GCSE
Physics
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Introduction to GCSE Physics (AQA) Coming soon
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1.1 Energy Stores, Transfers and Power
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1.2 Conservation and Dissipation of Energy Coming soon
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1.3 National and Global Energy Resources Coming soon
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2.1 Current, Potential Difference and Resistance Coming soon
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2.2 Series and Parallel Circuits Coming soon
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2.3 Domestic Uses and Safety Coming soon
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2.4 Energy Transfers Coming soon
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2.5 Static Electricity Coming soon
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3.1 Changes of State and the Particle Model Coming soon
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3.2 Internal Energy and Energy Transfers Coming soon
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3.3 Particle Model and Pressure Coming soon
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4.1 Atoms and Isotopes Coming soon
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4.2 Atoms and Nuclear Radiation Coming soon
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4.3 Hazards and Uses of Radioactive Emissions and of Background Radiation Coming soon
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4.4 Nuclear Fission and Fusion Coming soon
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5.1 Forces and their Interactions Coming soon
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5.2 Work Done and Energy Transfer Coming soon
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5.3 Forces and Elasticity Coming soon
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5.4 Moments, Levers and Gears Coming soon
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5.5 Pressure and Pressure Differences in Fluids Coming soon
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5.6 Forces and Motion Coming soon
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5.6.1 Describing Motion Along a Line
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5.6.2 Distance and Displacement
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5.6.3 Speed
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5.6.4 Velocity
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5.6.5 The Distance–Time Relationship
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5.6.6 Acceleration
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5.6.7 Forces, Accelerations and Newton's Laws of Motion
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5.6.8 Newton's First Law
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5.6.9 Newton's Second Law
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5.6.10 Newton's Third Law
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5.6.11 Forces and Braking
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5.6.12 Stopping Distance
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5.6.13 Reaction Time
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5.6.14 Factors Affecting Braking Distance
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5.6.1 Describing Motion Along a Line
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5.7 Momentum [HT] Coming soon
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6.1 Waves in Air, Fluids and Solids Coming soon
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6.2 Electromagnetic Waves Coming soon
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6.3 Black Body Radiation Coming soon
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7.1 Permanent and Induced Magnetism, Magnetic Forces and Fields Coming soon
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7.2 The Motor Effect Coming soon
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7.3 Induced Potential, Transformers and the National Grid [HT] Coming soon
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8.1 Solar System; Stability of Orbital Motions; Satellites Coming soon
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8.2 Red-Shift Coming soon
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9.1 Required Practicals Coming soon
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9.1.1 Required Practical Activity 1
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9.1.2 Required Practical Activity 2
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9.1.3 Required Practical Activity 3
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9.1.4 Required Practical Activity 4
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9.1.5 Required Practical Activity 5
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9.1.6 Required Practical Activity 6
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9.1.7 Required Practical Activity 7
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9.1.8 Required Practical Activity 8
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9.1.9 Required Practical Activity 9
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9.1.10 Required Practical Activity 10
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9.1.1 Required Practical Activity 1
1. Energy
6.3.2 Perfect Black Bodies and Radiation
In this lesson, we will explore the concept of radiation emitted by all bodies and how the intensity and wavelength distribution of this emission depend on the body's temperature.
Emission of Radiation
All bodies, regardless of their composition, emit radiation. This process is known as thermal radiation.
- The intensity and wavelength distribution of the emitted radiation depend on the temperature of the body.
- Hotter bodies emit more intense radiation, with a distribution that peaks at shorter wavelengths.
Absorption and Emission Equilibrium (HT only)
A body at a constant temperature absorbs radiation at the same rate as it emits radiation, establishing an equilibrium. When a body absorbs radiation faster than it emits radiation, its temperature increases.
Factors Influencing Earth's Temperature (HT only)
The temperature of the Earth is determined by various factors, including:
- Rates of Absorption and Emission: The balance between the incoming radiation absorbed from the Sun and the radiation emitted by the Earth affects its overall temperature.
- Reflection of Radiation: The reflection of solar radiation by the Earth's surface and atmosphere plays a role in controlling the amount of energy absorbed.
Temperature and Radiation Balance (HT only)
The temperature of a body is related to the balance between the incoming radiation absorbed and the radiation emitted.
- Everyday Examples: Examples from everyday life include a cup of coffee cooling down or a warm object reaching room temperature.
Radiation and Earth's Temperature (HT only)
- Solar Radiation: The Sun emits electromagnetic radiation, with a significant portion falling within the visible and infrared spectra, which interacts with the Earth's atmosphere and surface.
- Greenhouse Effect: Certain atmospheric gases, known as greenhouse gases, absorb and re-emit infrared radiation, trapping heat in the Earth's atmosphere and contributing to the overall temperature rise.
Conclusion
All bodies emit radiation, and the intensity and wavelength distribution of this emission depend on the body's temperature. A body at a constant temperature absorbs radiation at the same rate as it emits radiation, maintaining an equilibrium. The temperature of a body is determined by the balance between incoming radiation absorbed and radiation emitted.
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