miller/spoolman living in the environment · 14-1 what are the earth’s major geological processes...
TRANSCRIPT
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17TH MILLER/SPOOLMAN
LIVING IN THE ENVIRONMENT
Chapter 14
Geology and Nonrenewable Mineral Resources
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Core Case Study: The Real Cost of Gold
• Gold producers
• China
• South Africa
• Australia
• United States
• Canada
• Cyanide heap leaching
• Extremely toxic to birds and mammals
• Spills contaminate drinking water and kill birds and fish
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Gold Mine with Cyanide Leach Piles and Ponds in South Dakota, U.S.
Fig. 14-1, p. 346
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14-1 What Are the Earth’s Major Geological Processes and Hazards?
• Concept 14-1 Dynamic processes move matter within the earth and on its surface, and can cause volcanic eruptions, earthquakes, tsunamis, erosion, and landslides.
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The Earth Is a Dynamic Planet
• What is geology?
• Dynamic processes taking place on earth’s surface and in earth’s interior
• Three major concentric zones of the earth
• Core
• Mantle
• Including the asthenosphere
• Crust
• Continental crust
• Oceanic crust: 71% of crust
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Major Features of the Earth’s Crust and Upper Mantle
Fig. 14-2, p. 348
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Fig. 14-2, p. 348
Volcanoes
Folded mountain belt
Abyssal floor
Oceanic ridge
Abyssal floor Trench
Craton Abyssal hills Abyssal plain
Oceanic crust (lithosphere)
Continental shelf
Continental slope
Continental rise
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The Earth Beneath Your Feet Is Moving (1)
• Convection cells, or currents
• Tectonic Plates
• Lithosphere
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The Earth Beneath Your Feet Is Moving (2)
• Three types of boundaries between plates • Divergent boundaries
• Magma
• Oceanic ridge
• Convergent boundaries • Subduction zone
• Trench
• Transform boundaries: San Andreas fault
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The Earth’s Crust Is Made Up of a Mosaic of Huge Rigid Plates: Tectonic Plates
Fig. 14-3, p. 348
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Fig. 14-3, p. 348
Spreading center
Ocean trench
Subduction zone Oceanic crust Oceanic crust
Continental crust Continental crust
Material cools as it reaches the outer mantle
Cold dense material falls back
through mantle
Hot material
rising through
the mantle
Mantle convection cell
Two plates move towards each other. One is subducted back into the mantle on a falling convection current.
Mantle
Hot outer core
Inner core
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The Earth’s Major Tectonic Plates
Fig. 14-4, p. 349
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Fig. 14-4, p. 349
EURASIAN PLATE NORTH AMERICAN PLATE
JUAN DE FUCA PLATE
CARIBBEAN PLATE
AFRICAN PLATE INDIA PLATE
PACIFIC PLATE COCOS
PLATE SOUTH AMERICAN PLATE
ARABIAN PLATE PHILIPPINE
PLATE
CHINA SUBPLATE
ANATOLIAN PLATE
PACIFIC PLATE
NAZCA PLATE
SOMALIAN SUBPLATE
AUSTRALIAN PLATE
SCOTIA PLATE
ANTARCTIC PLATE
Divergent plate boundaries
Convergent plate boundaries
Transform faults
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The San Andreas Fault as It Crosses Part of the Carrizo Plain in California, U.S.
Fig. 14-5, p. 350
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Some Parts of the Earth’s Surface Build Up and Some Wear Down
• Internal geologic processes • Generally build up the earth’s surface
• External geologic processes • Weathering
• Physical, chemical, and biological
• Erosion • Wind
• Flowing water
• Human activities
• Glaciers
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Volcanoes Release Molten Rock from the Earth’s Interior
• Volcano
• Fissure
• Magma
• Lava
• 1991: Eruption of Mount Pinatubo
• Benefits of volcanic activity
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Creation of a Volcano
Fig. 14-6, p. 351
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Fig. 14-6b, p. 351
Extinct volcanoes
Eruption cloud
Ash Acid rain Ash flow
Lava flow
Mud flow
Landslide Central vent
Magma conduit
Magma reservoir
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Earthquakes Are Geological Rock-and-Roll Events (1)
• Earthquake • Seismic waves
• Focus
• Epicenter
• Magnitude
• Amplitude
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Earthquakes Are Geological Rock-and-Roll Events (2)
• Richter scale • Insignificant: <4.0 • Minor: 4.0–4.9 • Damaging: 5.0–5.9 • Destructive: 6.0–6.9 • Major: 7.0–7.9 • Great: >8.0
• Largest recorded earthquake: 9.5 in Chile in 1960
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Major Features and Effects of an Earthquake
Fig. 14-7, p. 351
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Fig. 14-7a, p. 351
Liquefaction of recent sediments causes buildings to sink
Two adjoining plates move laterally along the fault line
Earth movements cause flooding in low-lying areas
Landslides may occur on hilly ground
Shock waves
Focus Epicenter
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Earthquake Risk in the United States
Figure 16, Supplement 8
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World Earthquake Risk
Figure 17, Supplement 8
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Earthquakes on the Ocean Floor Can Cause Huge Waves Called Tsunamis
• Tsunami, tidal wave
• Travels several hundred miles per hour
• Detection of tsunamis
• Buoys in open ocean
• December 2004: Indian Ocean tsunami
• Magnitude 9.15 and 31-meter waves at shore
• Role of coral reefs and mangrove forests in reducing death toll
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Formation of a Tsunami and Map of Affected Area of Dec 2004 Tsunami
Fig. 14-8, p. 352
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Fig. 14-8, p. 352
Earthquake in seafloor swiftly pushes water upwards, and starts a series of waves
Waves move rapidly in deep ocean reaching speeds of up to 890 kilometers per hour.
As the waves near land they slow to about 45 kilometers per hour but are squeezed upwards and increased in height.
Waves head inland causing damage in their path.
Undersea thrust fault
Upward wave Bangladesh
India Myanmar
Thailand
Sri Lanka Malaysia Earthquake Sumatra
Indonesia
December 26, 2004, tsunami
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Shore near Gleebruk in Indonesia before and after the Tsunami on June 23, 2004
Fig. 14-9, p. 353
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14-2 How Are the Earth’s Rocks Recycled? • Concept 14-2 The three major types of rocks found
in the earth’s crust—sedimentary, igneous, and metamorphic—are recycled very slowly by the process of erosion, melting, and metamorphism.
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There Are Three Major Types of Rocks (1) • Minerals
• Element or inorganic compound in earth’s crust
• Usually a crystalline solid
• Regular and repeating arrangement of atoms
• Rock
• Combination of one or more minerals
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There Are Three Major Types of Rocks (2) 1. Sedimentary
• Sediments from eroded rocks or plant/animal remains
• Transported by water, wind, gravity
• Deposited in layers and compacted
• Sandstone
• Shale
• Dolomite
• Limestone
• Lignite
• Bituminous coal
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There Are Three Major Types of Rocks (3) 2. Igneous
• Forms below or at earth’s surface from magma
• Granite
• Lava rocks
3. Metamorphic • Preexisting rock subjected to high pressures, high temperatures,
and/or chemically active fluids
• Anthracite
• Slate
• Marble
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The Earth’s Rocks Are Recycled Very Slowly
• Rock cycle
• Slowest of the earth’s cyclic processes
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Natural Capital: The Rock Cycle
Fig. 14-10, p. 354
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Fig. 14-10, p. 354
Erosion
Transportation
Weathering
Deposition
Igneous rock Granite, pumice, basalt
Sedimentary rock Sandstone,
limestone
Heat, pressure
Cooling
Heat, pressure, stress Magma (molten rock)
Melting
Metamorphic rock Slate, marble, gneiss, quartzite
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14-3 What Are Mineral Resources, and What Are their Environmental Effects? • Concept 14-3 We can make some minerals in the
earth’s crust into useful products, but extracting and using these resources can disturb the land, erode soils, produce large amounts of solid waste, and pollute the air, water, and soil.
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We Use a Variety of Nonrenewable Mineral Resources (1)
• Mineral resource
• Can be extracted from earth’s crust and processed into raw materials and products at an affordable cost
• Metallic minerals
• Nonmetallic minerals
• Ore
• Contains profitable concentration of a mineral
• High-grade ore
• Low-grade ore
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We Use a Variety of Nonrenewable Mineral Resources (2)
• Metallic mineral resources
• Aluminum
• Iron for steel
• Copper
• Nonmetallic mineral resources
• Sand, gravel, limestone
• Reserves: estimated supply of a mineral resource
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Some Environmental Impacts of Mineral Use
• Advantages of the processes of mining and converting minerals into useful products
• Disadvantages
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The Life Cycle of a Metal Resource
Fig. 14-11, p. 355
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Fig. 14-11, p. 355
Mining Metal ore
Separation of ore from waste material
Smelting Melting metal
Conversion to product
Discarding of product
Recycling
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Surface
mining Metal ore Separation
of ore from
gangue
Smelting Melting
metal Conversion
to product Discarding
of product
Recycling
Stepped Art
Fig. 14-11, p. 355
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Extracting, Processing, Using Nonrenewable Mineral and Energy Resources
Fig. 14-12, p. 356
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Fig. 14-12, p. 356
Natural Capital Degradation
Extracting, Processing, and Using Nonrenewable Mineral and Energy Resources
Steps Environmental Effects
Mining Disturbed land; mining accidents; health hazards; mine waste dumping; oil spills and blowouts; noise; ugliness; heat
Exploration, extraction
Processing
Solid wastes; radioactive material; air, water, and soil pollution; noise; safety and health hazards; ugliness; heat
Transportation, purification, manufacturing
Use Noise; ugliness; thermal water pollution; pollution of air, water, and soil; solid and radioactive wastes; safety and health hazards; heat
Transportation or transmission to individual user, eventual use, and discarding
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There Are Several Ways to Remove
Mineral Deposits (1) • Surface mining
• Shallow deposits removed
• Overburden removed first
• Spoils: waste material
• Subsurface mining
• Deep deposits removed
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There Are Several Ways to Remove Mineral Deposits (2)
• Type of surface mining used depends on
• Resource
• Local topography
• Types of surface mining
• Open-pit mining
• Strip mining
• Contour strip mining
• Mountaintop removal
•
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Natural Capital Degradation: Open-Pit Mine in Arizona
Fig. 14-13, p. 357
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Area Strip Mining in Wyoming
Fig. 14-14, p. 357
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Natural Capital Degradation: Contour Strip Mining
Fig. 14-15, p. 358
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Fig. 14-15, p. 358
Undisturbed land
Overburden
Pit Bench
Spoil banks
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Mining Has Harmful Environmental Effects (1)
• Scarring and disruption of the land surface
• E.g., spoils banks
• Mountain top removal for coal
• Loss of rivers and streams
• Air pollution
• Groundwater disruption
• Biodiversity decreased
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Mining Has Harmful Environmental Effects (2)
• Subsurface mining
• Subsidence
• Acid mine drainage
• Major pollution of water and air
• Effect on aquatic life
• Large amounts of solid waste
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Spoils Banks in Germany from Area Strip Mining
Fig. 14-16, p. 358
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Mountaintop Coal Mining in West Virginia
Fig. 14-17, p. 359
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Ecological Restoration of a Mining Site in Indonesia
Fig. 14-18, p. 360
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Removing Metals from Ores Has Harmful Environmental Effects (1)
• Ore extracted by mining
• Ore mineral
• Gangue = waste material
• Smelting using heat or chemicals
• Air pollution
• Water pollution
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Removing Metals from Ores Has Harmful Environmental Effects (2)
• Liquid and solid hazardous wastes produced
• Use of cyanide salt of extract gold from its ore
• Summitville gold mine: Colorado, U.S.
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Individuals Matter: Maria Gunnoe
• West Virginia environmental activist
• Won $150,000 Goldman Environmental Prize for efforts against mountaintop coal mining
• Her home
• Flooded 7 times
• Coal sludge in yard
• Well contaminated
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14-4 How Long Will Supplies of Nonrenewable Mineral Resources Last?
• Concept 14-4A All nonrenewable mineral resources exist in finite amounts, and as we get closer to depleting any mineral resource, the environmental impacts of extracting it generally become more harmful.
• Concept 14-4B Raising the price of a scarce mineral resource can lead to an increase in its supply, but there are environmental limits to this effect.
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Mineral Resources Are Distributed Unevenly (1)
• Most of the nonrenewable mineral resources supplied by
• United States
• Canada
• Russia
• South Africa
• Australia
• Sharp rise in per capita use in the U.S.
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Mineral Resources Are Distributed Unevenly (2)
• Strategic metal resources
• Manganese (Mn)
• Cobalt (Co)
• Chromium (Cr)
• Platinum (Pt)
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Supplies of Nonrenewable Mineral Resources Can Be Economically Depleted (1)
• Future supply depends on
• Actual or potential supply of the mineral
• Rate at which it is used
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Supplies of Nonrenewable Mineral Resources Can Be Economically Depleted (2)
• When it becomes economically depleted
• Recycle or reuse existing supplies
• Waste less
• Use less
• Find a substitute
• Do without
• Depletion time: time to use a certain portion of reserves
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Natural Capital Depletion: Depletion Curves for a Nonrenewable Resource
Fig. 14-19, p. 361
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Fig. 14-19, p. 361
Mine, use, throw away; no new discoveries; rising prices
A
Recycle; increase reserves by improved mining technology, higher prices, and new discoveries
B
Pro
du
ctio
n
Recycle, reuse, reduce consumption; increase reserves by improved mining technology, higher prices, and new discoveries
C
Depletion time A
Depletion time B
Depletion time C
Present
Time
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A Mine, use, throw away;
no new discoveries;
rising prices
Depletion
time A
Recycle; increase reserves
by improved mining
technology, higher prices,
and new discoveries B
Depletion
time B
Recycle, reuse,
reduce consumption;
increase reserves by
improved mining
technology, higher
prices, and new
discoveries C
Depletion
time C
Pro
du
cti
on
Present
Time Stepped Art
Fig. 14-19, p. 361
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Market Prices Affect Supplies of Nonrenewable Minerals
• Subsidies and tax breaks to mining companies keep mineral prices artificially low
• Does this promote economic growth and national security?
• Scarce investment capital hinders the development of new supplies of mineral resources
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Case Study: The U.S. General Mining Law of 1872
• Encouraged mineral exploration and mining of hard-rock minerals on U.S. public lands
• Developed to encourage settling the West (1800s)
• Until 1995, land could be bought for 1872 prices
• Companies must now pay for clean-up
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Colorado Gold Mine Must Be Cleaned up by the EPA
Fig. 14-20, p. 363
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Is Mining Lower-Grade Ores the Answer? • Factors that limit the mining of lower-grade ores
• Increased cost of mining and processing larger volumes of ore
• Availability of freshwater
• Environmental impact
• Improve mining technology
• Use microorganisms, in situ
• Slow process
• What about genetic engineering of the microbes?
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Can We Extend Supplies by Getting More Minerals from the Ocean? (1)
• Mineral resources dissolved in the ocean -- low concentrations
• Deposits of minerals in sediments along the shallow continental shelf and near shorelines
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Can We Extend Supplies by Getting More Minerals from the Ocean? (2)
• Hydrothermal ore deposits
• Metals from the ocean floor: manganese nodules
• Effect of mining on aquatic life
• Environmental impact
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Natural Capital: Hydrothermal Deposits
Fig. 14-21, p. 364
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Fig. 14-21, p. 364
Black smoker
White smoker
Sulfide deposits
Magma
White clam White crab
Tube worms
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14-5 How Can We Use Mineral Resources More Sustainability?
• Concept 14-5 We can try to find substitutes for scarce resources, reduce resource waste, and recycle and reuse minerals.
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We Can Find Substitutes for Some Scarce Mineral Resources (1)
• Materials revolution
• Nanotechnology
• Ceramics
• High-strength plastics
• Drawbacks?
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We Can Find Substitutes for Some Scarce Mineral Resources (2)
• Substitution is not a cure-all
• Pt: industrial catalyst
• Cr: essential ingredient of stainless steel
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Science Focus: The Nanotechnology Revolution
• Nanotechnology, tiny tech
• Uses
• Nanoparticles
• Are they safe?
• Investigate potential ecological, economic, health, and societal risks
• Develop guidelines for their use until more is known about them
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We Can Recycle and Reuse Valuable Metals
• Recycling
• Lower environmental impact than mining and processing metals from ores
• Reuse
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Aluminum Cans Ready for Recycling
Fig. 14-22, p. 366
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We Can Use Mineral Resources More Sustainability
• How can we decrease our use and waste of mineral resources?
• Pollution and waste prevention programs
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Solutions: Sustainable Use of Nonrenewable Minerals
Fig. 14-23, p. 366
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Case Study: Pollution Prevention Pays
• Begun in 1975 by 3M company, a very large manufacturing company
• Redesigned equipment and processes
• Fewer hazardous chemicals
• Recycled or sold toxic chemical outputs
• Began making nonpolluting products
• Company saved $1.2 billion
• Sparked cleaner production movement
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Three Big Ideas
1. Dynamic forces that move matter within the earth and on its surface recycle the earth’s rocks, form deposits of mineral resources, and cause volcanic eruptions, earthquakes, and tsunamis.
2. The available supply of a mineral resource depends on how much of it is in the earth’s crust, how fast we use it, mining technology, market prices, and the harmful environmental effects of removing and using it.
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Three Big Ideas
3. We can use mineral resources more sustainably by trying to find substitutes for scarce resources, reducing resource waste, and reusing and recycling nonrenewable minerals.