Abstract:Several inorganic materials are used to illustrate that bands in infrared emission spectra of solids change shape as the particle size of the sample is altered, and that the way in which a particular band changes depends upon the value of its absorption coefficient. The relationship found to exist between corresponding band shape changes in emission and reflection spectra indicates that Kirchoff's law holds to a first‐order approximation for particulate, or mat, surfaces. The implications of band shape changes… Show more
“…Some minerals exhibit the phenomenon of reststrahlen in this spectral interval (Aronson, et al 1967;Hovis,1966;Hovis, et al 1968;Hunt and Vincent, 1968;Lyon, 1965). Laboratory measurements show a correlation of the location of the reststrahlen peaks in the spectral reflectance curves of various silicate bear ing minerals with their SiO 2 content.…”
The Michelson interferometer experiment carried on the Nimbus 3 satellite has successfully obtained thermal emission spectra of the earth and atmosphere between 400 and 2000 cm−1 with a resolution equivalent to 5 cm−1. Comparison of a measured spectrum with a spectrum calculated theoretically from near‐simultaneous radiosonde measurements indicates generally good agreement over most of the spectral range covered. A preliminary search for spectral features attributable to minor atmospheric constituents other than CO2 H2O, and O3 has resulted in a positive identification of only CH4 thus far. Comparisons of temperature profiles estimated from selected spectra with those obtained from radiosonde measurements on an individual basis and in the form of maps for selected locations and times indicate that meaningful atmospheric temperatures can be obtained, even in the presence of clouds. Similar comparisons of water vapor estimates with radiosonde measurements demonstrate that good humidity profiles can be obtained under almost clear sky conditions, but, when clouds are present within the field of view, the estimates become unreliable. Total ozone amounts in an atmospheric column obtained from the spectra are in generally good agreement with Dobson spectrometer measurements, and the estimates are found to be insensitive to clouds within the field of view under most circumstances. A global map of ozone, constructed from data taken over a 24‐hour period, shows anticipated correlations with a conventional 300‐mb pressure height map in the northern hemisphere. The possibility of obtaining information on surface composition is investigated by using a spectrum obtained over Egypt that shows a depression of as much as 10°K in brightness temperature in parts of the atmospheric window. This effect can be attributed to reststrahlen due to the presence of SiO2 in the desert soil.
“…Some minerals exhibit the phenomenon of reststrahlen in this spectral interval (Aronson, et al 1967;Hovis,1966;Hovis, et al 1968;Hunt and Vincent, 1968;Lyon, 1965). Laboratory measurements show a correlation of the location of the reststrahlen peaks in the spectral reflectance curves of various silicate bear ing minerals with their SiO 2 content.…”
The Michelson interferometer experiment carried on the Nimbus 3 satellite has successfully obtained thermal emission spectra of the earth and atmosphere between 400 and 2000 cm−1 with a resolution equivalent to 5 cm−1. Comparison of a measured spectrum with a spectrum calculated theoretically from near‐simultaneous radiosonde measurements indicates generally good agreement over most of the spectral range covered. A preliminary search for spectral features attributable to minor atmospheric constituents other than CO2 H2O, and O3 has resulted in a positive identification of only CH4 thus far. Comparisons of temperature profiles estimated from selected spectra with those obtained from radiosonde measurements on an individual basis and in the form of maps for selected locations and times indicate that meaningful atmospheric temperatures can be obtained, even in the presence of clouds. Similar comparisons of water vapor estimates with radiosonde measurements demonstrate that good humidity profiles can be obtained under almost clear sky conditions, but, when clouds are present within the field of view, the estimates become unreliable. Total ozone amounts in an atmospheric column obtained from the spectra are in generally good agreement with Dobson spectrometer measurements, and the estimates are found to be insensitive to clouds within the field of view under most circumstances. A global map of ozone, constructed from data taken over a 24‐hour period, shows anticipated correlations with a conventional 300‐mb pressure height map in the northern hemisphere. The possibility of obtaining information on surface composition is investigated by using a spectrum obtained over Egypt that shows a depression of as much as 10°K in brightness temperature in parts of the atmospheric window. This effect can be attributed to reststrahlen due to the presence of SiO2 in the desert soil.
“…Besides, in addition to these progressive modifications, the band shapes were markedly modified in comparison with those of the single crystal but the bands shapes did not evolve significantly with the increase in porosity between 500 and 900 cm -1 . Several authors [10,[15][16][17][18][19] showed that the band shape of the spectral emissivity was dependent on the grain size and the grain shape constituting the surface of the sample. Several types of behaviors appeared according to the particle size and the value of the absorption coefficient K (e.g.…”
Section: Roughness Effect In the Opaque Zonementioning
International audienceThermal and optical properties of ceramics are dependent on radiation scattering and cannot be determined by a knowledge of their chemical composition alone, as for single crystals. In this paper, extrinsic effects, such as roughness, porosity, and texture, on the spectral emissivity of alumina ceramics are investigated. Roughness effects have an influence mainly in the opaque zone; an important porosity dependence and the presence of a critical porosity threshold were observed in the semitransparent zone. Furthermore, it was shown that two ceramics with similar total porosities, but with different textures, possess radically different emissivities, showing that grain size, pore size, and spatial repartition of the grains are also crucial for an understanding of the thermal properties of the ceramics
“…Type 3 4 behavior involves an increase in spectral contrast with decreasing particle size. 10 The calcite ν3 anti-symmetric stretching mode shows type 1 behavior, whereas the [CO3 are dependent on the wavelength. The critical diameter for a transition in optical properties is related to the absorption coefficient (α) and is proportional to wavelength (λ) and (k) defined as 2,13 :…”
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