cvs4, fig. 8.1
DESCRIPTION
Geochemically scarce. Copper Nickel Cobalt Lead Zinc Chromium Tin Mercury Gold Silver Platinum Rare-earth elements. CVS4, Fig. 8.1. Solid Solution = Atomic Substitution. Cobaltian calcite, (Ca,Co)CO 3. Pure calcite, CaCO 3. Atomic Substitution in Al 2 O 3 , Corundum. Ruby. - PowerPoint PPT PresentationTRANSCRIPT
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EPSc 116: Resources of the Earth
Lecture 22 on Ch. 8: Geochemically Scarce Metals
Themes
Carefully read Focal Points, pp. 264-265.
Scarce metals (individually <0.1 wt. % of earth's crust)
35 scarce metals in TOTAL < 1 wt. % crust
Scarce metals enhance the efficiency of industry:
Alloys; special properties
"Enzymes" of industry
Elements most likely to run out
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CVS4, Fig. 8.1
Copper
Nickel
Cobalt
Lead
Zinc
Chromium
Tin
Mercury
Gold
Silver
Platinum
Rare-earth elements
Geochemically scarce
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How do scarce elements occur:
Usually not as their "own" minerals, e.g., NOT like Fe2O3 [hematite]
Atomic substitution or solid solution: e.g., of cobalt (Co) for calcium (Ca)
CaCO3 vs. (Ca,Co)CO3 [CaCO3 = calcite]
CaCO3 CaCO3 CaCO3 CaCO3 CaCO3 CoCO3 CaCO3 CaCO3 CaCO3 CaCO3
So, (1) element is dispersed, (2) desired mineral is dispersed, NOT massive
Effect on exploration, mining, processing, residues
Harder targets: smaller deposits, fewer deposits
May recover only small quantities of desired element
By-products: silver in solid solution in galena (PbS); cadmium in sphalerite (ZnS)
**What concentration is too little to bother with?
Special Considerations for Scarce Elements/Metals
Silver Cadmium
IF we do not deliberately separate out scarce elements from ore, they may "travel"
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Pure calcite, CaCO3
Cobaltian calcite, (Ca,Co)CO3
Solid Solution = Atomic Substitution
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Atomic Substitution in Al2O3, Corundum
Ruby Sapphire
Cr3+ Al 3+
Fe2+ + Ti4+ 2Al3+
Structure of corundum
Images from Wikipedia
Gemstones
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Natural Abundance Makes a Difference
Natural crustal abundance (top scale, in ppm) vs. concentration needed for mining (bottom, in wt.%)
The more vertical the connecting line , the lessenrichment needed over the “natural” abundance: Al, Fe.The more horizontal the line, the more enrichmentneeded: lead, gold.
The most abundant elements form “their own minerals”and occur in relatively large, rich deposits.The more scarce elements “hop a ride” in mineralsdominated by other elements; they also occur insmaller, less concentrated deposits.
Abundant Scarce
Grade (%)
Grade (%)
“Abundant” elements
“Scarce” elements
Currentmining
Currentmining
Enrichment
Crustalabundance
Minegrade
Logarithmic scale: 102 101 100 10-1
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Geochemistry Meets Economics
CVS4, Fig. 7.21
CVS3, Fig. 8.2
CVS4, Table 8.2
Crustal abund.
Enrich-ment
Minable grade
ppm
(from ore)
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Typical Types of Minerals that are Ores of Geochemically Scarce Metals
Dominated by sulfides, oxides, and native metals
CVS4, Table 8.3
Base-metal sulfides
Alloy- and specialty-metal oxides
Native-element precious metalsPlatinum-
group metals
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Ore deposits tend to be small in tonnage cf. abundant elements:
require huge-scale mining
Copper mine in Bisbee, Arizona
Special large-scalemining equipment
Special Needs for Scarce-Metal Mines
Geologic process or combination of
processes causes local
concentration and precipitation
Primary oremineral oxidized &dissolved here
Water’s metal contentreprecipitated assecondary oreminerals here
Primary ore
Surface
Secondary processing:
Oxidation + Reprecipitation
Open-pitmining
CVS4, Fig. 8.16
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Precipitation by Hot Waters
Groundwater heated by igneous intrusion. Local heat source creates convection currents in the water. Leaching and pptn.
As in porphyry copper deposit
CVS4, Fig. 8.20
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Porphyry copper deposits are clustered along coasts, above subduction zones.
Porphyry Copper Deposits of the World
CVS4,
Fig. 8.21
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http://www.pmel.noaa.gov/vents/nemo/education/curr_p1_11.html
More Hot Water
scienceblogs.com/highlyallochthonous/2007/07/precambrian_black_smokers.php
Black smoker on the sea floor near mid-ocean ridge and rift
Copper, iron, and zinc sulfides precipitated in smoker “chimneys”
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Cooler Waters (around 100°C)
Waters compressed out of sediments in a basin can move, leach metals, and precipitate minerals elsewhere.
CVS4, Fig. 8.24b
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Lead-Zinc Deposits from Cool Waters
About 2 hrs. south of St. Louis
CVS4, Fig. 8.24a
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Even Colder Water:
Ambient Temperature
Density separation and concentration of minerals by the flow of (river) water
CVS4, Fig. 8.32Examples = gold, diamonds
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South African Gold Deposits: Ancient Streams and Deltas
CVS4, Fig. 8.34
Discovered by two prospectors in 1886
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Ferrous/ferro-alloy metals: lend specific properties, especially to steels (Cr, V, Ni, Mo)
Nonferrous/base metals: Cu, Pb, Zn, Hg, Sn. Not very high in price (which annoyed the alchemists!)
Precious metals: Au and Ag, Pt, Pd, Os, Ir, Rh. "Noble metals”, meaning non-reactive (as well as”fit for a king”)
Specialty metals: Ta (electronics), Be (nuclear technology), Bi, Ga,Ge, Zr. Industry uses.
Rare-earth metals: heavily used in high-tech magnets; great needfor these in alternative/green energy producers (hybrid engines, windmills)
Classify Scarce Elements by Usage
Rare-Earth Metals
Non-ferrous base metalsFerrous metals
www.chemicalelements.com/
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Cr, chromium represents 0.0096 wt.% of crust = 9600 ppm
Uses: stainless steel (hard, non-corrosive)
Aircraft engines, weapons
Chemicals--pigments, etc.
Refractory – chromite linings in furnaces
Chromium: Example of a Ferro-Alloy Metal
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Geologically
Forms in large igneous rock bodies that cooled and crystallized
Formed layers that are 10's to 100's of miles long.
Dense crystals settle out of melt.
Represents how chromium builds up in melt after precipitation of minerals without chromium.
Politically
South Africa has 70% of world's chromium reserves.
Large supply of chromium. Limitations are political and social.
Chromium as a Strategic Metal: Essential to Well-Being of a Country
© Cédrick Gineste
Melt Crystals come out Chromium builds up
Chromitecrystallizes
Mineral chromite
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Copper: Example of a Base Metal
Cu or Au was first metal used by humans; both occur in elemental (native) state
Malleable, electrical conductor, corrosion resistant
Uses: coins, wires, pipes, alloy.
Several kinds of ore deposits; deposition frequently controlled by plate tectonics
Magmatic segregation: immiscible liquids (compare to lava light)
Hydrothermal veins near magma bodies; porphyry Cu from subduction and melting of crust
Sedimentary fluids in normal sedimentary basins transport & precipitate much copper
Gold as a by-product of some copper miningMain copper oremineral, chalcopyriteCuFeS2
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CVS4, Fig. 8.15
Growth in the copper industry (and use of copper) was spurred by the spread of electrification (copper wire)
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Copper’s Environmentally InducedChanges in Ore Processing
Smelting
Acid dissolution(leaching)
Microbially mediateddissolution
Need to get the copper out of the copper sulfide mineral, CuFeS2
Heap leachingon a pad
Heat copper sulfide mineral
Drive off sulfur gas (leaving metal behind)
Trap sulfur gas BEFORE it reaches atmosphere.
Learn from nature how microbes help to break down sulfide minerals and release metal
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From De Re Metallica (1558). Ancient metallurgists attempting to “win” various metals from their ore minerals by heating them.
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What 6 countries account for most of the metal reserves of the world? Why?
Geologic specificity of the location of individual metals (ore deposits): plate-tectonic localization of ores (broad scale),
structural geologic & geochemical control (at progressively finer scales)
Plate tectonic lectures and text Figs. 8.4, 8.13, 8.21, 8.28.
Relations (over time) between:production/use and reserves (text Fig. 8.23, page 291)minable ore grades (text Fig. 8.2 on copper, p. 268, Fig. 8.31 on gold, p. 300)
Recycling: text Fig. 7.14 (page 249)
Lessons to Learn from Geochemically Scarce Metals
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CVS4, Fig. 8.23
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CVS4, Fig. 8.2
Average grade (wt.% Cu) of copper ore mined in the U.S. over time.
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CVS4, Fig. 8.31 Average grade of gold ore mined in the US over time
~ 1 ppm