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Energy, power and climate change
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Energy, power and climate change

Jan 16, 2015

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Nothingnerdy

Presentation to accompany IB EPCC unit
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Page 1: Energy, power and climate change

Energy, power and climate change

Page 2: Energy, power and climate change

8.1 Energy degradation and power generation

1. Hot gas will cause the piston to move

2.But one stroke of the piston does not provide

much energy

3.The process needs to be cyclical

Page 3: Energy, power and climate change

Cyclical processes

The continuous production of energy can be obtained from a cyclical process

Not all of the heat can be converted to

work

Some is transferred to the surroundings

Page 4: Energy, power and climate change

Efficiency of heat engines

No heat engine can transfer all of it’s energy to work.

Some is always lost as heat to the surroundings.

Equation is not on the syllabus

Page 5: Energy, power and climate change

Sankey diagrams

You must be able to construct and analyse Sankey diagrams to show where energy is degraded.

100% 25%

Page 6: Energy, power and climate change

energy efficiency of a filament lamp

Page 7: Energy, power and climate change

Production of electrical power

1. Heat source

2. Steam generation

3. Turbines

4. Generator

5. Transmission lines

Page 8: Energy, power and climate change

The Generator

Hyperlink

Electrical energy is produced by the coils rotating in a magnetic field.

Page 9: Energy, power and climate change

8.2 World energy sources

Which energy resources produce CO2?

Which are renewable?

Which resources come from the sun?

What are the advantages and disadvantages of the types of energy sources? (Location, cost, pollution, energy density, continuity, availability….)

Define the energy density of a fuel

Energy density is measured in J kg–1.

Page 10: Energy, power and climate change

World use of energy sources91% Non-renewable

Only approximate values are needed

Page 11: Energy, power and climate change

Energy density of fuels

• Energy in GJ/tonne

• Uranium metal (U) 560,000

• Crude Oil 44.9

• Black Coal 29.0

• Wood 16.2

• Gas 54

Page 13: Energy, power and climate change

CO2 emissions

• Emission indices (Kg CO2/GJ)

• LPG 60Natural Gas 58 Crude Oil 76Coal (electricity) 290

Page 14: Energy, power and climate change

8.3 Fossil fuel power productionOutline the historical and geographical reasons for thewidespread use of fossil fuels

Students should appreciate that industrializationled to a higher rate of energy usage, leading toindustry being developed near to large deposits of fossil fuels.

Page 15: Energy, power and climate change

Amount of fuel for power production

Discuss the energy density of fossil

fuels with respect to the demands of

power stations.

Students should be able to estimate the rate of fuel consumption by power stations.

Page 16: Energy, power and climate change

Rate of coal use in a power station

• 1000 MW output of electricity

• Coal power stations are 40% efficient

• Coal has 29MJ/Kg

• Calculate the rate of use of coal

• (Approx 300 tonnes/hr)

Page 17: Energy, power and climate change

Discuss the relative advantages and disadvantages associated with the transportation and storage of fossilfuels.

Page 18: Energy, power and climate change

State the overall efficiency of powerstations fuelled by different fossil

fuels.

• Coal 35 – 42%

• Natural Gas 45 – 52%

• Oil 38 – 45%

Page 20: Energy, power and climate change

8.4 Non-fossil fuel power production

Describe how neutrons producedin a fission reaction may be used toinitiate further fission reactions (chainreaction).Students should know that only low-energyneutrons (≈ 1 eV) favour nuclear fission.

They shouldalso know about critical mass.

Page 21: Energy, power and climate change

Chain reactions

Each fission reaction releases neutrons that are used in further reactions.

Fast neutronsNeed to be

slowed down

Critical mass?

Page 23: Energy, power and climate change

Describe what is meant by fuelenrichment.

Natural U-235 occurs as 0.7% abundance. (3300C)

Enriched fuel contains 2.3% U-235, therefore increases the temperature (6000C)of the core of the reactor, therefore increases the efficiency and power output/Kg

Page 24: Energy, power and climate change

Describe the main energytransformations that take place in a

nuclear power station.

EK of fission

fragments

Page 25: Energy, power and climate change

Nuclear power station

Page 26: Energy, power and climate change

Discuss the role of the moderator and the control rods in the production of controlled fission in a thermal fissionreactor.

graphite moderator

boron control rod

heat exchangerfuel element channel

steel

concrete

hot gas

reactor core

cold gas

charge face

The moderator slows the neutrons down to enable them to allow fissions

The control rods absorb neutrons to control the power level

The heat exchanger isolates the water from the coolant and lets the hot gas boil the water.

What are the energy transformations?

Page 27: Energy, power and climate change

Energy transformations in a reactor

• Fission fragments have EK

• This heats the fuel rod• The coolant (gas) takes the heat from the

rod• The hot gas goes to the heat exchanger• The hot gas turns the water to steam• The steam drives the turbines• The turbines drive the generator

Page 28: Energy, power and climate change

Production of plutonium• Fissionable plutonium-239 can be

produced from non-fissionable uranium-238 by the reaction illustrated.

The bombardment of uranium-238 with neutrons triggers two successive beta decays with the production of plutonium.

Page 29: Energy, power and climate change

Fast breeder reactors• The U-238 is

converted to Pu-239• The Pu-239 is

fissionable by fast neutrons

• Therefore, the reactor can breed its’ own fuel

• Doesn’t need a moderator (saves space)

• Very high operating temperature, cooled by liquid sodium

Page 30: Energy, power and climate change

Risks of nuclear power• Meltdown – This is when the power goes out of control and

the reactor blows up. This may happen if the coolant is “interrupted”, or the control rods are removed.

• The waste produced is radioactive, as is hazardous to living things. It is expensive to store. The half life of some products is very long

• Uranium mining - Because uranium ore emits radon gas, uranium mining can be more dangerous than other underground mining

• The plutonium produced can be used for weapons manufacture

Page 31: Energy, power and climate change

Nuclear fusion• The plasma needs to be at a temperature of

about 108K (this takes a lot of energy).• This cannot come into contact with anything• Can be contained by a magnetic field.

Page 32: Energy, power and climate change

Solar power

1. photovoltaic cell

There are 2 types of solar power

In a sunny climate, you can get enough power to run a 100W light bulb from just one square metre of solar panel. Good for remote situations e.g. a yacht.

2. Solar water heating The Sun is used to heat water in glass panels on the roof

This means you don't need to use so much gas or electricity to heat your water at home.

Page 33: Energy, power and climate change

Solar PV cells

• Advantages • Solar energy is renewable and the Sun’s heat and light are free • Solar energy can be used to generate electricity in remote places

where other electricity supplies are hard to come by • It does not produce any carbon dioxide, which contributes to the

greenhouse effect • Energy is usually generated at or near to the location it will be used.

This keeps transmission and distribution costs to an absolute minimum

• Disadvantages• PV cells do not work so well when it is cloudy and do not work at

night • They only work in a very sunny country! Solar power works better in

hot places, so its use is therefore limited

Page 34: Energy, power and climate change

Solar constant • The solar constant is the amount of

incoming solar electromagnetic radiation per unit area.

• It is measured by satellite to be roughly 1.4 kWm-².

• This value must be reduced if …..• You are not at the Equator• It is not mid summer• PV cells are about 10% efficient.

Page 35: Energy, power and climate change

Hydroelectric power Hyperlink

water storage in lakes

Advantages   •Once the dam is built, the energy is virtually free. •No waste or pollution produced.•Much more reliable than wind, solar or wave power. •Water can be stored above the dam ready to cope with peaks in demand.•Hydro-electric power stations can increase to full power very quickly, unlike other power stations. •Electricity can be generated constantly•Disadvantages

•The dams are very expensive to build.However, many dams are also used for flood control or irrigation, so building costs can be shared. •Building a large dam will flood a very large area upstream, causing problems for animals that used to live there.•Finding a suitable site can be difficult - the impact on residents and the environment may be unacceptable. •Water quality and quantity downstream can be affected, which can have an impact on plant life.

Page 36: Energy, power and climate change

Tidal water storageHyperlink

•Tidal Power is renewable•Doesn't cause pollution, doesn't need fuel•A tidal barrage is very expensive to build•Only works when tide is going in or out •A tidal barrage affects a large area•There are very few places that you could sensibly build a Tidal barrage •Underwater turbines may be a better bet than a barrage - they are cheaper and don't have the huge environmental impact

Page 37: Energy, power and climate change

Pump storage

•It's a way of storing energy for when you need it in a hurry.•The biggest one is at Dinorwig, in Wales•Expensive to build•Most power stations take a long time to turn up to full power. Pumped Storage reservoirs mean that we can quickly get more energy for half an hour or so, to keep us going until the other power stations catch up

Dinorwig has the fastest "response time" of any pumped storage plant in the world - it can provide 1320 Mega Watts in 12 seconds. That's a lot of cups of tea!

Buy when cheap

Sell when expensiveGPE

KE Electric

Page 38: Energy, power and climate change

Question

• How much water must fall per second to produce 1,400 MW of electricity, if it falls through a height of 200m? Assume the turbine is 60% efficient.

Page 39: Energy, power and climate change

Wind powerThe wind blows the propeller round, which turns a generator to produce electricity

•Wind Power is renewable•Doesn't cause pollution, doesn't need fuel•Need a lot of generators to get a sensible amount of power•Need to put them where winds are reliable

Energy = ½ mv2

Mass per sec = ρx volume = ρx Area x speed = ρπr2v

Energy = ½ ρπr2v x v2 = ½ ρπr2v3

The wind does not stop after passing through the turbine, therefore not all the energy can be harnessed (max = 59%)

Page 40: Energy, power and climate change

Questions

• A wind generator is designed to work in winds of 10km/hr with a blade length of 3m. How much power can it produce?

• What would be the power output at 20km/hr?

• What would be the power output if the blade length were increased to 6m?

• ρair = 1.3Kgm-3

Page 41: Energy, power and climate change

Wave power (OWC)Hyperlink

Advantages   •The energy is free - no fuel needed, no waste produced. •Not expensive to operate and maintain. •Can produce a great deal of energy. Disadvantages •Depends on the waves - sometimes you'll get loads of energy, sometimes almost nothing. •Needs a suitable site, where waves are consistently strong. •Some designs are noisy. But then again, so are waves, so any noise is unlikely to be a problem.•Must be able to withstand very rough weather

Page 42: Energy, power and climate change

Waves

a

λ

L

Volume of water in red area = a x λ/2 x L Mass = Volume x density(ρ)

Loss of GPE of the wave = mgh = (a x λ/2 x L x ρ) x g x a

Number of waves per sec = Frequency = v/λ

Power = loss of GPE per sec = a2 x λ/2 x L x ρ x g x v/λ

Power per unit length = ½ a2ρgv

Page 43: Energy, power and climate change

OWC question

• Waves of amplitude 2m reach the beach every 15 seconds. The wavelength of the wave is 80m. Calculate

• The speed of the wave.

• The power per metre of the waves along the shore.

• The power available from a 3km beach.

Page 44: Energy, power and climate change

8.5 Greenhouse effectHyperlink

Short λ

not absorbed

Long λ

absorbed

Page 45: Energy, power and climate change

Solar constant

• The sun radiates 3.9x1026W

• The Earth is a distance of 1.5x1011m from the sun

• Calculate the power per m2 reaching the Earth.

Page 46: Energy, power and climate change

When the energy reaches the Earth, what happens to it?

Page 47: Energy, power and climate change

Albedo

the fraction of the incident sunlight that is reflected

Page 48: Energy, power and climate change

Variations in albedoSample albedos

Surface TypicalAlbedo

Fresh asphalt 0.04

Conifer forest(Summer)

0.08,0.09 to 0.15

Worn asphalt 0.12

Deciduous trees 0.15 to 0.18

Bare soil 0.17

Green grass 0.25

Desert sand 0.40

New concrete 0.55

Fresh snow 0.80–0.90

The albedo also varies with factors like season, latitude and cloud cover

The average value on Earth is 0.3

Page 49: Energy, power and climate change

Why does the reflected radiation not escape into space?

Page 50: Energy, power and climate change

Greenhouse gases

Page 51: Energy, power and climate change

Absorption of IR radiation

Carbon dioxide, water vapour , methane , nitrous oxide , and a few other gases are greenhouse gases. They all are molecules composed of more than two component atoms, bound loosely enough together to be able to

vibrate with the absorption of heat. The major components of the atmosphere N2 and O2 are two-atom molecules too tightly bound together to

vibrate and thus they do not absorb heat and do not contribute to the greenhouse effect.

The resonant frequency of greenhouse gases is in

the IR region

Page 52: Energy, power and climate change

Microwave simulation

Hyperlink

Page 53: Energy, power and climate change

Start of IR region 0.7 nm

Page 54: Energy, power and climate change
Page 55: Energy, power and climate change

Sources of greenhouse gases

• Burning of fossil fuels and deforestation leading to higher carbon dioxide concentrations

• Livestock CO2 and CH4

• Fertilisers N2O• CFC’s in refrigeration and fire extinguishers• When these gases are ranked by their contribution to the

greenhouse effect, the most important are:• water vapour, which contributes 36–70% • carbon dioxide, which contributes 9–26% • methane, which contributes 4–9% • ozone, which contributes 3–7%

Page 56: Energy, power and climate change

How much heat does the Earth radiate?

Page 57: Energy, power and climate change

The nature of black-bodyradiation.

λmax x T = Wien’s constantMicrosoft Equation 3.0

Page 58: Energy, power and climate change

Stefan–Boltzmann law

P = Power output

σ = Stefan–Boltzmann constant

A = Surface area of emitting body

T = Temperature of the emitter

Page 59: Energy, power and climate change

Black body simulation

Page 60: Energy, power and climate change

Emissivity

• The Earth is not a perfect Black Body radiator

• The emissivity is defined as

tempsameatbodyblackfromPower

objectbyradiatedpower

Therefore the Earth is not a perfect absorber or emitter of heat. Black objects have a high emissivity, white low.

Page 61: Energy, power and climate change

Values of emissivityAluminium: anodised 0.77

Aluminium: polished 0.05

Asbestos: board 0.96

Asbestos: fabric 0.78

Asbestos: paper 0.93

Asbestos: slate 0.96

Brass: highly polished 0.03

Brass: oxidized 0.61

Brick: common .81-.86

Brick: common, red 0.93

Brick: facing, red 0.92

Brick: fireclay 0.75

Brick: masonry 0.94

Brick: red 0.90

Carbon: candle soot 0.95

Carbon: graphite, filed surface 0.98

Page 62: Energy, power and climate change

What is the effect of the absorbed radiation on the temperature of the Earth?

Page 63: Energy, power and climate change

Surface Heat capacity Cs

Surface heat capacity is the energy required to raise the temperature of unit area of a planet’s surface by one degree, and is measured in

J m–2 K–1.

Page 64: Energy, power and climate change

Climate change modelStudents should appreciate that the change of aplanet’s temperature over a period of time is givenby:(incoming radiation intensity – outgoing radiation intensity) × time / surface heat capacity.

Page 65: Energy, power and climate change

Download

Greenhouse simulation

Page 66: Energy, power and climate change

Predictions

Page 67: Energy, power and climate change

Met office prediction

Page 68: Energy, power and climate change

Describe some possible models ofglobal warming.

Students must be aware that a range of models

has been suggested to explain global warming,

including changes in the composition of

greenhouse gases in the atmosphere, increased

solar flare activity, cyclical changes in the Earth’s

orbit and volcanic activity.

Page 69: Energy, power and climate change

State what is meant by the enhancedgreenhouse effect.

It is sufficient for students to be aware that

enhancement of the greenhouse effect is caused by human activities.

Page 70: Energy, power and climate change

Identify the increased combustion offossil fuels as the likely major cause of

the enhanced greenhouse effect

Students should be aware that, although debatable, the generally accepted view of most scientists is that human activities, mainly related to burning of fossil fuels, have released extra carbon dioxide into the atmosphere.

Page 71: Energy, power and climate change

Describe the evidence that linksglobal warming to increased levels of

greenhouse gases.

• For example, international ice core research produces evidence of atmospheric composition and mean global temperatures over thousands

of years (ice cores up to 420,000 years have been drilled in the Russian Antarctic base, Vostok).

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Evidence of Global warming

Page 77: Energy, power and climate change

The concentration of carbon dioxide measured at Mauna Loa

Observatory in Hawaii

Cyclical change?

Page 78: Energy, power and climate change

Outline some of the mechanismsthat may increase the rate of global

warming.Students should know that:

• global warming reduces ice/snow cover, which

in turn changes the albedo, to increase rate of

heat absorption

• temperature increase reduces the solubility

of CO2 in the sea and increases atmospheric

concentrations

• deforestation reduces carbon fixation.

Page 79: Energy, power and climate change

Define coefficient of volume expansion

Students should know that the coefficient of

volume expansion is the fractional change in

volume per degree change in temperature.

State that one possible effect of theenhanced greenhouse effect is a rise

in mean sea-level.

Page 80: Energy, power and climate change

Outline possible reasons for apredicted rise in mean sea-level.

Students should be aware that precise predictions are difficult to make due to factors such as:

• anomalous expansion of water

• different effects of ice melting on sea water

compared to ice melting on land.

Page 81: Energy, power and climate change

Identify climate change asan outcome of the enhancedgreenhouse effect.

i.e. man made