IR absorption spectrum (4200-3100 cm-1) of H2O and (H2O)2 in CCl4. Estimates of the equilibrium constant and evidence that the atmospheric water absorption continuum is due to the water dimer

Journal of Quantitative Spectroscopy and Radiative Transfer

Volumn 110, Issue 18, 2009, Pages 2060-2076

  Nicolaisen, Flemming M ^a  

^a UNIVERSITY OF COPENHAGEN   (Denmark)

Author keywords

Absorption coefficients; Atmospheric water absorption continuum; Dimerization equilibrium constant; Thermodynamic functions; Water dimer

Indexed keywords

ABSORPTION BAND; ABSORPTION COEFFICIENTS; ABSORPTION CONTINUUM; ATMOSPHERIC WATER; ATMOSPHERIC WATER ABSORPTION CONTINUUM; FREQUENCY SHIFT; GAS PHASE EQUILIBRIUM; GAS PHASE VALUE; GASPHASE; INTEGRATED ABSORPTION COEFFICIENTS; INTENSITY ENHANCEMENT FACTORS; IR ABSORPTION SPECTRA; IR SPECTRUM; SATURATED SOLUTIONS; SPECTRAL DATA; SPECTRAL REGION; STANDARD ENTHALPY OF FORMATION; THERMODYNAMIC FUNCTIONS; WATER DIMER; WATER DIMERS; WATER VAPOUR;

ABSORPTION SPECTRA; ABSORPTION SPECTROSCOPY; DIMERIZATION; EQUILIBRIUM CONSTANTS; GAS ABSORPTION; GAS DYNAMICS; GAS FUEL PURIFICATION; GASES; INFRARED ABSORPTION; LIGHT ABSORPTION; MONOMERS; PHASE EQUILIBRIA; THERMODYNAMICS; WATER VAPOR;

WATER ABSORPTION;

ABSORPTION COEFFICIENT; ABSORPTION SPECTRUM; ESTIMATION METHOD; PHASE EQUILIBRIUM; THERMODYNAMICS; WATER VAPOR;

EID: 69449097347     PISSN: 00224073     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jqsrt.2009.05.004     Document Type: Article

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