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emissivity |
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emissivity [‚ē·mə′siv·əd·ē] (thermodynamics) The ratio of the radiation emitted by a surface to the radiation emitted by a perfect blackbody radiator at the same temperature. Also known as thermal emissivity. Emissivity The ratio of the radiation intensity of a nonblack body to the radiation intensity of a blackbody. This ratio, which is usually designated by the Greek letter ε, is always less than or just equal to one. The emissivity characterizes the radiation or absorption quality of nonblack bodies. Published values are readily available for most substances. Emissivities vary with temperature and also vary throughout the spectrum. For an extended discussion of blackbody radiation and related information See Heat radiation. A spectral emissivity of zero means that the heat radiator emits no radiation at this wavelength. Strongly selective radiators, such as insulators or ceramics, have spectral emissivities close to 1 in some parts of the spectrum, and close to zero in other parts. Carbon has a high spectral emissivity throughout the visible and infrared spectrum, exceeding 0.90 in certain portions; thus carbon is a good blackbody radiator. Tantalum is the only metal with a spectral emissivity greater than 0.5 in the visible spectrum. All other metals have a lower spectral emissivity. Tungsten is a relatively good emitter, with a spectral emissivity of 0.43–0.47 within the visible region of the spectrum. See Blackbody How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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| Infrared temperature measurement of shiny rolls is said to be challenging because of the low and varying emissivity of the stainless steel surface as a result of aging and surface wear. Values for emissivity and film coefficients for pure magnesium indicated an expected temperature of 237-257F (114-125C), which could be too high for magnesium alloy AM50 to withstand without a significant reduction in mechanical properties. The goals of this campaign included evaluation of spatial variability to fully assess how accurately sea ice parameters can be derived; a study of new ice emissivity, heat, and salinity fluxes over coastal waters; and a determination of precise locations of ice edges. |
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