CHAPTER XXVII

THE IRON FAMILY

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| | | | |

| | | | APPROXIMATE |

| SYMBOL | ATOMIC | DENSITY | MELTING | OXIDES

| | WEIGHT | | POINT |

________|________|________|_________|_____________|________________

| | | | |

Iron | Fe | 55.9 | 7.93 | 1800° | FeO, Fe_{2}O_{3}

Cobalt | Co | 59.0 | 8.55 | 1800° | CoO, Co_{2}O_{3}

Nickel | Ni | 58.7 | 8.9 | 1600° | NiO, Ni_{2}O_{3}

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~The family.~ The elements iron, cobalt, and nickel form a group in the

eighth column of the periodic table. The atomic weights of the three are

very close together, and there is not the same gradual gradation in the

properties of the three elements that is noticed in the families in

which the atomic weights differ considerably in magnitude. The elements

are very similar in properties, the similarity being so great in the

case of nickel and cobalt that it is difficult to separate them by

chemical analysis.

The elements occur in nature chiefly as oxides and sulphides, though

they have been found in very small quantities in the native state,

usually in meteorites. Their sulphides, carbonates, and phosphates are

insoluble in water, the other common salts being soluble. Their salts

are usually highly colored, those of iron being yellow or light green as

a rule, those of nickel darker green, while cobalt salts are usually

rose colored. The metals are obtained by reducing the oxides with

carbon.

IRON

~Occurrence.~ The element iron has long been known, since its ores are

very abundant and it is not difficult to prepare the metal from them in

fairly pure condition. It occurs in nature in many forms of

combination,--in large deposits as oxides, sulphides, and carbonates,

and in smaller quantities in a great variety of minerals. Indeed, very

few rocks or soils are free from small amounts of iron, and it is

assimilated by plants and animals playing an important part in life

processes.

~Metallurgy.~ It will be convenient to treat of the metallurgy of iron

under two heads,--Materials Used and Process.

~Materials used.~ Four distinct materials are used in the metallurgy of

iron:

1. _Iron ore._ The ores most frequently used in the metallurgy

of iron are the following:

Hematite Fe_{2}O_{3}.

Magnetite Fe_{3}O_{4}.

Siderite FeCO_{3}.

Limonite 2Fe_{2}O_{2}·3H_{2}O.

These ores always contain impurities, such as silica,

sulphides, and earthy materials. All ores, with the exception

of the oxides, are first roasted to expel any water and carbon

dioxide present and to convert any sulphide into oxide.

2. _Carbon._ Carbon in some form is necessary both as a fuel

and as a reducing agent. In former times wood charcoal was used

to supply the carbon, but now anthracite coal or coke is almost

universally used.

3. _Hot air._ To maintain the high temperature required for the

reduction of iron a very active combustion of fuel is

necessary. This is secured by forcing a strong blast of hot air

into the lower part of the furnace during the reduction

process.

4. _Flux._ (a) _Purpose of the flux._ All the materials which

enter the furnace must leave it again either in the form of

gases or as liquids. The iron is drawn off as the liquid metal

after its reduction. To secure the removal of the earthy matter

charged into the furnace along with the ore, materials are

added to the charge which will, at the high temperature of the

furnace, combine with the impurities in the ore, forming a

liquid. The material added for this purpose is called the

_flux_; the liquid produced from the flux and the ore is called

_slag_.

(b) _Function of the slag._ While the main purpose of adding

flux to the charge is to remove from the furnace in the form of

liquid slag the impurities originally present in the ore, the

slag thus produced serves several other functions. It keeps the

contents of the furnace in a state of fusion, thus preventing

clogging, and makes it possible for the small globules of iron

to run together with greater ease into one large liquid mass.

(c) _Character of the slag._ The slag is really a kind of

readily fusible glass, being essentially a calcium-aluminium

silicate. The ore usually contains silica and some aluminium

compounds, so that limestone (which also contains some silica

and aluminium) is added to furnish the calcium required for the

slag. If the ore and the limestone do not contain a sufficient

amount of silica and aluminium for the formation of the slag,

these ingredients are added in the form of sand and feldspar.

In the formation of slag from these materials the ore is freed

from the silica and aluminium which it contained.

[Illustration: Fig. 85]

~Process.~ The reduction of iron is carried out in large towers called

blast furnaces. The blast furnace (Fig. 85) is usually about 80 ft. high

and 20 ft. in internal diameter at its widest part, narrowing somewhat

both toward the top and toward the bottom. The walls are built of steel

and lined with fire-brick. The base is provided with a number of pipes

T, called tuyers, through which hot air can be forced into the

furnace. The tuyers are supplied from a large pipe S, which circles

the furnace as a girdle. The base has also an opening M, through which

the liquid metal can be drawn off from time to time, and a second

opening P, somewhat above the first, through which the excess of slag

overflows. The top is closed by a movable trap C and C, called the

cone, and through this the materials to be used are introduced. The

gases produced by the combustion of the fuel and the reduction of the

ore, together with the nitrogen of the air forced in through the tuyers,

escape through pipes D, called downcomer pipes, which leave the

furnace near the top. These gases are very hot and contain combustible

substances, principally carbon monoxide; they are therefore utilized as

fuel for the engines and also to heat the blast admitted through the

tuyers. The lower part of the furnace is often furnished with a water

jacket. This consists of a series of pipes W built into the walls,

through which water can be circulated to reduce their temperature.

Charges consisting of coke (or anthracite coal), ore, and flux in proper

proportions are introduced into the furnace at intervals through the

trap top. The coke burns fiercely in the hot-air blast, giving an

intense heat and forming carbon monoxide. The ore, working down in the

furnace as the coke burns, becomes very hot, and by the combined

reducing action of the carbon and carbon monoxide is finally reduced to

metal and collects as a liquid in the bottom of the furnace, the slag

floating on the molten iron. After a considerable amount of the iron has

collected the slag is drawn off through the opening P. The molten iron

is then drawn off into large ladles and taken to the converters for the

manufacture of steel, or it is run out into sand molds, forming the bars

or ingots called "pigs." The process is a continuous one, and when once

started it is kept in operation for months or even years without

interruption.

It seems probable that the first product of combustion of the

carbon, at the point where the tuyers enter the furnace, is

carbon dioxide. This is at once reduced to carbon monoxide by

the intensely heated carbon present, so that no carbon dioxide

can be found at that point. For practical purposes, therefore,

we may consider that carbon monoxide is the first product of

combustion.

~Varieties of iron.~ The iron of commerce is never pure, but contains

varying amounts of other elements, such as carbon, silicon, phosphorus,

sulphur, and manganese. These elements may either be alloyed with the

iron or may be combined with it in the form of definite chemical

compounds. In some instances, as in the case of graphite, the mixture

may be merely mechanical.

The properties of iron are very much modified by the presence of these

elements and by the form of the combination between them and the iron;

the way in which the metal is treated during its preparation has also a

marked influence on its properties. Owing to these facts many kinds of

iron are recognized in commerce, the chief varieties being cast iron,

wrought iron, and steel.

~Cast iron.~ The product of the blast furnace, prepared as just described,

is called cast iron. It varies considerably in composition, usually

containing from 90 to 95% iron, the remainder being largely carbon and

silicon with smaller amounts of phosphorus and sulphur. When the melted

metal from the blast furnace is allowed to cool rapidly most of the

carbon remains in chemical combination with the iron, and the product is

called white cast iron. If the cooling goes on slowly, the carbon

partially separates as flakes of graphite which remain scattered through

the metal. This product is softer and darker in color and is called gray

cast iron.

~Properties of cast iron.~ Cast iron is hard, brittle, and rather easily

melted (melting point about 1100°). It cannot be welded or forged into

shape, but is easily cast in sand molds. It is strong and rigid but not

elastic. It is used for making castings and in the manufacture of other

kinds of iron. Cast iron, which contains the metal manganese up to the

extent of 20%, together with about 3% carbon, is called spiegel iron;

when more than this amount of manganese is present the product is called

ferromanganese. The ferromanganese may contain as much as 80% manganese.

These varieties of cast iron are much used in the manufacture of steel.

~Wrought iron.~ Wrought iron is made by burning out from cast iron most of

the carbon, silicon, phosphorus, and sulphur which it contains. The

process is called _puddling_, and is carried out in a furnace

constructed as represented in Fig. 86. The floor of the furnace F is

somewhat concave and is made of iron covered with a layer of iron oxide.

A long flame produced by burning fuel upon the grate G is directed

downward upon the materials placed upon the floor, and the draught is

maintained by the stack S. A is the ash box and T a trap to catch

the solid particles carried into the stack by the draught. Upon the

floor of the furnace is placed the charge of cast iron, together with a

small amount of material to make a slag. The iron is soon melted by the

flame directed upon it, and the sulphur, phosphorus, and silicon are

oxidized by the iron oxide, forming oxides which are anhydrides of

acids. These combine with the flux, which is basic in character, or with

the iron oxide, to form a slag. The carbon is also oxidized and escapes

as carbon dioxide. As the iron is freed from other elements it becomes

pasty, owing to the higher melting point of the purer iron, and in this

condition forms small lumps which are raked together into a larger one.

The large lump is then removed from the furnace and rolled or hammered

into bars, the slag; being squeezed out in this process. The product has

a stranded or fibrous structure. _The product of a puddling furnace is

called wrought iron._

[Illustration: Fig. 86]

~Properties of wrought iron.~ Wrought iron is nearly pure iron, usually

containing about 0.3% of other substances, chiefly carbon. It is tough,

malleable, and fibrous in structure. It is easily bent and is not

elastic, so it will not sustain pressure as well as cast iron. It can be

drawn out into wire of great tensile strength, and can also be rolled

into thin sheets (sheet iron). It melts at a high temperature (about

1600°) and is therefore forged into shape rather than cast. If melted,

it would lose its fibrous structure and be changed into a low carbon

steel.

~Steel.~ Steel, like wrought iron, is made by burning out from cast iron a

part of the carbon, silicon, phosphorus, and sulphur which it contains;

but the process is carried out in a very different way, and usually,

though not always, more carbon is found in steel than in wrought iron. A

number of processes are in use, but nearly all the steel of commerce is

made by one of the two following methods.

[Illustration: Fig. 87]

1. _Bessemer process._ This process, invented about 1860, is by far the

most important. It is carried out in great egg-shaped crucibles called

converters (Fig. 87), each one of which will hold as much as 15 tons of

steel. The converter is built of steel and lined with silica. It is

mounted on trunnions T, so that it can be tipped over on its side for

filling and emptying. One of the trunnions is hollow and a pipe P

connects it with an air chamber A, which forms a false bottom to the

converter. The true bottom is perforated, so that air can be forced in

by an air blast admitted through the trunnion and the air chamber.

White-hot, liquid cast iron from a blast furnace is run into the

converter through its open necklike top O, the converter being tipped

over to receive it; the air blast is then turned on and the converter

rotated to a nearly vertical position. The elements in the iron are

rapidly oxidized, the silicon first and then the carbon. The heat

liberated in the oxidation, largely due to the combustion of silicon,

keeps the iron in a molten condition. When the carbon is practically all

burned out cast iron or spiegel iron, containing a known percentage of

carbon, is added and allowed to mix thoroughly with the fluid. The steel

is then run into molds, and the ingots so formed are hammered or rolled

into rails or other forms. By this process any desired percentage of

carbon can be added to the steel. Low carbon steel, which does not

differ much from wrought iron in composition, is now made in this way

and is replacing the more expensive wrought iron for many purposes.

~The basic lining process.~ When the cast iron contains

phosphorus and sulphur in appreciable quantities, the lining of

the converter is made of dolomite. The silicon and carbon burn,

followed by the phosphorus and sulphur, and the anhydrides of

acids so formed combine with the basic oxides of the lining,

forming a slag. This is known as the basic lining process.

2. _Open-hearth process._ In this process a furnace very similar to a

puddling furnace is used, but it is lined with silica or dolomite

instead of iron oxide. A charge consisting in part of old scrap iron of

any kind and in part of cast iron is melted in the furnace by a gas

flame. The silicon and carbon are slowly burned away, and when a test

shows that the desired percentage of carbon is present the steel is run

out of the furnace. _Steel may therefore be defined as the product of

the Bessemer or open-hearth processes._

~Properties of steel.~ Bessemer and open-hearth steel usually contain only

a few tenths of a per cent of carbon, less than 0.1% silicon, and a very

much smaller quantity of phosphorus and sulphur. Any considerable amount

of the latter elements makes the steel brittle, the sulphur affecting it

when hot, and the phosphorus when cold. This kind of steel is used for

structural purposes, for rails, and for nearly all large steel articles.

It is hard, malleable, ductile, and melts at a lower temperature than

wrought iron. It can be forged into shape, rolled into sheets, or cast

in molds.

~Relation of the three varieties of iron.~ It will be seen that wrought

iron is usually very nearly pure iron, while steel contains an

appreciable amount of alloy material, chiefly carbon, and cast iron

still more of the same substances. It is impossible, however, to assign

a given sample of iron to one of these three classes on the basis of its

chemical composition alone. A low carbon steel, for example, may contain

less carbon than a given sample of wrought iron. The real distinction

between the three is the process by which they are made. The product of

the blast furnace is cast iron; that of the puddling furnace is wrought

iron; that of the Bessemer and open-hearth methods is steel.

~Tool steel.~ Steel designed for use in the manufacture of edged tools and

similar articles should be relatively free from silicon and phosphorus,

but should contain from 0.5 to 1.5% carbon. The percentage of carbon

should be regulated by the exact use to which the steel is to be put.

Steel of this character is usually made in small lots from either

Bessemer or open-hearth steel in the following way.

A charge of melted steel is placed in a large crucible and the

calculated quantity of pure carbon is added. The carbon dissolves in the

steel, and when the solution is complete the metal is poured out of the

crucible. This is sometimes called crucible steel.

~Tempering of steel.~ Steel containing from 0.5 to 1.5% carbon is

characterized by the property of "taking temper." When the hot steel is

suddenly cooled by plunging it into water or oil it becomes very hard

and brittle. On carefully reheating this hard form it gradually becomes

less brittle and softer, so that by regulating the temperature to which

steel is reheated in tempering almost any condition of temper demanded

for a given purpose, such as for making springs or cutting tools, can be

obtained.

~Steel alloys.~ It has been found that small quantities of a number of

different elements when alloyed with steel very much improve its quality

for certain purposes, each element having a somewhat different effect.

Among the elements most used in this connection are manganese, silicon,

chromium, nickel, tungsten, and molybdenum.

The usual method for adding these elements to the steel is to first

prepare a very rich alloy of iron with the element to be added, and then

add enough of this alloy to a large quantity of the steel to bring it to

the desired composition. A rich alloy of iron with manganese or silicon

can be prepared directly in a blast furnace, and is called

ferromanganese or ferrosilicon. Similar alloys of iron with the other

elements mentioned are made in an electric furnace by reducing the mixed

oxides with carbon.

~Pure iron.~ Perfectly pure iron is rarely prepared and is not adapted to

commercial uses. It can be made by reducing pure oxide of iron in a

current of hydrogen at a high temperature. Prepared in this way it

forms a black powder; when melted it forms a tin-white metal which is

less fusible and more malleable than wrought iron. It is easily acted

upon by moist air.

~Compounds of iron.~ Iron differs from the metals so far studied in that

it is able to form two series of compounds in which the iron has two

different valences. In the one series the iron is divalent and forms

compounds which in formulas and many chemical properties are similar to

the corresponding zinc compounds. It can also act as a trivalent metal,

and in this condition forms salts similar to those of aluminium. Those

compounds in which the iron is divalent are known as _ferrous_

compounds, while those in which it is trivalent are known as _ferric_.

~Oxides of iron.~ Iron forms several oxides. Ferrous oxide (FeO) is not

found in nature, but can be prepared artificially in the form of a black

powder which easily takes up oxygen, forming ferric oxide:

2FeO + O = Fe_{2}O_{3}.

Ferric oxide is the most abundant ore of iron and occurs in great

deposits, especially in the Lake Superior region. It is found in many

mineral varieties which vary in density and color, the most abundant

being hematite, which ranges in color from red to nearly black. When

prepared by chemical processes it forms a red powder which is used as a

paint pigment (Venetian red) and as a polishing powder (rouge).

Magnetite has the formula Fe_{3}O_{4} and is a combination of FeO and

Fe_{2}O_{3}. It is a very valuable ore, but is less abundant than

hematite. It is sometimes called magnetic oxide of iron, or lodestone,

since it is a natural magnet.

~Ferrous salts.~ These salts are obtained by dissolving iron in the

appropriate acid, or, when insoluble, by precipitation. They are usually

light green in color and crystallize well. In chemical reactions they

are quite similar to the salts of magnesium and zinc, but differ from

them in one important respect, namely, that they are easily changed into

compounds in which the metal is trivalent. Thus ferrous chloride treated

with chlorine or aqua regia is changed into ferric chloride:

FeCl_{2} + Cl = FeCl_{3}.

Ferrous hydroxide exposed to moist air is rapidly changed into ferric

hydroxide:

2Fe(OH)_{2} + H_{2}O + O = 2Fe(OH)_{3}.

~Ferrous sulphate~ _(copperas, green vitriol)_ (FeSO_{4}·7H_{2}O). Ferrous

sulphate is the most familiar ferrous compound. It is prepared

commercially as a by-product in the steel-plate mills. Steel plates are

cleaned by the action of dilute sulphuric acid upon them, and in the

process some of the iron dissolves. The liquors are concentrated and the

green vitriol separates from them.

~Ferrous sulphide~ (FeS). Ferrous sulphide is sometimes found in nature as

a golden-yellow crystalline mineral. It is formed as a black precipitate

when a soluble sulphide and an iron salt are brought together in

solution:

FeSO_{4} + Na_{2}S = FeS + Na_{2}SO_{4}.

It can also be made as a heavy dark-brown solid by fusing together the

requisite quantities of sulphur and iron. It is obtained as a by-product

in the metallurgy of lead:

PbS + Fe = FeS + Pb.

It is used in the laboratory in the preparation of hydrosulphuric acid:

FeS + 2HCl = FeCl_{2} + H_{2}S.

~Iron disulphide~ _(pyrites)_ (FeS_{2}). This substance bears the same

relation to ferrous sulphide that hydrogen dioxide does to water. It

occurs abundantly in nature in the form of brass-yellow cubical crystals

and in compact masses. Sometimes the name "fool's gold" is applied to it

from its superficial resemblance to the precious metal. It is used in

very large quantities as a source of sulphur dioxide in the manufacture

of sulphuric acid, since it burns readily in the air, forming ferric

oxide and sulphur dioxide:

2FeS_{2} + 11O = Fe_{2}O_{3} + 4SO_{2}.

~Ferrous carbonate~ (FeCO_{3}). This compound occurs in nature as

siderite, and is a valuable ore. It will dissolve to some extent in

water containing carbon dioxide, just as will calcium carbonate, and

waters containing it are called chalybeate waters. These chalybeate

waters are supposed to possess certain medicinal virtues and form an

important class of mineral waters.

~Ferric salts.~ Ferric salts are usually obtained by treating an acidified

solution of a ferrous salt with an oxidizing agent:

2FeCl_{2} + 2HCl + O = 2FeCl_{3} + H_{2}O,

2FeSO_{4} + H_{2}SO_{4} + O = Fe_{2}(SO_{4})_{3} + H_{2}O.

They are usually yellow or violet in color, are quite soluble, and as a

rule do not crystallize well. Heated with water in the absence of free

acid, they hydrolyze even more readily than the salts of aluminium. The

most familiar ferric salts are the chloride and the sulphate.

~Ferric chloride~ (FeCl_{3}). This salt can be obtained most conveniently

by dissolving iron in hydrochloric acid and then passing chlorine into

the solution:

Fe + 2HCl = FeCl_{2} + 2H,

FeCl_{2} + Cl = FeCl_{3}.

When the pure salt is heated with water it is partly hydrolyzed:

FeCl_{3} + 3 H_{2}O <--> Fe(OH)_{3} + 3HCl.

This is a reversible reaction, however, and hydrolysis can therefore be

prevented by first adding a considerable amount of the soluble product

of the reaction, namely, hydrochloric acid.

~Ferric sulphate~ (Fe_{2}(SO_{4})_{3}). This compound can be made by

treating an acid solution of green vitriol with an oxidizing agent. It

is difficult to crystallize and hard to obtain in pure condition. When

an alkali sulphate in proper quantity is added to ferric sulphate in

solution an iron alum is formed, and is easily obtained in

large crystals. The best known iron alums have the formulas

KFe(SO_{4})_{2}·12H_{2}O and NH_{4}Fe(SO_{4})_{2}·12H_{2}O. They are

commonly used when a pure ferric salt is required.

~Ferric hydroxide~ (Fe(OH)_{3}). When solutions of ferric salts are

treated with ammonium hydroxide, ferric hydroxide is formed as a

rusty-red precipitate, insoluble in water.

~Iron cyanides.~ A large number of complex cyanides containing iron are

known, the most important being potassium ferrocyanide, or yellow

prussiate of potash (K_{4}FeC_{6}N_{6}), and potassium ferricyanide, or

red prussiate of potash (K_{3}FeC_{6}N_{6}). These compounds are the

potassium salts of the complex acids of the formulas H_{4}FeC_{6}N_{6}

and H_{3}FeC_{6}N_{6}.

~Oxidation of ferrous salts.~ It has just been seen that when a ferrous

salt is treated with an oxidizing agent in the presence of a free acid a

ferric salt is formed:

2FeSO_{4} + H_{2}SO_{4} + O = Fe_{2}(SO_{4})_{3} + H_{2}O.

In this reaction oxygen is used up, and the valence of the iron is

changed from 2 to 3. The same equation may be written

2Fe^{++}, 2SO_{4}^{--} + 2H^{+}, SO_{4}^{--} + O

= 2Fe^{+++}, 3SO_{4}^{--} + H_{2}O.

Hydrogen ions have been oxidized to water, while the charge of each iron

ion has been increased from 2 to 3.

In a similar way the conversion of ferrous chloride into ferric chloride

may be written

Fe^{++}, 2Cl^{-} + Cl = Fe^{+++}, + 3Cl^{-}.

Here again the valence of the iron and the charge on the iron ion has

been increased from 2 to 3, though no oxygen has entered into the

reaction. As a rule, however, changes of this kind are brought about by

the use of an oxidizing agent, and are called oxidations.

The term "oxidation" is applied to all reactions in which the valence of

the metal of a compound is increased, or, in other words, to all

reactions in which the charge of a cation is increased.

~Reduction of ferric salts.~ The changes which take place when a ferric

salt is converted into a ferrous salt are the reverse of the ones just

described. This is seen in the equation

FeCl_{3} + H = FeCl_{2} + HCl

In this reaction the valence of the iron has been changed from 3 to 2.

The same equation may be written

Fe^{+++}, 3Cl_{-} + H = Fe^{++}, + H^{+} + 3Cl_{-}

It will be seen that the charge of the iron ions has been diminished

from 3 to 2. Since these changes are the reverse of the oxidation

changes just considered, they are called reduction reactions. The term

"reduction" is applied to all processes in which the valence of the

metal of a compound is diminished, or, in other words, to all processes

in which the charge on the cations is diminished.

NICKEL AND COBALT

These elements occur sparingly in nature, usually combined with arsenic

or with arsenic and sulphur. Both elements have been found in the free

state in meteorites. Like iron they form two series of compounds, but

the salts corresponding to the ferrous salts are the most common, the

ones corresponding to the ferric salts being difficult to obtain. Thus

we have the chlorides NiCl_{2}·6H_{2}O and CoCl_{2}·6H_{2}O; the

sulphates NiSO_{4}·7H_{2}O and CoSO_{4}·7H_{2}O; the nitrates

Ni(NO_{3})_{2}·6H_{2}O and Co(NO_{3})_{2}·6H_{2}O.

Nickel is largely used as an alloy with other metals. Alloyed with

copper it forms coin metal from which five-cent pieces are made, with

copper and zinc it forms German silver, and when added to steel in small

quantities nickel steel is formed which is much superior to common steel

for certain purposes. When deposited by electrolysis upon the surface of

other metals such as iron, it forms a covering which will take a high

polish and protects the metal from rust, nickel not being acted upon by

moist air. Salts of nickel are usually green.

Compounds of cobalt fused with glass give it an intensely blue color. In

powdered form such glass is sometimes used as a pigment called smalt.

Cobalt salts, which contain water of crystallization, are usually cherry

red in color; when dehydrated they become blue.

EXERCISES

1. In the manufacture of cast iron, why is the air heated before being

forced into the furnace?

2. Write the equations showing how each of the following compounds of

iron could be obtained from the metal itself: ferrous chloride, ferrous

hydroxide, ferrous sulphate, ferrous sulphide, ferrous carbonate, ferric

chloride, ferric sulphate, ferric hydroxide.

3. Account for the fact that a solution of sodium carbonate, when added

to a solution of a ferric salt, precipitates an hydroxide and not a

carbonate.

4. Calculate the percentage of iron in each of the common iron ores.

5. One ton of steel prepared by the Bessemer process is found by

analysis to contain 0.2% carbon. What is the minimum weight of carbon

which must be added in order that the steel may be made to take a

temper?

An Elementary Study of Chemistry · 第 27 / 32 章