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Outline: Lecture 6. Global Energy Dynamics Human Energy Transformation Global Energy Flow Climate Change The Future?. Sources of Human Energy Resources Where do we get energy for: Heating and Cooling Lighting Transportation Industrial Processing Electricity.
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Outline: Lecture 6 Global Energy Dynamics Human Energy Transformation Global Energy Flow Climate Change The Future?
Sources of Human Energy Resources Where do we get energy for: Heating and Cooling Lighting Transportation Industrial Processing Electricity
Electricity Generation Majority of electricity in USA produced using fossil fuel resources
Sources of Human Energy Resources Fossil Fuels: coal, petroleum, natural gas Biomass: wood, grass, dung, ethanol Nuclear: fission (fusion) Wind Hydro Solar Geothermal H Fuel-Cell
Nuclear Energy Nuclear Fission Splitting large atoms in a chain reaction U235 + neutron >>>> unstable U236 >>>> Mo103 + Sn131 + neutrons + heat
Nuclear Energy Nuclear Fission Problem of waste Radioactive Long half-life
Nuclear Fusion Controlled hydrogen bomb Fusing smaller atoms together to form a larger atom and energy Not commercially developed, but conducted briefly under laboratory conditions
Nuclear Fusion This is the same reaction occurring in the core of stars, including the sun Deuterium (H2) + Tritium(H3) >>>> Helium (He4) + neutron + energy Deuterium (H2) + Deuterium (H2) >>>> Helium (He3) + neutron + energy
Nuclear Fusion Energy released would be captured to make steam, spin a turbine, and generate electricity. Fuels are readily available and radioactive wastes are minimal
Hydrogen Fuel Cell Technology Proton Exchange Membranes (PEM) protons (H+) pass through membrane electrons (e-) move through conductor
Global Energy Flow and Climate Incident sunlight energy (solar constant) Fate of incoming energy Reflection Scattering Absorption and reemission
Pattern of energy flow and reemission Reemission energy is infrared (heat) Clouds (particulate matter) reflect light Ultraviolet light absorbed by stratospheric ozone gas O3
Greenhouse Effect Greenhouse gases absorb and reemit heat Natural phenomenon not caused by humans
Greenhouse Gases Carbon dioxide Water vapor Ozone Methane Nitrogen oxides CFCs HFC PFC SF6
Changes in either atmospheric particulate (cloud cover) or greenhouse gases influences atmospheric temperature on a global scale Trace gases are most readily changed by human intervention
Intensification of the Greenhouse Effect would cause Greenhouse Warming Carbon Dioxide concentrations are increasing and have been since 1800
Sources of Carbon Dioxide Fossil Fuel combustion Biomass combustion Deforestation Volcanoes
Anthropogenic Greenhouse Gas Emissions, USA 2001 Million metric tons carbon equivalents
Greenhouse Gases Carbon dioxide Water vapor Ozone Methane (23 x CO2 GWP) Nitrogen oxides (296 x CO2 GWP) CFCs (4600-14000 x CO2 GWP) HFC (120-12000 x CO2 GWP) PFC (5700-12000 x CO2 GWP) SF6 (22000 x CO2 GWP)
Global Temperature Change from Mean 1961-1990 1850 1900 1950 2000
Is there a relationship between carbon dioxide concentration and global temperature?
Sources of Human Energy Resources Fossil Fuels: coal, petroleum, natural gas Biomass: wood, grass, dung, ethanol Nuclear: fission (fusion) Wind Hydro Solar Geothermal H Fuel-Cell