1. Energy Consumption 1
Transcript of 1. Energy Consumption 1
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Energy Consumption 1
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New Reserves
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Exajoules
/yr
(exa = 1018)
10
100
1000
2000
Annual World Energy Consumption
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Year
Annual World Energy Consumption
(exa = 1018)
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Annual World Energy Consumption
Gtoe=Gigatons of oil equivalent
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Recent World Temperature
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Global average ~ 2 kW ~ 173 MJ/da
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Per Capita Energy Consumption
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Per Capita Quality of Life Consumption
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Carbon Emission vs GDP
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11World Fastest Growing City
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Dubai
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Consumption/Population
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Mean Global Energy Consumption, 1998
4.52
2.72.96
0.286
1.21
0.286
0.828
0
1
2
3
4
5
TW
Oil Coal Biomass NuclearGas Hydro Renew
Total: 12.8 TW U.S.: 3.3 TW (99 Quads)
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Energy From Renewables, 1998
10-5
0.0001
0.001
0.01
0.1
1
Elect Heat EtOH Wind Solar PVSolar Th.Low T Sol HtHydro Geoth MarineElec Heat EtOH Wind Sol PV SolTh LowT Sol Hydro Geoth Marine
TW
Biomass
5E-5
1E-1
2E-3
1E-4
1.6E-3
3E-1
1E-2
7E-5
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(in the U.S. in 2002)
Today: Production Cost of Electricity
1-4 2.3-5.0 6-8 5-7 6-7
25-50
0
5
10
15
20
25
Coal Gas Oil Wind Nuclear Solar
Cost
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Energy Costs
0
2
4
6
8
10
12
14
$/GJ
Coal Oil Biomass Elect
Brazil E
urope
$0.05/kW-hr
www.undp.org/seed/eap/activities/wea
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Energy Reserves and Resources
0200004000060000
80000100000120000140000160000
180000
(Exa)J
Oil
Rsv
Oil
Res
Gas
Rsv
Gas
Res
Coal
Rsv
Coal
Res
Unconv
Conv
Reserves/(1998 Consumption/yr) Resource Base/(1998 Consumption/yr)
Oil 40-78 51-151
Gas 68-176 207-590
Coal 224 2160
Rsv=Reserves
Res=Resources
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Conclusions
Abundant, Inexpensive Resource Base of Fossil Fuels
Renewables will not play a large role in primary power generationunless/until:
technological/cost breakthroughs are achieved, orunpriced externalities are introduced (e.g., environmentally
-driven carbon taxes)
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ENERGY RESOURCE TIME SCALES
OIL 10s of years
COAL 100s of years FISSION 1000s of years
FUSION 1000s of years
(10,000s of years)
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P(t),
TW
Hubbert Model Applied to WorldResources
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GLOBAL CHANGE TIME HORIZONS
ATMOSPHERE 100s of years
FORESTS 75 years SCIENTIFIC
INSTITUTIONS 15+ years
GOVERNMENTS 5 years
Matching Supply and
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Matching Supply andDemand
Currently end use well-matched to physical properties of resources
Oil (liquid)
Gas (gas)
Coal (solid)
Transportation
Home/Light Industry
ManufacturingConv to e-
Pump it around
Move to user
Matching Supply and
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Matching Supply andDemand
If deplete oil (or national security issue for oil), then liquify gas,coal
Oil (liquid)
Gas (gas)
Coal (solid)
Transportation
Home/Light Industry
ManufacturingConv to e-
Pump it around
Move to user
Matching Supply and
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Matching Supply andDemand
If carbon constraint to 550 ppm and sequestration works
Oil (liquid)
Gas (gas)
Coal (solid)
Transportation
Home/Light Industry
ManufacturingConv to e-
Pump it around
Move to user
-CO2
CO2 sequestration, the storage of carbon dioxide as a solid through biological or physical processes
Matching Supply and
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Matching Supply andDemand
If carbon constraint to
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Matching Supply andDemand
If carbon constraint to 550 ppm andsequestration does notwork
Oil (liquid)
Gas (gas)
Coal (solid)
Transportation
Home/Light Industry
Manufacturing
Pump it around
Nuclear
Solar ?
?
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Nuclear Energy
1963 Responsible men spoke of atomic power so cheap it wouldntpay to meter it.
NH lights no switches for 5 years!
MAJOR NUCLEAR PROBLEMS:
Environmental Damage
Nuclear Waste
Weapons Potential
Catastrophic Disasters
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Alternatives to Nuclear energy
Coal
Conservation and Cogeneration
Small Hydro Oil and Natural Gas
Biomass
Other Renewables Fusion
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Globe and Mail (Spring 2007)
Gas Mileage
(mpg)
Purchase
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The Difficult Energy Questions
Should we build nuclear reactors?
How can we reduce CO2 emissions? (Coming!)
Population increase impact?
What is the environmental impact of our energyconsumption?
Does energy policy affect national security?
Should an energy policy be independent ofadministrative Ideology?
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LLE
The LLE is the product of the probability fora risk to cause death and theconsequences in terms of lost lifeexpectancy if it does cause death. As an
example, statistics indicate that an average40-year-old person will live another 37.3years, so if that person takes a risk thathas a 1% chance of being immediatelyfatal, it causes an LLE of 0.373 years (0.01x 37.3).
It should be clear that this does not meanthat he will die 0.373 years sooner as a
result of taking this risk. But if 1,000 peoplehis age took this risk, 10 might dieimmediately, having their lives shortenedby 37.3 years, while the other 990 wouldnot have their lives shortened at all.Hence, the average lost lifetime for the1,000 people would be 0.373 years.
Of course, most risks are with us to varyingextents at all ages and the effects must beadded up over a lifetime, which makes thecalculations somewhat complex.
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Energy Policy
1. There is disagreement even widespread ignorance aboutsome fundamental facts.
2. There is great uncertainty about what results the most commonlysuggested energy policies might produce.
3. There is no easy way to choose between short-term and long-term objectives. What is best for most of us this year may makethings very unpleasant in 1990 and vice versa.
4. There is no clear national consensus on the major long-term goalsof the United States (Canadas?) energy policy
S.H. Schurr, et. al., Energy in Americas Future,
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The Difficult Energy Questions
Should we build nuclear reactors?
How can we reduce CO2 emissions? (Coming!)
Population increase impact?
What is the environmental impact of our energyconsumption?
Does energy policy affect national security?
Should an energy policy be independent ofadministrative Ideology?
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Human Population Analogy
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Billions
Population History
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Population History
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Population!
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THE DIFFICULT ENERGY QUESTIONS
Should we build nuclear reactors?
How can we reduce CO2 emissions? (Coming!)
Population increase impact?
What is the environmental impact of our energyconsumption?
Does energy policy affect national security?
Should an energy policy be independent ofadministrative Ideology?