A zero-dimensional model is used to study the processes of physical and chemical reactions in atmospheric plasma with different ionization degrees near the ground(0 km). The temporal evolutions of CO, CO2and other main reactants(namely OH and O2), which affect the conversion of CO and CO2, are obtained for afterglow plasma with different initial values. The results show that the consumption rate of CO is largest when the initial electron number density ne0=1012cm-3, i.e. the ionization degree is 0.000004%. The number density of CO2is relatively small when ne0=1016cm-3, i.e. the ionization degree is 0.04%, whereas they are very close under the condition of other ionization degrees. Considering the total number densities of CO and CO2and the consumption rate of CO comprehensively, the best condition is ne0=1013cm-3, i.e. the ionization degree is 0.00004% for reducing the densities of CO and CO2in the atmospheric plasma.The temporal evolutions of N+, Ar+, CO+and CO+2are also shown, and the influences on the temporal evolutions of CO and CO2are analyzed with increasing ionization degree.
A zero-dimensional model is used to study the processes of physical and chemical reactions in atmospheric plasma with different ionization degrees near the ground (0 km). The temporal evolutions of CO, C02 and other main reactants (namely OH and O2), which affect the conversion of CO and C02, are obtained for afterglow plasma with different initial values. The results show that the consumption rate of CO is largest when the initiM electron number density neo=1012 cm-3, i.e. the ionization degree is 0.000004%. The number density of CO2 is relatively small when neo=1016 cm-3, i.e. the ionization degree is 0.04%, whereas they are very close under the condition of other ionization degrees. Considering the total number densities of CO and C02 and the consumption rate of CO comprehensively, the best condition is neo=1013 cm-3, i.e. the ionization degree is 0.00004% for reducing the densities of CO and CO2 in the atmospheric plasma. The temporal evolutions of N+, Ar+, CO+ and CO+ are also shown, and the influences on the temporal evolutions of CO and C02 are analyzed with increasing ionization degree.