APES Lesson 7 - Demogrphy

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Presentation transcript:

APES Lesson 7 - Demogrphy AP Environmental Science Mr. Grant Lesson 92 Sources of Energy & Fossil Fuels and Their Extraction (Part 1)

APES Lesson 91 - Soures of Energy & Coal, Natural Gas, and Oil Objectives: Define the term fossil fuels. Identify the energy sources that we use. Describe the nature and origin of coal, and evaluate its extraction and use. Describe the nature and origin of natural gas, and evaluate its extraction and use.

APES Lesson 91 - Soures of Energy & Coal, Natural Gas, and Oil Define… Fossil Fuels Forms of stored solar energy created from incomplete biological decomposition of dead organic matter. Include coal, crude oil, and natural gas.

Identify the energy sources that we use. APES Lesson 91 - Soures of Energy & Coal, Natural Gas, and Oil Identify the energy sources that we use. Many renewable and nonrenewable energy sources are available to us. Since the industrial revolution, nonrenewable fossil fuels – including coal, natural gas, and oil – have become our primary sources of energy. Energy sources and energy consumption are each unevenly distributed across the world. The concepts of net energy and EROI allow us to compare the amount of energy obtained from a source with the amount invested in its extraction and production. We face a choice in whether to pursue new low-quality fossil fuel choices such as oil sands or whether to develop alternative sources of clean renewable energy.

Nature offers us a variety of energy sources We use energy in our homes, machinery, and vehicles and to provide comfort and conveniences Most of our energy comes from the sun Solar, wind, hydroelectric, photosynthesis, biomass Fossil fuels = highly combustible substances from the remains of organisms from past geologic ages A great deal of energy emanates from Earth’s core Geothermal power Immense amounts of energy reside in an atom’s bonds This energy provides us with nuclear power

Fossil fuels are indeed created from fossils Fossil fuels we burn today were formed from the tissues of organisms that lived 100-500 million years ago Organic material is broken down in an anaerobic environment = one that has little or no oxygen Bottoms of deep lakes, swamps, and shallow seas Organic matter is eventually converted into crude oil, natural gas, or coal

Nature offers us a variety of energy sources Renewable energy: supplies will not be depleted by our use Sunlight, geothermal energy, and tidal energy Nonrenewable energy: once depleted, supplies will be replaced within any time span useful to our civilization Oil, coal, natural gas To replenish the fossil fuels we have depleted so far would take millions of years We will use up Earth’s accessible store of fossil fuels in decades to centuries

We use a variety of energy sources We use these energy sources in our homes, our machinery, to fuel our vehicles, and provide the comfort and conveniences A great deal of energy emanates from Earth’s core, enabling us to harness geothermal power An immense amount of energy resides within the bonds among protons and neutrons in atoms, and this energy provides us with nuclear power Most of our energy comes from the Sun Solar radiation Photosynthesis Fossil fuels = highly combustible substances formed from the remains of organisms Solar, Wind, Geothermal, Tidal/Wave

Fossil fuels dominate our energy use Oil, coal, and natural gas have replaced biomass as our dominant sources of energy Global consumption is at its highest level ever The high-energy content of fossil fuels makes them efficient to burn, ship, and store Used for transportation, manufacturing, heating, cooking and generating electricity Electricity = a secondary form of energy that is easy to transfer and apply to a variety of uses

Fossil fuels are our dominant source of energy We use oil, coal, and natural gas Fossil fuels have replaced biomass as our dominant source of energy The high-energy content of fossil fuels makes them efficient to burn, ship, and store These fuels generate electricity = a secondary form of energy that is easier to transfer and apply to a variety of uses

Fossil fuels dominate our energy use Societies differ in how they use energy Energy use in industrialized nations is evenly divided between transportation, industry, and other uses Developing nations use a greater portion of their energy for subsistence activities Agriculture, food preparation, and home heating Less for transportation Often rely on manual or animal energy, not fossil fuels Industrialized nations rely more on technology and equipment so use more fossil fuels Fossil fuels supply 82% of the U.S. energy demand

Figure 19.3

Energy sources and consumption are unevenly distributed Industrialized nations use up to 100 times more energy per person than developing nations The United States has only 4.4% of the world’s population but consumes 19% of its energy OECD = Organization for Economic Co-operation and Development (20 developed countries)

Regions vary greatly in energy consumption

Energy sources and consumption are unevenly distributed Some regions have substantial reserves of oil, coal, and natural gas, whereas others have very few Half of the world’s proven reserves of crude oil lie in the Middle East, which is also rich in natural gas Russia holds the most natural gas The United States possesses more coal than any other country Russia and China also have large coal reserves

Fossil fuel reserves are unevenly distributed Some regions have substantial reserves, whereas others have very few How long a nation’s reserves will last depends on: How much the nation extracts, uses, and exports Nearly 67% of the world’s proven reserves of crude oil lie in the Middle East The U.S. possesses more coal than any other country

It takes energy to make energy We don’t get energy for free To harness, extract, process, and deliver energy requires substantial inputs of energy Mining oil sands requires powerful vehicles and machinery, roads, pipelines, waste ponds, storage tanks, housing, etc. All this requires energy Net energy = the difference between energy returned and energy invested Net energy = Energy returned - Energy invested

It takes energy to make energy Energy returned on investment (EROI) EROI = Energy returned/Energy invested Higher ratios mean we receive more energy than we invest Fossil fuels have historically high EROI

It takes energy to make energy EROI ratios can change They rise as technology improves They decline when we extract the easiest deposits first U.S. oil EROI ratios have gone from 30:1 in the 1950s to 20:1 in the 1970s to around 11:1 today EROI estimates for oil sands are mostly from 3:1 to 5:1

It takes energy to make energy To harness, extract, process, and deliver energy requires substantial inputs of energy Roads, wells, vehicles, storage tanks Net energy = the difference between energy returned and energy invested Net energy = energy returned – energy invested

Where will we turn in the future for energy? The astonishing advances of the 20th century were powered by abundant fossil fuels Over time we depleted the easy-to-reach sources EROIs rose, and fuel became more expensive We developed new technologies to reach new fossil fuel deposits and get more fuel from old ones We have included new, poorer quality sources such as oil sands and shale oil

Where will we turn in the future for energy? An alternate strategy to finding more fossil fuels is to switch to clean and renewable energy sources The switch has begun, but fossil fuels still dominate Scientists warn that we must switch now or drive our climate into unprecedented territory

Describe the origin and nature of major types of fossil fuels. APES Lesson 91 - Soures of Energy & Coal, Natural Gas, and Oil Describe the origin and nature of major types of fossil fuels. Fossil fuels are formed very slowly as buried organic matter is transformed by heat, pressure, and/or anaerobic decomposition Coal, our most abundant fossil fuel, results from organic matter that undergoes compression but little decomposition. Crude oil is a thick, liquid mixture of hydrocarbons that is formed underground under high temperature and pressure. Natural gas consist mostly of methane and can be formed in two ways. Oil sands contain bitumen, a tarry substance formed from oil that was degraded by bacteria. This can be processed into synthetic crude oil. Shale oil and methane hydrate are fossil fuel sources with potential for future use.

Fossil fuels are formed from ancient organic matter Fossil fuels we use today were formed from organisms that lived 100–500 million years ago The chemical energy in their tissues was concentrated as the hydrocarbons were altered and compressed Aerobic decomposition = organic material is broken down and recycled in the presence of air

Fossil fuels are formed from ancient organic matter Anaerobic decomposition = occurs with little or no air In deep lakes, swamps, shallow seas Produces fossil fuels The fossil fuel produced depends on a number of conditions at the start of and throughout the process

Coal Coal = a hard blackish substance formed from organic matter (woody plant material) compressed under very high pressure to form dense, solid carbon structures Very little decomposition occurred to the starting organic material Coal is the world’s most abundant fossil fuel Created 300–400 million years ago in swampy environments

Coal Coal varies from deposit to deposit in water and carbon content and its amount of potential energy Peat = organic material that is broken down anaerobically It is wet, near the surface, and not well compressed Additional pressure, heat, and time turn peat into coal Scientists classify coal into four different types

Oil and natural gas Crude oil (petroleum) = a sludgelike liquid mixture of hundreds of different types of hydrocarbon molecules Natural gas = methane (CH4) and other volatile hydrocarbons Both formed when dead organic material was buried in marine sediments and transformed by time, heat, and pressure Organic matter is turned into kerogen, the source material for both crude oil and natural gas If the kerogen is 1.5–3 km (1–2 mi) below the surface, it becomes crude oil If below 3 km, it becomes natural gas

Oil and natural gas Thermogenic gas = methane and other gases that arise from kerogen through compression and heat deep underground Most of the gas that is extracted commercially Often accompanies coal or crude oil deposits Biogenic gas = nearly pure methane created at shallow depths by bacterial anaerobic decomposition of organic matter “Swamp gas” Generated by the decay process in landfills; is being captured and sold as fuel

Oil sands and Oil shale Oil sands (tar sands) = sand and clay deposits with 1%–20% bitumen = a form of petroleum rich in carbon, poor in hydrogen Comes from crude oil deposits that have been degraded and chemically altered by water and bacteria Oil shale = sedimentary rock filled with kerogen Can be processes to produce shale oil = a liquid form of petroleum Forms when kerogen was not buried deeply enough or was not subject to enough heat and pressure

Methane hydrate Methane hydrate (methane clathrate or methane ice) = molecules of methane in a crystal lattice of ice molecules Occurs in sediments in the Arctic and the ocean floor Stable at the temperatures and pressures found in those locations Most formed by bacterial decomposition in anaerobic environments Some from thermogenic formation deep below the surface

Methane hydrate shows potential Methane hydrate (methane ice) = molecules of methane in a crystal lattice of water ice molecules Occurs in arctic locations and under the seafloor Formed by bacterial decomposition in anaerobic environments Immense amounts could be present, from twice to 20 times the amount of natural gas Extraction could destablize marine ecosystems Landslides and tsunamis release of large amounts of methane (a greenhouse gas)