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Volume 14 (1867) (436 pages)

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Page: of 436

The Mining antl Scientific Dress,
Communications.
In THIS NRPARTMENT we invite the FRRE Discussion of all
roper subjeets—correspondciits alone being responsible for
he ideas and theories they advance.
iWritten for the Mining and Setentific Press.]
Progress of Metallurgy and Saving of Fuel.
Messrs. Hnrrors.—It seems strange that
with the abundance of ore we have in our
mines, and the qnantity of fuel at our command, we are still obliged to send oves
abroad for reduction, and afterward buy the
metals at snch prices as the sméliers may
choose to place uponthem. Itmustseem to
outside observers that we neither possess the
ores or fuel, so often mentioned in your valnable paper, or that we laek the knowledge
of extracting the metals from the ores. Yet
the fact is, we have both ores and talent in
abundance ; and having in our favor the expeusive transport of ore to Europe aud the
metal back again, we surely onght to compete suecessfully with the foreign manufacturers, not ouly in gold, silver and copper
ores, but in ironaswell. If metallurgy had
made no progress, and we had to resort to
old modes of smelting, we still eould retain
the field; but if we take into consideration
the improvements made in the saving of fuel
by various inventions, foremostamong which
stands C. W. Siemeu’s, we shall find that we
possess all wo need in our midst if we ouly
take advantage thereof.
Various experiments have been mace in
the way of smelting works in California, and
as far as gold and silver ore is concerued, I
believe I was the owner of the only successful works ever erected in this State. For
copper ores various experiments have been
made with very poor success. The parties
engaged in those experiments here had some
theoretical, but not the practical knowledge
necessary to make the proper calculation for
desired results ; for if it had been otherwise,
and they had formed a full knowledge of the .
fuel and ore which they expected to mauipulate, they would not have speut their
friends’ money in vain, and destroyed all,
confidence in further euterprise.
The impression has goue out that, as the
Antioch smelting works were a failure,
Mount Diablo coal is not fit for smelting
ores. To this I respectfully dissent by saying it makes but little difference with regard
to the character of the coal, whether it he
anthracite, bituminous, lignite, or eveu wood,
peat or sawdust; any material containing
hydro-caxbon may be employed to raise as
high a degree of heat as is necessary to smelt
any metal or ore. Ali that is necessary is
the proper Imowledge of the fuel and its apphecation ; with that we need never fail to
produce the degree of heat requisite to effect
the reduction of the ores of metals. Few of
our mineralogisis have given this subject
the proper attention it deserves ; but men of
the greatest ability, like Professor Faraday,
haye greatly ventilated the subject. I will
give you a short abstract of what he has said
on the subject of fuel, in connection with
gas regenerating furnaces :
‘Gaseous fuel is obtained by the mutual
action of coal, air and water, at a moderate
ved heat, A brick chamber, perhaps six
feet by twelve, and about ten feet high, is
constructed with one of its end walls converted into a fire grate, 7. ¢., about half way
down it is a solid plate, and for the rest of
the distance consists of strong horizoutal
plate bars, where air enters, the whole being
at an inclination, such as that which the side
of a heap of coals wonld naturally take.
Coals are poured through openings above,
upon this combination wall and grate, and
being fired at the under surface, they burn
at the place where the air enters ; but asthe
layer of coal is from two to three feet thick,
various operations go on in those parts of
the fuel which cannot burn, for want of aiz.
“Thus the upper and cooler part of the coal
produces a large body of hydro-carbons ; the
cinders or coke which are not volatilized, approach, in descending, towards the grate;
that part which is nearest the grate burns,
with the entering air, into carbonic acid, and
the heat evolved ignites the mass above it.
The carbonic acid passes slowly through the
ignited carbon, becomes converted into carbonie oxyd, and mingles in the upper part of
the chamber (or gas producer) with the former hydrdé-carbons. The water, which is
purposely introduced at the bottom of the
arrangement, is first vaporized by the heat
and theu decomposed by the ignited fnel,
and re-arranged as hydrogen aud carbonic
oxyd; and only the ashes of the coal are removed, as solid matter from the chamber at
the bottom of the fire bars.
‘These mixed gases form the gaseous fuel,
The nitrogen which enters with the air at
the grate, is mingled with them, constituting about one-third of the whole volume.
The gas vises up a large vertical tube, from
twelve to fifteen feet, after which it proceeds
horizontally for any required distance, and
then desceuds to the heat regenerator,
throngh which it passes before it enters the
furnaces.
“A yegenerator is a chamber packed with
fire bricks, separated so as to allow of the
free passage of air or gas between them.
There are geuerally four of them placed uuder a furnace. The gas ascends through one
of these ehambers while air ascends through
the neighboring ehamber, and both are conducted through one end of the furnace
where, mingled, they burn, produciug the
heat due to their chemieal action. Passing
onward to the other end of the furnace, they
(the combined gases) find precisely similar
outlets down which they pass ; and traversing the two remaining regenerators from
above downwards, heat them intensely, especially the upper part; and so travel ou in
their cooled state to the chimney.
‘Now the passages between the four regenerators and the gas aud air are supplied with
yalves aud deflecting plates, which are like
four way cocks in their action ; so that by
the use of a lever these regulators admit air
or gas to the furnace.
“Tt is to be observed that the intensity of
the heated flame, which leaves the furnace
for the stack, always proceeds downwards
through the regeuerators ; so that the upper
part thereof is most intensely ignited, keeping back, as it does, the inteuse heat. So
effectually is this accomplished, that the
gases which enter the stack to be cast into
the air, are not heated above three hundred
degrees of Fahrenheit.
“Tt is cousidered that when the furnace
is in full order, the heat carried forward to
be evolved by the chemical action of combustion is aboutfour thousand degrees, whilst
that carried back by the regenerator is about
three thousand degrees; making an intensity of power which, unless moderated,
would fuse furnace and all else exposed to
its action.
“Thus the regeuerators are alternately
heated and cooled by the outgoing aud cutering gases and air.
“Great facility is afforded in the management of a gas fuynace. Not merely can the
supply of gas and air to the furuace be goyerned by valvesin the passages, but the very
manufacture of the gas fuel itself can be diminished, or eveu stopped, by cutting off the
supply of air to the grate of the gas producer ;
and this is important, inasmuch as there
is no gasometer required.
“‘The economy in fuel is estimated practically as oue-half, even wheu the cheapest
kind of fuel is used. Carbon, when burnt
perfectly into carbonic acid, in a gas producer, evolves about four thousaud degrees of
heat; but if burnt into carbonic oxyd, it
only evolves twelve hundred degrees. The
carbonic oxyd, in its fuel form, carries ou
with it the twenty-eight hundred degrees in
chemical force which it evolves when burning in the real furnace, with a suflicient supply of air.
“The remaining twelve hundred degrees
are employed in the gas producer, in distilling hydro-carbons, decomposing water, ete. .
The whole mixed gaseous fnel cau evolve
about four thousand degrees in the furnace, .
to which the regenerator can return about)
three thousand more.”
In addition to the above, I can produce
other statements, from more than fifty establishments where gas furnaces are used, and
where a saving of more than 50 per cent. of
fuel is effected. IT have not only seeu, but
built and worked such furnaces ; and if our
people would adopt them for metallurgical
operations, we should not be obliged to send
any more ore to a foreign country for reductiou.
In my next I will give you a description
of the application of petrolenm and coal tar
for heating boilers, smelting and glass furnaces. J. Mosuemer.
An Avanancaz.—A gang of Chiuamen at
work on the Central Pacific Railroad, were
buried by asnow-shde on the 22d December.
Some four or five were dead when exhumed.
The snow is from ten to fifteeu feet deep on
the Summit.
(Written for the Mining and Seicntifie Press.)
PROCESS OF ROASTING ORES, ETO,
Translated from the Germau of F. Plattner, for the Mining
aud Gas-Light Jonrnal, New York.
— ‘
BY J. H. TIEMANN, M. E.
Numner Five.
8. Matt.—This mill product consists chiefly of
F.25, Fe S in different proportions, so that either
the F,?5 is in larger proportions than tho F, 8,
or—which less frequently occurs—that the Fe § is
in larger proportions than the Fe2S. Iu the
former case we may suppose the matt composed of
x(Fo 2S, Fo S)4+4(Fe 2S, Fe S) and in the latter
case a8 x (Fe 2S, Fe S)+(Fe 28, nFo S), in which
case, however, a small part of the protosulphide
and subsulphide is sometimes replaced by other
metals, as snbsulphide of copper, sulphides of lead,
zinc, Manganese and silver; the matt also often
contains slag mechanically combined, which, in a
furnace matt containing sulphide of zine, and consequently difficulily fusible, may often amount to
twenty per cent. When,ores consisting chicfly of
pyrites, partly in a natural and partly in a roasted
state, are smelted to a matt in a furnacc, under a
covering of slag, the sesquoxyd of iron in the
roasted part is reduced, ut the expense of the sulphur of the raw part which escapes as a vapor to
a protoxyd, and combines as such with the earthy
materials forming a slag, which afterwards combines with the slag used as a covering.* When the
slaging (fluxing) is imperfect, wbich occurs when
there is a lack of earthy material, particularly
quartz, a part of the protoxyd of iron may be taken
np by the matt, an oxysulphuret may be formed
(™Fo25+I, O) and a matt may be formed haying the fermula, Fo? S+nyFe (8, O). If the ore
was not free from other metals, which are likewise
inclined to separate as sulphurets, they will be
included in the compound.
Pulverized matt, when roasted, acts similar to
magnetic pyrites. If it be roasted at a low temperature and with proper precautions at first, besides free sequoxyd of iron, considerable quantities
of protosulphate is formed, which, afterwards, a,
an increased temperature, as in the case of that
formed from mugnetie pyrites, is changed to persulphate under evolution of sulphurous acid; the
anount fermed is abeut twenty-ono per cent., having seven per ccnt. of sulphuric acid.
4. Kupferkies (copper pyrites) Cu? S, Fo? S38
when roasted, acts similar to magnetie pyrites,
except that besides a small quantity of persulphate
of iron, a sulphato and free oxyd of copper is
formed, If coarsely pulverized, copper pyrites be
roasted at a dark-red heat and constantly stirred,
and atmospheric air admitted until the smell of sulphurous acid disappears, it changes to a spongy
powder, which, when cooling, chauges to a dark
red color. This powder consists chiefly of sesquoxyd of iron, a suboxyd and protoxyd of copper,
and contains protosulphate and persulphate of iron,
and sulphate of copper—the latter in considerable
quantities. If this product be now submitted to a
bright red heat, and air admitted, the protesulphate
of iron (as in the case of pyrites and magnetie
pyrites) changes to persulphate; and there remains,
besides the sesquoxyd of iron and the protoxyd of
copper, only sulphate of copper and a little persulphate of iron with twenty per cent. of sulphurie
acid. If the temperatnre be still increased, thcso
sulphates are decomposed, leaving the free oxyds
of iren and copper, the sulphuric aeid escaping
partly as such, and partly as sulplmrous acid and
oxygen. ~
5. Kupferstein’ (copper matt). This mill product, when containing a high percentage of copper,
consists principally of mCu 25, Fe S; when centaining a medium pereentage of copper Cz 8, Fe 2 8;
and when having a low percentage, m(Cu? 8,
F,2S)+Fe §, or in the latter ease is a mixture of
eopper matt mCu2S, Fe S, witb iron matt Fe 2 8,
F, §, in variable proportions, so that a eopper
matt, with a very low pereentago of copptr, may
have tbe composition (Cy 28, Fo 25)+Fe S$).
The copper matt sometimes contains other sulpur
metals, as lead, zine, manganese and silver, which
replace one another; and is not always free from
a mixtnro of sulphide of antimony or arsenic,
which unito with the disulphide of copper, and pass
jnto the matt.
When pulverized copper matt is exposed to a
dark red heat, and air admitted, it glows readily in
consequence of the oxydation of its components ;
at first it is converted into suboxyd of copper, sesquoxyd and protosnlpbate of iron, sulphurous aeid
* When a part of the sesquoxyd has been reiuced only to
magnetic oxyd (sesquoxyd plus protoxyd), and is present in any quantity, 1t crystallizes in beautiful glistening
octahedrons, if the slag, iu a Jarge mass, be allowed to cool
j slowly.
passing off; but after the sulphides, being kept
constantly stirred, have heen mostly oxydized, and
the temperature increased decomposing the protosulphate of iron, it is converted into free oxyd of
copper and sesquosyd of iron, with sulphate of copper and persulphate of iron, having abont eighteen
per cent. of sulphnric acid; by continued roasting
and constant stirring, tbe sulphates of copper and
iron—the fermer only at a bright red heat—are
decomposed, leaving free oxyds, while sulphurous
acid, oxygen and sulphurie acid pass off—the latter
in tho form of white vapors.
6, Bleiglanz (sulphide of lead) Pp S, when pulyerized and exposed to a dark red: beat, air being
admitted, glows of itself in consequence of the ox_
ydation, evolves sulphurons acid, and at a continned
dark red beat is converted into sulphate and free
oxyd of lead. A higher temperature, not sufficient,
however, to cause a sintering or smelting of tho
free oxyd, produces no further ebange, for tho
reason that the sulphate formed during the roasting eannot he decomposed and cenverted into fico
oxyd. As the proportion between the snlphate
and free oxyd varies in proportion to the amonnt
of other metals present, this portion_of our snbject
will he treated more fully further on, when wo
come to explain the chemical changes which take
place in the roasting of sulphur metals.
7, Wismnthglang (sulphurct of bismuth) B; 2 83,
In a powder, when beated on a clay saucer ina
muffel, just to redness, air being admitted, clows of
itself, evolves sulphurous acid, and is very soon
conyerted into a light grey powder without sintering (caking). This powder cousists of an oxyd
and sulphate of hismuth. If the substanée contained copper pyrites, the product when cool has a
dark yellowish green color. If this be heated in a
glass tube to a bright red, it smelts, with the evolution of 2 little sulphurie acid, to a light brownish
grey mass, which on the edges is translucent.
8. Zinkblond (sulphuret of zinc), yellow and
brown, Zy S and Black F, S+3Z» §, is, of all
sulphur metals whieb require to be treated by fire,
the most difficult to roast. Even when in a fine
pewder, it requircs an uninterupted red heat and
strong draught of air for its complete oxydation,
under whicb circumstances sulphurous acid is
evolved, while free oxyd and more or less sulphate
of zinc (nentral and hasic) is formed. If the blend
contains irou sulphuret, cither as a component
(blackjack) or as an admixture, this is converted
into free seequoxyd. If, during thio roasting, the
temperature be kept pretty high, bnt a small quantity of neutral sulphate of zinc is formed, and that
which has been already formed at a lower temperature, in large quantities, resolves itself into basic
sulphate, evolving sulpbnrie acid, oxygen, and
anhydrous sulphuric acid. The basie sulphate is
decompescd to a free oxyd, only at a white heat.
Tf the blend contains sulphide of cadmium, this acts
in precisely the same manner as the sulphide of
zainc,
9. Sulphuret of manganese, M" Se or MnS,
found in combination with most of the sulphurets,
and mill products from sulphur metals, whon
heated to a red heat and air admitted, is decomposed to sulphate and red oxyd of manganese ;
coutinued rousting at a red heat produces no
change; at a higher tempcrature the sulphate
formed is decemposed to sniphurous acid, oxygen,
anhydrous sulphuric acid, and red oxyd.
[To be Continued.)
Dazu’s Maun.—The loss of this mill by
fire on the 21st December, was a serious
affair. The Virginia Union says:
The ruin was complete, as nota fraction
of machinery was saved. Whatever of
amalgam or bullion was in pans, will of
course be saved. Several hundred tons of
ore were awaiting reduction. There was a
large amount of salt in the mill, on storage,
valued at $12,000, which was badly damaged. The insurance on the mill amounted
to $15,000, There was about $15,110 insurance on the outbuildings, which, however,
were saved. The entire value of the mill
was probably not less than $150,000, Wo
learn that Mr. Schamp, the superintendent,
has, without any delay, leased the Ophir
mill, and will immediately proceed to improve and fix it up after the style of the
Dall mill.
Asrertcan Cxtep Iron.—Five Amerieau chilled railway wheels have arrived in
Londen. ‘They will be broken experimentally, and further wheels of this kind will
be sent over for trial under Eughsh rolling
stock. , We have samples of the iron from
which these wheels are cast, and it is of
magnificent quality. The fracture is a rich
dark gray, medinm grained, and shows
great toughness, the particles appearing to
have been irregularly torn, rather than
broken short off ‘The specific gravity
ranges from 7.25 to 7.3185, and the tensile
strength from 32,000 to 35,102 Ibs., or say
1414 to 16 tons per square inch. The iron
is that known as the Salisbury cold-blast
charcoal iron, and is worth about £10 per
tou in New York.—Lngineering.
Sl
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