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Linhan Shen1, Thinh Bui1, John Eiler2, Mitchio Okumura1

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Presentation on theme: "Linhan Shen1, Thinh Bui1, John Eiler2, Mitchio Okumura1"— Presentation transcript:

1 Linhan Shen1, Thinh Bui1, John Eiler2, Mitchio Okumura1
MEASUREMENTS OF DOUBLY-SUBSTITUTED METHANE ISOTOPOLOGUE ABUNDANCE USING FREQUENCY STABILIZED MID-IR CAVITY-RINGDOWN SPECTROSCOPY Linhan Shen1, Thinh Bui1, John Eiler2, Mitchio Okumura1 Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA

2 Methane Isotopologue Abundances
Cardinal Mass Isotopologue Relative Abundance Exact Mass 16 12CH4 98.8% 16.031 17 13CH4 1.11% 17.035 12CH3D 616 ppm 17.038 18 13CH3D 6.92 ppm 18.041 12CH2D2 144 ppb 18.044 Other 13CH2D2, 12CHD3, 13CHD3, 12CD4, 13CD4 1.64 ppb -- Carry Important Molecular Information about the Formation Conditions of Methane (e.g. Temperature)

3 Current State of Clumped Isotope Methane Measurements
Isotope Ratio Mass Spectrometry (IRMS) The Panorama Mat 253-Ultra Eiler Group (Caltech) Young Group (UCLA) Limitations of IRMS Measurements Difficult to differentiate 13CH3D and 12CH2D2 Long averaging time in order to reach < 1‰ precision High cost and large size Isotopologue Precision (‰) Time Average 13CH3D 0.43 4 hours 13CH3D + 12CH2D2 0.3 Isotopologue Precision (‰) Time Average 13CH3D 0.2 26 hours 12CH2D2 0.7 Courtesy of the John Eiler Group

4 Current State of Clumped Isotope Methane Measurements
Tunable Infrared Laser Direct Absorption Spectroscopy (TILDAS) Measure abundance of 13CH3D Astigmatic Herriott Cell 0.2‰ precision with 0.42 mmol of pure methane. Limitations of TILDAS Measurements Can only measure 13CH3D Requires large amount of sample S. Ono, et al. Anal. Chem., 2014, 86 (13),

5 Goals and Difficulties
Measure abundance of 12CH2D2 to less than 1‰ precision. Difficulties: Small abundance Large interferences from higher abundant isotopologues Hard to standardize

6 Mid-IR FS-CRDS Spectrometer Tuning Range (2200 cm-1 – 2300 cm-1)
L ~ 150cm 4.5 μm QCL Tuning Range (2200 cm-1 – 2300 cm-1) InSb Detector PZT AOM Avalanche Detector FS-HeNe λ/4 125 MHz Si Detector λ/2 Polarizer EOM Servo

7 Mid-IR FS-CRDS Spectrometer
For 12CH2D2 detection at ~ 2268 cm-1: δτ/τ ~ 0.2 % αmin ~ 4.7 × cm-1 Data acquisition rate ~ 50 Hz NEA ~ × 10-9 cm-1Hz-1/2

8 Mid-IR Methane Lineshapes
12CH3D Pressure: 20 Torr Pure Methane Natural Abundance Line Center: cm-1 E” = cm-1

9 Mid-IR Methane Lineshapes
12CH3D Pure Methane Natural Abundance Center: cm-1 E” = cm-1

10 12CH2D2 Abundance Measurements
Goal: Measure δ12CH2D2 [12CH2D2]/[12CH4] Very low Abundance Unassigned line strength Difficult to standardize [12CH3D]/[12CH4] Can be easily measured [12CH2D2] [12CH2D2]/[12CH3D] Higher Abundance Assigned line strength Can be calibrated with IRMS Measurements [12CH3D]

11 Spectra of Methane Isotopologues
Simulation Conditions: 1 Torr Pure Methane HITRAN 2012 Kitt Peak Data: Courtesy of JPL High Resolution Spectroscopy Group (Keeyoon Sung, Linda Brown)

12 Line Selections for [12CH2D2]/[12CH3D] Measurements
HITRAN Simulation Conditions: 1 Torr Pure Methane Kitt Peak Line Intensities Unassigned. HITRAN 2012 Kitt Peak Data: Courtesy of JPL High Resolution Spectroscopy Group (Keeyoon Sung, Linda Brown)

13 Pure Methane 12CH3D and 12CH2D2 Measurements
Pressure: 5 Torr Pure Methane Natural Abundance 12CH3D Line Center: cm-1 E” = 58.8 cm-1 With known line strength, [12CH3D] can be derived. Galatry Profile Fit SNR = 300:1

14 Pure Methane 12CH3D and 12CH2D2 Measurements
Pressure: 5 Torr Pure Methane Natural Abundance Unassigned 12CH2D2 Line Identified from Kitt Peak FTIR Data Line Center: cm-1 Galatry Profile Fit SNR = 85:1

15 Natural Abundant 12CH2D2 Measurement
Total Average Time: 1.5 Hours Comparable to 26 hours of averaging on IRMS.

16 Future Work What we need to reach [12CH2D2]/[12CH4] measurement?
Calibrate 12CH3D abundance measurement with IRMS Calibrate 12CH2D2 abundance measurement using an equilibrated pure methane sample with known isotope abundances. What we need to reach δ12CH2D2 measurements? Improve sample input system to avoid fractionation. Calibrate δ12CH3D and δ13CH3D measurements with IRMS.

17 Acknowledgement Funding:
Student Fellowships: Linhan Shen and Thinh Q. Bui are both supported by NASA NESSF fellowship. Support: David Long for providing us ringdown mirrors JPL high resolution spectroscopy group for providing us FTIR spectra of 13CH3D and 12CH2D2.


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