plays a crucial role in heat transfer, allowing energy to move through space without a medium. This process involves visible light, radio waves, and . The amount and color of emitted depend on an object's temperature and surface properties.
The describes how radiant heat power relates to an object's temperature. As temperature increases, the peak of emitted radiation shifts, changing the color we perceive. This phenomenon explains why heated objects glow and stars have different colors.
Electromagnetic Radiation and Heat Transfer
Heat transfer by electromagnetic radiation
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Electromagnetic radiation transfers energy through space as waves without requiring a medium (vacuum)
Includes visible light, radio waves, X-rays, and infrared radiation
occurs when an object emits electromagnetic waves due to its temperature
Energy carried by these waves can be absorbed by another object, increasing its temperature
Amount of thermal radiation emitted depends on object's temperature and surface properties
Hotter objects emit more thermal radiation than cooler objects
Objects with higher (ability to emit thermal radiation) radiate more energy than those with lower (matte black vs shiny metal)
Temperature and radiated color relationship
Color of radiated energy related to temperature of emitting object
As temperature increases, peak wavelength of emitted radiation shifts to shorter wavelengths ()
λmax=Tb, where λmax is peak wavelength, T is absolute temperature, and b is Wien's displacement constant (2.898×10−3 m·K)
Cooler objects emit most radiation in infrared region, not visible to human eye (room temperature objects)
As temperature increases, object begins to emit radiation in visible spectrum
Color changes from red to orange to yellow to white to blue as temperature increases (heated metal, stars)
Sun, with surface temperature of ~5,800 K, emits most radiation in visible region, peaking in yellow-green part of spectrum
Stefan-Boltzmann law for heat transfer
Describes relationship between rate of heat transfer by radiation and temperature of an object
Total radiant heat power (energy per unit time) emitted by an object proportional to its absolute temperature raised to the fourth power
Equation for Stefan-Boltzmann law: P=ϵσAT4
P is radiant heat power (watts)
ϵ is emissivity of object's surface (unitless, 0 to 1)
σ is (5.67×10−8 W·m−2·K−4)
A is surface area of object (m2)
T is absolute temperature of object (K)
To calculate net heat transfer rate between two objects: Pnet=ϵσA(T14−T24)
T1 is absolute temperature of hotter object
T2 is absolute temperature of cooler object
Small changes in temperature result in significant changes in rate of heat transfer by radiation due to fourth-power dependence on temperature (doubling temperature increases radiation by factor of 16)
Electromagnetic spectrum and radiation properties
The encompasses all types of electromagnetic radiation, including radio waves, microwaves, infrared, visible light, ultraviolet, X-rays, and gamma rays
Each type of radiation is characterized by its wavelength and
Wavelength is the distance between consecutive wave crests
Frequency is the number of wave cycles passing a fixed point per second
Photons are the fundamental particles of electromagnetic radiation, carrying discrete amounts of energy
radiation refers to the theoretical perfect emitter and absorber of electromagnetic radiation
Real objects approximate blackbody behavior to varying degrees
and of radiation:
Absorption occurs when an object takes in electromagnetic energy
Emission is the process by which an object releases electromagnetic energy