Mineral Processing: converting a mineral to an ore
There are some basic principles in mining and mineral processing
that often get overlooked or at least not paid enough attention to.
This is especially true when people start dealing with minerals that
have a special hold on them (gold being a good, but not the only,
example).
A good place to begin is with an ore. An ore is a
natural occurrence of materials (rocks) from which a mineral of some
value can be recovered with profit on a large scale. More goes
into a having a mine than just the minerals in the ground.
You can have a high grade mineral deposit, that is easily mineable,
but due to socio, political, and environmental issue you do not have
an ore body and do not have a mine. On the other hand with the
proper conditions a low grade, difficult to mine deposit can be
economical making it an ore body and a mine.
I looked at a deposit that averages around 1 oz/ton (31 g/tonne) of
gold and can be recovered by dredging from a depth of 10 to 20 feet.
But due to those conditions, it is not economic to mine and thus
should not be considered an ore.
More commonly the issue is if the mineral can be extracted
economically from the rock. When the percent of the value mineral is
too low for profitable extraction the rock ceases to be an ore.
Mineral processing, mineral beneficiation, or ore dressing is the
process of separating and saving valuable minerals from the
valueless material of an ore, where the valuable minerals are
concentrated into smaller bulk and weight by discarding some of the
waste. It is also the process of separating two or more
minerals, which combined have little value, into two or more
products, each of increased value.
The advantages gained by concentrating the valuable minerals into a
smaller bulk are: first, that the cheaper mechanical method of
rejecting the waste material is substituted for the more expensive
chemical method of the smelting furnace; and second, the rejected
waste material is not shipped, and this saves freight. In some
cases, particularly with non-metalliferous ores, such as coal and
precious stones, smelting may not be an option.
The advantage gained by separating two valuable minerals from each
other lies in the fact that the mineral of less prominence is
advanced from being of no value or even a positive detriment, to
being a standard ore, salable to smelting works; while the mineral
of more prominence has advanced in selling value from being a poorer
grade of ore to being a better one, and commands a higher price in
consequence.
Rock Properties for Mineral Processing: what makes it work (or not)
Above I discussed that it takes more than a high grade to make a
mine. It also takes physical properties of the rocks and ore.
Mineral processing is often divided into two parts, severing and
separating. It is the properties of the minerals and rocks
that explain how these parts work (or do not work). Mineral
processing makes use of the physical properties of minerals and
rocks; and the difference in behavior between the valuable and waste
minerals affords methods for the severing and separation.
Severing (or Detaching). – Also called comminution. The
valuable minerals as they occur in the rock are attached to waste
minerals, and to sever the one from the other, the various steps of
breaking, crushing, and grinding are used. The method depends
on the type of rock. With solid rocks, which are to be separated
without essentially change the nature of the rock, the almost
universal method is some form of breaking or comminution.
Chemical severance (often related to in-situ mining or leaching)
usually involves either dissolution in a solution or decompositions
of rock at high temperatures, with or without a selective phase
change.
The main physical properties of interest are
Hardness or softness
Tenacity, brittleness or friability
Structure and fracture
Aggregation
Separating - After the crushing has severed the valuable minerals
from the waste, the two are still mixed together; and the true
separation, which puts the good ore into the store bin and sends the
waste to the dump, must then take place. Separation methods are much
more diversified than those of severance. In mineral processing they
are based upon utilization of some property in which the
intermingled severed minerals differ either in kind or degree, to
effect a differential response to some impulsive force.
The main physical properties of interest are:
Specific gravity and settling power
Hydrophilic/hydrophobic
Electro-conductivity
Magnetic susceptibility
Dissolution
Optical Characteristics (Color and luster, etc.)
Adhesion
Change in properties on heating
non-magnetic to magnetic.
dense to porous.
Breaking of chemical bonds.
Breaking up can be hard to do
Yes breaking up can be difficult, but understanding what allows it,
can make it easier to do.
Properties for Comminution: severing the good from the bad
This is a continuation of a previous post on the physical properties
that make mineral processing work (or not) (1). Previously I
discussed the overall groupings, in this post I will discuss the
properties that effect severing. A following post will discuss
the properties that effect separating.
Hardness
or Softness.
Minerals differ greatly in their hardness, ranging from the
hardness of the diamond to the softness of talc, their ability to
scratch one another being considered the measure of hardness. The
table of hardness adopted by Dana in his "Mineralogy" is as follows
10 Diamond
9 Sapphire
8 Topaz
7 Quartz
6 Feldspar
5 Apatite
4 Fluorite
3 Calcite
2 Gypsum
1 Talc
Each mineral in the list can scratch all those below it. Hardness
affects the wear of crushing machines - the harder the mineral the
greater the wear. It does not necessarily affect the tendency of the
minerals to produce fines or slimes in crushing.
Tenacity,
Brittleness or Friability
Some minerals, such as native copper, mica, talc, and gypsum, are
very tough though they may at the same time be soft, and this makes
them difficult to break. Some forms of hornblende and feldspar
exhibit extraordinary toughness, although they are not very hard;
other minerals are brittle and break up with comparative ease, as,
for example, some varieties of quartz. A hard, brittle mineral will,
when in agitation, make more fines or slime much more than one which
is soft and tough.
Structure
and Fracture.
The structure of a mineral tends to modify the shape of the
particles resulting from crushing. Cleavable minerals may break into
cubical blocks, as galena; into elongated fragments, as galena,
feldspar, calcite, and sphalerite; into needle-like or thread-like
shapes, as asbestos; or into flat scales, as galena, mica, graphite,
and talc. Granular minerals will drop naturally into separate
rounded grains when broken up, as magnetite, garnet, and some
varieties of galena. Minerals with massive structure, free from any
special tendency to break in one more than in another direction, may
have earthy fracture, as hematite; or conchoidal (oyster shell
like), as pyrite crystal, quartz crystal, and obsidian. The shapes
of these grains have an important bearing upon their power to settle
in water or in air.
Mineral
Aggregation
The valuable minerals may occur in pure masses, as in the banded
vein structure and in pockets or vugs. They may also be in large
crystals mixed with the waste minerals. Both these conditions are
favorable for complete separation. On the other hand they may occur
much intermingled with the waste minerals: either in granular
structure (such as a porphyry), rounded grains or small, compact
crystals; or a radiating mass of slender, needle-like crystals
(acicular structure, the valuable and waste minerals penetrating
each other in all directions, to the eye a hopeless tangle; or,
finally, of laminated structure, in thin layers alternately of good
and worthless mineral. All of the latter structures add difficulty
to the problem of mineral processing.
Properties for Beneficiation: separating the good from the bad (or
the better from the not quite as good)
You have an ore body, mined the ore, and broken it up into smaller
pieces. It is now time
to separate the good from the bad. To do this you use the physical
properties described above.
Specific
Gravity
The difference in densities of equal volumes of materials (often
referred to as specific gravity) allows for their separation, and
this property may be employed in two different ways, namely, as
affecting settling power, or as affecting momentum.
Settling Power - In general for two particles of the same size and
shape, the heavier will settle faster than the lighter, and for two
particles of different specific gravities and the same settling
velocity, the higher specific gravity particle will be of smaller
diameter. The ratio between these two diameters will have an
approximately constant value under similar conditions, and called
the settling ratio.
Momentum - When a particle is given a high velocity in a horizontal
direction, the path it follows is called its trajectory. Of two
particles of the same size and shape, the heavier will have the
longer trajectory, and of two particles with different specific
gravities but the same trajectory, that with the higher specific
gravity will be of smaller diameter than the other.
Hydrophobic/hydrophilic
The basis of froth flotation is the difference in wettability of
minerals. Particles range from those that are easily wettable by
water (hydrophilic) to those that are water-repellent (hydrophobic).
If a mixture of hydrophobic and hydrophilic particles are suspended
in water, and air is bubbled through the suspension, then the
hydrophobic particles will tend to attach to the air bubbles and
float to the surface. The froth layer that forms on the surface will
then be heavily loaded with they hydrophobic mineral, and can be
removed as a separated product. The hydrophilic particles will have
much less tendency to attach to air bubbles, and so it will remain
in suspension and be flushed away.
Particles can either be naturally hydrophobic, or the
hydrophobicity can be induced by addition of chemicals (reagents).
Naturally hydrophobic materials include hydrocarbons, and non-polar
solids such as elemental sulfur. Coal is a good example of a
material that is typically naturally hydrophobic. Chemical
treatments (addition of reagents) to render a surface hydrophobic
are essentially methods for selectively coating a particle surface
with a monolayer of non-polar oil.
Electro-Conductivity
The fact that some minerals are relatively good conductors, while
others are relatively poor conductors, of electricity makes it
possible to separate them. It has been found that the greater part
of the sulphide minerals and the metals themselves are, in varying
degrees, conductors of electricity, while the gangue minerals are,
in general, very poor conductors. If neutral ore particles are
brought into contact with an electrode containing a static charge,
the better conductors become similarly charged and are repelled, in
the same way that pith balls would be under like conditions, while
the poorer conductors are not repelled so far.
Magnetic Susceptibility
The attraction to the magnet is quite strong in some minerals and
metals, notably magnetite, some forms of pyrrhotite, cast iron,
wrought iron, steel, nickel, and cobalt. Other minerals, such as
franklinite, chromite, or iron-bearing sphalerite, garnet, etc.,
have very weak magnetism. Still others, such as quartz, calcite,
gypsum, feldspar, etc., exhibit no attraction at all. By using
properly constructed magnets this property may be made of great
value, not only separating the magnetic from the non-magnetic, but
those that are more magnetic from those that are less so.
Dissolution
Various chemical solutions (lixiviants) can selectively dissolve
minerals and elements allowing their separation from the rock.
Lixiviants may work by altering the reduction-oxidation reaction
state of an ore, or by altering the pH. Acidic lixiviants, such as
sulfuric acid, are commonly used to leach base metals such as
copper, whereas basic lixiviants such as a solution of sodium
cyanide are used to leach precious metals. A key component is to
have this reaction be reversible.
Optical Properties
Under the stimulation of electrical magnetic radiation, some
minerals have distinctive optical properties. Thea easiest to
observe are color and luster which was (and is) used in hand picking
and optical sorting. Slight differences in color or in luster - for
instance, the brass yellow of chalcopyrite, the pale yellow of
pyrite, the vitreous luster of quartz, the resinous of sphalerite,
the adamantine of diamond, the dull of chalk, and the pearly of talc
can furnish aids in hand picking and can be used for optical
sorting. Further on in the spectrum particular under
ultra-violet or even on to x-rays, the fluorescence is used to sort.
Other properties
Adhesion - As with hydrophobic/hydrophilic characteristics, some
minerals will preferentially adhere to other substances. The
most common are gold adhering to mercury in plate amalgamation and
the use of grease tables in diamond recovery.
Change of Property by Heating - Heating of some minerals will change
their basic characteristics so that separation that was not feasible
becomes possible. Examples include autoclaving to convert from
sulphide to oxide. Some minerals, when heated, decrepitate or
fly to pieces through the unequal expansion which overcomes the
cohesion of the molecules. Calcite, fluorite, and barite are
examples of this. A mineral which decrepitates may be separated from
one which does not, by decrepitating and sifting; the latter mineral
will be found on the sieve, while that which was finely decrepitated
will have gone through.
The Use of Supplementary Principles
A process usually consists of two or more successive steps, in which
the later is supplementary to the earlier. Thus, sorting in
classifiers is followed by sizing on slime tables; and sizing by
screens is followed by sorting on jigs. In each case the first step
prepares the ore for the second, and the second supplements and
completes the work which the first step was incapable of performing
alone. Neither step is complete without the other.
The use of graded crushing and graded separation to diminish the
amount of fines or slimes produced is quite frequently resorted to
with brittle minerals.
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40+ years’ experience in the mining industry with strong mineral
processing experience in precious metals, copper, industrial
minerals, coal, and phosphate
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Operational experience in precious metals, coal, and phosphate plus
in petrochemicals.
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Extensive experience performing studies and determining feasibility
in the US and international (United States, Canada, Mexico, Ecuador,
Columbia, Venezuela, Chile, China, India, Indonesia, and Greece).
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E-mail:
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