CHAPTER XXIX.

THE METALS.

WHAT METALS ARE—CHARACTERISTICS AND GENERAL PROPERTIES OF

METALS—CLASSIFICATION—SPECIFIC GRAVITY—DESCRIPTIONS.

We have learnt that the elements are divided into metalloids and

metals, but the line of demarcation is very faint. It is very difficult

to define what a metal is, though we can say what it is not. It is

indeed impossible to give any absolute definition of a metal, except as

“an element which does not unite with hydrogen, or with another metal

to form a chemical compound.” This definition has been lately given by

Mr. Spencer, and we may accept it as the nearest affirmative definition

of a metal, though obviously not quite accurate.

A metal is usually supposed to be solid, heavy, opaque, ductile,

malleable, and tenacious; to possess good conducting powers for heat

and electricity, and to exhibit a certain shiny appearance known as

“metallic lustre.” These are all the conditions, but they are by

no means necessary, for very few metals possess them all, and many

non-metallic elements possess several. The “alkali” metals are lighter

than water; mercury is a fluid. The opacity of a mass is only in

relation to its thickness, for Faraday beat out metals into plates so

thin that they became transparent. All metals are not malleable, nor

are they ductile. Tin and lead, for example, have very little ductility

or tenacity, while bismuth and antimony have none at all. Carbon is a

much better conductor of electricity than many metals in which such

power is extremely varied. Lustre, again, though possessed by metals,

is a characteristic of some non-metals. So we see that while we can

easily say what is not a metal, we can scarcely define an actual metal,

nor depend upon unvarying properties to guide us in our determination.

[Illustration: Fig. 396.—Laminater.]

The affinity of metals for oxygen is in an inverse ratio to their

specific gravity, as can be ascertained by experiment, when the

heaviest metal will be the least ready to oxidise. Metals differ in

other respects, and thus classification and division become easier. The

fusibility of metals is of a very wide range, rising from a temperature

below zero to the highest heat obtainable in the blow-pipe, and even

then in the case of osmium there is a difficulty. While there can be no

question that certain elements, iron, copper, gold, silver, etc., are

metals proper, there are many which border upon the line of demarcation

very closely, and as in the case of arsenic even occupy the debatable

land.

SPECIFIC GRAVITY is the relation which the weight of substance bears

to the weight of an equal volume of water, as already pointed out in

PHYSICS. The specific gravities of the metals vary very much, as will

be seen from the table following—water being, as usual, taken as 1:—

Aluminium 2·56

Antimony 6·7

Arsenic 6·

Bismuth 9·7

Cadmium 8·6

Calcium 1·5

Chromium 6·8

Cobalt 8·9

Copper 8·9

Gold 19·3

Indium 7·3

Iridium 21·1

Iron 7·8

Lead 11·3

Lithium ·593

Magnesium 1·74

Manganese 8·

Mercury 13·5

Molybdenum 8·6

Nickel 8·8

Osmium 21·4

Palladium 11·8

Platinum 21·5

Potassium ·865

Rhodium 12·1

Rubidium 1·5

Ruthenium 11·4

Silver 10·5

Sodium ·972

Strontium 2·5

Thallium 11·8

Tin 7·2

Titanium 5·3

Tungsten 17·6

Uranium 18·4

Zinc 7·1

Zircon 4·3

Some metals are therefore lighter and some heavier than water.

The table underneath gives the approximate fusing points of some of the

metals (Centigrade Scale)—

(Ice melts at 0°.)

Platinum[21] about 1500°

Gold ” 1200°

Silver ” 1000°

Cast iron 1000-1200°

Wrought iron ” 1500°

Copper ” 1100°

Antimony ” 432°

Zinc ” 400°

Lead ” 330°

Bismuth ” 265°

Tin ” 235°

Sodium ” 97°

Potassium ” 60°

Mercury ” 40°

There are some metals which, instead of fusing,—that is, passing from

the solid to the liquid state,—go away in vapour. These are volatile

metals. Mercury, potassium, and sodium, can be thus distilled. Some do

not expand with heat, but contract (like ice), antimony and bismuth,

for instance, while air pressure has a considerable effect upon the

fusing point. Some vaporise at once without liquefying; others, such as

iron, become soft before melting.

ALLOYS are combinations of metals which are used for many purposes, and

become harder in union. Amalgams are alloys in which mercury is one

constituent. Some of the most useful alloys are under-stated:—

Name of Alloy. Composition.

Aluminium bronze Copper and aluminium.

Bell metal Copper and tin.

Bronze ” ”

Gun metal ” ”

Brass Copper and zinc.

Dutch metal ” ”

Mosaic gold ” ”

Ormulu ” ”

Tombac ” ”

German silver Copper, nickel, and zinc.

Britannia metal Antimony and tin.

Solder ” ”

Pewter Tin and lead.

Type metal Lead and antimony (also copper at times).

Shot Lead and arsenic.

Gold currency Gold and copper.

Silver currency Silver and copper.

Stereotype metal Lead, antimony, and bismuth.

Metals combine with chlorine, and produce chlorides,

Metals ” ” sulphur ” ” sulphides,

Metals ” ” oxygen ” ” oxides, and so on.

The metals may be classed as follows in divisions:—

Metals of the alkalies as POTASSIUM, SODIUM, LITHIUM, AMMONIUM.

Metals of the alkaline earths as BARIUM, CALCIUM, MAGNESIUM, STRONTIUM.

Metals of the earths as {ALUMINIUM, Cerium, Didymium, Erbium,

{Glucinium, Lanthanum, Terbium,

{Thorium, Yttrium, Zirconium.

Metals proper—

Common Metals as {IRON, MANGANESE, COBALT, NICKEL,

{COPPER, Bismuth, LEAD, TIN, ZINC,

{CHROMIUM, Antimony.

Noble Metals as {MERCURY, SILVER, GOLD, PLATINUM,

{Palladium, Rhodium, Ruthenium,

{Osmium, Iridium.

We cannot attempt an elaborate description of all the metals, but we

will endeavour to give a few particulars concerning the important ones,

leaving many parts for Mineralogy to supplement and enlarge upon. We

shall therefore mention only the most useful of the metals in this

place. We will commence with POTASSIUM.

METALS OF THE ALKALIES.

POTASSIUM has a bright, almost silvery, appearance, and is so greatly

attracted by oxygen that it cannot be kept anywhere if that element be

present—not even in water, for combustion will immediately ensue on

water; and in air it is rapidly tarnished. It burns with a beautiful

violet colour, and a very pretty experiment may easily be performed

by throwing a piece upon a basin of water. The fragment combines with

the oxygen of the water, the hydrogen is evolved, and burns, and the

potassium vapour gives the gas its purple or violet colour. The metal

can be procured by pulverizing carbonate of potassium and charcoal, and

heating them in an iron retort. The vapour condenses into globules in

the receiver, which is surrounded by ice in a wire basket. It must be

collected and kept in naphtha, or it would be oxidised. Potassium was

first obtained by Sir Humphrey Davy in 1807. Potash is the oxide of

potassium, and comes from the “ashes” of wood.

[Illustration: Fig. 397.—Preparation of potassium.]

The compounds of potassium are numerous, and exist in nature, and by

burning plants we can obtain potash (“pearlash”). Nitrate of potassium,

or nitre (saltpetre), (KNO_{3}), is a very important salt. It is found

in the East Indies. It is a constituent of gunpowder, which consists of

seventy-five parts of nitre, fifteen of charcoal, and ten of sulphur.

The hydrated oxide of potassium, or “caustic potash” (obtained from the

carbonate), is much used in soap manufactories. It is called “caustic”

from its property of cauterizing the tissues. Iodide, bromide, and

cyanide of potassium, are used in medicine and photography.

Soap is made by combining soda (for hard soap), or potash (for soft

soap), with oil or tallow. Yellow soap has turpentine, and occasionally

palm oil, added. Oils and fats combine with metallic oxides, and oxide

of lead with olive oil and resin forms the adhesive plaister with which

we are all familiar when the mixture is spread upon linen. Fats boiled

with potash or soda make soaps; the glycerine is sometimes set free

and purified as we have it. Sometimes it is retained for glycerine

soap. Fancy soap is only common soap coloured. White and brown Windsor

are the same soap—in the latter case browned to imitate age! Soap is

quite soluble in spirits, but in ordinary water it is not so greatly

soluble, and produces a lather, owing to the lime in the water being

present in more or less quantity, to make the water more or less “hard.”

[Illustration: Fig. 398.—Machine for cutting soap in bars.]

[Illustration: Fig. 399.—Soap-boiling house.]

SODIUM is not unlike potassium, not only in appearance, but in its

attributes; it can be obtained from the carbonate, as potassium is

obtained from its carbonate. _Soda_ is the oxide of sodium, but the

most common and useful compound of sodium is the chloride, or common

salt, which is found in mines in England, Poland, and elsewhere. Salt

may also be obtained by the evaporation of sea water. Rock salt is

got at Salzburg, and the German salt mines and works produce a large

quantity. The _Carbonate of Soda_ is manufactured from the chloride of

sodium, although it can be procured from the salsoda plants by burning.

The chloride of sodium is converted into sulphate, and then ignited

with carbonate of lime and charcoal. The soluble carbonate is extracted

in warm water, and sold in crystals as soda, or (anhydrous) “soda ash.”

The large quantity of hydrochloric acid produced in the first part

of the process is used in the process of making chloride of lime. A

few years back, soda was got from Hungary and various other countries

where it exists as a natural efflorescence on the shores of some lakes,

also by burning sea-weeds, especially the common bladder wrack (_Fucus

vesiculosus_), the ashes of which were melted into masses, and came

to market in various states of purity. The bi-carbonate of soda is

obtained by passing carbonic acid gas over the carbonate crystals. Soda

does not attract moisture from the air. It is used in washing, in glass

manufactories, in dyeing, soap-making, etc.

_Sulphate of Soda_ is “Glauber’s Salt”; it is also employed in

glass-making. Mixed with sulphuric acid and water, it forms a freezing

mixture. Glass, as we have seen, is made with silicic acid (sand),

soda, potassa, oxide of lead, and lime, and is an artificial silicate

of soda.

LITHIUM is the lightest of metals, and forms the link between alkaline

and the alkaline earth metals. The salts are found in many places in

solution. The chloride when decomposed by electricity yields the metal.

CÆSIUM and RUBIDIUM require no detailed notice from us. They were first

found in the solar spectrum, and resemble potassium.

AMMONIUM is only a conjectural metal. _Ammonia_, of which we have

already treated, is so like a metallic oxide that chemists have come

to the conclusion that its compounds contain a metallic body, which

they have named hypothetically AMMONIUM. It is usually classed amongst

the alkaline metals. The salts of ammonia are important, and have

already been mentioned. Muriate (chloride) of ammonia, or sal-ammoniac,

is analogous to chloride of sodium and chloride of potassium. It is

decomposed by heating it with slaked lime, and then gaseous ammonia is

given off.

[Illustration: Fig. 400.—Mottled soap-frames.]

THE METALS OF THE ALKALINE EARTHS.

BARIUM is the first of the four metals we have to notice in this

group, and will not detain us long, for it is little known in a free

condition. Its most important compound is heavy spar (_sulphate of

baryta_), which, when powdered, is employed as a white paint. The oxide

of barium, BaO, is termed baryta.

_Nitrate of Baryta_ is used for “green fire,” which is made as

follows:—Sulphur, twenty parts; chlorate of potassium, thirty-three

parts; and nitrate of baryta, eighty parts (by weight).

[Illustration: Fig. 401.—Soda furnace.]

* * * * *

CALCIUM forms a considerable quantity of our earth’s crust. It is the

metal of lime, which is the oxide of calcium. In a metallic state it

possesses no great interest, but its combinations are very important to

us. _Lime_ is, of course, familiar to all. It is obtained by evolving

the carbonic acid from carbonate of lime (CaO).

The properties of this lime are its white appearance, and it develops

a considerable amount of heat when mixed with water, combining to make

hydrate of lime, or “slaked lime.” This soon crumbles into powder, and

as a mortar attracts the carbonic acid from the air, by which means it

assumes the carbonate and very solid form, which renders it valuable

for cement and mortar, which, when mixed with sand, hardens. Caustic

lime is used in whitewashing, etc.

_Carbonate of Lime_ (CaCO_{3}) occurs in nature in various forms, as

limestone, chalk, marble, etc. Calc-spar (arragonite) is colourless,

and occurs as crystals. Marble is white (sometimes coloured by metallic

oxides), hard, and granular. Chalk is soft and pulverizing. It occurs

in mountainous masses, and in the tiniest shells, for carbonate of lime

is the main component of the shells of the crustacea, of corals, and

of the shell of the egg; it enters likewise into the composition of

bones, and hence we must regard it as one of the necessary constituents

of the food of animals. It is an almost invariable constituent of

the waters we meet with in Nature, containing, as they always do, a

portion of carbonic acid, which has the power of dissolving carbonate

of lime. But when gently warmed, the volatile gas is expelled, and the

carbonate of lime deposited in the form of white incrustations upon the

bottom of the vessel, which are particularly observed on the bottoms of

tea-kettles, and if the water contains a large quantity of calcareous

matter, even our water-bottles and drinking-glasses become covered with

a thin film of carbonate of lime. These depositions may readily be

removed by pouring into the vessels a little dilute hydrochloric acid,

or some strong vinegar, which in a short time dissolves the carbonate

of lime.

_Sulphate of Lime_ (CaSO_{4}) is found in considerable masses, and

is commonly known under the name of _Gypsum_. It occurs either

crystallized or granulated, and is of dazzling whiteness; in the latter

form it is termed _Alabaster_, which is so soft as to admit of being

cut with a chisel, and is admirably adapted for various kinds of works

of art. Gypsum contains water of crystallization, which is expelled at

a gentle heat. But when ignited, ground, and mixed into a paste with

water, it acquires the property of entering into chemical combination

with it, and forming the original hydrate, which in a short time

becomes perfectly solid. Thus it offers to the artist a highly valuable

material for preparing the well-known plaster of Paris figures, and

by its use the noblest statues of ancient and modern art have now

been placed within the reach of all. Gypsum, moreover, has received a

valuable application as manure. In water it is slightly soluble, and

imparts to it a disagreeable and somewhat bitterish, earthy taste. It

is called “selenite” when transparent.

_Phosphate of Lime_ constitutes the principal mass of the bones of

animals, and is extensively employed in the preparation of phosphorus;

in the form of ground bones it is likewise used as a manure. It appears

to belong to those mineral constituents which are essential to the

nutrition of animals. It is found in corn and cereals, and used in

making bread; so we derive the phosphorus which is so useful to our

system.

_Chloride of Lime_ is a white powder smelling of chlorine, and is

produced by passing the gas over the hydrate of lime spread on trays

for the purpose. It is the well-known “bleaching powder.” It is also

used as a disinfectant. The _Fluoride of Calcium_ is Derbyshire spar,

or “Blue John.” Fluor spar is generally of a purple hue. We may add

that hard water can be softened by adding a little powdered lime to it.

* * * * *

MAGNESIUM sometimes finds a place with the other metals, for it bears a

resemblance to zinc. Magnesium may be prepared by heating its chloride

with sodium. Salt is formed, and the metal is procured. It burns very

brightly, and forms an oxide of magnesia (MgO). Magnesium appears in

the formation of mountains occasionally. It is ductile and malleable,

and may be easily melted.

_Carbonate of Magnesia_, combining with carbonate of lime, form the

Dolomite Hills. When pure, the carbonate is a light powder, and when

the carbonic acid is taken from it by burning it is called Calcined

Magnesia.

The _Sulphate of Magnesia_ occurs in sea-water, and in saline springs

such as Epsom. It is called “Epsom Salts.” Magnesium wire burns

brightly, and may be used as an illuminating agent for final scenes in

private theatricals. _Magnesite_ will be mentioned among Minerals.

* * * * *

STRONTIUM is a rare metal, and is particularly useful in the

composition of “red-fire.” There are the carbonate and sulphate of

strontium; the latter is known as _Celestine_. The red fire above

referred to can be made as follows, in a _dry mixture_. Ten parts

nitrate of strontia, 1½ parts chlorate of potassium, 3½ parts of

sulphur, 1 part sulphide of antimony, and ½ part charcoal. Mix well

without moisture, enclose in touch paper, and burn. A gorgeous crimson

fire will result.

METALS OF THE EARTHS.

ALUMINIUM (Aluminum) is like gold in appearance when in alloy with

copper, and can be procured from its chloride by decomposition with

electricity. It occurs largely in nature in composition with clays

and slates. Its oxide, _alumina_ (Al_{2}O_{3}), composes a number of

minerals, and accordingly forms a great mass of the earth. Alumina is

present in various forms (_see_ Minerals) in the earth, all of which

will be mentioned under Crystallography and Mineralogy. The other nine

metals in this class do not call for special notice.

HEAVY METALS

IRON, which is the most valuable of all our metals, may fitly head

our list. So many useful articles are made of it, that without

consideration any one can name twenty. The arts of peace and the

glories of war are all produced with the assistance of iron, and its

occurrence with coal has rendered us the greatest service, and placed

us at the head of nations. It occurs native in meteoric stones.

Iron is obtained from certain ores in England and Sweden, and these

contain oxygen and iron (_see_ Mineralogy). We have thus to drive away

the former to obtain the latter. This is done by putting the ores in

small pieces into a blast furnace (fig. 402) mixed with limestone

and coal. The process of severing the metal from its ores is termed

smelting, the air supplied to the furnace being warmed, and termed the

“hot blast.” The “cold blast” is sometimes used. The ores when dug from

the mine are generally stamped into powder, then “roasted,”—that is,

made hot, and kept so for some time to drive off water, sulphur, or

arsenic, which would prevent the “fluxes” acting properly. The fluxes

are substances which will mix with, melt, and separate the matters to

be got rid of, the chief being charcoal, coke, and limestone. The ore

is then mixed with the flux, and the whole raised to a great heat; as

the metal is separated it melts, runs to the bottom of the “smelting

furnace,” and is drawn off into moulds made of sand; it is thus cast

into short thick bars called “pigs,” so we hear of pig-iron, and

pig-lead. Iron is smelted from “ironstone,” which is mixed with coke

and limestone. The heat required to smelt iron is so very great, that

a steam-engine is now generally employed to blow the furnace. (Before

the invention of the steam-engine, water-mills were used for the same

purpose.) The smelting is conducted in what is called a blast furnace.

When the metal has all been “reduced,” or melted, and run down to the

bottom of the furnace, a hole is made, out of which it runs into the

moulds; this is called “tapping the furnace.”

[Illustration: Fig. 402.—Blast furnace.]

Smelting is often confounded with melting, as the names are somewhat

alike, but the processes are entirely different; in melting, the metal

is simply liquefied, in smelting, the metal has to be produced from

ores which often have no appearance of containing any, as in the case

of ironstone, which looks like brown clay.

The cone of the furnace, A, is lined with fire-bricks, _i_ _i_, which

is encased by a lining, _l_ _l_; outside are more fire-bricks, and

then masonry, _m_ _n_; C is the throat of the furnace; D the chimney.

The lower part, B, is called the _boshes_. As soon as the ore in

the furnace has become ignited the carbon and oxygen unite and form

carbonic acid, which escapes, and the metal fuses at last and runs

away. The coal and ore are continually added year after year. The

glassy scum called “slag “ protects the molten iron from oxidation.

The metal drawn from the blast furnace is “pig iron,” or “cast” iron,

and contains carbon. This kind of iron is used for casting operations,

and runs into sand-moulds. It contracts very little when cooling. It is

hard and brittle.

[Illustration: Fig. 403.—General foundry, Woolwich Arsenal.]

[Illustration: Fig. 404.—Wire rollers.]

[Illustration: Fig. 405.—Cutting edges.]

_Bar Iron_ is the almost pure metal. It is remarkably tenacious, and

may be drawn into very fine wire or rolled. But it is not hard enough

for tools. It is difficult to fuse, and must be welded by hammering at

a red heat. Wire-drawing is performed by taking the metal as a bar,

and passing it between rollers (fig. 404), which flattens it, and

then between a new set, which form cutting edges on the rolled plate

(fig. 405), the projections of one set fitting into the hollows of the

other closely as in the illustration. The strips of metal come out at

the aperture seen at A in the next illustration. These rods are drawn

through a series of diminishing holes in a steel plate, occasionally

being heated to keep it soft and ductile. When the wire has got to a

certain fineness it is attached to a cylinder and drawn away, at the

same time being wound round the cylinder over a small fire. Some

metals can be drawn much finer than others. Gold wire can be obtained

of a “thickness” (or thinness) of only the 5,000th part of an inch,

550 feet weighing one grain! But platinum has exceeded this marvellous

thinness, and wire the 30,000th part of an inch has been produced.

Ductility and malleability are not always found in the same metal in

proportion. The sizes of wires are gauged by the instrument shown in

the margin. The farther the wire will go into the groove the smaller

its “size.”

[Illustration: Fig. 406.—Rollers.]

[Illustration: Fig. 407.—Wire size.]

Steel contains a certain amount of carbon, generally about 1 to 2

per cent. Cast steel is prepared from cast iron. Steel from bar-iron

has carbon added, and is termed bar-steel. The process is called

“cementation,” and is carried on by packing the bars of iron in

brick-work boxes, with a mixture of salt and soot, or with charcoal,

which is termed “cement.” Steel is really a carbide of iron, and Mr.

Bessemer founded his process of making steel by blowing out the excess

of carbon from the iron, so that the proper amount—1·5 per cent.—should

remain.

[Illustration: Fig. 408.—Coarse wire-drawing.]

A brief summary of the Bessemer process may be interesting. If a bar of

steel as soft as iron be made red-hot and plunged into cold water, it

will become very hard. If it be then gently heated it will become less

hard, and is then fitted for surgical instruments. The various shades

of steel are carefully watched,—the change of colour being due to

the varying thickness of the oxide; for we know that when light falls

upon very thin films of a substance,—soap-bubbles, for instance,—the

light reflected from the under and upper surfaces interfere, and cause

colour, which varies with the thickness of the film. These colours in

steel correspond to different temperatures, and the “temper” of the

steel depends upon the temperature it has reached. The following table

extracted from Haydn’s “Dictionary of Science” gives the “temper,” the

colour, and the uses of the various kinds of steel.

[Illustration: Fig. 409.—Fine wire-drawing.]

Temperature | Colour. | Uses of Steel.

Cent. Fahr.| |

------------+-------------------+-------------------------------------

220° = 430° | Faint yellow | Lancets.

232° = 450° | Pale straw | Best razors and surgical instruments.

243° = 470° | Yellow | Ordinary razors, pen-knives, etc.

254° = 490° | Brown | Small shears, scissors, cold chisels,

etc.

265° = 510° | Brown and purple | Axes, pocket-knives, plane-irons, etc.

spots

277° = 530° | Purple | Table-knives, etc.

288° = 550° | Light blue | Swords, watch-springs, etc.

293° = 560° | Full blue | Fine saws, daggers, etc.

316° = 600° | Dark blue | Hand and pit saws.

The _Bessemer_ process transfers the metal into a vessel in which

there are tubes, through which air is forced, which produces a much

greater heat than a bellows does. Thus in the process the carbon of the

iron acts as fuel to maintain the fusion, and at the same time by the

bubbling of the carbonic acid mixes the molten iron thoroughly.

During the bubbling up of the whole mass of iron, and the extreme

elevation of temperature caused by the union of the carbon of the

impure iron with the oxygen of the air, the oxide of iron is formed,

and as fast as it forms fuses into a sort of glass; this unites with

the earthy matters of the “impure” iron, and floats on the upper part

as a flux, thus ridding the “cast iron” of all its impurities, with no

other fuel than that contained in the metal itself, and in the air

used. When the flame issuing from the “converter” contracts and changes

its colour, then the time is known to have arrived when the iron is “

de-carbonized.” The amount of carbon necessary is artificially added,

ebullition takes place, a flame of carbonic oxide comes out, and the

metal is then run into ingots.

The compounds of iron which are soluble in water have a peculiar

taste called _chalybeate_ (like ink). Many mineral springs are so

flavoured, and taste, as the immortal Samuel Weller put it, “like warm

flat-irons.” Iron is frequently used as a medicine to renew the blood

globules.

_Protoxide of Iron_ is known only in combination.

_Sesqui-Oxide of Iron_ is “red ironstone.” Powdered it is called

English _rouge_, a pigment not altogether foreign to our use. In a pure

state it is a remedy for arsenical poisoning, and is really the “rust”

upon iron.

[Illustration: Fig. 410.—Bessemer’s process.]

_Bisulphide of Iron_ is iron pyrites, and is crystalline.

_Chloride of Iron_ is dissolved from iron with hydrochloric acid. It is

used in medicine.

_Cyanide of Iron_ makes, with cyanide of potassium, the well-known

prussiate of potash (ferro-cyanide of potassium), which, when heated,

precipitates Prussian blue (cyanogen and iron).

The _Sulphate of the Protoxide_ is known as copperas, or _green

vitriol_, and is applied to the preparation of Prussian blue.

* * * * *

MANGANESE is found extensively, but not in any large quantities, in one

place; iron ore contains it. It is very hard to fuse, and is easily

oxidised. The binoxide is used to obtain oxygen, and when treated with

potassium and diluted, it becomes the permanganate of potassium, and is

used as “Condy’s fluid.” It readily oxides organic matters, and is thus

a disinfectant. It crystallizes in long, deep, red needles, which are

dissolved in water. It is a standard laboratory test. There are other

compounds, but in these pages we need not detail them.

* * * * *

COBALT and NICKEL occur together. They are hard, brittle, and fusible.

The salts of cobalt produce beautiful colours, and the chloride yields

an “invisible” or sympathetic ink. The oxide of cobalt forms a blue

pigment for staining glass which is called “smalt.” Nickel is chiefly

used in the preparation of German silver and electro-plating. The

salts of nickel are green. Nickel is difficult to melt, and always is

one of the constituents of meteoric iron, which falls from the sky in

aërolites. It is magnetic like cobalt, and is extracted from the ore

called kupfer-nickel. A small United-States coin is termed a “nickel.”

* * * * *

COPPER is the next metal we have to notice. It has been known for

centuries. It is encountered native in many places. The Cornish copper

ore is the copper pyrites. The fumes of the smelting works are very

injurious, containing, as they do, arsenic and sulphur. The ground near

the mines is usually bare of vegetation in consequence of the “smoke.”

Sheet copper is worked into many domestic utensils, and the alloy with

zinc, termed _Brass_, is both useful and ornamental. _Red brass_ is

beaten into thin leaves, and is by some supposed to be “gold leaf”; it

is used in decorative work. Bronze is also an alloy of copper, as are

gun-metal, bell-metal, etc.

[Illustration: Fig. 411.—Native copper.]

Next to silver, copper is the best conductor of electricity we have.

It is very hard and tough, yet elastic, and possesses malleability

and ductility in a high degree. It forms two oxides, and there are

several sulphides; the principal of the latter are found native, and

worked as ores. The sulphate of copper is termed _blue vitriol_, and

is used in calico-printing, and from it all the (copper) pigments are

derived. It is also used in solution by agriculturists to protect wheat

from insects. When copper or its alloys are exposed to air and water,

a carbonate of copper forms, which is termed _verdigris_. All copper

salts are poisonous; white of eggs is an excellent remedy in such cases

of poisoning.

* * * * *

LEAD is obtained from galena, a sulphide of lead. It is a soft

and easily-worked metal. When freshly cut it has quite a bright

appearance, which is quickly tarnished. Silver is often present in

lead ore, and is extracted by Pattison’s process, which consists in the

adaptation of the knowledge that lead containing silver becomes solid,

after melting, at a _lower_ temperature than lead does when pure. Pure

lead therefore solidifies sooner.

One great use of lead is for our domestic water-pipes, which remind us

in winter of their presence so disagreeably. Shot is made from lead,

and bullets are cast from the same metal. Shot-making is very simple,

and before the days of breech-loading guns and cartridges, no doubt

many readers have cast bullets in the kitchen and run them into the

mould over a basin of water or a box of sand. For sporting purposes

lead is mixed with arsenic, and when it is melted it is poured through

a sort of sieve (as in the cut) at the top of a high tower. (_See_

figs. 413 and 414). The latter illustration gives the section of the

shot tower; A is the furnace, B is the tank for melting the lead, and

the metal is permitted by the workman at C to run through the sieve

in fine streams. As the lead falls it congeals into drops, which are

received in water below to cool them. They are, of course, not all

round, and must be sorted. This operation is performed by placing them

on a board tilted up, and under which are two boxes. The round shot

rush over the first holes and drop into the second box, but the uneven

ones are caught lagging, and drop into box No. 1. They are accordingly

sent to the furnace again.

[Illustration: Fig. 412.—Shot tower.]

The next process is to sort the good shot for size. This is done

by sieves—one having holes a _little larger_ than the size of shot

required. This sieve passes through it all of the right size and

smaller, and keeps the bigger ones. Those that have passed this

examination are then put into another sieve, which has holes in it a

_little smaller_ than the size of shot wanted. This sieve retains the

right shot, and lets the smaller sizes pass, and so on. The shot are

sized and numbered, glazed by rolling them in a barrel with graphite,

and then they are ready for use. Bullets are made by machinery by the

thousand, and made up into cartridges with great speed.

[Illustration: Fig. 413.—Sieve for making shot.]

The compounds of lead are also poisonous, and produce “colic,” to

which painters are subject. Red lead, or minium, is a compound of the

protoxide and the binoxide, and may be found native. The former oxide

is _litharge_; _white_ lead, or the _carbonate of lead_, is a paint,

and is easily obtained by passing a stream of carbonic acid into a

solution of acetate of lead. It is used as a basis of many paints.

[Illustration: Fig. 414.—Section of shot tower.]

[Illustration: Fig. 415.—Preparing lead for bullets.]

TIN is another well-known metal. It is mentioned by Moses. It possesses

a silver-like lustre, and is not liable to be oxidised. The only really

important ore is called Tinstone, from which the oxygen is separated,

and the metal remains. Cornwall has extensive tin mines. Tin is

malleable and ductile, and can be beaten into _foil_ or “silver leaf,”

or drawn into wire. It prevents oxidation of iron if the latter be

covered with it, and for tinning copper vessels for culinary purposes.

The Romans found tin in Cornwall, and the term “Stanneries” was applied

to the courts of justice among the tin miners in Edward the First’s

time. We have already mentioned the alloys of tin. The oxides of tin,

“Stannous” and “Stannic,” are useful to dyers. The latter is the

tinstone (SnO_{2}). Sulphide of tin is called “Mosaic gold,” and is

much used for decorative purposes.

ZINC is procured from _calamine_, or carbonate of zinc, and _blende_,

or sulphide of zinc. It has for some years been used for many purposes

for which lead was once employed, as it is cheap and light. Zinc is a

hard metal of a greyish colour, not easily bent, and rather brittle;

but when made nearly red-hot, it can be rolled out into sheets or

beaten into form by the hammer. Zinc is about six-and-three-quarter

times heavier than water. Like many other metals, it is volatile

(when heated to a certain extent it passes off into vapour), and the

probable reason that it was not known or used of old is that it was

lost in the attempt to smelt its ores. Zinc is now obtained by a sort

of distillation; the ores are mixed with the flux in a large earthen

crucible or pot.

We have already noticed the alloy of zinc with copper (brass), and the

use of zinc to galvanize iron by covering the latter with a coating

of zinc in a bath is somewhat analogous to electro-plating. The metal

is largely used as the _positive_ element in galvanic batteries, and

for the production of hydrogen in the laboratory. Zinc forms one oxide

(ZnO), used for zinc-white. The sulphate of zinc is white vitriol, and

the chloride of zinc is an “antiseptic.” Certain preparations of the

metal are used in medicine as “ointments” or “washes,” and are of use

in inflammation of the eyelids.

CHROMIUM. This “metallic element” is almost unknown in the metallic

state. But although little known, the beautiful colours of its

compounds make it a very interesting study. The very name leads one to

expect something different to the other metals—_chroma_, colour. The

metal is procured from what is known as chrome-ironstone, a combination

of protoxide of iron and sesqui-oxide of chromium (FeOCr_{2}O_{3}). By

ignition with potassium we get chromic acid and chromate of potassium,

a yellow salt which is used to make the other compounds of chromium.

The metal is by no means easy to fuse.

Sesqui-Oxide of Chromium is a fine green powder employed in painting

porcelain.

Chromate of Lead is termed “chrome yellow,” and in its varieties is

employed as a paint.

Chromate of Mercury is a beautiful vermilion. There are numerous other

combinations which need not be mentioned here.

[Illustration: Fig. 416.—Type-casting.]

ANTIMONY was discovered by Basil Valentine. The Latin term is Stibium,

hence its symbol, Sb. It is very crystalline, and of a peculiar

bluish-white tint. It will take fire at a certain high temperature,

and can be used for the manufacture of “Bengal Lights,” with nitre and

sulphur in the proportions of antimony “one,” the others two and three

respectively.

The compounds of antimony are used in medicine, and are dangerous when

taken without advice. They act as emetics if taken in large quantities.

Our “tartar emetic” is well known.

Antimony, in alloy with lead and a little tin, form the _type metal_

to which we are indebted for our printing. Type-casting is done by

hand, and requires much dexterity. A ladle is dipped into the molten

metal, and the mould jerked in to fill it properly, and then the

type is removed and the mould shut ready for another type; and a

skilful workman can perform these operations five hundred times in an

hour,—rather more than eight times a minute,—producing a type each

time; this has afterwards to be finished off by others. The metal of

which type is made consists of lead and antimony; the antimony hardens

it and makes it take a sharper impression. The letters are first cut in

steel, and from these “dies” the moulds are made in brass, by stamping,

and in these the types are cast.

Stereotype consists of plates of metal taken, by casting, from a

forme of type set up for the purpose: an impression was formerly

carried on by plaster-of-Paris moulds, but lately what is termed the

_papier-maché_ process is adopted. The paper used is now made in

England, and the prepared sheet is placed upon the type and beaten

upon it. Paste is then filled in where there are blanks, and another

and thicker sheet of the prepared paper is placed over all, dried,

and pressed. When this is properly done the paper is hardened, and

preserves an impression of the type set up. The paper mould is then

put into an iron box, and molten metal run in. In a very short time a

“stereotype” plate is prepared from the paper, which can be used again

if necessary. The metal plate is put on the machine.

There are several compounds of antimony, which, though valuable to

chemists, would not be very interesting to the majority of readers. We

will therefore at once pass to the Noble Metals.

THE NOBLE METALS.

There are nine metals which rank under the above denomination:—Mercury,

Silver, Gold, Platinum, Palladium, Rhodium, Ruthenium, Osmium, Iridium.

We will confine ourselves chiefly to the first four on the list.

MERCURY, or QUICKSILVER, is the first of the metals which remain

unaltered by exposure to atmospheric air, and thus are supposed to earn

their title of nobility. Mercury is familiar to us in our barometers,

etc., and is fluid in ordinary temperatures, though one of the heaviest

metals we possess. It is principally obtained from native cinnabar, or

sulphide of mercury (vermilion), and the process of extraction is very

easy. Mercury was known to the ancients, and is sometimes found native.

In the mines the evil effects of the contact with mercury are apparent.

This metal forms two oxides,—the black (mercurous) oxide, or suboxide

(Hg_{2}O), and the red (mercuric) oxide, or red precipitate. The

chlorides are two,—the subchloride, or calomel, and the perchloride,

or corrosive sublimate. The sulphides correspond with the oxides; the

mercuric sulphide has been mentioned. Its crimson colour is apparent in

nature, but the Chinese prepare it in a particularly beautiful form.

Many amalgams are made with mercury, which is useful in various ways

that will at once occur to the reader.

SILVER is the whitest and most beautiful of metals, and its use for

our plate and ornaments is general. It is malleable and ductile, and

the best conductor of electricity and heat that we have. It is not

unfrequently met with in its native state, but more generally it is

found in combination with gold and mercury, or in lead, copper, and

antimony ores. The mines of Peru and Mexico, with other Western States

of America, are celebrated—Nevada, Colorado, and Utah in particular.

The story of the silver mine would be as interesting as any narrative

ever printed. The slavery and the death-roll would equal in horror

and in its length the terrible records of war or pestilence. We have

no opportunity here to follow it, or its kindred metals with which

it unites, on the sentimental side; but were the story of silver

production written in full, it would be most instructive.

[Illustration: Fig. 417.—Native silver.]

Silver is found with lead (galena), which is then smelted. The lead

is volatilized, and the silver remains. It is also extracted by the

following process, wherein the silver and golden ore is crushed and

washed, and quicksilver, salt, and sulphate of copper added, while heat

is applied to the mass. From tank to tank the slime flows, and deposits

the metals, which are put into retorts and heated. The mercury flies

off; the silver and gold remain in bars.

In some countries, as in Saxony and South America, recourse is had

to another process, that of amalgamation, which depends on the easy

solubility of silver and other metals in mercury. The ore, after being

reduced to a fine powder, is mixed with common salt, and roasted at a

low red heat, whereby any sulphide of silver the ore may contain is

converted into chloride. The mixture is then placed, with some water

and iron filings, in a barrel which revolves round its axis, and the

whole agitated for some time, during which process the chloride of

silver becomes reduced to the metallic state. A portion of mercury is

then introduced, and the agitation continued. The mercury combines

with the silver, and the amalgam is then separated by washing. It

is afterwards pressed in woollen bags to free it from the greater

part of the mercury, and then heated, when the last trace of mercury

volatilizes and leaves the silver behind.

_Nitrate of Silver_ is obtained when metallic silver is dissolved in

nitric acid. It is known popularly as _lunar caustic_, and forms the

base of “marking inks.” _Chloride of silver_ is altered by light, but

the iodide of silver is even more rapidly acted on, and is employed

in photography. _Fulminating silver_ is oxide of silver digested in

ammonia. It is very dangerous in inexperienced hands. It is also

prepared by dissolving silver in nitric acid, and adding alcohol. It

cools in crystals. Fulminating mercury is prepared in the same way.

GOLD is the most valuable of all metals,—the “king of metals,” as it

was termed by the ancients. It is always found “native,” frequently

with silver and copper. Quartz is the rock wherein it occurs. From the

disintegration of these rocks the gold sands of rivers are formed, and

separated from the sands by “washing.” In Australia and California

“nuggets” are picked up of considerable size.

It is a rather soft metal, and, being likewise costly, is never used

in an absolutely pure state. Coins and jewellery are all alloyed with

copper and silver to give them the requisite hardness and durability.

Gold is extremely ductile, and very malleable. One grain of gold may

be drawn into a wire five hundred feet in length, and the metal may be

beaten into almost transparent leaves 1/200000 of an inch in thickness!

[Illustration: Fig. 418.—Native gold.]

Aqua-regia, a mixture of hydrochloric and nitric acids, is used to

dissolve gold, which is solved only by selenic acid, though the free

chlorine will dissolve it. Faraday made many experiments as to the

relation of gold to light. (_See_ “Phil. Trans.,” 1857, p. 145.) The

various uses of gold are so well known that we need not occupy time

and space in recording them. Gilding can be accomplished by immersing

the articles in a hot solution of chloride of gold and bicarbonate of

potash mixed; but the electro process is that now in use, by which the

gold precipitates on the article to be plated.

We have already described the process of electro-plating in the case

of silvered articles, and we need only mention that electro-gilding is

performed very much in the same way. But gilding is also performed in

other ways; one of which, the so-called water gilding, is managed as

follows. Gilding with the gold-leaf is merely a mechanical operation,

but water-gilding is effected by chemistry.

Water-gilding is a process (in which, however, no water is used)

for covering the surface of metal with a thin coating of gold; the

best metal for water-gilding is either brass, or a mixture of brass

and copper. A mixture of gold and mercury, in the proportion of one

part of gold to eight of mercury, is made hot over a fire till they

have united; it is then put into a bag of chamois-leather, and the

superfluous mercury pressed out. What remains is called an “amalgam”;

it is soft, and of a greasy nature, so that it can be smeared over any

surface with the fingers. The articles to be gilt are made perfectly

clean on the surface, and a liquid, made by dissolving mercury in

nitric acid (aqua-fortis), is passed over them with a brush made of

fine brass wire, called a “scratch-brush.” The mercury immediately

adheres to the surface of the metal, making it look like silver; when

this is done, a little of the amalgam is rubbed on, and the article

evenly covered with it. It is then heated in a charcoal fire till all

the mercury evaporates, and the brass is left with a coating of gold,

which is very dull, but may be burnished with a steel burnisher and

made bright if necessary. In former times articles were inlaid with

thin plates of gold, which were placed in hollows made with a graver,

and melted in, a little borax being applied between.

When a solution of “chloride of gold” is mixed with ether, the ether

takes the gold away from the solution, and may be poured off the top

charged with it. This solution, if applied to polished steel by means

of a camel-hair pencil, rapidly evaporates, leaving a film of gold

adhering to the steel, which, when burnished with any hard substance,

has a very elegant appearance. In this way any ornamental design in

gold may be produced, but it is not very durable. The gilt ornaments,

scrolls, and mottoes on sword-blades, are sometimes done in this way.

PLATINUM is the heaviest of all metals, gold being next. Platinum

is practically infusible, and quite indifferent to reagents. It is

therefore very useful in certain manufactories, and in the laboratory.

It can be dissolved by _aqua-regia_. The stills for sulphuric acid are

made of platinum, and the metal is used for Russian coinage, but must

be very difficult to work on account of its infusible property.

In the finely-divided state it forms a gray and very porous mass, which

is known as _spongy platinum_, and possesses the remarkable property

of condensing gases within its pores. Hence, when a jet of hydrogen

is directed upon a piece of spongy platinum, the heat caused by its

condensation suffices to inflame the gas. This singular power has been

applied to the construction of a very beautiful apparatus, known as

Döbereiner’s lamp, which consists of a glass jar, _a_, covered by a

brass lid, _e_, which is furnished with a suitable stop-cock, _c_,

and in connection with a small bell jar, _f_, in which is suspended,

by means of a wire, a cylinder of metallic zinc, _z_. When required

for use, the outer jar is two-thirds filled with a mixture of one

part sulphuric acid and four parts water, and the stop-cock opened to

allow the escape of atmospheric air, the spongy platinum contained

in the small brass cylinder, _d_, being covered by a piece of paper.

The stop-cock is then closed, and the bell jar, _f_, allowed to fill

with hydrogen, and after it has been filled and emptied several times,

the paper is removed from the platinum and the cock is again opened,

when the gas, which escapes first, makes the metal red-hot and finally

inflames. This property of platinum is also used in the “Davy” lamp.

[Illustration: Fig. 419.—Döbereiner’s lamp.]

The remaining metals do not call for detailed notice.

In conclusion, we may refer to the following statement, which in

general terms gives the properties of the metals, their oxides and

sulphides for ordinary readers.

GENERAL CLASSIFICATION OF THE METALS.

(Transcriber’s Note: The table has been divided into two parts to fit

within width constraints)

The metals admit of being really distinguished by the following table,

in which they are presented in several groups, according to their

peculiar properties, and each distinguished by a particular name:—

---------------------------------------

| |

| METALS. |

| |

--------------------------------------+

| (A.) _Light Metals._ |

| |

|Specific gravity from 0·8 to 1; |

| never occur in the uncombined |

| state. |

--------------------------------------+

| (a.) _Alkaline Metals._ |

| |

| 1. Potassium. |

| 2. Sodium. |

| (Ammonium.) |

| |

| |

| |

--------------------------------------+

|(b.) _Metals of the Alkaline Earths._|

| |

| 3. Calcium. |

| 4. Barium. |

| 5. Strontium. |

--------------------------------------+

|(c.) _Metals of the Earths proper._ |

| |

| 6. Magnesium. |

| 7. Aluminium. |

--------------------------------------+

| (B.) _Heavy Metals._ |

| |

|Specific gravity from 5 to 21; are |

| found chiefly in combination |

| with oxygen, and frequently |

| with sulphur and arsenic; some |

| are native. |

--------------------------------------+

| (a.) _Common Metals._ |

| |

| Become oxidized in the air. |

| |

| 8. Iron. 14. Lead. |

| 9. Manganese. 15. Tin. |

|10. Cobalt. 16. Zinc. |

|11. Nickel. 17. Chromium. |

|12. Copper. 18. Antimony. |

|13. Bismuth. |

--------------------------------------+

| (b.) _Noble Metals._ |

| |

| Unchangeable in the air. |

| |

|19. Mercury. 21. Gold. |

|20. Silver. 22. Platinum. |

---------------------------------------

--------------------------------------------------------------------------

| Properties of the |

|------------------------------------------------------------------------|

| Oxides. | Sulphides. |

+----------------------------------+-------------------------------------|

A|Powerful bases; possessing a |Powerful bases, which oxidize in |

| strong affinity for water, and | the air, and form sulphates; |

| form with it hydrates. They | when treated with acids evolve |

| yield their oxygen to carbon | hydrosulphuric acid. |

| only at a white heat. | |

+----------------------------------+-------------------------------------|

a|Highly caustic; powerful bases, |Caustic; strong bases; very soluble |

| separate all other oxides from | in water, and dissolve a |

| their combinations with acids; | large quantity of sulphur, which |

| are very soluble in water, and | is separated on addition of an |

| do not lose their water of | acid as a white powder, termed |

| hydration at the highest | _milk of sulphur_; they were |

| temperatures; attract carbonic | formerly termed _liver of sulphur_.|

| acid rapidly from the air. | |

+----------------------------------+-------------------------------------|

b|Caustic; strong bases; slightly |Caustic; strong bases; dissolve |

| soluble in water; lose their | sulphur, and are partly soluble |

| water of hydration at a moderate| in water, and partly insoluble. |

| heat, and powerfully absorb | |

| carbonic acid. | |

+----------------------------------+-------------------------------------|

c| { Weak bases, |Insoluble in water. |

|Feebly caustic. { insoluble in| |

|Not caustic. { water. | |

| | |

+----------------------------------+-------------------------------------|

B|Feebler bases than the foregoing, |Neutral compounds; insoluble in |

| some are acids; insoluble in | water; antimony and several |

| water, and lose their water of | of the rarer metals produce |

| hydration at a moderate heat. | compounds with sulphur, which |

| | deport themselves as acids. |

| | |

| | |

+----------------------------------+-------------------------------------|

a|With few exceptions, are soluble |Those occurring in nature are |

| in acids, and, when ignited with| somewhat brass-like in appearance, |

| carbon at a red heat, yield | and are termed _pyrites_ |

| their oxygen; are, for the most | and _blendes_. Those which are |

| part, fusible and non-volatile. | artificially prepared have |

| | peculiarcolours; by heat they |

| | are converted into sulphates. |

| | |

| | |

| | |

+----------------------------------+-------------------------------------|

b|Have more the properties of acids |With the exception of sulphide |

| than of bases; are decomposed | of mercury, they leave the pure |

| by ignition into oxygen and | metal when ignited. |

| metal. | |

| | |

| | |

--------------------------------------------------------------------------

FOOTNOTES:

[21] Requires oxy-hydrogen blow-pipe.

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