Upload
genna
View
75
Download
4
Embed Size (px)
DESCRIPTION
Energy carriers. Energy carriers in our daily lives. Biomass (food, fuel, fertilizer) Fossil fuels: oil (liquid), coal (solid), natural gas Heat (solar, geothermal) Electricity: through electric grid Electricity: through battery or fuel cell (chemical energy). Uses for specific carriers. - PowerPoint PPT Presentation
Citation preview
Energy carriers
Energy carriers in our daily lives
Biomass (food, fuel, fertilizer)
Fossil fuels: oil (liquid), coal (solid), natural gas
Heat (solar, geothermal)
Electricity: through electric grid
Electricity: through battery or fuel cell (chemical energy)
Uses for specific carriers
What can you use for heat? Solar radiation, geothermal, burn biomass or any fossil fuel, dissipate electricity in a resistance => EVERYTHING
What can you use for transportation?Yourself (biomass), animals (biomass), oil (cars,buses, trains, planes), compressed or liquid natural gas (cars, buses, trains), coal (trains), electricity (grid transportation: bus, tram, train), electric unit (battery or fuel cell) => almost everything.
Then why is oil the best transportation fuel ever?
What can you use for light? Electricity, oil, gas, biomass
What can you use for appliances? ELECTRICITY
Important properties of energy carriers
1) Abundance
2) Availability
3) Cost (economic)
4) Rate of supply (renewable vs. fossil)
5) Energy density (MJ/kg)
6) Time-dependence of supply
7) Storage
8) Distribution
9) Production: centralized or distributed
10) Environmental impacts (local: pollution / global: climate)
Why does energy matter?
Not everyone has enough energy (ACCESS)
Some energy supplies are uncertain (SECURITY)
Some energy sources are in finite global supply (SCARCITY)
Energy sources are not equally geographically distributed (DISTRIBUTION)
Some energy sources are intermittent (STORAGE)
Local environmental impacts from energy use (POLLUTION)
Environmental impacts from energy use are changing the earth's climate (GLOBAL CATASTROPHE)
Energy densities
What do you estimate the density of different energy carriers to be?
For food: need ~ 2500 kcal/day
1000 kcal ~ 4 MJ
so ~ 10 MJ per day.
How many kg of rice or pasta (carbohydrates) or cookies (carbohydrates + fat) do you need to eat per day?
0.75 kg or rice or pasta: 15 MJ/kg or 360 kcal/100g
0.5 kg of cookies: 20 MJ/kg or 500 kcal/100g
Energy densities of selected carriers
Food dry weight: fat = 39.2 MJ/kgprotein = carbohydrates = 17.2 MJ/kg
(reason why food labels are in weight, not calories)
Biomass: 10 MJ/kg (green wood) => 20 MJ/kg (sugar cane bagasse, cotton hulls, oven-dried wood)
Coal: 17 MJ/kg (lignite) => 31.4 MJ/kg (anthracite)
Oil: 42 MJ/kg (crude) => 46 MJ/kg (kerosene)
Methane: 55.5 MJ/kg
Hydrogen: 142 MJ/kg
Uranium in light water reactor: 443'000 - 3'456'000 (enriched 3.5%) MJ/kg
foodbiomass
foodbiomass
Sources: USA Energy Information Agency Annual Energy Review 2005 , USA Census Measuring America (2002)
USA per capita energy consumption 1795-2006(does not include biomass for food)
0
50
100
150
200
250
300
350
40017
95
1809
1823
1837
1851
1865
1879
1893
1907
1921
1935
1949
1963
1977
1991
2005
Year
Ener
gy in
GJ
per c
apita
Coal
Natural gas
Petroleum
Nuclear
Hydroelectric
Geothermal
Solar PV
Wind
Wood
Total
2000 Watt society
USA per capita energy consumption 1795-2006
0
50
100
150
200
250
300
350
40017
95
1809
1823
1837
1851
1865
1879
1893
1907
1921
1935
1949
1963
1977
1991
2005
Year
En
erg
y in
GJ
per
cap
ita
Total fossil
Nuclear
Total renewable
Total
Sources: USA Energy Information Agency Annual Energy Review 2006 , USA Census Measuring America (2002)
USA total energy consumption 1795-2006
0
20
40
60
80
10017
95
1809
1823
1837
1851
1865
1879
1893
1907
1921
1935
1949
1963
1977
1991
2005
Year
Ener
gy in
Exa
Joul
esPo
pula
tion
in 1
00%
Total fossil
Nuclear
Total renewable
Total
Population (100% = 2006)
Sources: USA Energy Information Agency Annual Energy Review 2006 , USA Census Measuring America (2002)
Austria Domestic Energy Consumption 1830-1995
Source: Krausmann 2002
Includes food biomass
Comparison of per capita DEC in the UK and Austria 1830-2000
Source: Krausmann 2007
Includes food biomass
Fossil Abundance
Proved reserves (BP 2008)
0
5,000
10,000
15,000
20,000
1981 1986 1991 1996 2001 2006
Exaj
oule
s
Oil: Proved reserves
Natural gas: Proved reserves
Coal: Proved reserves
Abundance, but for how long?
Calculate R/P = Reserves / Production
Result is years left if nothing changes (no new discoveries, no change in production rates)
In 1980, R/P for oil 30 years, gas 60 years
In 2007, R/P for oil 40 years, gas 60 years (???)
For coal: 2007 R/P is 145 years, down from 180 in 2004
Total fossil R/P in 2007 is 80 years, down from 90 in 2004
OIL
Abundance, access, distribution: OIL
Source: BP Statistical Review of World Energy 2008
Peak Oil?
Prediction of Marion King Hubbert, 1956
Hubbert's peak
Zittel, Schindler et al 2004:(non-OPEC countries)
Proven reserves: no peak oil.
Source: BP Statistical Review of World Energy 2008
Reasons for increase: extraction/prospection improvements?inflation of reported reserves for OPEC quotas ?or to avert economic loss of confidence?
World crude oil prices, 1968-2006
0102030405060708090
Pri
ce o
f one
bar
rel i
n U
SD EIA Nominal
EIA "Real" 2000
Using 2000 CPI
Using 2006 CPI
Source: EIA 2007 http://www.eia.doe.gov/emeu/international/oilprice.htmlCPI from http://oregonstate.edu/cla/polisci/faculty/sahr/sahr.htmOwn calculation
Crude oil prices, constant $
0
20
40
60
80
100
120
1860 1880 1900 1920 1940 1960 1980 2000
2007
$ p
er b
arre
l
Any reasons for fluctuations?
Sou
rce
http
://w
ww
.wtr
g.co
m/p
rices
.htm
More recent prices: light crude futures
Sou
rce:
200
8 ht
tp:/
/fut
ures
.tra
ding
char
ts.c
om/
This week
World-wide oil trade
Source: BP Statistical Review of World Energy 2004
Transportation of oil: ship, pipeline, truck
Kazakhstan, source USA Energy Information Agency 2004-2005
Eurasia and pipelines
Source USA EIA 2004-2005
Pipelines, continued
Source USA CIA 2003 (via EIA)
Geopolitics and pipelines: blue stream
Source: Radio Free Europe Free Liberty
Coal
“Down the mine” by Orwell (1937)
“ Our civilization, pace Chesterton, is founded on coal, more completely than one realizes until one stops to think about it. The machines that keep us alive, and the machines that make machines, are all directly or indirectly dependent upon coal. In the metabolism of the Western world the coal-miner is second in importance only to the man who ploughs the soil. He is a sort of caryatid upon whose shoulders nearly everything that is not grimy is supported. For this reason the actual process by which coal is extracted is well worth watching, if you get the chance and are willing to take the trouble. “
“ There are still living a few very old women who in their youth have worked underground, with the harness round their waists, and a chain that passed between their legs, crawling on all fours and dragging tubs of coal. They used to go on doing this even when they were pregnant. And even now, if coal could not be produced without pregnant women dragging it to and fro, I fancy we should let them do it rather than deprive ourselves of coal. “
Integral text online: http://www.george-orwell.org/Down_The_Mine/0.html
King Coal
Source: BP Statistical Review of World Energy 2007
Lots of coal left: what does it mean?
Coal is currently mainly used for electricity generation (thermal power plants).
When oil runs out or becomes too expensive, coal can be transformed into a high energy density liquid through the process of "coal liquefaction" (already done by the Nazis and Apartheid South Africa).
Break-even costs for coal liquefaction? estimated at 30-60 $/barrel (currently above 60 $/barrel since mid-2005).
Prediction difficulties
Source: Nebojsa Nakicenovic, UNU, 1997
Evolution of CO2/energy?
CO2 emissions per unit primary commercial energy
15.8
16.0
16.2
16.4
16.6
16.8
17.0
17.2
17.4
17.6
1970 1975 1980 1985 1990 1995 2000 2005
Ton
s C
arbo
n / T
eraj
oule
Cumulative CO2 emissions
Cumulative CO2 fossil emissions since 1965
0
100,000
200,000
300,000
400,000
500,000
600,000
700,000
800,000
900,000
1,000,000
1960 1965 1970 1975 1980 1985 1990 1995 2000 2005 2010
Mil
lio
n t
on
nes
Electricity and electricity mixes
Uses: electricity
Important properties of energy carriers
1) Abundance
2) Availability
3) Rate of supply (renewable vs. fossil)
4) Energy density (MJ/kg)
5) Time-dependence of supply
6) Storage
7) Distribution
8) Production: centralized or distributed
9) Environmental impacts (risk, pollution)
Electricity: a final energy from many primary sources
Hydraulic (via solar and atmospheric processes and water pressure turning mechanical turbines)
Nuclear (via supernova nucleosynthesis and galactic processes, extraction, refining, controlled fission heating water and turning mechanical turbines)
Wind (via via solar and atmospheric processes and air pressure turning mechanical turbines)
Photovoltaic Solar (solar radiation via the photoelectric effect in high-tech Si chips)
Fossil (Solar radiation, geothermal processes, time, extraction, refining, burning to heat water and turn mechanical turbines)
Energy carrier properties for electricity
Energy carrier Storage Distribution Environmental impacts
Electricity Requires electric grid Can be both
Gasoline Possible VERY LOCAL
Natural Gas VERY LOCAL
Coal Possible LOCAL
Nuclear Pollution risks Pollution risks LOCAL
Solar Decentralized
Wind Not possible Decentralized
Production: centralized or
distributedNot possible
(except in repumping
dams)
Depends on production mechanism, usually fossil
Requires tanker ships, pipelines
Air pollution, water pollution, climate change
Possible but difficult
Possible but difficult (pipelines, LNG infrastructure)
Air pollution, water pollution, climate change (but cleaner than
oil)Ship, train, truck (no passive transport like
pipelines over long distances)
Air pollution, water pollution, climate change (much worse than
oil)
Waste disposal is unsolved problem. Uranium itself may be as
toxic as lead.Not possible
(except in plants)
Worldwide, more or less
Depends on technology choice, trade-offs in land-use choices.
Sea coast, mountain ridges
Landscape, usually considered not very high
Hydro good storage large river systems LOCAL Ecosystem disruption, methane
CO2 emissions from electricity
Electricity Source
Units
Fossil power plants
3.44 0.03 0.275
3.84 0.01 0.338
Oil 3.45 0.01 0.238Natural Gas 3.1 0.01 0.167
Nuclear power plants 3.52 0.01 0.002
RenewableWind 0.05 4 0.003
Solar Photovoltaic 0.38 6.5 0.020Hydraulic dam 0.01 1.28 0.001
Primary energy (non-renewable)
Primary energy
(renewable)
CO2 emissions
MJ primary /MJ final
MJ primary / MJ final
kg CO2 / MJ final
Hard Coal (anthracite or bituminous)
Soft Coal (sub-bituminous or lignite)
Source: EcoInvent Database
What is in coal-generated electricity?
110 times more Particulates per kWh compared to natural gas
23 times more SO2 per kWh
16 times more mercury per kWh (380 kg/yr for a 1000 MW plant)
radioactive trace elements
Coal is 1-10 ppm Uranium, 2.5-25 ppm Thorium
Uranium energy density in coal is 25% the energy density of coal! Sources: EcoInvent and A. Gabbard, ORNL
Uses: transport
Energy used for transport (IEA)
0
500000
1000000
1500000
2000000
2500000
Kilo
Tonn
e O
il E
quiv
alen
t (kt
oe)
Electricity
Combustible Renewables and Waste
Natural Gas
Petroleum Products
Coal and Coal Products
Transportation
Growing energy use for transportation worldwide.
Principally based on petroleum products
Generally two types of transportation:
1) Electric grid + rail or road (tram, train, buses)
2) Liquid fuel-based– kerosene + airports: planes,– diesel + ports: ships– gasoline + diesel + highways + parking: cars,
trucks, buses
3)Animal or human powered.
Metrics for transportationPersonal transportation: passenger*kilometre
Freight transportation: tonne*kilometre
Source OECD 1996
Primary energy cost of passenger transport
Transport mode Primary energy CO2 emittedMJ / p-km kg / p-km
Plane 9.83 0.36Car 3.25 0.18Bus 1.87 0.11
Train 1.06 0.06
Source EcoInvent Database
Primary energy cost of freight transport
Transport mode Primary energy CO2 emittedMJ / t-km kg / t-km
Plane 17.71 1.1116tonne truck 6.13 0.3532tonne truck 2.81 0.16
Train 0.75 0.04Barge 0.65 0.04
Ocean Tanker 0.09 0.01
Source EcoInvent Database
0.036
0.044
0.005
The global carbon cycle
What happens when we burn so much fossil fuels?
Climate change in the past
Source T. Stocker 2005
current level 380 ppm
(Can extend graph to 850'000, T. Stocker 2006)
Homo Sapiens appears
Agriculture begins
Climate change in the present
CO2 and energy carriers
Source: J. Siirola, GRC 2006
Causes of CO2 increase in atmosphere
Volcanoes ?
Agriculture / deforestation ?
Burning biomass ?
Burning fossil fuels ?
Sun-driven global warming?
at 380 ppm, CO2 in atmosphere corresponds to 730 GigaTonnes Carbon (GTC)
or 2650 GigaTonnes CO2 (GTCO2)(3.664 factor between CO2 and C)
a 30% increase since 1900.
Source: J. Siirola, GRC 2006
Remember CO2 in atmosphere is
currently 730 GTC!
CO2 content of proved fossil reserves
FUEL Reserves Production Consumption
Units tonnes CO2 percent tonnes CO2 tonnes CO2Oil 7.01E+011 26.45% 1.21E+010 1.19E+010
Anthracite 1.32E+012lignite 1.45E+012Coal 2.77E+012 104.49% 1.66E+010 1.69E+010Gas 3.41E+011 12.88% 5.25E+009 5.22E+009
Total 3.81E+012 143.82% 3.40E+010 3.40E+010
Proportion to current CO2 in
atmosphere
Source for proven reserves: BP Statistical Review of World Energy 2006
CO2 in atmosphere at 380 ppm: 2.65e12 tonnes
Food
A few facts about food
In Switzerland, fossil primary energy spent on food is estimated to be 34 GJ/person/year
Fossil primary energy spent on private transportation is 42 GJ/person/year
An average person eats 4.75 GJ/person/year in nutritional calories
Primary fossil / nutritional energy = 7
Source: Keanzig et Jolliet 2006, Consommation respectueuse de l'environnement, Rapport pour l'OFEV
Swiss agriculture and climate change
Source BLW, Rapport Agricole 2003
Agriculture and climate change (2)
Source BLW, Rapport Agricole 2003
Methane et Nitrous oxide
Methane = CH4
(natural gas) 8% of CO
2-eq. in Switz., of which 63% from agriculture
1 kg CH4 = 21 kg CO
2-eq.
In agriculture, methane comes from animal digestion and organic fertilizer.
Nitrous oxide = N2O
7% of CO2-eq in Switz., of which 72% from agriculture
1 kg N2O = 310 kg CO
2-eq.
Soil processes and various fertilizer.
Agriculture world-wide has emitted as many greenhouse gases as fossil fuel burning since 1900. Livestock world-wide emits as much GHG/yr as global transport. (Source: FAO 2006, Livestock’s long shadow)
8
Source BLW, Rapport Agricole 2003
Cause of the reduction of Swiss agricultural methane
Source BLW, Rapport Agricole 2005
ConséquencePlus de farines animales: donc fourrage importé:
Dont soja du Brésil et de l'Argentine (déforestation, perte de biodiversité)
Source BLW, Rapport Agricole 2002
Example of an industrial symbiosis with a bad ending …
Feeding animals with animal remains
Result: Spongiform encephalitis – Mad cow disease.
Soybean in Brazil
Source M. Shean, United States Department of Agriculture, 2004
Soybean area in Brazil (2)
Source M. Shean, United States Department of Agriculture, 2004