Unit 7 - The Geochemically Scarce Metals Flashcards

1
Q

Which of the geochemically scarce metals form minerals that can be found in common rocks?

A

Only copper, zinc, and chromium—the most common of the geochemically scarce metals—are able to form minerals in common rocks.

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2
Q

Describe the process of atomic substitution, and explain how a metal forms a mineral.

A

Atomic substitution, or solid solution, occurs when atoms of geochemically scarce metals take the place normally occupied by other atoms in a mineral. If the amount of those substituted atoms reaches saturation for that solid solution (about 0.1 per cent), a new mineral must form.

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3
Q

What factors may change the minimum concentration above background of geochemically scarce minerals to make them economical to mine?

A

The minimum concentration factor can change with demand and, by extension, price.

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4
Q

What are the modern industrial uses of chromium?

A

Chromium has a number of important uses. Chromium plating on steel and chromium alloys, such as stainless steel, keep the metal corrosion-resistant. Chromium-steel alloys are used in aircraft engines, military vehicles, weapons, and chemical industry, so the metal is considered strategic to national defence and industry. Added to steel for machine tools, it increases hardness and resistance to wear. Chromium is also used for making pigments and for tanning animal hides.

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5
Q

Differentiate between podiform and stratiform chromium deposits. Which type of deposit contains the world’s largest chromium resources? Where is the largest deposit located?

A

Chromite, the major ore mineral of chromium, is found in ultramafic rock. Podiform deposits (which have an elongated, lenticular shape) are found in highly faulted and deformed portions of tectonically active zones. The chromite appears as rounded granules enclosed in dunites and serpentinites, which are thought to be displaced fragments of the upper crust mantle. Stratiform deposits are layers of pure chromite which occur in large, mafic intrusions. Current research indicates that the chromite “grew” at the bottom of a cooling magma chamber during fractional crystallization when the magma periodically became contaminated with the melting country rock. Stratiform deposits contain the most abundant chromium resources, and the largest such deposit is in the Bushveld Igneous complex of South Africa.

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6
Q

Briefly discuss the uncertainty about present and future world chromium supplies.

A

South Africa accounts for seventy per cent of the world’s chromium supplies. While the demand is high, the supply could be affected by civil, political unrest.

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7
Q

What valuable properties does vanadium give to steel? What are the primary industries in which vanadium is used?

A

Vanadium makes steel hard enough to use in armour plating. The American automobile industry relies on vanadium-steel alloy because it increases steel’s strength, high temperature abrasion resistance, ductility, and ease of welding. Because the weight of an automobile body need not be as great with vanadium steel as with carbon steel, using vanadium-steel alloy increases the efficiency of vehicles. Vanadium steel is also used widely in gas and oil transmission pipelines.

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8
Q

Although vanadium is one of the most common geochemically scarce elements, vanadium ore deposits are rare. Why?

A

Vanadium-rich magnetites are the most important ore deposits. Vanadium, however, is easily able to substitute for ferric iron, and thus enters into solid solution with the abundant iron minerals. This substitution is so common that localized deposits with concentrations of more than about two per cent vanadium are rare.

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9
Q

Explain why vanadium deposits are found in both igneous and sedimentary geological environments.

A

Occurring in igneous rocks, vanadium ore is similar to chromium ore. It appears to have formed in cooling magma chambers by fractional crystallization. The difference between chromium ore and vanadium ore is that vanadium ore is found near the top of the magma chamber.
In the sedimentary situation, vanadium weathers out of the igneous rock and is oxidized to a more soluble state. Transported long distances in solution by surface or groundwater, it eventually precipitates by evaporation or in contact with organic matter, which reduces it to a less soluble state. This process is similar to those undergone by uranium and copper; in fact, vanadium is often found in concentration with uranium. Vanadium is also found associated with coal, crude oil, and the bitumen of tar sands.

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10
Q

How could Alberta become an important world producer of vanadium?

A

If the large scale mining of the Athabasca Oil Sands (in Alberta) continues, it has been estimated that over two million tonnes of vanadium could be recovered.

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11
Q

Describe the process of nickel plating. List the characteristics of nickel that make it valuable as an alloying agent for iron.

A

In the electroplating of nickel, a metal plate of nickel is attached to the anode of a battery, submerged in a solution, and an electric current is passed through the battery. The nickel from the nickel plate dissolves and migrates to the object connected to the cathode, where it is deposited as a thin layer. Nickel resists corrosion, can be polished to a high lustre, and adds strength.

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12
Q

Describe the formation of the nickel ore, pentlandite, which involves liquid immiscibility in the process of magmatic segregation.

A

Crystallization of a mineral compound from solution is a function of both temperature and concentration. When a mineral compound reaches its saturation point in a cooling magma, it begins to crystallize. If the temperature of the melt is higher than the compound’s melting point, however, the compound must remain a concentrated liquid droplet within the melt. The elements will not combine within the compound droplet: they are immiscible (cannot be mixed). This often happens within the iron sulphide mineral, pyrrhotite. The droplets gather atoms of other elements (including nickel) from the melt, and form an iron-nickel-copper-sulphide liquid. Being denser than the silicate magma, the droplets settle to the bottom and form a sulphide-rich zone at the base of the chamber. When this zone eventually crystallizes, pyrrhotite forms along with grains of nickel ore, called pentlandite. Ores with a nickel content of three or four per cent can be formed like this.

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13
Q

Describe the process responsible for forming garnierite in laterite ores of nickel.

A

When mafic and ultramafic igneous rocks undergo chemical weathering in a hot, humid climate, the silicate minerals decompose to form hydrous compounds and the iron oxidizes to the ferric state. The nickel present is released and either forms nickel silicate minerals or becomes part of the structure of other weathering minerals. The nickel silicate minerals are known as garnierite; they often have a nickel content of four to five per cent. Residual ores formed from weathering in this manner are called laterite ores.

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14
Q

Which three countries have the largest reserves of sulphide and laterite nickel ores?

A

Canada, Russia, and Australia (in that order) account for the largest reserves of sulphide ores of nickel. The largest reserves of laterite nickel ores are found in New Caledonia, the Philippines, and Cuba (in that order).

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15
Q

Describe the important properties and uses of molybdenum.

A

Most of the molybdenum mined today is used as an alloy with steel and cast iron. Used as a superalloy, molybdenum gives hardness, toughness, and corrosion and abrasion resistance, and adds strength at high temperatures. It is used throughout industry, especially in the production of cutting tools, in transportation, and in oil and gas production equipment. Nonmetallic uses include lubricants, catalysts, and pigments.

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16
Q

Describe the geological occurrence of nearly all known molybdenum ores.

A

Molybdenite, the chief metallic mineral of molybdenum, occurs in porphyry-type deposits (porphyry: very hard red, green, or purple igneous rock). Such deposits are associated with subduction zones at the edges of continental plate boundaries. In fact, a large percentage of molybdenum production is associated with porphyry copper mining.

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17
Q

Which countries have the largest reserves of molybdenum?

A

The USA and Chile contain the largest reserves of molybdenum, although significant reserves are also found in Canada, Russia, China, Mexico, and Peru.

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18
Q

What are the important qualities of cobalt alloys? Why is cobalt considered a strategic metal?

A

Cobalt alloys retain their strength at high temperatures and are resistant to corrosion by hot gases. Consequently, they are important in the production of jet engines, rocket nozzles, and gas turbines, and are thus considered to be strategic from a military standpoint.

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19
Q

With which three minerals is cobalt commonly associated?

A

Cobalt is often associated with copper and silver in stratiform copper sulphide ores. It also concentrates wherever nickel is concentrated.

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20
Q

Which countries contain the largest reserves of cobalt and dominate production of the metal?

A

The African countries of Congo and Zambia are dominant in cobalt reserves and production.

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21
Q

What are the important qualities of tungsten, and what are its uses?

A

Tungsten is the metal with the highest melting point and the highest tensile strength. Tungsten steels are used where toughness, durability, and impact resistance is important. The hardness of tungsten carbide is close to that of diamond, and is used in tools, drill bits, cutting edges, and armour-piercing projectiles. Because of its high melting point, tungsten is important in producing filaments for electric light bulbs, heating elements, and distributor points in automobiles.

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22
Q

Describe the geological occurrence of tungsten.

A

Tungsten is found in hydrothermal vein deposits and is associated with limestone and marble created by contact metamorphism.

23
Q

Which three countries contain the largest reserves of tungsten ore?

A

China, Canada, and Russia have the largest reserves of tungsten ore.

24
Q

Describe the formation of hydrothermal solutions.

A

Hydrothermal solutions consist of heated underground water with a high concentration of dissolved minerals, especially the silicate minerals. Water at high temperatures is an excellent solvent and is capable of dissolving substances normally considered insoluble. Water may percolate from the surface to depths which are naturally hot or to areas adjacent to magma bodies, where heat causes the water to become an effective solvent. Water may also result from the cooling of a magma, in which highly mineralized water is released to the surrounding area in liquid form or as steam.

25
Q

How do porphyry copper deposits form, how valuable are they, and why are they mined?

A

Magma cooled and non-hydrous minerals crystallized in a conduit or chamber beneath a volcano. This process increased the water content of the remaining magma, resulting in steam explosions that fractured the surrounding rock. In this process, the hydrothermal solutions escaped through the fractures, cooling and crystallizing the contained minerals—including copper—and effectively filling in the fractures.
Since this type of ore consists of tiny veins of copper, the entire body of the rock must be mined and processed to remove the metal. Porphyry copper deposits, therefore, are of a relatively low grade. However, since they are usually deposited near the surface and have a somewhat cylindrical shape (which makes mining easier), they are commonly mined.

26
Q

Describe the formation of volcanogenic massive sulphide deposits, and discuss their value in copper mining.

A

Volcanogenic massive sulphide deposits form after hot springs or sea water are heated at depth along volcanic rifts at spreading centers. When they erupt into the cold water at the ocean floor, the minerals instantly precipitate. The minerals are always sulphides, including the copper sulphide, chalcopyrite. Although relatively free of impurities, the deposits found, so far, are not rich enough in the important ore minerals to justify the high cost of underwater mining. The only massive sulphide ores mined today are ancient fragments of the ocean crust now located on the continents.

27
Q

What are stratiform ore deposits? Outline two theories about their formation.

A

Stratiform ore deposits consist of native copper and sulphite minerals found in clastic, marine sedimentary rock, in layered patterns. One theory as to their formation is that they represent massive sulphide deposits that have intruded into overlying layers of sediment or sedimentary rock. Another theory is that hydrothermal solutions circulate into coarse, clastic sedimentary layers beneath highly mineralized shale. The ore minerals are thought to have resulted from reactions between the solutions and the minerals in the shale.

28
Q

What proportion of the world’s copper production comes from each type of copper deposit?

A

Porphyry and skarn deposits account for sixty per cent of the world’s copper production; sediment-hosted stratiform deposits make up twenty per cent; and massive sulphide deposits make up twelve per cent. The rest is accounted for as by-product from the mining of nickel, lead, and zinc.

29
Q

What are the principal uses of lead and zinc?

A

Lead is mainly used in the production of storage batteries, as an anti-knock additive in gasoline, for cable coverings, in paint pigments, for flashings in building construction, in ammunition, in bearings, and as an alloy. Zinc is used in galvanizing, as an alloy, and in paint pigments, ointments, lotions, and creams.

30
Q

List the four types of lead-zinc deposits, and describe the formation of Mississippi-Valley type deposits.

A

The four types of lead-zinc deposits are hydrothermal vein deposits, volcanogenic massive sulphide deposits, Mississippi-Valley-type (MVT) deposits, and sediment hosted stratiform deposits.
MVT deposits occur where hydrothermal solutions, originating in sedimentary basins, flow laterally into limestone beds, and the ore minerals galena and sphalerite either replace the limestone or are precipitated between the fragments of limestone breccia.

31
Q

Which country has the largest reported reserves of lead? Zinc?

A

While the USA has the largest reserves of lead, Canada has the largest reserves of zinc.

32
Q

What are the primary uses of tin?

A

Both historically and in modern times, tin has been used as an alloy in creating bronze and pewter. Today, it is also used as a coating agent for corrosive metals and as a major constituent of solder.

33
Q

What is the most important tin mineral, and where is it found?

A

The principal ore mineral of tin is cassiterite. It is mined from pegmatites and hydrothermal deposits related to andesite or rhyolitic volcanism. Cassiterite is often found in placer deposits.

34
Q

Which three major tin producing countries recover their own ore strictly from placer deposits?

A

Malaysia, Thailand, and Indonesia recover tin from placer deposits only.

35
Q

What is the important ore mineral for mercury?

A

The only important mercury mineral is cinnabar.

36
Q

What are the modern uses of mercury?

A

About forty percent of mercury produced is used in scientific measuring instruments; other uses include batteries (thirty percent) and chemical production (thirty percent).

37
Q

With which other metallic ore mineral is cadmium associated, and why?

A

Although cadmium minerals are rare, they are usually found in trace amounts in the zinc ore mineral, sphalerite. This is because cadmium replaces zinc by atomic substitution. All cadmium production today is a by-product of zinc mining.

38
Q

What are the main uses of gold in the modern world?

A

Historically, gold was used for ornamentation and for coinage. Today, its use as currency is quite limited, but it is used as a standard to back paper currency. The industrial use of gold has skyrocketed, and over half of the world’s annual gold production is now used in electronic products, aerospace applications, special alloys, and dentistry.

39
Q

Why does gold commonly occur in placer deposits, while few ferro-alloy or base metals do so?

A

Because gold is dense, is malleable, and does not readily combine with other elements, it may be quickly separated from the rock it was formed in during the tumbling action involved in alluvial transport. Later, it can concentrate in favourable locations in stream beds. In the same circumstances, ferro-alloy or base metals would most likely be chemically altered and dissolved.

40
Q

Where are the world’s largest gold deposits, and how were they formed?

A

The largest gold deposits in the world are the Witwatersrand deposits in South Africa. The gold is found in conglomerates which have been lithified from ancient coarse, clastic, deltaic deposits. It is thought that these 2.3–2.8 billion-year-old deposits represent placers.

41
Q

What are the important modern uses of silver? On what unique properties are these uses based?

A

Because silver has high electrical conductivity, it is widely used in electrical contact and conductors where extreme sensitivity is desired. Its industrial uses include the manufacture of batteries, catalytic converters, solders and cell phones. Silver also has medical applications because it helps reduce infections. In dentistry, it is used for dental amalgams. Because silver compounds are light sensitive, a large proportion of silver used to be directed towards the production of photographic film. However, over the last two decades, the emergence of digital photography has seen the steady replacement of photographic film by digital technology. As a result, the use of silver in photography has decreased significantly.

42
Q

About seventy-five per cent of all silver mined today is a by-product of mining which two metals?

A

Silver is recovered largely as a by-product of mining copper and lead.

43
Q

Which countries account for the world’s greatest annual production of silver?

A

While Mexico has the largest annual production of silver, Peru, the United States, and Canada are also leading producers.

44
Q

What are the six platinum group metals, and why are they always found together?

A

The six platinum group metals are platinum, palladium, rhodium, iridium, ruthenium, and osmium. They always occur together, because their chemical and physical properties are similar, and because they often substitute for each other by atomic substitution.

45
Q

Which properties of these metals account for their use today?

A

All of these metals are corrosion-resistant, have high melting points, and act as catalysts in chemical reactions.

46
Q

Describe the two geological settings in which the platinum group metals are found.

A

Platinum group metals are often found in mafic and ultramafic rocks where they are concentrated in chromite horizons and sulphide-rich layers. They are also found in placer deposits that have presumably resulted from the weathering and erosion of the aforementioned deposits.

47
Q

Which country accounts for the world’s largest annual production of platinum group metals? Which country has the largest reserves?

A

Russia and South Africa are, by far, the largest producers of platinum group metals. These two countries also have the largest reserves.

48
Q

How did the “special metals” acquire their name?

A

The special metals are known by that name because they possess exceptional properties and have specialized functions in modern technology.

49
Q

What are the main uses of niobium and tantalum?

A

Niobium is used in high-strength alloys for applications such as gas turbines and jet engines. It is also used in superconducting magnets.
Tantalum is used in capacitors and rectifiers in the electronics industry. It is also used in high temperature cutting tools. Because tantalum resists corrosion, it is also used for surgical tools.

50
Q

Discuss the geological environments in which niobium and tantalum are found.

A

Niobium and tantalum occur as columbite ((FeMn)Nb2O6) and tantalite ((FeMn)Ta2O6). The two are always produced together because columbite is always found with some tantalum in solid solution, while tantalite always has some niobium. The minerals occur in a number of igneous rocks, especially nepheline syenites, carbonatites, and pegmatites. Columbite and tantalite are hard and resistant to weathering, so they often concentrate in placer deposits when the parent igneous rocks disintegrate.

51
Q

What are the main uses of arsenic, antimony, and bismuth? These scarce metals are produced as by-products of which more abundant metals?

A

Arsenic, antimony, and bismuth are produced as by-products of smelting processes for other metals such as lead, zinc and copper.
Arsenic is mainly used in fungicides, insecticides, pesticides, and chemical compounds used to preserve wood.

Antimony forms important alloys and is used to strengthen the lead in lead batteries. It also alloys well with other base metals, giving them corrosion-resistant properties. Uses of chemical compounds of antimony include the production of pigments for paints, plastics, and glass stabilizers as well as a range of other applications.

Bismuth finds use in the production of pharmaceuticals and cosmetic compounds. It is also used in the manufacture of low melting alloys.

52
Q

Which properties of germanium, gallium, and indium make them valuable materials for the electronics industry?

A

Germanium possesses excellent electrical conductivity and is used in the manufacture of semiconductors for computers. Gallium expands on crystallization and is used in the production of alloys. Indium melts at very low temperatures and is soft and malleable. All three are used in the electronics industry.

53
Q

Name a major source of the mineral beryl, from which the metal beryllium is extracted.

A

Beryllium has two major occurrences: one is the mineral beryl, which is found in pegmatites. Beryl, however, always occurs in either small quantities or low concentrations. Another source of beryllium is the mineral bertrandite, which is found in hydrothermal deposits associated with rhyolite extrusions. Such deposits too, always occur in small quantities.

54
Q

Why are rare-earth elements (REE) known by that name?

A

Rare-earth elements (REE) were given that name because when they were initially discovered, only their oxides were known and they appeared to resemble the oxides of alkaline earth elements such as CaO and BaO. Hence, it was believed they did not form common minerals, so they were described as the rare earths.