This paper describes the experimental results for negative ion mobility in O2 at 0.5–2.0 atm. The ion mobility is observed using a high-pressure ion drift tube with a positive corona gap (Geiger counter), which is constructed from a point plate gap and acts as a negative ion detector. The variation of waveforms in the burst pulse is observed by varying the voltage applied to the ion detector to find the optimum voltage that must be applied across the ion detector in O2. This is investigated carefully to ensure the precise determination of mobility. The distortion of the electric field near the mesh electrode, which operates as the cathode of the ion detector and as the anode of the ion drift gap, is then examined to determine the optimum applied voltage to suppress its effect on the measurement of mobility. The mobility is subsequently measured at a reduced electric field intensity of 2.83 × 10−3 to 2.83. The observed mobility of 2.31 ± 0.03 cm2 V−1 s−1 in O2 is concluded to be that of . This value is also obtained in experiments over a wide range of gas pressures (0.5–2.0 atm) and drift lengths (1.00–9.00 cm). The mobilities of and O− are also obtained experimentally.
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