Frequently Asked Questions about the ASTEC Systems

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10. What is the difference between solar radiation and thermal radiation?

Solar (sun) radiation travels to earth by electromagnetic waves at the speed of light (186,286 miles per second or 300,000 kilometers per second). The electromagnetic spectrum carries different kinds of rays (gamma, x-ray, visible, infrared, etc.) each with a different wavelength between 0.1 to 150 micrometers long (a micrometer, μm, or a micron is one millionth of a meter) and each with its own frequency. The frequency is measured in hertz/sec and it represents the number of waves produced per second. Not all solar radiation reaches the earth but the radiation which penetrates the atmosphere [ultraviolet (0.29 to 0.40 μm), visible (0.40 to 0.76 μm), and near infrared rays (0.76 to 150 μm] has a high energy content (per m2). This energy is converted to heat energy when it is absorbed in the roof of a building or any object.

Reflectivity is the ability to "deflect" or reject radiant energy like a mirror reflects light. Solar reflectivity is the numerical measurement from 0 to 100% of the total amount of incident solar radiation that is not absorbed by the surface.

Thermal radiation is emitted from objects on earth by electromagnetic waves (infrared rays) of low energy content (therefore, containing less heat) due to the temperature (internal energy) of the object.

Thermal radiation refers to wavelengths extending from 1.50 to 1000 μm. It includes:

The "longer" wavelengths from the middle infrared (1.50 to 5.60 μm), to the far infrared (5.60 to 15.00 μm), and the     extreme infrared (15.00 to 1000 μm).

The "longer" wavelength radiation has a very low energy content compared to shorter wavelength radiation. The lower the object's temperature, the longer the wavelength emitted and the lower the rate and energy emitted.

Emissivity: a body continually emits radiant energy at a rate that is related to its temperature and the nature of its surface (E = εσT4SURFACE).

Thermal emissivity is the rate at which a body emits radiant energy compared to a "perfect blackbody" emitter at the same temperature.

Electromagnetic radiation that is absorbed by matter is converted into internal energy, which can be stored, transferred by conduction, converted back into electromagnetic radiation that is given off (emitted) by the material itself.

The amount of radiation heat emitted should equal the amount of heat absorbed minus that conducted (towards the heat sink) because the laws of thermophysics demonstrate that energy is never lost (Law of Conservation of Energy).

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