resources as level. the greenhouse effect - global warming

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Page 1: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

RESOURCESRESOURCES

AS Level

Page 2: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE GREENHOUSE EFFECT - THE GREENHOUSE EFFECT - GLOBAL WARMINGGLOBAL WARMING

Page 3: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

LEARNING OUTCOMESLEARNING OUTCOMES

• Explain that infrared radiation is absorbed by C=O, O–H and C–H bonds in CO2, H2O and CH4, and this contributes to global warming.

• Explain that the greenhouse effect of a given gas is dependent both on its atmospheric concentration and its ability to absorb infrared radiation.

Page 4: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE GREENHOUSE EFFECT DEFINITIONTHE GREENHOUSE EFFECT DEFINITION

The greenhouse effect is the process in which the absorption and subsequent emission of infrared radiation by atmospheric gases warms the lower atmosphere and the planet’s surface.

Page 5: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

What has this got to do with chemistry???

Page 6: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE GREENHOUSE EFFECTTHE GREENHOUSE EFFECT

energy from the sun is in the ultra violet, visible and infra red regions

Page 7: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE GREENHOUSE EFFECTTHE GREENHOUSE EFFECT

energy from the sun is in the ultra violet, visible and infra red regions

47% reaches the earth

Page 8: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE GREENHOUSE EFFECTTHE GREENHOUSE EFFECT

energy from the sun is in the ultra violet, visible and infra red regions

radiation re-emitted from the earth is in the infra red region

47% reaches the earth

Page 9: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE GREENHOUSE EFFECTTHE GREENHOUSE EFFECT

energy from the sun is in the ultra violet, visible and infra red regions

radiation re-emitted from the earth is in the infra red region

70% of the radiation returns to space

47% reaches the earth

Page 10: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE GREENHOUSE EFFECTTHE GREENHOUSE EFFECT

energy from the sun is in the ultra violet, visible and infra red regions

radiation re-emitted from the earth is in the infra red region

70% of the radiation returns to space

47% reaches the earth

greenhouse gasesabsorb the remainder

Page 11: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE GREENHOUSE EFFECTTHE GREENHOUSE EFFECT

energy from the sun is in the ultra violet, visible and infra red regions

radiation re-emitted from the earth is in the infra red region

70% of the radiation returns to space

47% reaches the earth

greenhouse gasesabsorb the remainder

energy is returned to earth to keep it warm

Page 12: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

Carbon dioxide and

water molecules will

vibrate as energy is absorbed

Page 13: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

GREENHOUSE GASESGREENHOUSE GASES

Different covalent bonds have different strengths due to the masses of different atoms at either end of the bond. As a result, they vibrate at different frequencies (imagine two balls on either end of a spring) . The frequency of vibration can be found by detecting when the molecules absorb electro-magnetic radiation.

Page 14: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

GREENHOUSE GASESGREENHOUSE GASES

Different covalent bonds have different strengths due to the masses of different atoms at either end of the bond. As a result, they vibrate at different frequencies (imagine two balls on either end of a spring) . The frequency of vibration can be found by detecting when the molecules absorb electro-magnetic radiation.

Various types of vibration are possible. Bending and stretching are two examples and are found in water molecules. Each occurs at a different frequency.

Page 15: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

GREENHOUSE GASESGREENHOUSE GASES

Different covalent bonds have different strengths due to the masses of different atoms at either end of the bond. As a result, they vibrate at different frequencies (imagine two balls on either end of a spring) . The frequency of vibration can be found by detecting when the molecules absorb electro-magnetic radiation.

Various types of vibration are possible. Bending and stretching are two examples and are found in water molecules. Each occurs at a different frequency.

Symmetric Bending Asymmetricstretching stretching

Page 16: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

GREENHOUSE GASESGREENHOUSE GASES

Different covalent bonds have different strengths due to the masses of different atoms at either end of the bond. As a result, they vibrate at different frequencies (imagine two balls on either end of a spring) . The frequency of vibration can be found by detecting when the molecules absorb electro-magnetic radiation.

Various types of vibration are possible. Carbon dioxide also undergoes bending and stretching.

Bending in a carbon dioxide molecule

Page 17: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

DETECTING GREENHOUSE GASESDETECTING GREENHOUSE GASES

The frequencies lie in the INFRA REDINFRA RED part of the electromagnetic spectrum and can be detected using infra red spectroscopy.

An infra red spectrum of atmospheric air

.

H2O

H2OCO2

CO2

Page 18: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

1. The Earth receives most of its energy in the form of electromagnetic radiation from the Sun. (Most from visible, some from UV and IR regions).

2. The incoming radiation is relatively unaffected by the gases in the Earth’s atmosphere.

3. Most IR radiation goes back into space, however certain gases absorb this radiation, some is re-emitted back towards the Earth.

4. This traps the heat in the lower atmosphere.

THE GREENHOUSE EFFECT SUMMARYTHE GREENHOUSE EFFECT SUMMARY

Page 19: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

The greenhouse effect isn’t all bad

Without greenhouse gases our planet would be covered in ice with an average temperature 35oC less than present.

Page 20: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

The temperature of our planet has more to do with the greenhouse effect than with our proximity to the sun!

Page 21: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE GREENHOUSE THE GREENHOUSE EFFECTEFFECT

The greenhouse effect creates an equilibrium.

The atmospheric gases absorb energy at the same rate it radiates it, thus maintaining a steady temperature.

Page 22: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

GREENHOUSE GASESGREENHOUSE GASES

CARBON DIOXIDE CO2 contains C = O bonds

WATER VAPOUR H2O contains O - H bonds

METHANE CH4 contains C - H bonds

The ‘Greenhouse Effect’ of a given gas is dependent on its...

• atmospheric concentration

• ability to absorb infrared radiation

Page 23: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE THREE MAIN GREENHOUSE GASESTHE THREE MAIN GREENHOUSE GASES

Water vapour – from evaporation of lakes and oceans. Most abundant.

Carbon dioxide – produced by volcanic eruptions, respiration of animals and burning of organic matter (plants).

Methane – emitted during the production of fossil fuels, rotting waste in landfill sites and released from certain animals (cows). Least amount but greatest contributor.

Page 24: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

Clathrates – contain 3000x as much methane as found in the atmosphere, if released this would have a huge effect on greenhouse gases.

There is some speculation that release

of these methane bubbles have added to

global warming, but there is no concrete proof.

Page 25: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

SO WHAT’S THE PROBLEM?SO WHAT’S THE PROBLEM?

The greenhouse effect is a natural process, keeping our planet at a temperature capable of supporting life.

The problem: Human activity is producing more greenhouse gases, which threaten to upset this fine natural balance, resulting in global warming.

Page 26: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

An increase in the concentration of greenhouse gases leads to climate change / global warming.

What do you think?

Page 27: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

GLOBAL WARMING POTENTIAL GLOBAL WARMING POTENTIAL (GWP)(GWP)

• The ability of a trace gas to cause global warming is described by its GWP.

• GWP is related to the lifetime of a gas in the atmosphere as well as the ability of a gas to absorb IR radiation.

• Since banning use of CFC’s their effect is diminishing.

Page 28: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

QUESTIONSQUESTIONS

1. Name the three greenhouse gases

2. Outline the molecular processes that enable heat to be kept close to the Earth.

3. What factors contribute to a gas’s contribution to global warming?

Page 29: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

CLIMATE CLIMATE CHANGECHANGE

Page 30: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

Learning objectivesLearning objectives

• Explain the importance of controlling global warming caused by atmospheric increases in greenhouse gases.

• Outline the role played by chemists through the provision of scientific evidence that global warming is taking place.

• Understand the role of chemists in monitoring progress of initiatives such a Kyoto protocol.

Page 31: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

WHAT IS CLIMATE CHANGE?WHAT IS CLIMATE CHANGE?

• An increase in the concentration of greenhouse gases

leads to climate change / global warming.

• Global warming is defined as ‘an increase in the average temperature of the Earth’s atmosphere, especially a sustained increase big enough to cause climate change’

• What does this mean?

•The temperature goes up (warmer summers, mild winters)•Plants and crops may not be able to grow in the same places•Extreme storms, hurricanes and floods may become more common•Sea levels may rise causing flooding

Page 32: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

HOW DO WE FIND OUT IF GLOBAL WARMING IS HAPPENING?

We need to record the temperature and the weather at lots of places across the Earth.

After many years, we can see a pattern in the data.

Scientists try to decide what the pattern means.

Page 33: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

GLOBAL WARMING CAN BE SEEN IN:

• In the Arctic, ice and permafrost disappearing• In the Antarctic, ice sheets melting into the oceans• Tropical areas experiencing more frequent and

destructive storms and floods• In Europe, glaciers are disappearing and there

have been extreme heat waves.

Page 34: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

REDUCING GREENHOUSE EMISSIONS

• Earth Summit in 1992 – international agreement that climate change must be prevented, but there was little action.

• Kyoto Protocol – 0ver 100 countries. Countries must reduce emissions of six greenhouse gases by 5% by 2012.

• USA – biggest emitter (25% of global emissions) – refused to sign.

• Carbon emissions need to be reduced by 70-80%,

Page 35: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

INTERNATIONAL CO-OPERATIONINTERNATIONAL CO-OPERATION

KYOTO PROTOCOL (1997)KYOTO PROTOCOL (1997)

Page 36: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

INTERNATIONAL CO-OPERATIONINTERNATIONAL CO-OPERATION

KYOTO PROTOCOL (1997)KYOTO PROTOCOL (1997)• over 50 developed countries pledged to cut greenhouse gas emissions• gases included carbon dioxide CO2

methane CH4

hydrofluorocarbons HFC’sperfluorocarbons PFC’ssulphur hexafluoride SF6

• some countries agreed to make larger cuts• developing countries were not required to cut emissions• the US didn’t sign up; it would have significantly affected their economy

Page 37: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

INTERNATIONAL CO-OPERATIONINTERNATIONAL CO-OPERATION

KYOTO PROTOCOL (1997)KYOTO PROTOCOL (1997)• over 50 developed countries pledged to cut greenhouse gas emissions• gases included carbon dioxide CO2

methane CH4

hydrofluorocarbons HFC’sperfluorocarbons PFC’ssulphur hexafluoride SF6

• some countries agreed to make larger cuts• developing countries were not required to cut emissions• the US didn’t sign up; it would have significantly affected their economy

But... Many experts say that the protocol is futile without US support as they are the world’s largest emitter of greenhouse gases.

Countries such as India and China are going through greatindustrial change and they do not have to cut emissions.

Cuts weren’t big enough according to many scientists, who say that a 60% cut is required to avoid the risks of global warming.

Page 38: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

EU STRATEGYEU STRATEGY

In 2007 the EU agreed a strategy to fight against global warming.

The deal set the following targets to be reached by 2020:

1. 20% of energy used in the EU will come from renewable sources.

2. 10% of transport fuels will come from biofuels.3. EU greenhouse emissions will be reduced to

20% below 1990 levels.

Page 39: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

THE GREENHOUSE EFFECTTHE GREENHOUSE EFFECT

What can chemists do to minimise climate change from global warming?

• provide scientific evidence to governments to confirm it is taking place

• monitor progress against initiatives such as the Kyoto protocol

• investigate solutions to environmental problems

Page 40: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

GOVERNMENTS LISTEN TO SCIENTISTS

• Politicians are now slowly believing what scientists have been saying for years “Human activity is contributing to global warming”.

• Politicians are now looking for measures to reduce carbon emissions.

• Kyoto Protocol and EU initiatives prove governments are listening.

Page 41: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

QUESTIONSQUESTIONS

1. List three consequences of global warming for the Earth.

2. Petrol contains a mixture of hydrocarbons, including isomers of C8H18.

a) Write a balanced equation for the complete combustion of C8H18 (assume petrol contains just this).

b) Calculate the reduction in CO2 emission from a car per km in 2012 (130g CO2 per km) compared with 2005 (162g CO2 per km) by volume.

Page 42: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING
Page 43: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

LEARNING OUTCOMESLEARNING OUTCOMES

• Outline how chemists investigate solutions to environmental problems, such as carbon capture and storage (CCS).

• Understand the removal of waste carbon dioxide as a liquid injected deep in the oceans.

• Outline carbon storage in deep geological formations, by reaction with metal oxides to form stable carbonate minerals.

Page 44: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

CAPTURE AND STORAGE OF COCAPTURE AND STORAGE OF CO22

BENEATH THE NORTH SEABENEATH THE NORTH SEA

Page 45: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

CCARBON DOXIDE ARBON DOXIDE CCAPTURE & APTURE & SSTORAGETORAGE

Page 46: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

CCARBON DOXIDE ARBON DOXIDE CCAPTURE & APTURE & SSTORAGETORAGE

What is it?

• CO2 is collected from industrial processes and power generation

• it is separated and purified

• it is then transported to a suitable long-term storage site

Page 47: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

CCARBON DOXIDE ARBON DOXIDE CCAPTURE & APTURE & SSTORAGETORAGE

What is it?

• CO2 is collected from industrial processes and power generation

• it is separated and purified

• it is then transported to a suitable long-term storage site

Storage possibilities

• gaseous storage in deep geological formations

• liquid storage in the ocean

• solid storage by reaction as stable carbonates

Page 48: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

CCARBON DOXIDE ARBON DOXIDE CCAPTURE & APTURE & SSTORAGETORAGE

What is it?

• CO2 is collected from industrial processes and power generation

• it is separated and purified

• it is then transported to a suitable long-term storage site

Storage possibilities

• gaseous storage in deep geological formations

• liquid storage in the ocean

• solid storage by reaction as stable carbonates

How can it help?

• could reduce CO2 emissions from power stations by 80%

• could be used to store CO2 emitted from fermentation processes

Page 49: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

STORAGE AS CARBONATESSTORAGE AS CARBONATES

Mineral storage aims to store carbon in stable minerals. That is to react CO2 with metal oxides to produce stable carbonates. This is how limestone rock has been produced.

For example: CaO + CO2 CaCO3

MgO + CO2 MgCO3

The process is very slow and much energy is needed to increase the rate of reaction.

More research is needed if mineral storage is to become a viable form of CSS.

Page 50: RESOURCES AS Level. THE GREENHOUSE EFFECT - GLOBAL WARMING

What is mineral storage and what are the current problems with its attempted use?