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![GC-MS analysis of reaction products in nitrogen and methane GC-MS analysis of reaction products in nitrogen and methane](https://pdfprof.com/Listes/18/13488-18367.pdf.pdf.jpg)
2Department of Experimental Physics, Comenius University, Mlynska dolina F-2, 842 48 Bratislava, Slovakia
3Department of Physics and Astronomy, Open University, Walton Hall, Milton Keynes MK7 6AA, UK
4Planetary and Space Sciences Research Institute, Open University, Walton Hall, Milton Keynes MK7 6AA, UK
Abstract: Recent space missions have revolutionized our knowledge of planetary atmospheres in the solar system, most notably those of Mars and Titan. Simultaneously laboratory plasmas have been used to mimic the physical and chemical processes within such planetary atmospheres both to benchmark physico-chemical models and to interpret observations e.g. by providing plausible candidates for both spectral and mass spectrometric studies. In this paper we report the products formed in a gliding arc discharge fed by a 2 or 5% N2-CH4 gas mixture which mimics Titan"s atmosphere. Gas samples from the
discharge exhaust were analyzed by GC-MS. Acetylene, hydrogen cyanide, and acetonitrile were found to be the major products. Minor detected products were: ethane, ethene, cyanogen, propene, propane, propyne, 1,2-propadiene, 1-butene-3-yne, 1,3-butadiene, 1,3-butadiyne, 2-propenenitrile, 2-propanenitril, 2-
methylpropanenitrile, 2-methylpropanenitrile, benzene, and toluene. Whilst many of these compounds have been predicted and/or observed in Titan atmosphere the present plasma experiments provides evidence both of the chemical complexity of Titan and the mechanisms by which larger species grow prior to forming the dust that covers much of Titan"s surface Keywords: reaction nitrogen-methane gas mixture, gliding arc discharge, cold trap, Gas Chromatography-Mass Spectrometry.1. Introduction
Titan is the largest moon in Saturn"s lunar system and has been a subject of interest to astronomers and planetary scientists for a long time because the atmospheric conditions are thought to have resembled those conditions on the Earth several billion years ago [1]. Its atmospheric composition is principally nitrogen with 2-6 % of methane and some other gases that could be generated at low power discharges in the methane clouds [1]. The most important minor compounds detected by Cassini-Huygens space mission are nitriles (HCN, HC3N, HC5N, C2N2) believed to be formed as a
result of dissociation of nitrogen and methane either by solar induced photolysis or by electron impact [2] and hydrocarbons (C2H2, C2H4, C2H6, C3H8, C3H4
[2]). In order to understand the physical and chemical processes leading to such observed phenomena additional laboratory simulations are required. Discharges have been shown to be good mimics of planetary atmospheres providing insights into both physical and chemical processes. DBD, glow, microwave, RF and corona discharges [3-11], have been all used in order to study electron-molecule and
ion-molecule reactions in planetary atmospheres. In particular in recent years several of these discharges have been used to mimic Titan"s atmosphere and shown that various complex compounds can be formed, for example the higher hydrocarbons, nitriles or even amino acids. This paper presents the results of organic synthesis in a Titan like atmosphere operated in a Gliding Arc Discharge (GAD). We observe the production of C6 to C9hydrocarbons from methane in the discharge. To understand the molecular kinetics during the discharge, the energy distribution as well as knowledge of plasma composition is necessary. In this paper we provide our results of a qualitative
and quantitative GC-MS analysis of gliding arc discharges fed by a CH4 - N2 gas mixture.
2. Experiment
The apparatus used in our experiments is shown schematically in Figure 1. The flow rates through the reactor for both CH4 and N2 were regulated using
MKS mass flow controllers. The measurements were
carried out in a flow regime over a range from 100 and 200 ml min -1 at atmospheric pressure and laboratory temperature. The discharge electrode system had the standard configuration of a classical gliding arc. A pair of stainless steel holders was positioned in parallel to the iron electrodes, but in this case the plasma was not gliding due to the low flow rate. Astable abnormal glow plasma occurred between the electrodes at their shortest distance of2 mm, and a plasma channel with diameter of 1 mm
was formed. The electrical parameters were measured by a Tektronix oscilloscope using high voltage probe and Rogowsky current probe. The reactor chamber had a volume of 0.3 L. The discharge was powered by a DC HV source. The discharge was ignited at 5500 V, then voltage drop reached a value at about 400 V but with increasing current (between 15 and 40 mA) the voltage was found to slightly decrease from 400 to 350 V. The present experiments were performed for different N2:CH4 ratios in range from 2 % and 5 % methane in
nitrogen. Gaseous samples of the products formed in the discharge were taken out for GC-MS analysis through a gas outlet into a cold trap. The cold trap was subsequently heated and the resultant gas sample for GC-MS analysis was taken using a lock syringe before being immediately analyzed usingGas Chromatography and Mass spectrometry. GC-
MS analysis was carried out using an AgilentTechnologies 6890 gas chromatograph coupled to a 5973 mass spectrometer. Separation was performed on a J&W GS-Q PLOT column (30 m in length, 0.32 mm internal diameter). Helium with a column flow rate of 2 sccm was used as the carrier gas. Injection was at a 5:1 split and injector temperature
was 220 °C. The GC oven temperature was held for