1 AOSC 634 Air Sampling and Analysis Lesson Cavity Ring Down Spectroscopy A source of terrific sensitivity. Copyright Dickerson 2015 Quick Review How lasers work Light Amplification by Stimulated Emission of Radiation. Generate light with great spatial and spectral coherence. Produce tight pattern over distance Narrow wavelength interval. Requires: A population inversion Resonant optical cavity to generate a standing wave. How lasers work A gain medium must be pumped into an inversion inside a resonant cavity. The medium could be Solid Nd-YAG, (Yttrium Aluminum Garnet) or ruby. Liquid such as a dye Gas such as a mixture of He and Ne or N2 and CO2. Pumping can be supplied by a flash lamp, electrical discharge, or chemical reaction. The resonant cavity is usually a highly (99.9%) reflective and a semi reflective (99%) mirror. Example: He-Ne laser • A mixture of He and Ne (10:1 at ~1 hPa) is exposed to a high voltage, low current electric field (think neon sign). • The electric field generates a plasma, mostly of excited He atoms. • The excited He atoms collide with Ne and transfer their energy. • The excited Ne atoms relax to the ground state, emitting light. How lasers work In the plasma, He is excited to the metastable 21S0 state that just happens to have the same energy as Ne with an electron in the 5s orbital. The population of excited states exceeds that of the ground state, forming an inversion. The transition from 5s to 3p is rapid and is accompanied by emission of 633 nm (red) light. 6 A pair of mirrors provides the optical cavity. A standing wave is formed. 7 8 Cavity ringdown uses a laser and a laser cavity. Effective path lengths of km’s are possible. Example: NO2 9 CRDS Method 11 1 N c o t I (t ) I o exp o t I (t ) I o exp 10 Chemiluminescence is the Customary Method to Measure NOx or NOY A. 375oC Mo Catalyst – Actually measures NOy – Widely used in NOx monitoring networks – 50 pptv/2 min detection limit – 10% uncertainty B. – – – Zero Air Photolysis Specific to NO2 LEDs impart little heat Conversion efficiency <100% Cooled PMT NO + O3 NO2 + O3 O3 O3 O3 O3 NO2 NO Sample Air Exhaust 11 Variety of Methods to Measure NO2 DOAS3 TDLAS4 A specific, reliable, fast, economical method for monitoring NO2 in rural and urban environments is 1 MIESR needed LIF2 12 CRDS Method • Empty Cavity: • R = mirror reflectivity • l = length of the cavity • K = coefficient of miscellaneous scattering or absorption dI c t I [(1 R ) K ] I (t ) I o exp( ) dt l 0 • Cavity with Analyte: dI c I [(1 R ) Nl K ] dt l t I (t ) I o exp( ) 11 1 N c o 13 Los Gatos NO2 CRDS instrument. Laser out Mirror Cavity Mirror Detector Inlet Outlet Laser 30 cm Inlet Pressure Controller 14 NO2 Molecule Absorption5 Cross Section [cm2 molecule-1] SO2 3x10-24 PAN 5x10-21 O3 2x10-23 H2 O 1x10-25 Kirsme et al., JGR (1997) • Single wavelength diode 405 nm laser – Technique is insensitive to lamp fluctuations • Highly reflective, low curvature mirrors result in ~ 1 km path-lengths – Highly sensitive 15 Before the instrument is reliable: • Characterize Instrument – – – – Drift Zero Calibration Response Time • Modify Instrument for increased sensitivity – Remove interferences: Water, Particles – Establish a background: τo • Compare to chemiluminescence 16 Modifications: Chemical zero. • FeSO4 – Cheap – Drawback: powder, H2O sensitive • Metal oxide O3 Scrubber – Efficient and already in easy to install casing – Proprietary mixture of metal oxides 17 Gas Phase Titration Calibration GPT: Mixed a small flow of NO-in-Nitrogen with excess ozone Calculated [NO2] from: • Monitored change in ozone (equal to [NO2]) • From standard dilution flow rates. 18 Summary of Performance Statistics Detection Response Power Limit Time Draw Internal Dimensions Pressure Weight NO2 to NO [pptv] [s] [W] [torr] WxHxD [cm] [kg] CRDS Analyzer 60 (60 s) 18 (95%) 90 170 42.5 x 21.9 x 58.4 16 NOAA Chemiluminescence 100 (60 s) 3 (95%) 1000 30 42 x 33 x 58.4 ~30 Photolysis Thermo Electron Corp. Model 42i TL 50 (120 s) 60 300 200-450 42.5 x 21.9 x 58.4 25 Hot Mo The fixed internal pressure, low power draw, and compact size of the CRDS instrument makes it ideal for aircraft use at altitudes up to ~10 km. 19 Intercomparison Study • Measured alongside the NOAA chemiluminescence device from January 516, 2009 outside the UMD laboratory window – Sampling next to parking lot close to car exhaust (very dirty!) – Calibrated both instruments every other day using GPT 20 NO NO2 by Chemi. NO2 by CRDS 21 y = 0.96x + 0.28 y = 0.93x - 0.61 R = 0.995 R = 0.982 22 • Fluctuations in the power supply resulted in variations in the pumping speed, and instrument sensitivity • Sharp increase in CRDS noise associated with particles entering the cavity 23 References • Modification of a Commercial Cavity Ring-Down Spectroscopic NO2 Detector for Enhanced Sensitivity, P. Castellanos, W. T. Luke, P. J. Kelley, J. W. Stehr, S. H. Ehrman, and R. R. Dickerson, Rev. Sci. Instrum., 80(11), DOI: 10.1063/1.3244090, 2009. • Evaluation of the use of a commercially available cavity ringdown absorption spectrometer for measuring NO2 in flight, and observations over the Mid-Atlantic States during DISCOVER-AQ, L.C. Brent, W.J. Thorn, M. Gupta, B. Leen, J.W. Stehr, H. He, H.L. Arkinson, A. Weinheimer, C. Garland, S.E. Pusede, P.J. Wooldridge, R.C. Cohen, R.R. Dickerson, J. Atmos. Chem., DOI 10.1007/s10874-013-9265-6, 2013. • High-accuracy continuous airborne measurements of greenhouse gases (CO2 and CH4) using the cavity ring-down spectroscopy (CRDS) technique, Chen, H.; Winderlich, J.; Gerbig, C.; et al. ATMOSPHERIC MEASUREMENT TECHNIQUES Volume: 3 Issue: 2 Pages: 375-386, 2010. 24 PICARRO G2401 Picarro GHG analyzer CRDS Analyzer CO2IR + laser CO + CH4 + H2O • Near The world’s only field-deployable analyzer capable of • 0.25 m cell with pathtrace length measuring the four main atmospheric gases simultaneously and continuously. up to 20 km. • Wavelength scanning for selectivity. • Ringdown time is independent of laser intensity. • Precision in ppb range. • Global #1 in precision, accuracy, and portability • Capable of meeting WMO Data Quality Objectives for CO, CO2 & CH4 • Guaranteed lowest drift of any continuous greenhouse gas measurement instrument • Unique water correction automatically reports dry gas mol fraction Meeting the WMO Standard: The World Meteorological Organization has published exact requirements on the precision of greenhouse gas and carbon monoxide measurements made at its Global Atmosphere Watch (GAW) stations and the G2401 provides the level of precision needed to meet these standards. The unique combination of continuous 4species measurement, high precision, field deployability, and long-term reliability makes the G2401 the instrument of choice for greenhouse gas measurements. Picarro’s Patented CRDS Technology: The heart of 25 Picarro CO2 Detector 26 27 • Wavelength is scanned to measure ringdown time on and off absorption peaks. • Temperature, pressure, and water vapor are monitored for correction. • Advertised uncertainty 0.050 ppm (out of 400). • Outstanding stability and sensitivity – at a price.