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Mineral Resources
Mineral Resources
• Backbone of modern societies
• Availability of mineral resources as a measure of
  the wealth of a society
• Important in people’s daily life as well as in
  overall economy
• Processed materials from minerals account for 5%
  of the U.S. GDP
• Mineral resources are nonrenewable
Mineral Value
• Direct value
  – Raw, recycles
  – Import, export
• Indirect value
  – Processes
• Value added
  – E.g., agriculture
Common Use of Mineral
     Products


                   METALLIC
                  HYDROCARBON
                  NON-METALLIC
Mineral Resources and Reserves
• Mineral resources: Usable economic commodity
  extracted from naturally formed material
  (elements, compounds, minerals, or rocks)
• Reserve: Portion of a resource that is identified
  and currently available to be extracted legally and
  profitably
• Defining factors: Geologic, technological,
  economic, and legal factors
Reserves vs. Resources

• Reserves                      • Resources
  – Natural resources that        – Deposits that we know
    have been discovered &          or believe to exist, but
    can be exploited                that are not exploitable
    profitably with existing        today because of
    technology                      technological,
                                    economical, or political
  – Oil – 700 billion barrels       reasons
                                  – Oil – 2 trillion barrels
Mineral Resources Problems
• Nonrenewable resources
   – Finite amount of mineral resources and growing demands for
     the resources
• Supply shortage due to global industrialization
   – More developed countries consuming disproportionate share of
     mineral resources
• Erratic distribution of the resources and uneven
  consumption of the resources.
   – Highly developed countries use most of the resources; supply
     varies
Major Import Sources (Table 14.2)

• Friends
  – Canada: Metals
  – United Kingdom: platinum, rare earths
• Other
  – China: graphite, tin, tungsten…
  – South Africa : platinum, fluorspar
  – Chile: arsenic, iodine
Responses to Limited
         Availability

• Find more sources
• Find a substitute
• Recycle
• Use less and make more efficient use of
  what is available
• Do without
Responses to Limited
                  Availability




Figure 14.3
Geology of Mineral Resources
• Metallic ore: Useful metallic minerals that can be
  mined for a profit
• Technology, economics, and politics
• Concentration factor: Concentration necessary
  for profitable mining
  – Variable with types of metals
  – Variable over time
Genesis of Mineral Resources
Some Important Minerals and there Uses
•   Galena [PbS] – source of lead – car batteries
•   Magnetite, Hematite [FexOy] – iron ore
•   Bauxite [Al2O3*2H2O] – aluminum ore
•   Chalcopyrite [CuFeS2] – copper ore
•   Quartz [SiO2] – glass and electronic components
•   Gypsum [CaSO4*2H2O] – sheetrock, plater of paris
•   Sphalerite [ZnS] – zinc ore
•   Calcite [CaCO3] – portland cement, soil conditioner, antacids
•   Garnet [Al2(SiO4)3+other metals] – abrasives
•   Olivine [(Fe,Mg)2SiO4] – silicon chips for computers
•   Sulfur [S] – insecticides, rubber tires, paints, papermaking, etc.
•   Halite [NaCl] – Table salt
•   Graphite [C] – lubricant, pencil lead
•   Feldspars [K,Ca,Na,Al, silicates] – porcelain, source of K
•   Any other element that is not a major component of a mineral
•   Gold [Au], Silver [Ag], Platinum [Pt], Titanium [ Ti], Tin [Sn], etc .
Plate Tectonics and Mineral
               Resources
• Plate boundaries are related to the origins of
  many ore deposits
• Plate tectonic processes (high temperature, high
  pressure, and partial melting) promote release
  and enrichment of metals along plate
  boundaries
• Common metal ores along plate boundaries are
  Fe, Au, Cu, and Hg, etc.
Daily Questions
• Within your groups, identify one task you
  all have completed today. Collectively
  think about the task and brainstorm.
  Produce a list of all of the mineral resources
  that were used in that task.
Geochemically Abundant Elements
(GAE)
• Elements comprise > 0.1% (by
  weight) of the crust
• Form as principal component
  in minerals within common
  rocks – i.e. iron (Fe) Fe2O3
• Form very large deposits
• Form rock deposits
Geochemically Scarce Elements
(GSE)
  • Elements that comprise < 0.1% (by weight) of the
    crust
  • Do not form as principal component in minerals
    within common rocks, usually occur as a
    substitute in rock forming minerals
  • Form small deposits
  • Ore minerals include sulfides, native elements, etc.
Mineral Deposits
• Elements need to be concentrated
• Minimum Grade - minimum amount of element
  necessary to economically mine element
• Minimum Concentration Factor (MCF) –
  Minimum Grade divided by the Crustal
  Abundance
  – GAE have MCF < 100
  – GSE have MCF > 100
Comparison of Concentrations of Elements in the
   Earth’s Crust with Concentrations needed to operate
                   a Commercial Mine
Element      Natural               Concentration Required    Enrichment
             Concentration in      to Operate a commercial   Factor
             Crust (% by Weight)   mine (% by Weight)

  Aluminum            8                     24-32                  3-4
    Iron             5.8                      40                   6-7
   Copper           0.0058                 0.46-0.58             80-100
   Nickel           0.0072                   1.08                 150
    Zinc            0.0082                   2.46                 300
  Uranium          0.00016                   0.19                 1200
    Lead           0.00010                    0.2                 2000
    Gold          0.0000002                 0.0008                4000
   Mercury         0.000002                   0.2                100,000
Process that concentrate elements
• Igneous Processes
  – Hydrothermal
  – Magmatic
• Sedimentary Processes
  – Mechanical
  – Chemical
• Metamorphism Processes
• Groundwater Processes
Hydrothermal Processes
• Precipitation of metallic
  ions from hot, ion-rich
  fluid
• Fluid could be
   – Magmatic
   – Groundwater
   – Oceanic water
• Magmas heat up the water
• Water flows into fractures,
  faults, joints, etc. where it
  cools and precipitates
  (deposits) the metals
Magmatic Processes
• Gravity Settling
   – Dense, early-crystallizing
     minerals sink to the bottom
     of the magma chamber
• Filter Pressing
   – Tectonic force compress a
     magma chamber and force
     the still-liquid portion into
     fractures, creating large
     crystals
• These processes have
  produced large bodies of
  iron, chromium, titanium,
  and nickel
Sedimentary Processes
• Clastic
  – Weathering of
    rock also weathers
    out elements of
    interest
  – Generally, the
    elements are heavy
    and are deposited
    when a streams
    competence is low.
  – Placer deposits,
    i.e. gold
Placer Gold
Sedimentary Processes
• Chemical
  Precipitates
  – Water with high
    concentrations of
    elements is
    evaporated
  – Evaporation of
    water leaves the
    elements
  – Ex. Salts, Iron,
    etc.
Metamorphism
• Alteration of rock
  concentrates the
  elements
• The heat and
  pressure force out
  the GSE
  (“impurities”)
Weathering
• Chemical weathering removes
  soluble material.
• Ore material (elements of
  interest) are left behind in a
  concentrated residue.
Groundwater
• Secondary enrichment
• Groundwater dissolves and carries elements in
  solution
• Chemical conditions change and the elements are
  precipitated (deposited) out.
• Ex. Lead
Groundwater
• Secondary enrichment
• Groundwater dissolves and carries
  insignificant elements in solution
• Insoluble elements of interest remain.
• Ex. Aluminum
Ore Mineral
• Ability to separate and readily process the
  metal (element) from the ore material.
• Need to look at
  – The energy to process the material
  – The cost to process the material
  – The value of the metal
• Basically, is it profitable to mine the metal?
Mineralogical Barrier
    • Increase in energy and cost associated with
      the production of GSE
                                       Metals trapped in
                                       minerals (silicates)
Energy and Cost
  per mass of
     metal                           Mineralogical Barrier
                                                        Metals the have been
                                       GSE              concentrated
      $                  GAE
                                                                    Fixed
                                                                    Costs


            Low     Grade of metal (element) in rock High
Ways to overcome the
       mineralogical barrier
• Improve technology
• Recycle
• Come up with cheap energy to break
  silicate bonds
Daily Assignment
                  Place the following on
                  the Venn Diagram
                  1.Gold
                  2.Oil
5       4         3.Coal
    1
                  4.Iron
                  5.Copper
        2, 3, 6
                  6.Gravel
Plate Tectonics and Resources

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Tai nguyen khoang san 1

  • 2. Mineral Resources • Backbone of modern societies • Availability of mineral resources as a measure of the wealth of a society • Important in people’s daily life as well as in overall economy • Processed materials from minerals account for 5% of the U.S. GDP • Mineral resources are nonrenewable
  • 3. Mineral Value • Direct value – Raw, recycles – Import, export • Indirect value – Processes • Value added – E.g., agriculture
  • 4. Common Use of Mineral Products METALLIC HYDROCARBON NON-METALLIC
  • 5. Mineral Resources and Reserves • Mineral resources: Usable economic commodity extracted from naturally formed material (elements, compounds, minerals, or rocks) • Reserve: Portion of a resource that is identified and currently available to be extracted legally and profitably • Defining factors: Geologic, technological, economic, and legal factors
  • 6. Reserves vs. Resources • Reserves • Resources – Natural resources that – Deposits that we know have been discovered & or believe to exist, but can be exploited that are not exploitable profitably with existing today because of technology technological, economical, or political – Oil – 700 billion barrels reasons – Oil – 2 trillion barrels
  • 7.
  • 8. Mineral Resources Problems • Nonrenewable resources – Finite amount of mineral resources and growing demands for the resources • Supply shortage due to global industrialization – More developed countries consuming disproportionate share of mineral resources • Erratic distribution of the resources and uneven consumption of the resources. – Highly developed countries use most of the resources; supply varies
  • 9. Major Import Sources (Table 14.2) • Friends – Canada: Metals – United Kingdom: platinum, rare earths • Other – China: graphite, tin, tungsten… – South Africa : platinum, fluorspar – Chile: arsenic, iodine
  • 10. Responses to Limited Availability • Find more sources • Find a substitute • Recycle • Use less and make more efficient use of what is available • Do without
  • 11. Responses to Limited Availability Figure 14.3
  • 12. Geology of Mineral Resources • Metallic ore: Useful metallic minerals that can be mined for a profit • Technology, economics, and politics • Concentration factor: Concentration necessary for profitable mining – Variable with types of metals – Variable over time
  • 13. Genesis of Mineral Resources
  • 14. Some Important Minerals and there Uses • Galena [PbS] – source of lead – car batteries • Magnetite, Hematite [FexOy] – iron ore • Bauxite [Al2O3*2H2O] – aluminum ore • Chalcopyrite [CuFeS2] – copper ore • Quartz [SiO2] – glass and electronic components • Gypsum [CaSO4*2H2O] – sheetrock, plater of paris • Sphalerite [ZnS] – zinc ore • Calcite [CaCO3] – portland cement, soil conditioner, antacids • Garnet [Al2(SiO4)3+other metals] – abrasives • Olivine [(Fe,Mg)2SiO4] – silicon chips for computers • Sulfur [S] – insecticides, rubber tires, paints, papermaking, etc. • Halite [NaCl] – Table salt • Graphite [C] – lubricant, pencil lead • Feldspars [K,Ca,Na,Al, silicates] – porcelain, source of K • Any other element that is not a major component of a mineral • Gold [Au], Silver [Ag], Platinum [Pt], Titanium [ Ti], Tin [Sn], etc .
  • 15. Plate Tectonics and Mineral Resources • Plate boundaries are related to the origins of many ore deposits • Plate tectonic processes (high temperature, high pressure, and partial melting) promote release and enrichment of metals along plate boundaries • Common metal ores along plate boundaries are Fe, Au, Cu, and Hg, etc.
  • 16. Daily Questions • Within your groups, identify one task you all have completed today. Collectively think about the task and brainstorm. Produce a list of all of the mineral resources that were used in that task.
  • 17. Geochemically Abundant Elements (GAE) • Elements comprise > 0.1% (by weight) of the crust • Form as principal component in minerals within common rocks – i.e. iron (Fe) Fe2O3 • Form very large deposits • Form rock deposits
  • 18. Geochemically Scarce Elements (GSE) • Elements that comprise < 0.1% (by weight) of the crust • Do not form as principal component in minerals within common rocks, usually occur as a substitute in rock forming minerals • Form small deposits • Ore minerals include sulfides, native elements, etc.
  • 19. Mineral Deposits • Elements need to be concentrated • Minimum Grade - minimum amount of element necessary to economically mine element • Minimum Concentration Factor (MCF) – Minimum Grade divided by the Crustal Abundance – GAE have MCF < 100 – GSE have MCF > 100
  • 20. Comparison of Concentrations of Elements in the Earth’s Crust with Concentrations needed to operate a Commercial Mine Element Natural Concentration Required Enrichment Concentration in to Operate a commercial Factor Crust (% by Weight) mine (% by Weight) Aluminum 8 24-32 3-4 Iron 5.8 40 6-7 Copper 0.0058 0.46-0.58 80-100 Nickel 0.0072 1.08 150 Zinc 0.0082 2.46 300 Uranium 0.00016 0.19 1200 Lead 0.00010 0.2 2000 Gold 0.0000002 0.0008 4000 Mercury 0.000002 0.2 100,000
  • 21. Process that concentrate elements • Igneous Processes – Hydrothermal – Magmatic • Sedimentary Processes – Mechanical – Chemical • Metamorphism Processes • Groundwater Processes
  • 22. Hydrothermal Processes • Precipitation of metallic ions from hot, ion-rich fluid • Fluid could be – Magmatic – Groundwater – Oceanic water • Magmas heat up the water • Water flows into fractures, faults, joints, etc. where it cools and precipitates (deposits) the metals
  • 23. Magmatic Processes • Gravity Settling – Dense, early-crystallizing minerals sink to the bottom of the magma chamber • Filter Pressing – Tectonic force compress a magma chamber and force the still-liquid portion into fractures, creating large crystals • These processes have produced large bodies of iron, chromium, titanium, and nickel
  • 24. Sedimentary Processes • Clastic – Weathering of rock also weathers out elements of interest – Generally, the elements are heavy and are deposited when a streams competence is low. – Placer deposits, i.e. gold
  • 26. Sedimentary Processes • Chemical Precipitates – Water with high concentrations of elements is evaporated – Evaporation of water leaves the elements – Ex. Salts, Iron, etc.
  • 27. Metamorphism • Alteration of rock concentrates the elements • The heat and pressure force out the GSE (“impurities”)
  • 28. Weathering • Chemical weathering removes soluble material. • Ore material (elements of interest) are left behind in a concentrated residue.
  • 29. Groundwater • Secondary enrichment • Groundwater dissolves and carries elements in solution • Chemical conditions change and the elements are precipitated (deposited) out. • Ex. Lead
  • 30. Groundwater • Secondary enrichment • Groundwater dissolves and carries insignificant elements in solution • Insoluble elements of interest remain. • Ex. Aluminum
  • 31. Ore Mineral • Ability to separate and readily process the metal (element) from the ore material. • Need to look at – The energy to process the material – The cost to process the material – The value of the metal • Basically, is it profitable to mine the metal?
  • 32. Mineralogical Barrier • Increase in energy and cost associated with the production of GSE Metals trapped in minerals (silicates) Energy and Cost per mass of metal Mineralogical Barrier Metals the have been GSE concentrated $ GAE Fixed Costs Low Grade of metal (element) in rock High
  • 33. Ways to overcome the mineralogical barrier • Improve technology • Recycle • Come up with cheap energy to break silicate bonds
  • 34. Daily Assignment Place the following on the Venn Diagram 1.Gold 2.Oil 5 4 3.Coal 1 4.Iron 5.Copper 2, 3, 6 6.Gravel
  • 35. Plate Tectonics and Resources