Abstract

Laser spectroscopy in the linear regime of radiation–matter interaction is a powerful tool for measuring thermodynamic quantities in a gas at thermodynamic equilibrium. In particular, the Doppler effect can be considered a gift of nature, linking the thermal energy to an optical frequency, namely the line centre frequency of an atomic or molecular spectral line. This is the basis of a relatively new method of primary gas thermometry, known as Doppler broadening thermometry (DBT). This paper reports on the efforts that have been carried out, in the last decade, worldwide, to the end of making DBT competitive with more consolidated and accurate methodologies, such as acoustic gas thermometry and dielectric constant gas thermometry. The main requirements for low-uncertainty DBT, of both theoretical and technical nature, will be discussed, with a special focus on those related to the line shape model and to the frequency scale. A deep comparison among the different molecules that have been selected in successful DBT implementations is also reported. Finally, for the first time, to the best of my knowledge, the influence of refractive index effects is discussed.

Highlights

  • Precision spectroscopy in molecular systems is a very active and fascinating research field, in which tests of2016 The Authors

  • This paper has outlined the present status of Doppler broadening thermometry (DBT)

  • It deals with a relatively new method of primary gas thermometry linking the thermal energy to an absolute frequency, namely the line centre frequency of an atomic or molecular resonance, and a frequency interval, which is the Doppler width of the line

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Summary

Introduction

Precision spectroscopy in molecular systems is a very active and fascinating research field, in which tests of. If the spectroscopic parameters of a particular line of a given species are known (as a function of the gas temperature), the absorber gas density can be accurately determined by using laser absorption spectroscopy [4] This is a possible way to determine the vertical profiles of water, carbon dioxide and other trace constituents of the Earth atmosphere in air- or balloon-borne experiments through punctual (in situ) measurements at different altitudes [4]. Where νD is the Doppler half-width at half maximum (HWHM), ν0 is the line centre frequency, c is the speed of light, T is the thermodynamic temperature, kB is the Boltzmann constant and M is the absorber mass This equation represents the basis of a relatively new method of primary gas thermometry, known as Doppler broadening thermometry (DBT) [5]. In the sixth section, refractive index effects in DBT are discussed for the first time

Line shape theory
The carbon dioxide experiment
The water experiment
Refractive index effects
Conclusion
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