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IB PHYSICS Topic 8: Energy Production

8.1 Energy Sources

  • Specific Energy and Energy Density of Fuel Sources

    • Specific energy and energy density are vital for quantifying the energy released during combustion.

    • Specific energy: energy per unit mass (energy/mass).

    • Energy density: energy per unit volume (energy/volume).

    • Sankey Diagrams and Energy Degradation

    • Cyclical processes are needed for continuous conversion of thermal energy to work.

    • Some energy is lost to the surroundings, termed degraded energy.

    • Sankey diagrams visually represent energy flows.


8.2 Thermal Energy Transfer

  • Conduction, Convection, and Thermal Radiation

    • Conduction and convection require a medium; radiation can transfer through a vacuum.

  • Black-Body Radiation

    • A black body absorbs all incident electromagnetic radiation.

    • Black-body radiation follows the Stefan-Boltzmann law.

  • Albedo and Emissivity

    • Albedo

      • Measures the ratio of total scattered (reflected) radiation to total incident radiation.

      • Influenced by season, latitude, and terrain.

    • Emissivity

      • Objects radiate a fraction compared to a black body.

      • Emissivity = power per unit area radiated by the object / power per unit area radiated by a black body at the same temperature.

  • The Solar Constant

    • Amount of energy falling on 1m^2 of Earth's atmosphere per second.

    • Solar constant is approximately 1366 W/m^2.

  • The Greenhouse Effect

    • Greenhouse Gasses

      • Absorb infrared radiation due to natural frequencies.

    • Mechanism

      • Incoming solar radiation takes the form of ultraviolet and visible radiation.

      • Greenhouse gasses trap infrared radiation, leading to the greenhouse effect.

    • Chain Reaction

      • Global warming reduces ice/snow cover, affecting albedo.

      • Carbon dioxide solubility in the sea decreases, increasing atmospheric carbon dioxide.

    • Effects

      • Rising mean sea levels, extreme weather events.

  • Energy Balance in the Earth Surface–Atmosphere System

    • Describes how incoming solar energy is used and returned to space.

    • Balanced energy flow maintains a constant Earth temperature.

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IB PHYSICS Topic 8: Energy Production

8.1 Energy Sources

  • Specific Energy and Energy Density of Fuel Sources

    • Specific energy and energy density are vital for quantifying the energy released during combustion.

    • Specific energy: energy per unit mass (energy/mass).

    • Energy density: energy per unit volume (energy/volume).

    • Sankey Diagrams and Energy Degradation

    • Cyclical processes are needed for continuous conversion of thermal energy to work.

    • Some energy is lost to the surroundings, termed degraded energy.

    • Sankey diagrams visually represent energy flows.


8.2 Thermal Energy Transfer

  • Conduction, Convection, and Thermal Radiation

    • Conduction and convection require a medium; radiation can transfer through a vacuum.

  • Black-Body Radiation

    • A black body absorbs all incident electromagnetic radiation.

    • Black-body radiation follows the Stefan-Boltzmann law.

  • Albedo and Emissivity

    • Albedo

      • Measures the ratio of total scattered (reflected) radiation to total incident radiation.

      • Influenced by season, latitude, and terrain.

    • Emissivity

      • Objects radiate a fraction compared to a black body.

      • Emissivity = power per unit area radiated by the object / power per unit area radiated by a black body at the same temperature.

  • The Solar Constant

    • Amount of energy falling on 1m^2 of Earth's atmosphere per second.

    • Solar constant is approximately 1366 W/m^2.

  • The Greenhouse Effect

    • Greenhouse Gasses

      • Absorb infrared radiation due to natural frequencies.

    • Mechanism

      • Incoming solar radiation takes the form of ultraviolet and visible radiation.

      • Greenhouse gasses trap infrared radiation, leading to the greenhouse effect.

    • Chain Reaction

      • Global warming reduces ice/snow cover, affecting albedo.

      • Carbon dioxide solubility in the sea decreases, increasing atmospheric carbon dioxide.

    • Effects

      • Rising mean sea levels, extreme weather events.

  • Energy Balance in the Earth Surface–Atmosphere System

    • Describes how incoming solar energy is used and returned to space.

    • Balanced energy flow maintains a constant Earth temperature.