41 Facts about thermal radiations


Facts about thermal radiations
1.     Most of the solar radiations reaching the earth are in the thermal radiation ranges.
2.     Thermal radiations are emitted as a result of  thermal agitations
3.     Thermal agitations are as a result of increase in temperature.
4.     Heat and light spectra of electromagnetic radiations falls under thermal radiations.
5.     Electromagnetic radiations with wavelength between 0.2 to 10000 micrometer are part of thermal radiations
6.     Thermal radiations are the visible light, ultra violet and the infrared portions.
7.     Thermal radiations can be divided into short wave and the long wave.
8.     The visible light is part of thermal radiations and falls with wavelength between 0.39 to 0.77micrometer.
9.     The intensity of solar radiation impinging on a surface depends on angle of incident, time of the year and atmospheric condition.
10.                        The infrared region is divided into near infra red and far infra red.
11.                        Emission of radiations is due to oscillations and transitions of electrons that comprise matter and is sustained by the thermal energy of the matter.
12.                        Emission correspond to heat transfer from the matter and hence a reduction in thermal energy stored by the matter.
13.                        Radiation may also be intercepted absorbed by matter.
14.                        Absorption of radiation result to heat transfer by the matter and hence an increase in energy stored by the matter.
15.                        Emission from gas or transparent liquid or solid is a volumetric phenomenon.
16.                        Emission from an opaque solid or liquid is a surface phenomenon.
17.                        For an opaque object emission from atoms and molecules within one micrometer depth to the surface.
18.                        All bodies emit radiations at temperature above 0k, absolute zero.
19.                        A transparent body will transmit all radiations that falls on it.
20.                        A translucent body will scatter radiation falling on it.
21.                         An opaque object will absorb or reflect radiation falling on it.
22.                        Scatting is the diffused reflection of light in a body.
23.                        The absorption and reflection of radiations depend on the color and size of the molecules of the object involved.
24.                        When a body absorb radiations it temperature rises and it start to emit radiations.
25.                        It is only a black body that can absorb or reflect all wavelength of light at temperature and all angles of incidence.
26.                        When wavelength of radiation is greater than size of atom or molecules a body the wave will be scattered.
27.                        Change in temperature in matter cause charge oscillations which in turn produce electromagnetic radiations.
28.                        Sunlight is part of electromagnetic radiations produced by the hot plasma of the sun.
29.            Absorptivity , reflectivity and emissivity of all objects depend on wavelength of radiations.
30.            The frequency of distribution of thermal radiations is given by plank’s law.
31.            Increase in the rate of thermal radiation is proportional to the 4th root of its temperature T4.
32.            Objects absorb much of the frequency range they can emit.
33.            The rate at which objects radiates (or absorb) depends on the nature of the surface.
34.            Object that is a good emitter is also a good absorber.
35.            The hotter an object is the more light it emits.
36.            Stephan-Boltzmann law states that the total energy radiated per unit surface area of a blackbody across all wavelengths per unit time is proportional to the fourth power of its absolute temperature.
37.            Emissivity is the measure of the effectiveness of emission of thermal radiation by a surface.
38.            Absorptivity of a surface is the measure of its effectiveness in absorption of radiations.
39.             The spectral distribution of radiation intensity is explained by plank’s law.
40.            Reflectivity is the ratio of the reflected to the incident radiation impinging a surface.
41.            Transmissivity is the ratio of transmitted to incident



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