Atmos | Heatable long pathlength gas cells

Better value long pathlength gas cell | AtmosTM
AtmosTM is our range of long pathlength gas cells for measuring the infrared spectra of trace gases and vapors. Available in fixed pathlengths of 2.5, 5.0, 10.0, 20.0 meters for maximum versatility. Each cell has been individually optimized for maximum optical throughput and signal-to-noise

Quick Enquiry See all product options
  • Wide pathlength range (2.5 to 20m)
  • Vacuum (torr) (3 x 10-3) to 125 psi operation (80 psi for 20m version)
  • Up to 200 °C with heating jacket
  • Ni-coated aluminium body
  • Gold mirrors (protected)
  • Viton or FFKM 'O' ring seals
  • CaFor ZnSe windows
  • Purgeable transfer optics box
  • Leverlock series baseplate mounting
Optional Features
  • Heating Jacket
  • Sample monitoring thermocouple
  • Vacuum (Torr) (3 x 10-3) / gas inlet & outlet taps
  • Pressure gauge
  • Desiccant storage caps
Model A2.5 A5 A10 A20
Pathlength (m) 2.5 5.0 10 20
Base pathlength (mm) 104 139 250 455
Number of passes 24 36 40 44
Volume (L) 0.27 0.63 2.12 3.68
The Atmos™ range of cells are heatable to 200 °C with the addition of a heating jacket and temperature controller. Why Atmos™?
  • Optimized optical path for unmatched signal-to-noise
  • Low cell volume for fast gas exchange
  • Ni-coated Al cell bodies for improved thermal transfer from heating jackets. Also holds higher gas pressure than glass.
  • Inert stainless-steel mirror substrates and avoidance of glues to prevent outgassing
  • 125 psi (8.6 bar) maximum cell pressure (80 psi - 5.44 bar for 20m version)
  • Retrofittable heating jacket option for up to 200 °C
Which pathlength should I choose? The absorbance of a gas depends on the distance travelled by the IR light beam through the gas sample. The relationship between absorbance, A, concentration, C, and pathlength, L, is given by Beer’s Law: A = -log10 (I/I0) = a.C.L Atmospheric concentrations of gases are usually expressed in C.L units of ppm.m – the number of molecules that would be encountered by the infrared beam across a 1.0 m path. A gas at 0.1 ppm atmospheric concentration will absorb as much IR light over a pathlength of 100 m as would the same gas at 1 ppm over 10 meters or at 10 ppm over 1 meter. Accordingly, the pathlength of cell should be chosen to give absorbance values within the spectrometer’s linear range for a given concentration. The following table may be taken as a guide:
Gas name formula v (cm-1) ppm.m absorbance
Carbon dioxide CO2 2360 100 0.40
Carbon monoxide CO 2170 100 0.04
Methane CH4 3020 100 0.10
C2 to C6 n-alkanes 2960 100 0.10
Nitrogen dioxide NO2 1630 100 0.15
Nitric oxide NO 1900 100 0.015
Sulfur dioxide SO2 1370 100 0.09
Hydrogen sulfide H2S 1300 1000 0.002
Ammonia NH3 960 100 0.12
Hydrogen chloride HCl 2940 100 0.04
Water H2O 1650 1000 0.20
Vinyl chloride CH2CHCl 950, 900 100 0.06
Acetaldehyde CH3CHO 2750 100 0.015
Benzene C6H6 670 10 0.09
Toluene C6H5CH3 730, 690 100 0.10
Methanol CH3OH 1040 100 0.10
Ethanol CH3CH2OH 1050 100 0.05
Carbonyl sulfide COS 2070 100 0.40
Nitrous oxide N2O 2235 100 0.15
Sulfur hexafluoride SF6 950 10 0.40

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Purge Tubes (Bellows) Pair

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