2001
DOI: 10.1016/s0009-2614(00)01388-9
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Cavity-enhanced absorption spectroscopy of methane at 1.73 μm

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Cited by 30 publications
(16 citation statements)
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“…(6) with Beer-Lambert law, one may conclude that the absorption path length of the transmission signals is enhanced by a factor 4F c /π. It is worth noting that the enhancement factor of a planar FPC is 2F/π [25,26] where F is the finesse of the planar FPC [27]. Considering the different definitions of the finesses F c and F, the effective absorption path length of the planar and confocal FPC are the same.…”
Section: High Sensitivity From Back Cavity Mirror Signalsmentioning
confidence: 99%
“…(6) with Beer-Lambert law, one may conclude that the absorption path length of the transmission signals is enhanced by a factor 4F c /π. It is worth noting that the enhancement factor of a planar FPC is 2F/π [25,26] where F is the finesse of the planar FPC [27]. Considering the different definitions of the finesses F c and F, the effective absorption path length of the planar and confocal FPC are the same.…”
Section: High Sensitivity From Back Cavity Mirror Signalsmentioning
confidence: 99%
“…Gas chromatographic methods for the measurement of ambient mixing ratios and the isotopic ratio of methane (and other hydrocarbons) are robust and versatile, but the time per analysis is long, so some effort has gone into developing more real-time and portable systems for specialized applications like plume tracking. Cavity ring-down (and variants like CEAS) 57,58 has begun to be explored for direct real-time spectroscopic measurement of hydrocarbons. Hydrocarbons (especially alkanes) are transparent in the visible and near-UV regions of the spectrum where the best combinations of tunable sources, high quality mirrors, and highly sensitive detectors for cavity ring-down are usually found.…”
Section: Volatile Hydrocarbonsmentioning
confidence: 99%
“…Changes in the steady state output power are due to intracavity losses from molecular absorption. [19][20][21] The Harvard ICOS instrument is designed for in situ sampling on high-altitude aircraft in the middle and UTLS and is currently configured to measure the four primary isotopologues of water ͑H 2 O, HDO, H 2 18 O, and H 2 17 O͒ as well as methane ͑CH 4 ͒ in the mid-IR at 6.7 m. In situ airborne sampling requires fast time response, high accuracy and precision, and low contamination from the instrument inlet and plumbing. The Harvard instrument is able to measure water vapor from 1 ppmv to a few thousand ppmv, values typical of the middle and UTLS, as well as simultaneous measurements of the less abundant isotopologues.…”
Section: Introductionmentioning
confidence: 99%