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G2201-i isotope analyzer measures the δ 13C of CH4 and CO2

NegotiableUpdate on 02/24
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Measure the δ 13C of CH4 and CO2
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G2201-iIsotope analyzer

Measure CH4And CO2The δ13C


Picarro G2201-iThe isotope analyzer integrates two Picarro δ 13C carbon isotope instruments used for measuring CO2 and CH4 into one instrument. The information provided by stable isotope ratios can now be easily and conveniently obtained, and researchers can track the movement of carbon from source to sink using a single instrument. This dual-purpose analyzer makes research work simple and fast. This analyzer is compact in size, sturdy in structure, and easy to transport to the site; Researchers can use the real-time results generated by the analyzer to change the ongoing work process and obtain the best results for time limited on-site activities.

Only on-site deployable analyzers can synchronize high-precision measurement of δ 13C in CO2 and CH4

Three measurement modes: CO2 only mode, CH4 only mode, and CO2 and CH4 combined mode

Achieve excellent accuracy with a small fraction of IRMS operating costs - reducing calibration, minimizing maintenance, and eliminating the need for consumables

This analyzer has three operating modes: 1) CO2 only mode, 2) CH4 only mode, and 3) CO2 and CH4 combined mode. In combination mode, staggered measurements of CO2 and CH4 are taken every few seconds to generate a faster sampling rate than the gas conversion time in the chamber. When the analyzer is in CO2 only mode or CH4 only mode, the accuracy will be improved because more measurement time can be used for individual molecules. In all modes, this analyzer can accurately measure the concentrations of CO2, H2O, and CH4, and it requires less calibration than other instruments based on spectral absorption. The G2201-i analyzer can be paired with various peripheral devices to extend and expand its functionality.

Picarro G2201-i Performance Specifications
δ 13C accuracy (1- σ, 1-hour window, 5-minute average) Single CO2 isotope ratio model Single CH4 isotope ratio model CO2-CH4 composite mode
δ13C-CO2 <> Not Applicable <>
δ13C-CH4 Not Applicable

High precision mode:<>

High dynamic range mode:<>

High precision mode:<>

High dynamic range mode:<>

Maximum drift of δ 13C (standard temperature and pressure, within 24 hours,

The difference between the maximum values of the 1-hour average

Single CO2 isotope ratio model Single CH4 isotope ratio model CO2-CH4 composite mode
δ13C-CO2 <> Not Applicable <>
δ13C-CH4 Not Applicable High precision and high dynamic range mode:<1.15 ‰, at 10='' ppm=''>1.15>
Concentration accuracy (1- σ, 30 second average) Single CO2 isotope ratio model Single CH4 isotope ratio model CO2-CH4 composite mode
CO2

200 ppb+0.05% reading (12C)

10 ppb+0.05% reading (13C)

1 ppm+0.25% reading (12C)

200 ppb+0.05% reading (12C)

10 ppb+0.05% reading (13C)

CH4 50 ppb+0.05% reading (12C)

High precision mode: 5 ppb+0.05% reading (12C), 1 ppb+0.05% reading (13C)

High dynamic range mode: 50 ppb+0.05% reading (12C), 10 ppb+0.05% reading (13C)

H2O 100 ppm
dynamic range Single CO2 isotope ratio model Single CH4 isotope ratio model CO2-CH4 composite mode
CO2 ensures accuracy range 380–2000 ppm 200–2000 ppm 380–2000 ppm
CO2 measurement range 100–4000 ppm 0–4000 ppm 100–4000 ppm
CH4 ensures accuracy range 1.8–500 ppm

High precision mode: 1.8-12 ppm

High dynamic range mode: 10-1000 ppm

High precision mode: 1.8-12 ppm

High dynamic range mode: 10-500 ppm

CH4 measurement range 0–1000 ppm

High precision mode: 1.2-15 ppm

High dynamic range mode: 1.8-1500 ppm

H2O ensures accuracy range 0–2.4%
H2O measurement range 0–5%
General specifications Single CO2 isotope ratio model Single CH4 isotope ratio model CO2-CH4 composite mode
Measurement Interval ≈ 3 seconds ≈ 5 seconds
Environmental temperature dependence Ensure<±='' 0.06 ‰/℃, typical=''><±=''>
Rise/fall time (10-90%/90-10%) Typical value ≈ 30 seconds
Application precautions

The concentration measurements of H2O and CO2 will be disturbed when they significantly exceed the specified dynamic range.

Similarly, certain organic compounds, ammonia, ethane, ethylene, or sulfur-containing compounds can also affect the measurement. Users should verify whether the test samples are suitable.

If unsure, please contact us to discuss the specific situation of the experiment. In the application of closed-loop measurement, attention should be paid to the possibility of pressure drop in the air path causing external air to enter the system.


Picarro G2201-i System Operating Specification
measurement Cavity ring down spectroscopy (CRDS) technology
Measurement pool temperature control ±0.005 ℃
Measurement pool pressure control ± 0.0002 atmospheric pressure
Shock and vibration testing Complies with MIL-STD-810F testing standards. After the impact and vibration tests, the instrument can still meet the performance specifications.
Sample temperature -10 to 45 ℃
Sample pressure 300 to 1000 Torr (40 to 133 kPa)
Sample flow rate <50='' standard milliliters per minute (sccm='') (typical value='' ≈ 25='' sccm), at='' 760=''>
Sample humidity <99%='' Relative humidity (at 40='' ℃=''>
Temperature range 10 to 35 ℃ (during instrument operation), -10 to 50 ℃ (instrument storage conditions)
ambient humidity < 99%=''>
attachment Vacuum pump (external), keyboard, mouse, LCD display (optional)
data output RS-232, Ethernet, USB
Air inlet connector ¼ inch Swagelok ®
Installation form Workbench or 19 inch rack mounted chassis
External dimensions 17 inches wide x 7 inches high x 17.5 inches long (43.2 x 17.8 x 44.6 centimeters), excluding 0.5-inch legs
weight 56 pounds (25.4 kilograms), including external pump
Power requirements 100-240 volts AC, 47-63 Hz (automatic detection),<260='' watts='' total power on, 125='' watts (analyzer), 35=''>