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Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011
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Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

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Page 1: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 Physics for Decision Makers:The Global Energy Crisis

Lecture 12 - Fossil Fuels

Fall 2011

Page 2: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Assignments

Energy Audit 3Assignment #3:

Prepare a report of your inventory of identified energy consumers gathered from your building walk thru. Include estimates of uncertainties in your numbers (we expect you to estimate, not count every light fixture, for example). Compare this to the measured consumption and give possible explanations for the discrepancies – what do you think you missed? Length: ~2 pages. Upload to ELMS. Due Date: Oct 13 (20 pts.)

Reading Assignment Finish - Chapter 5 Wolfson Post editorial about the Keystone XL pipeline (On Elms)

EXAM – Likely November 1

Page 3: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

On this project my group members are doing a:1. A+ job2. A job3. B job4. C job5. no comment yet

Page 4: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

As to reading chapter 5 of Wolfson

1. I have read it2. I have skimmed it3. I plan on reading it4. I don’t have the book5. I have the book but don’t plan on reading it

Page 5: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

How I get to/around campus:

1. Bus2. Walk3. Bike4. Car5. Metro6. Bus/walk7. Bike/walk8. Car/bike9. Car/walk

Page 6: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Home heating - First Law vs. Second Law

First Law Efficiency:- Energy out/energy in Example: resistive electric heat ~ 100% efficient (1st

Law) Heating requires relatively low temperatures

(don’t want 500 deg air blowing out of ducts)- Need to go from Toutside

~ 273 K to Tinside ~ 300 K- Wouldn’t we be better off moving heat around, especially since the indoor and outdoor temperatures are not too different?

- Second Law Efficiency:- Energy of absolute best process (Carnot)/(energy in)- Tinside

/(Tinside-Toutside)=300 K/27k= 11 (Coefficient of Performance)

- Now electric heat is 9% efficient (2nd law) : We have lots of room for improvements!

Page 7: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

My (parents) home is heated with…

1. Natural gas2. Propane3. Oil4. Electric (resistive) heat5. Heat Pump6. Solar7. I have no clue.

Page 8: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

FurnacesOil -popular in New EnglandNatural gasPropane

Very efficient (1st Law)>90%

Not a lot of room for improvements

Home heating

Page 9: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Heat Pumps

Move heat from outside to inside ( a refrigerator run backwards - cooling the outdoors)

Page 10: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Heat Pumps

Rated with SEER rating (Seasonal Energy Efficiency rating)

SEER = ratio of seasonally averaged cooling power in BTU/h compared to Watts of electricity used (measured when used as air conditioner)

e.g. SEER of 16 produces almost 5X more cooling power than it uses in electricity

upgrading from SEER 9 to SEER 13, the power consumption is reduced by 30% (equal to 1 − 9/13) can save ~$300/yr

-remember - we are moving heat so we can have a 1st Law efficiency > 1!

-Why don’t we all have heat pumps?

Page 11: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

A Cool Idea

Dig down 20 ft. and the ground temperature is about 55 F- Why not use this as a source of heat in the winter, and as a

place to dispose of heat in the summer?

Page 12: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

FOSSIL FUELS

Page 12

Page 13: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.
Page 14: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Crude Oil Prices

Oil touches $140 a barrel Today $85 a barrel 1 barrel of oil = 42 US gallons

Page 15: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Gasoline Prices

Page 16: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011Marquee Lecture 4/12/11

How much do we (US) spend on oil?

The United States consumed 18.8 million barrels per day of petroleum products during 2009.

At the current price ~$100/barrel – this is ~$2B/day or $700B/yr

Discretionary spending US Govt.: $1.368 trillion - -$663.7 billion Department of Defense-Total US Government discretionary spending $700B/yr

Page 17: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

How much would raising gas prices

$1/gallon cost the average US family?

1. $500/yr2. $1000/yr3. $1500/yr4. $2000/yr5. $2500/yr

Page 18: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Cost to Average Consumer

Assume Driver goes 12,000 miles/year Car gets 24mi/gallon 500 gallons/year Each $1/gallon cost $500/year/car

Page 19: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Cost to Average Consumer

If you have 2 drivers per family $1,000 year

Page 20: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Cost to Average Consumer

Taxes are NOT a percentage of the cost

Now around 13% $0.45/gallon Germany Tax - $4/gallon

O

Page 21: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.
Page 22: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Why did oil prices rise so much recently?

1. We are running out of oil2. Demand is greater than

supply3. Conspiracy of oil

companies4. Weak US dollar5. Speculators are bidding

price up6. OPEC is restricting supply7. The Iraq War has

introduced uncertainty

Page 23: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Fossil Fuels

Oil (petroleum)

Natural Gas (methane)

Coal

Peat Note: propane is derived from oil

Page 24: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

When were there dinosaurs on earth

1. Never2. 100 thousand years ago3. 1 million years ago4. 25 million years ago5. 50 million years ago6. 100 million years ago7. 250 million years ago8. 500 million years ago9. 1 billion years ago10.3 billion years ago

Page 24

Page 25: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Geological Time scale

Page 26: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Where Fossil Fuels Come From

Page 27: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Where Fossil Fuels Come From

There are three major forms of fossil fuels: coal, oil and natural gas. All three were formed hundreds of millions of years ago before the time of the dinosaurs - hence the name fossil fuels. Many were formed in the Carboniferous Period. It was part of the Paleozoic Era. "Carboniferous" gets its name from carbon, the basic element in coal and other fossil fuels.

The Carboniferous Period occurredfrom about 360 to 286 million years ago. At the time, the land was covered with swamps filled with huge trees, ferns and other large leafy plants. The water and seas were filled with algae.

Page 28: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

How do we know hold old rocks are?

Relative time- In layered formations, lower layers are older

Page 29: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

How do we know how old rocks are?

Absolute time- Radiometric dating

- Certain isotope naturally decay (radioactivity) with a characteristic “half-life”- E.g. U235-> Pb207 t1/2 = 703.8 million years

- When rock forms, all U, no Pb - “clock starts”- Measure ratio of U235/Pb207- If = 1, T = 704 million yrs.- If =1/3, T = 2X 704 million yrs.

- This is exponential decay (the opposite of exponential growth)

Page 30: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Peat

As trees and plants die in swampy areas, they sink to the bottom of the water. If it is deficient in oxygen, it does not decay and eventually builds layers of a spongy material called peat.

Peat is 75% water, 15% carbon

Up to 2% of world’s land has peat

If burned peat is recent, can be thought of as renewable

Page 31: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Coal

Over many hundreds of years, the peat was covered by sand and clay and other minerals, compressing it into a form of sedimentary rock.

More and more rock piled on top of more rock, and it weighed more and more. It began to press down on the peat. The peat was squeezed and squeezed until the water came out of it and it eventually, over millions of years, it turned into coal.

Page 32: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Coal

Coal is a hard, black colored rock-like substance. It is made up of carbon, hydrogen, oxygen, nitrogen and

varying amounts of sulfur. There are three main types of coal – Anthracite (90% carbon)- the hardest and has more carbon, which

gives it a higher energy content Lignite (30% carbon)- the softest and is low in carbon but high in hydrogen and

oxygen content. Bituminous is in between. (50-75% carbon)

Charcoal is NOT coal

Page 33: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

US Coal reserves

Page 34: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

World Coal reserves

Will the US give up coal?

Page 35: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Proved recoverable coal reserves 2006 (million tonnes)

Page 36: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Mining Coal

3,000-5,000 mining deaths per yr. in China20-50 in USBlack lung disease…

Page 37: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Mountaintop removal in WV

Check out ilovemountains.org

Page 38: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Powder River Basin (Nebraska & Montana)

Page 38

Page 39: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Powder River Basin Coal

Powder River Basin coal is classified as "sub-bituminous" and contains an average of approximately 8,500 btu/lb, with low SO2. Contrast this with eastern, Appalachian bituminous coal containing an average of 12,500 btu/lb and high SO2. PRB coal was essentially worthless until air pollution emissions from power plants became a concern.

It gets harder to get as more is mined. USGS estimate that at most half will be practical to mine.

Page 39

Page 40: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Cautionary Note…

Coal is probably not the best energy source- Environmentally damaging- Major source of air pollution- Major source of global warming gases- Causes health problems/deaths in miners

- BUT:- US has 27% of world coal supply- US has 2.4% of world’s oil supply- US has 38X more energy in coal than oil…

-What happens when oil runs out?

Page 41: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Burn more coal…

Page 42: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Oil

Most scientists agree that oil comes from creatures the size of a pinhead. These one-celled creatures, known as diatoms, aren't really plants, but share one very important characteristic with them - they take light from the sun and convert it into energy

Diatoms float in the top few meters of the oceans (and lakes - which is part of the reason why not ALL oil comes from ocean deposits!) and also happen to be a major source of food for many forms of ocean swimmers.

Page 43: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Plankton

Two types - Phytoplankton: Plants of the Sea- Zooplankton: Sea Animals

Plankton either float passively in the water, or possess such limited powers of swimming that they are carried from place to place by the currents.

Page 44: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Plankton range in size from tiny microbes, which are invisible to the naked eye, to jellyfish meters long.

Apart from bacteria, planktonic organisms are the most abundant life form on earth

They are a critical part of the carbon energy chain The total amount of carbon in the ocean is about 50 times

greater than the amount in the atmosphere, and is exchanged with the atmosphere on a time-scale of several hundred years.

At least 1/2 of the oxygen we breathe comes from the photosynthesis of marine plants.

Page 45: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Oil

Oil is formed from the preserved remains of prehistoric plankton (diatoms) and algae which have been settled to the sea (or lake) bottom in large quantities in water depleted of oxygen.

Terrestrial plants, on the other hand, tend to form coal. Over geological time this organic matter, mixed with mud,

is buried under heavy layers of sediment. The resulting high levels of heat and pressure cause the organic matter to chemically change, first - into a waxy material known as kerogen which is found in

various oil shales around the world, - then with more heat into liquid and gaseous

hydrocarbons->Oil and Natural Gas

Page 46: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Depending on the balance of fresh water versus evaporation this can change with time and reverse providing different layers

This is why oil is often found just off shore or in regions that used to be water covered- Like the Middle East and

Gulfs

Page 47: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Source Rock

Oil comes from rocks (source rocks)– not big caverns There is "oil window" which is the temperature range that

oil forms in—below the minimum temperature oil remains trapped in the form of kerogen, and above the maximum temperature the oil is converted to natural gas

This corresponds to a certain depth in the earth

A rock won’t have oil if:- It wasn’t a rock with lots of

organic material- If the rock hasn’t been that deep- It was deeper than that depth

Page 48: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Three conditions must be present for oil reservoirs to form: - a source rock rich in organic material buried deep enough

for subterranean heat to cook it into oil; - a porous and permeable reservoir rock for it to

accumulate in; - a cap rock (seal) or other mechanism that prevents it

from escaping to the surface. Within these reservoirs fluids will typically organize

themselves like a three-layer cake with a layer of water below the oil layer and a layer of gas above it, although the different layers vary in size between reservoirs.

Page 49: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Page 49

Page 50: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

The vast majority of oil that has been produced by the earth has long ago escaped to the surface and been biodegraded by oil-eating bacteria.

Oil companies are looking for the small fraction that has been trapped by this rare combination of circumstances.

Oil sands are reservoirs of partially biodegraded oil still in the process of escaping, but contain so much migrating oil that, although most of it has escaped, vast amounts are still present - more than can be found in conventional oil reservoirs. It is usually in the form of asphalt and is mined…

On the other hand, oil shales are source rocks that have never been buried deep enough to convert their trapped kerogen into oil.

Page 51: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011Marquee Lecture 4/12/11

US Oil Production

1991 – 7.4 million barrels/day

2009 – 5.3 million barrels/day

(1 barrel = 42 gallons)

Page 52: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Hubbert

Marion King Hubbert (1903–1989) geoscientist at Shell Oil

Predicted the end of the Oil Age

“Our ignorance is not so vast as our failure to use what we know.”

Page 53: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Hubbert’s basic idea

There is only so much oil recoverable on Earth- Therefore we eventually use it all up

Am

ount

use

d

0

100%

time

Page 54: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Hubbert’s basic idea

We can instead plot the rate of usage

Am

ount

use

d/yr

0

time

“Hubbert’s peak“Peak Oil”

Page 55: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Hubbert’s peak

Page 56: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Hubbert Theory with Norway's production

Page 57: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

World Oil

Page 58: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

World Oil - except OPEC

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Page 60

1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 200965000

70000

75000

80000

85000

90000

World Total Oil Supply

World

Page 60: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Have we already reached peak oil?

Page 61

1. Yes2. No3. Not sure

Page 61: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.
Page 62: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Best Fit World Data

Page 63: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Look at rate of discoveries…

Page 64: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Assume 300 billion bbls new discoveries Assume 600 billion bbls new discoveries

Peak Oil - 2012 Peak Oil - 2040

Oil & Gas Journal May 07, 2007 volume 105, issue 17

Author(s) : Steve H. Mohr Geoffrey M. Evans

Some current predictions

Page 65: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.
Page 66: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Page 67

Page 67: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

OPEC

Page 68: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Criticisms of “Peak Oil”

Doesn’t account for new technology- Production- Discovery

Oil companies are overly conservative in what “proven” means Where there is a will there is a way…-If the price is high enough, other sources will be tapped

Page 69: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Oil (Tar) Sands

Oil sands or tar sands, are a type of unconventional petroleum

A mixture of sand, clay, water, and a dense and extremely viscous form of petroleum technically referred to as bitumen

Oil sands are found in large amounts in Canada and Venezuela

It is a thick, sticky form of crude oil, so heavy and viscous (thick) that it will not flow unless heated or diluted with lighter hydrocarbons

Page 70

Page 70: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Keystone Xl Pipeline

a

Page 71

Page 71: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Offshore drilling in the US

Most areas were put off limits in 1981 by congress, 1989 by Pres. Bush(Sr) after Exxon Valdez spill

Sept. 30, 2007 - Congress lets ban expire…except for Eastern Gulf of Mexico

Page 72: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

What can (should) the US do?

Drill offshore Drill in ANWR

Estimates: ANWR: 5- 10 billion bbls.US offshore: 45 billion bbls.

World: 1237 billion bbls.

“The projections in the OCS access case indicate that access to the Pacific, Atlantic, and eastern Gulf regions would not have a significant impact on domestic crude oil and natural gas production or prices before 2030. “ - US Dept. of Energy 2007 report

Page 73: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Hirsch Report of DoE 2005

World oil peaking is going to happen, and will likely be abrupt.

Oil peaking will adversely affect global economies, particularly those most dependent on oil.

Oil peaking presents a unique challenge (“it will be abrupt and revolutionary”).

The problem is liquid fuels (growth in demand mainly from transportation sector).

Page 74: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Hirsch report

Mitigation efforts will require substantial time.- 20 years is required to transition without substantial

impacts- A 10 year rush transition with moderate impacts is

possible with extraordinary efforts from governments, industry, and consumers

- Late initiation of mitigation may result in severe consequences.

Both supply and demand will require attention. It is a matter of risk management (mitigating action must

come before the peak). Government intervention will be required.- Economic upheaval is not inevitable (“given enough lead-

time, the problems are soluble with existing technologies.”)

- More information is needed to more precisely determine the peak timeframe.

Page 75: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011Deepwater Horizon

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Physics 105 – Fall 2011

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Physics 105 – Fall 2011

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Physics 105 – Fall 2011

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Physics 105 – Fall 2011 Page 80

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Physics 105 – Fall 2011

Page 81: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Wed. March 31 Pres. Obama gives speech from Andrews Air force base

Tuesday, April 20 Deepwater Horizon suffers explosion in the Gulf of Mexico

Wed. April 21 Firefighters and rescue ships fight ongoing fire on Deepwater Horizon

Thursday, April 22, Earth Day, Deepwater Horizon sinks. Eleven crew missing

April to July, approx. 52,000 to 63,000 Barrels per day (3 Million Gals. per day) leaked

July 15, 2010 Cut-off well head capped

Sept 19, 2010 Well declared dead after filling top and bottom with cement

Page 82: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Should the US drill in

1. ANWR2. Offshore3. Both4. Neither

Page 83: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

OLDUVAI THEORYONE VIEW OF THE FUTURE World Energy Production, Population Growth, And the Road to the Olduvai Gorge Richard C. Duncan Institute on Energy and Man As published in Population and Environment, May-June 2001.Named for the Olduvai Gorge in Tanzania where remains found are crucial to understanding human evolution were

found

Page 84: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Olduvai Theory

Defined by the ratio of world energy production and population.

It states that the life expectancy of Industrial Civilization is less than or equal to 100 years: 1930-2030.

After more than a century of strong growth — energy production per capita peaked in 1979.

Moreover, it says that energy production per capita will fall to its 1930 value by 2030, thus giving Industrial Civilization a lifetime of less than or equal to 100 years.

This analysis predicts that the collapse will be strongly correlated with an 'epidemic' of permanent blackouts of high-voltage electric power networks — worldwide.

Page 85: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.
Page 86: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

World Energy Production per Capita: 1920-1999

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Page 88: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

When you are 50 years old, the world’s standard of living will be

1 2 3 4

0% 0%0%0%

1. Better than today2. About the same3. Somewhat worse4. Catastrophically worse

Page 89: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Duncan’s View

A keen question is posed: "Why are you confident about the Olduvai theory?" - My response: "Because Mother Nature then solves for us

the (apparently) insuperable problem of the Tragedy of the Unmanaged Commons, which the human race seems either incapable or unwilling to solve for itself.”

- Governments have lost respect. World organizations are ineffective. Neo- tribalism is rampant. The population is over six billion and counting. Global warming and emerging diseases are headlines. The reliability of electric power networks is falling. And the instant the power goes out, you are back in the Dark Age. If God made the Earth for human habitation, then He made it for the Stone Age mode of habitation.

- The Olduvai theory is thinkable.

Page 90: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

The earth's immune system, so to speak, has recognized the presence of the human species and is starting to kick in. The earth is attempting to rid itself of an infection by the human parasite. — Richard Preston, 1994

Page 91: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Natural Gas

Since the late 1990s, natural gas has been the fuel of choice for the majority of new generating units, resulting in a 99.0 percent increase in natural gas-fired capacity since 1999.

The construction of natural gas plants began increasing in 1999, peaked during 2002 and 2003, but has since declined considerably.

On December 31, 2006, natural gas-fired generating capacity represented 388,294 MW or 39.4 percent of total net summer generating capacity. Although new natural gas-fired combined-cycle plants produce electricity more efficiently than older fossil-fueled plants, high natural gas prices can work against full utilization of these plants if such prices adversely affect economic dispatch

Page 92: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Natural Gas proven reserves

1. Russia 25%2. Iran 16%3. Qatar 14%4. Saudi Arabia 4%5. US 3%6. United Arab Emirates 3%7. Venezuela 3%8. Algeria 2%

World Reserves/Production Ratio - 60 years

Page 93: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

An alternative transportation fuel

Metro: 164 CNG buses (out of 1600)

Honda Civic GX - on sale in CA, NY

Page 94: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Energy usage will continue to increase

Page 95: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Growth in developing countries

Page 96: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Fossil Fuel consumption will increase

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Physics 105 – Fall 2011

China will burn a lot of coal

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Physics 105 – Fall 2011

It will depend (somewhat) on the global economy

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Physics 105 – Fall 2011

Depends on prices

Page 100: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Natural Gas

Page 101: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

International organization of 30 countries that accept the principles of representative democracy and free-market economy. Most OECD members are high-income economies

Page 102

Page 102: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Physics 105 – Fall 2011

Coal

Page 103: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

• Fossil fuels: petroleum, natural gas and coal (organic)• Relatively short-lived, ~ 500 years• Currently 85% of current US energy from from fossil fuels • Expected oil production peak: 2010-2030• Consumption currently increasing• Projected world oil production will be exhausted by 2100• Produces significant and diverse pollution problems

o Greenhouse gasseso Gaseous Sulfur and nitrogen oxideso Land-based disturbances

The Era of Fossil Fuels

Page 104: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Total energy consumption for the United States, 1950-1999.

Page 105: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

© 2003 John Wiley and Sons Publishers

Proven world oil reserves in 1998.

Page 106: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

© 2003 John Wiley and Sons Publishers

Major trade routes for the world’s oil, emphasizing the countries that use Middle Eastern oil.

Page 107: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

© 2003 John Wiley and Sons Publishers

Estimating cost of driving with increased fuel economy.

Page 108: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

© 2003 John Wiley and Sons Publishers

Taxes for 1 gal of gasoline in U.S. dollars equivalent for selected countries, 1995.

Page 109: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Sources: International Energy Annual 2005 and BP Statistical Review

2006 World Conventional Hydrocarbon Resources

2

Total World Resources19,960 Quadrillion Btu

6,970 Quadrillion Btu6,500 Quadrillion Btu

CoalOil

Natural Gas

Page 110: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Source: International Energy Annual 2005

Total World Production: 417 quadrillion Btu

2006 World Conventional Hydrocarbon Production

3

Page 111: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

2006 World Conventional Hydrocarbon Consumption

Source: International Energy Annual 2005

4

World Consumption All Energy:Consumption Conventional Hydrocarbons:

465 quadrillion Btu417 quadrillion Btu

Page 112: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

2006 Coal Trade Patterns

Source: International Energy Agency, Coal Information 2007

5

World Coal Exports: 815 mmt

Page 113: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Potential Demand for Electrification

(2005 kwh per capita)

Source: International Energy Agency, Key World Energy Statistics 2007

6

Page 114: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Source: World Resource Institute (http://earthtrends.wri.org/text/energy-resources/variables.html)

Potential Demand for Liquid Fuel(cars per 1,000 people)

7

Page 115: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Key Assumptions: EIA’s International Energy ForecastPotential impacts of proposed legislation or standards

are not reflected in the projectionsPotential impacts of legislation for which implementing mechanisms are not set also are not reflected in the projections

Projections come from an integrated set of 16 regional models that reflect each region’s existing energy use patterns, energy infrastructure, and costs for existing and alternative energy technologies

For further details see: http://www.eia.doe.gov/oiaf/ieo/pdf/0484(2007).pdf

8

Page 116: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Annual Growth in Electricity Generation by Region (2004-2030)

Non-OECD

OECD – Organization for Economic Co-operation and Development

Source: EIA, International Energy Outlook 2007

9

Page 117: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Non-OECD

OECD

Annual Growth in Liquids Consumption by Region (2004-2030)

Source: EIA, International Energy Outlook 2007

10

0.0

1.9

2.3

2.2

Page 118: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

World Energy Use by Fuel Type (1980 – 2030)

Source: EIA, International Energy Outlook 2007

0

50

100

150

200

250

300

1980 1990 2000 2010 2020 2030

Qu

adri

llio

n B

tu

Oil Natural Gas Coal Nuclear Renewables

11

Page 119: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

World Coal Consumption by Region (2004 – 2030)

Source: EIA, International Energy Outlook 2007

0

50

100

150

200

250

2004 2010 2015 2020 2025 2030

Qu

ad

rilli

on

Btu

China United States India Rest of World

12

114.5

136.4151.6

167.2182.9

199.1

Page 120: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

20

2

2224

2

26

31

2 2

35

0

5

10

15

20

25

30

35

40

Electricity Industrial Coal-to-Liquids Total

Qu

ad

rill

ion

Btu

2004 2015 2030

U.S. Coal Consumption by Sector (2004, 2015, 2030)

Source: EIA, Annual Energy Outlook 2007

13

Page 121: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

2316

3

4139

23

3

65

56

37

3

95

0

10

20

30

40

50

60

70

80

90

100

Electricity Industrial Other Sectors Total

Qu

adri

llio

n B

tu

2004 2015 2030

Chinese Coal Consumption by Sector (2004, 2015, 2030)

Source: EIA, International Energy Outlook 2007

14

Page 122: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Carbon Dioxide Emissions from Coal Use by Region (2004, 2030)

Source: EIA, International Energy Outlook 2007

15

Page 123: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

0

10,000

20,000

30,000

40,000

50,000

1990 2000 2010 2020 2030

Millio

n M

etr

ic T

on

s C

arb

on

Dio

xid

e

Carbon Dioxide Emissions by Region

Source: EIA, International Energy Outlook 2007

World

U.S., China & India

Europe & Eurasia

Japan, South Korea, Australia, New Zealand, & Other Asia

Middle East

16

Africa

Central & SouthAmerica

Page 124: Physics 105 Physics for Decision Makers: The Global Energy Crisis Lecture 12 - Fossil Fuels Fall 2011.

Future Challenges and Options

85% of that increase is in the U.S., China, India, & other Asia

U.S., China and India account for 86% of the increase in global coal use

Global CO2 emissions increase by 60%

90% of the increase in CO2 emissions occurs in the U.S., China, India, & other Asia

Coal accounts for 49% of global CO2 emission growth

Oil accounts for 29%Natural Gas accounts for

21%

Source: EIA, International Energy Outlook 2007

World Primary Energy Consumption over Next 25

Years Without Carbon Constraining Technology

17

World primary energy consumptionIncreases 57%