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Associate Professor, Physical Chemistry

B.S. 1991, St. John's University
Ph.D. 1996, North Dakota State University
Postdoctoral: 1996-1998, Columbia University

Email: quandt@ilstu.edu
Phone: (309)438-8576
Office: 324 Science Laboratory Building

My research entails using Cavity Ringdown (CRD) absorption spectroscopy to study the kinetics and dynamics of gas phase reactions that are important in both atmospheric and combustion chemistry.

CRD
Currently, the most commonly used methods of measuring electronic spectra of gas phase molecules are LIF and REMPI. While often quite successful for small systems, they are problematic for larger polyatomics due to dynamical processes such as internal vibrational redistribution (IVR), internal conversion (IC), and predissociation. In these cases a direct absorption measurement is preferable, but often not practical due to low sensitivity. One solution is the use of a novel multipass absorption method termed "cavity ringdown".

A CRD cell is essentially a high-quality optical cavity enclosed by a pair of highly reflective mirrors. Pulsed laser light from a Nd:YAG pumped dye laser that is injected into the cavity oscillates between the mirrors with a small amount (1-R) transmitting on each pass. If the transmitted light is monitored at the output mirror as a function of time, the decay time of the cavity can be determined. The intensity at the output mirror is given by I(t) = Ioe-t/t where t is the "ringdown" time, that is, the time for the signal to decay to 1/e of Io. If an absorbing species is placed between the cavity mirrors, the ring down time is shortened. The total round trip loss G, due to absorption, is then G = 1-e-2L/ct. A plot of G versus wavelength gives the absorption spectrum for the species of interest. The sensitivity of this technique is limited by the reflectivity of the mirrors, and the precision with which t can be determined. Under the right conditions, an effective path length of up to 70 km is possible, and absorptions with cross sections on the order of 10-28 cm2 can be seen.

HFCs and HCFCs
It has been shown conclusively that the use of chlorofluorocarbons (CFCs) as refrigerants, aerosol propellants, and etchants, in semiconductor manufacturing, has significantly contributed to stratospheric ozone destruction. (The "ozone hole") Since 1987, the search for suitable alternatives to CFCs has centered on hydrochlorofluorocarbons (HCFCs) and hydrofluorocarbons (HFCs). These compounds’ environmental acceptability stems from the fact that the presence of one or more C-H bonds allows them to be oxidized relatively quickly by OH radicals in the troposphere. This gives HCFCs and HFCs a mean atmospheric lifetime on the order of 3 to 6 months as opposed to the decade long lifetimes associated with CFCs. However, because of various atmospheric phenomenon, some of these HCFCs can reach the stratosphere. Therefore, to determine the impact of these compounds on the ozone layer detailed knowledge of the UV and VUV photochemistry of CFCs and HCFCs is needed. In our lab, we study the photodissociation dynamics of several different HCFCs. This is done by flash photolysis using an ArF excimer laser operating at 193 nm to photodissociate the species of interest, and the CRD technique to probe the energy distribution of the photoproducts.

Combustion Chemistry
Combustion of fossil fuels is the most commonly used method of energy production in the world today. Reactions of O(3P) with alkenes are key intermediate steps in the combustion chemistry of these fossil fuels. Despite the importance of these types of reactions very little work has been done on systems larger than O(3P) + C2H4. In our lab we want to measure the energy distribution of various reaction products from O(3P) reactions with alkenes, in specific we are interested in the HCO product. Due to its unique electronic structure HCO is difficult to detect using traditional techniques. However, it is relatively easy to detect using CRD.


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Illinois State University
Normal, IL  61790-4160
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Fax: (309)438-5538
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