L4 - Platinum group elements (PGE) Flashcards

1
Q

Where are PGEs highly enriched?

A

In the core, mantle, and extraterrestrial bodies.

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2
Q

What are the melting and condensation properties of PGEs?

A
  • High melting and condensation temperatures.
  • Early condensation from the solar nebula and mantle processes.
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3
Q

What are the concentrations of PGEs in meteorites and the crust?

A
  • Meteorites: 400-900 ppb.
  • Crust: 0.4-0.5 ppb
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4
Q

Why are PGEs siderophile elements?

A

They bond with iron and sulfides.

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5
Q

How are PGEs transported?

A

As sulfur (S) and chlorine (Cl) complexes.

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6
Q

What was the first application of PGEs in catalytic reactions?

A

Davy’s safe lamp (1817) used a platinum wire to limit combustion of flammable gases

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7
Q

What properties make PGEs suitable for industrial applications?

A
  • Resistance to corrosion and oxidation.
  • Stability at high temperatures
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8
Q

What are the catalytic applications of PGEs?

A
  • Automotive: Oxidation of exhaust gases.
  • Petrochemical: Improving fuel octane rating.
  • Chemical: Fertilizer, explosives, nitric acid, and hydrogen cyanide production.
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9
Q

What are other applications of PGEs?

A
  • Jewelry.
  • Electrical contacts and wires.
  • Electronics (hard drives, LCD displays).
  • Medical and dental uses
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10
Q

What sulfide minerals are PGEs associated with?

A
  • Pyrrhotite (Fe₁₋ₓS).
  • Pentlandite.
  • Chalcopyrite
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11
Q

Name accessory PGE minerals

A
  • Sperrylite.
  • Laurite.
  • Erlichmanite.
  • Irarsite.
  • Braggite.
  • Cooperite
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12
Q

What is the typical economic ore grade for PGEs?

A

2.5-10 g/t (ppm), which represents an enrichment of <25,000x

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13
Q

Name significant locations for PGE reserves.

A
  • Stillwater Complex.
  • Sudbury Basin.
  • Great Dyke.
  • Stella Intrusion.
  • Bushveld Complex.
  • Norilsk.
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14
Q

What are the main deposit types for PGEs?

A

Layered igneous intrusions (orthomagmatic).

Placer deposits.

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15
Q

What is the Bushveld Complex?

A

The largest layered igneous intrusion, located in NE South Africa, a primary source of PGEs.

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16
Q

What rocks dominate the Bushveld Complex?

A

Mafic and ultramafic rocks.

Some granitic and sedimentary country rocks

17
Q

Describe the stratigraphy of the Bushveld Complex

A
  • Distinct layers of ultramafic (lower) and mafic (upper) rocks.
  • Feldspar absent in ultramafic rocks but present in mafic rocks.
  • Chromite bands contain high PGE concentrations.
18
Q

What are the main PGE reefs in the Bushveld Complex?

A

Merensky Reef (3-20 g/t PGE, first discovered in 1926).

UG-2 Reef (4-7 g/t PGE, primary source today).

19
Q

How do PGEs form in layered intrusions?

A

Partial melting of the mantle incorporates sulfides, which scavenge PGEs.

Sulfides bond with PGEs, becoming dense and forming cumulates as they crystallize.

20
Q

What is the role of fractional crystallization in PGE formation?

A
  • Dense minerals (olivine, pyroxene) crystallize first.
  • Sulfides saturate the melt, forming droplets that collect PGEs.
21
Q

How does magma mixing impact PGE formation?

A
  • Injection of melt into magma chambers disrupts crystallization.
  • Mixing promotes PGE scavenging by sulfide droplets
22
Q

What are the key exploration methods for PGEs?

A
  • Gravimetry: Detects density variations.
    Seismic techniques:
  • Identifies features >25m, such as potholes
23
Q

How are PGEs produced?

A
  • Underground mining (500-2000m depth).
  • Flotation processes separate hydrophilic feldspar and hydrophobic PGEs using foam
24
Q

What are the environmental impacts of PGEs?

A

Emissions from cars, smelters, and medical facilities.
Potential bioavailability of PGE nanoparticles.

25
Q

Why are PGEs considered critical resources?

A
  • Rare in the crust, requiring high enrichment for economic extraction.
  • Essential for catalytic, electronic, medical, and jewelry applications.