Production of Perchlorate by Laboratory Simulated Lightning Process
2012
Rao, Balaji | Mohan, Suhas | Neuber, Andreas | Jackson, William Andrew
Perchlorate (ClO 4 â ), a thyroid hormone disruptor, is both naturally occurring and a man-made contaminant increasingly found in a variety of terrestrial environments. The environmental presence of ClO 4 â is considered to be the result of atmospheric formation and deposition processes. The ultimate processes, particularly heterogeneous-based reactions, leading to natural ClO 4 â formation are not well understood. Oxidation of chlorine species by an energetic source such as lightning is considered to be one of the potential heterogeneous sources of natural ClO 4 â . Currently, there is very little information available on lightning-induced ClO 4 â . We designed a laboratory electrical discharge reactor capable of evaluating ClO 4 â formation by the oxidation of âdryâ sodium chloride (NaCl) aerosols (relative humidity (RH) <70%) in electrical discharge plasma at voltages and energies up to 24 kV and 21 kJ, respectively. Similar to other non-electrochemical ClO 4 â production processes, the amount of ClO 4 â produced (0.5â4.8 μg) was 3 orders of magnitude lower than the input Clâ (7.1â60.1 mg). The amount of ClO 4 â generated increased with peak voltage (V) and theoretical maximum discharge energy with ÎClO 4 â /ÎVâ=â0.28âÃâ10â3 μg Vâ1 (R 2â=â0.94) and ÎClO 4 â /ÎEâ=â0.44âÃâ10â3 μg Jâ1 (R 2â=â0.83). The total ClO 4 â generated decreased with an increase in relative humidity from 2.8â±â0.1 μg (RHââ¼46%) to 0.9â±â0.1 μg (RHââ¼62%) indicating that the presence of moisture inhibits the formation of ClO 4 â . Additional modifications to the reactor support the hypothesis of ClO 4 â formation due to the action of plasma on Clâ aerosols as opposed to direct oxidation on the surface of the electrodes. Finally, the contribution of lightning-induced ClO 4 â in North America is calculated to have a wide range from 0.006âÃâ105 to 5âÃâ105 kg/year and is within the range of the measured ClO 4 â depositional flux in precipitation samples obtained across the USA (0.09âÃâ105â1.2âÃâ105 kg/y).
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