used as a solvent

for resins, sulphur, phosphorus, gutta percha

and many other substances that do not dissolve

in water. It is almost insoluble in water, but

mixes readily with alcohol, ether and many

kinds of oil. It is exceedingly inflammable,

and its vapor forms explosive mixtures with

air. The vapor of carbon disulphide takes fire,

when heated in contact with air to 300° F., and

this circumstance, taken in connection with the

volatility of the substance and the explosive-

ness of its vapor when mixed with air, renders

the use of the disulphide exceedingly dangerous

in the presence of any sort of a flame, or even

in the presence of bodies heated as hot as 300°

F. As ordinarily met with in commerce, car-
bon disulphide possesses an exceedingly offen-
sive odor; but this is due to impurities, and
when these are removed, the pure disulphide
has an ethereal odor, which is not objectionable.
The vapor of carbon disulphide is poisonous,
even when greatly diluted with air.

The known compounds that contain sulphur

in combination with two or more other ele-

ments are almost innumerable, as are also the

uses to which sulphur is put in the arts. Among

the simpler compounds containing sulphur with

two or more other elements, the various salts of

sulphurous and sulphuric acids are exceedingly

important. For data concerning sulphur black

and the sulphur compounds that are in general

use in the coal tar color industry, consult

Cain and Thorpe, 'The Synthetic Dyestuffs and

Intermediate Products'; also Wahl and Atack,

'The Manufacture of Organic Dyestuffs.'

SULPHUR SPRINGS, Tex., city, county-
seat of Hopkins County, on the Missouri, Kan-
sas and Texas, and the Saint Louis South-
western railroads, about 240 miles northeast
of Austin, the capital, and 75 miles northeast
of Dallas. It is in an agricultural and stock-
raising region and has an extensive domestic
export trade in cotton products, wheat, corn,
fruit (peaches and plums), honey, poultry and
livestock. It has two national banks with a
combined capital of $200,000. The educational'
insitutions are the Central College (Methodist
Episcopal, South), opened in 1876, and public.
schools. Pop. about 5,151.

SULPHURETTED HYDROGEN (H,S),

a gaseous compound of hydrogen and sulphur,

found abundantly in nature in gases issuing.

from crevices in volcanic regions, and oc-

casionally in natural gas. It is one of the com-

mon products of decomposition of vegetable

substances, especially those of the leguminous

family. It occurs in illuminating gas, from

which it is scrupulously removed at consider-

able expense. It is prepared on a large scale

by heating together equal parts of vaseline or

paraffin and sulphur.

Sulphuretted hydrogen is a colorless, in-

flammable gas, burning with a bluish flame, and

having an extremely offensive odor, similar to

that of rotten eggs. It is very poisonous; when

inhaled in small quantity producing nausea and

headache, and in large quantity, asphyxiation.

One part of the gas in 200 parts of air is fatal

to horses, and one part of gas to 800 of air

is fatal to dogs. It is soluble in water in the

proportion of 4.4 volumes of gas to 1 volume

of water at 32° F. At higher temperatures

less of the gas is held in solution. Alcohol at

32° dissolves 17.9 times its own volume.

The aqueous solution of sulphuretted hy-
drogen is known as hydrosulphuric acid.
smells of the gas, and decomposes on standing,
depositing sulphur, and the hydrogen oxidizing
into water. Its solution in glycerine, how
ever, keeps good for a long time.

The gas may be liquefied at ordinary tem-
peratures by submitting it to a pressure of
17 atmospheres that is, about 250 pounds

to the square inch. Liquid sulphuretted
hydrogen is a colorless, mobile liquid which
freezes or soldiñes at 117° F., and boils at
-79°. In its liquid form it is nearly inert
chemically.

Sulphuretted hydrogen is used in large

quantities in the manufacture of sulphuric acid to remove the arsenic which is found in larger or smaller percentage in all acid made from pyrites. It is also used to precipitate copper from solutions containing salts of copper, and for precipitating gold and silver from sweepings and other waste material. In the chemist's laboratory it is one of the most valuable reagents.

SULPHURIC ACID, or OIL OF VITRIOL, a common and exceedingly important oxy-acid of sulphur, having the chemical formula H2SO..... It was first prepared by Geber, in the 8th century, by distilling alum; and in the 15th century it was manufactured by burning sulphur with saltpetre, though the identity of the product so obtained with that described by Geber was not established until near the end of the 16th century. Considerable quantities of sulphuric acid were formerly manufactured by the distillation of ferrous sulphate, the practice of this method dating from the early part of the 18th century. At the present time practically all of the sulphuric acid that is used is prepared from sulphur dioxide gas, either by the "chamber process," or by the more recently perfected "contact process," both of which are described in this article.

When pure and free from water, sulphuric acid is a colorless liquid with an oily appearance, and a specific gravity of 1.89. It may be readily frozen, the solidified acid melting again at 50.9° F. It exhibits the phenomenon of surfusion to a marked extent, and the liquid acid can be cooled, much below the melting point here given, without inducing solidification; but if a crystal of the solid acid, or a small amount of sulphur trioxide, be added to the supercooled fluid, crystallization begins at once, and the temperature rises until it becomes 50.9° F., after which no further solidification Occurs. The presence of a trace of water in the acid lowers the freezing point nearly to 32° F. If five parts (by weight) of sulphuric acid be mixed with nearly one part of water, and the solution is cooled by a freezing mixture, a definite hydrate of sulphuric acid, having the composition H2SO1 + H2O, crystallizes out at 45° F. Another solid hydrate, having the composition H2SO. + 4H,O, may also be prepared by cooling, to a much lower temperature, a mixture of sulphuric acid and water, containing 57.6 per cent of water. Several other hydrates are also believed to exist, and special study has been expended upon them, on account of their importance in the illustration of the "hydrate" theory of solutions. (Consult Mendeléeff, 'Principles of Chemistry, Vol. II). Sulphuric acid has no really definite boiling point. It begins to boil at about 550° F., the distillate containing sulphuric acid, water and sulphur trioxide. (See SULPHUR). The temperature of the liquid may be raised to 640° F., however, before a state corresponding in definiteness to the boiling point of water is attained, the vapor that passes off then consisting entirely of water vapor and free sulphur trioxide. At higher temperatures the decomposition is even more complete. Thus if a stream of the acid be allowed to flow over redhot bricks, it is broken up into sulphur dioxide (SO2), free oxygen and water-vapor. If the gases sulting from this decomposition are passed

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through cool water, and the steam that they contain is condensed and the sulphur dioxide removed by solution, a supply of pure oxygen gas is obtained. Pure anhydrous sulphuric acid has a specific heat, at ordinary temperatures, of about 0.34, and a coefficient of expansion (Fahrenheit scale) of about 0.000310. The concentrated acid is a powerfully corrosive poison, destroying organic tissues rapidly, and even charring paper and wood. It is also poisonous (though far less violently so) when administered in any considerable quantity in a highly dilute form. Concentrated sulphuric acid has a powerful affinity for water, its combination with water being attended by the evolution of a large amount of heat. The strong acid is used as a drying agent, for removing moisture from gases. For this purpose it is sometimes sufficient to allow the gas to stand for a time in a receiver containing a dish of the concentrated acid; but a more effective mode of procedure consists in passing the gas through tubes that are partially filled with fragments of pumice that have been wetted with the acid.

Chemically, sulphuric acid is dibasic, either or both of its hydrogen atoms being replaceable by metals or other bases, the compounds that are thus formed being termed "sulphates." With the metals of the alkalis (which are monovalent), sulphuric acid therefore forms two kinds of sulphates, which may be sufficiently illustrated by the potassium salts. If one of the hydrogen atoms of the acid is replaced by potassium, the resulting salt, HKSO., is called "hydrogen potassium sulphate," or "acid potassium sulphate"; while if both are replaced, the resulting salt has the formula K.SÓ, and is known as "normal potassium sulphate." Many of the sulphates of the metals occur native in large quantities, and many of them are of great value in the arts. Those that are of especial importance are described, in this encyclopedia, under the metals (or other bases) with which the acid is combined. The sulphate of barium is perhaps the most insoluble salt known. It is formed whenever a soluble barium salt (such as the chloride) is added to a solution of a soluble sulphate; and its formation constitutes a valuable test for sulphuric acid and the sulphates. See CHEMICAL ANALYSIS.

When sulphur trioxide is dissolved in anhydrous sulphuric acid in the proportion of one molecule of the trioxide to one of the acid, a definite compound having the formula H2SO, (or H2SO4.SO3) is obtained. When pure, this substance is known as "pyrosulphuric acid." It is a dibasic acid, forming salts which are termed "pyrosulphates," but which are of comparatively little practical importance. Pyrosulphuric acid forms large crystals, which melt at 95° F., and it is easily decomposed by heat into ordinary sulphuric acid and free sulphur trioxide. Fuming sulphuric acid (now commonly known in the arts as "oleum" but formerely called "Nordhausen oil of vitriol") consists of a mixture of pyrosulphuric acid and ordinary sulphuric acid and may be regarded as a solution of sulphur trioxide in sulphuric acid, the trioxide not being present in sufficient quantity to convert the ordinary acid entirely into pyrosulphuric acid. It fumes strongly in the air, gives off sulphur trioxide when heated,

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