High-temperature Pressure Broadening of Water: Experimental Evidence for Negative Temperature Exponents
TL;DRAbstract
Fourier transform spectra of H2O-air mixtures have been measured at 296, 742, and 980 K for total pressures of 0.5 and 1.0 atm with a H2O VMR of 0.5% in the Þ2 band (range 1550-2300 cm-1) at a spectral resolution of 0.01 cm-1. These measurements were initially carried out in the frame of two EC projects aiming at a spectroscopic database for non-intrusive aircraft exhaust measurement. A special cell for high temperatures, good temperature homogeneity, 16 cm absorption path, equipped for continuous gas flow, has been developed to be operated stand-alone and inside the evacuated sample compartment of the Bruker IFS 120 HR FT spectrometer. Thermal emission compensation and proper transmittance calculation required high resolution sample and reference spectra for the IR source switched on and off. Temperatures were deduced from CO line intensity measurements. Line positions, linestrengths and Lorentzian halfwidths have been retrieved from the spectra. For the following analysis only air-b
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Fourier transform spectra of H2O-air mixtures have been measured at 296, 742, and 980 K for total pressures of 0.5 and 1.0 atm with a H2O VMR of 0.5% in the Þ2 band (range 1550-2300 cm-1) at a spectral resolution of 0.01 cm-1. These measurements were initially carried out in the frame of two EC projects aiming at a spectroscopic database for non-intrusive aircraft exhaust measurement. A special cell for high temperatures, good temperature homogeneity, 16 cm absorption path, equipped for continuous gas flow, has been developed to be operated stand-alone and inside the evacuated sample compartment of the Bruker IFS 120 HR FT spectrometer. Thermal emission compensation and proper transmittance calculation required high resolution sample and reference spectra for the IR source switched on and off. Temperatures were deduced from CO line intensity measurements. Line positions, linestrengths and Lorentzian halfwidths have been retrieved from the spectra. For the following analysis only air-b
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