Cavity Ring Down at Low Temperatures: Application to Atmospheric Chemistry Carlos E. Manzanares Department of Chemistry & Biochemistry Baylor University.

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Cavity Ring Down at Low Temperatures: Application to Atmospheric Chemistry Carlos E. Manzanares Department of Chemistry & Biochemistry Baylor University Waco, Texas 76798

Acknowledgements Baylor University Dr. Ernest K. LewisDr. Craig J. Moehnke Dr. Alfredo Lopez-CalvoDr. Juan G. Navea Helena Diez y RiegaYasnahir Perez Delgado Nicholas HernandezJenny Barroso David Camejo Universidad Simon Bolivar, Caracas, Venezuela: Dr. Mary C. Salazar, Dr. Antonio J. Hernandez The Robert A. Welch Foundation The Quantum Optics Initiative funded by the O.N.R., Texas A&M, and the Vice Provost for Research at Baylor University

Atmospheric Chemistry

Earth: Temperature Profile

Atmospheric Photolysis Rates

Calculated (J) for H 2 SO 4 Photolysis H 2 SO 4 + h ν -> SO 3 + H 2 O Vaida et al., Science, (2003), 299,

How to obtain σ  Experimental: Multipass ‘White’ Cell Experimental: Cavity Ring Down Theoretical: Calculations of Overtone Intensities

PS-CRD Signal

Experimental Technique

Low Temperature Cryostat

Methane

Ethylene

Integrated Cross Section

Atmospheric Photolysis Rates

Ethyl acetate

Ethyl acetate: activation energy

+ Ethyl acetate: transition state h

Titan

Titan’s Atmosphere

Summary A Cavity ring down spectrometer has been constructed to obtain high vibrational overtone spectra of molecules. Experiments at low pressures and low temperatures ( K) provide σ( ) values simulating atmospheric conditions. Low temperature ( K) quantum yields of chemical reactions are being obtained for vibrationally excited molecules under atmospheric conditions.