Gas Sensing with a 9 µm Peltier-cooled Quasi-CW Distributed Feedback Quantum Cascade Laser Damien Weidmann, Gerard Wysocki, Anatoliy Kosterev, and Frank K. Tittel Rice University, 6100 Main Street, Houston, TX, 77005, USA Thierry Aellen, Mattias Beck, Daniel Hofstetter, and Jerome Faist Université de Neuchâtel, Rue A. L. Bréguet 1, 2000 Neuchâtel, Switzerland Stéphane Blaser Alpes Laser SA, 1-3 Max.-de-Meuron, CP 1766, 2000 Neuchâtel, Switzerland
http://www.ece.rice.edu/lasersci
Towards CW Mode Operation of DFB QCLs
Direct Absorption Based Gas Sensor Architecture
SO2 and NH3 Direct Absorption Spectra
Direct Absorption Sensitivity Determination Calibrated NH3:N2 Mixture
• NH3:N2 mixture
• Pure SO2 5 torr
• Main drawbacks of QCL pulsed operation
San Francisco, California, USA May 16 – 21, 2004
• Flow configuration
Mixture NH3 in N2 1038 ± 21 ppm
Pulse to pulse intensity variation Linewidth broadening by thermal chirp Requirement of nanosecond electronics
• Retrieved concentration
• Efforts towards achieving quasi-RT CW DFB QCLs
• CW QCL Characteristics • CW QCL Structure
80 cm cavity
Quasi-CW Operation of 9.1 µm QCL In CW mode, laser threshold is close to maximum current ⇒ Hence limited wavelength tuning range • Quasi CW: Square signal
Quantum Cascade Laser Linewidth Study Study with pure SO2 at 1114.1741 cm-1
∆νobs=72 ± 7 MHz
Active zone temperature
τ = 30 µs
Wavelength tuning is ensured by self heating
Detected Signals – Wavelength Calibration
Emissions from burning fossil fuel Emissions from volcanoes Precursor of acid rains Precursor of sulfate aerosols formation
σ = 0.045 mV
• In a Gaussian lineshape approximation: ∆νobs2
= ∆νDop + 2
∆νLas2
⇒ ∆νLas = 47 MHz
• Detector noise is insignificant • Residual Etalon noise • Current source noise ⇒ Laser linewidth contribution
recognition with HITRAN 2k database
Effective tuning rate: ∆σ/∆i = 17.5 = 525 MHz/mA And ∆i = ± 0.05 mA ⇒ ∆ν = 52 MHz
• NH3 monitoring
Toxic industrial chemicals Agricultural emissions 3rd most abundant nitrogen containing compound Precursor of ammonium aerosols formation Study of possible environmental impact Study of nitrogen cycle
• Application of a 1038 ppm NH3:N2 mixture
• Demonstration of quasi CW Peltier cooled QCL operation for trace gas monitoring
⇒ Intensity noise enhancement on absorption line edge
⇒ Improvement by a factor of 3 compared to direct absorption spectroscopy
Conclusions
Noise Sources of QCL Based Gas Sensor
• Direct absolute calibration using spectral
Modulation depth 4.2 mA
1σ extrapolated sensitivity 6 ppm per meter of absorption
cm-1/A
Wavelength Modulation Spectroscopy
Quasi CW + Wavelength modulation
NH3 SO2
• SO2 monitoring
σ = 2.8×10-3
• Current applied:
Frequency 1-10 Hz with 10 to 50% duty cycle
Example: 5 Hz, 50% 5 torr SO2
HITRAN 2K survey
18 ppm per meter of absorption 1 scan, 25 ms acquisition time
• Fit based on HITRAN data and Levenberg Marquardt fitting routine
Peltier cooled operation
• Selection from
• Extrapolated 1σ sensitivity
• SNR variation due to laser power variation
Potential Target Molecules
Potential sources of discrepancy HITRAN
• Limiting noise: unexpected etalon fringes
⇒ Reduces laser threshold from 750 to 520 mA ⇒ 3 cm-1 total tuning range
T. Aellen et al., Applied Physics Letters, 83, 1929, 2003
NH3 stickiness
M. Beck et al., Science, 295, 301-305, 2002 T. Aellen et al., Applied Physics Letters, 83, 1929, 2003 A. Evans, et al., Applied Physics Letters, 84, 314, 2004 [NON DFB QCL]
9.1 µm Peltier Cooled CW DFB-QCL
1163 ppm
P = 99.4 torr L = 21”
No requirement for cryogenic cooling No need for nanosecond electronics Smaller QCL linewidths: ~ 47 MHz Compact size Etalon effects are the main limitation
• Application to SO2 for wavelength calibration • Application to NH3 detection
Direct Absorption Spectroscopy : 18 ppm.m (25 ms) Wavelength Modulation Spectroscopy : 82 ppb.m/√Hz