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heat |
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heatForm of energy possessed by a substance by virtue of the vibrational movement (kinetic energy) of its molecules or atoms. Heat energy is transferred by conduction, convection, and radiation. It always flows from a region of higher temperature (heat intensity) to one of lower temperature. Its effect on a substance may be simply to raise its temperature, or to cause it to expand, melt (if a solid), vaporize (if a liquid), or increase its pressure (if a confined gas). MeasurementQuantities of heat are usually measured in units of energy, such as joules (J) or calories (cal). The specific heat of a substance is the amount of heat that is needed to raise the temperature of 1 kg of the substance by 1 K (°C).Conduction, convection, and radiationConduction is the passing of heat along a medium to neighbouring parts with no visible motion accompanying the transfer of heat; for example, when the whole length of a metal rod is heated when one end is held in a fire. Convection is the transmission of heat through a fluid (liquid or gas) in currents; for example, when the air in a room is warmed by a fire or radiator. Radiation is heat transfer by infrared rays. It can pass through a vacuum, travels at the same speed as light, and can be reflected and refracted; for example, heat reaches the Earth from the Sun by radiation. For the transformation of heat, see thermodynamics. |
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| It is important that the thermal load profile closely follow the electric load profile so as to make maximum use of the waste heat energy from the cogenerator. For instance, Sussman explains mow heat energy from the sun is converted into the moving energy of the wind, how it evaporates water to power the water cycle, and how it's trapped on Earth by the greenhouse effect. Some of the heat energy radiates back toward Earth, and some radiates higher into the atmosphere, eventually escaping into space. |
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