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Isothermal Process |
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isothermal process [¦ī·sə¦thər·məl ′prä·səs]
(thermodynamics) Any constant-temperature process, such as expansion or compression of a gas, accompanied by heat addition or removal from the system at a rate just adequate to maintain the constant temperature. Isothermal process A thermodynamic process which occurs with a heat addition or removal rate just adequate to maintain constant temperature. The change in the internal energy per mole U accompanying a change in volume in an isothermal process is given by the equation below, where T is the ![]() Isothermal Process a process that occurs in a physical system at constant temperature. To create an isothermal process a system is usually placed in a thermostat (a massive body in thermoequilibrium) of high thermal conductivity, so that heat exchange with the system proceeds quite rapidly and the difference between the temperature of the system and that of the thermostat is negligible. Another method is to use heat sources or heat sinks while checking for constant temperature by means of thermometers. Boiling a fluid and melting a solid at constant pressure, for example, are isothermal processes. For an ideal gas, the product of pressure by volume is constant during an isothermal process (the Boyle-Mariotte law). Generally speaking, a certain amount of heat is conveyed to (or given off from) the system in an isothermal process, and external work is performed. The work performed by an ideal gas in an isothermal process is equal to NkT log (V2/V1), where N is the number of particles of the gas, T is the temperature, and K2 are the volumes of the gas at the start and completion of the process, and k is Boltzmann’s constant. In solids and in most liquids an isothermal process changes the volume of a body very little, as long as there is no phase transition. V. L. POKROVSKII [10–291—4] Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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