1970
DOI: 10.1364/ao.9.000222
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An Optical Cell for Long Pathlengths at Low Temperatures

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Cited by 17 publications
(7 citation statements)
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“…A few years later two longpath cooling cells were built with optical lengths of 230 and 165 m, minimum temperatures of 77 and 80 K, and maximum pressures of 3 and 10 bar, respectively. 23,24 The temperature of the latter of the two cells could be adjusted between 80 and 125 K by use of a cryogenerator that worked with a liquid coolant such as nitrogen. Based on this design, another cell was built with 110 m of optical length that could be cooled down to 20 K with a two-stage cryogenerator.…”
Section: Existing Collisional Cooling Cellsmentioning
confidence: 99%
“…A few years later two longpath cooling cells were built with optical lengths of 230 and 165 m, minimum temperatures of 77 and 80 K, and maximum pressures of 3 and 10 bar, respectively. 23,24 The temperature of the latter of the two cells could be adjusted between 80 and 125 K by use of a cryogenerator that worked with a liquid coolant such as nitrogen. Based on this design, another cell was built with 110 m of optical length that could be cooled down to 20 K with a two-stage cryogenerator.…”
Section: Existing Collisional Cooling Cellsmentioning
confidence: 99%
“…For this reason long paths are almost universally used in air pollution spectroscopic analysis. To increase the net absorption the multipass optical cell was developed [9][10][11][12][13][14] , which has, in some cases, increased the effective sample length to several hundred meters.…”
Section: Introductionmentioning
confidence: 99%
“…The sensitivity of CRDS [8,52], phase-shift cavity ring down spectroscopy (PS-CRD) [6] and Fourier transform phase-shift cavity ring down spectroscopy [53] have been demonstrated by using several bands in the very weak forbidden b 1 + g ← X 3 − g transitions on gaseous molecular oxygen. Using the highly sensitive CRDS, the absorption spectra of the A-band of the 16 [54,55]. In addition, calculation of the atmospheric transmission function [38] and the magnetic dipole transition moment for the red atmospheric oxygen bands [56] have been made.…”
Section: Discussionmentioning
confidence: 99%
“…Other investigations that involve low temperature CRD experiments using a static cell have measured the collision induced absorption bands of oxygen [10,11]. Before the introduction of the CRD technique, multiple transversal cell or White cells [12] for gases operating at low temperatures were pioneered by Herzberg [13] cooled with liquid N 2 (78 K) and 80 m path length to give spectroscopic evidence for H 2 in the atmospheres of Uranus and Neptune, Watanabe and Welsh [14], using liquid H 2 (18 K), liquid N 2 (77 K) and 13 m path length studied the collision induced absorption of H 2 and D 2 at low temperatures, Ewing and co-workers [15] using liquid nitrogen (77 K), liquid Ar (87 K) and 230 m path length showed the collision induced absorption spectrum of O 2 , McKellar and co-workers [16] describe a variable temperature (80-125 K) with 165 m path length cell, and Horn and Pimentel [17] describe a variable temperature (120-300 K) and variable path length cell (60 to 2540 m) to study the absorption of constituents of Martian atmosphere. These cells have been very useful to reproduce conditions of planetary atmospheres and obtain spectroscopic constants and molecular structures of van der Waals molecules.…”
Section: Introductionmentioning
confidence: 99%