Abstract Recently, electrical discharges have been identified as a potentially significant source of the atmosphere's most important oxidant, the hydroxyl radical. Measurements of hydroxyl, the closely related hydroperoxyl radical, and the nitrogen oxides from sparks and subvisible discharges were made in the laboratory under different environmental and electrical conditions representing those found in the troposphere. However, there were still several conditions not yet investigated that could impact hydroxyl and hydroperoxyl production in electrical discharges. In this study, the production of electrically generated hydroxyl and hydroperoxyl (LHOx) and nitrogen oxides (LNOx) was measured under three new conditions not tested previously, including lower pressure, different temperatures, and the presence of cloud droplet‐sized water droplets. In spark discharges, LHOxwas mostly independent of pressure, increased with increasing temperature, and was unaffected by the water droplets. LNOxgeneration was independent of temperature from −10 to 40°C and the presence of water droplets, but increased 1.5‐fold with decreasing pressure. LNOxgeneration was also found to be sensitive to changes in spark intensity and air flow in the laboratory setup. Increasing temperature also made it more likely that a discharge was visible instead of subvisible, but did not impact LHOxproduction in subvisible discharges. Even under these new conditions, the laboratory results agree with results of LHOxfrom a field campaign, demonstrating the relevance of the laboratory experiments to the atmosphere.
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gas-tight shock tube apparatus for laboratory volcanic lightning under varying atmospheric conditions
Explosive volcanic eruptions generate electrical discharges, a phenomenon termed volcanic lightning (VL). VL is increasingly well-investigated and monitored for modern eruptions, however volcanism has been active since Earth’s origin. Thus, investigating VL under different atmospheric conditions is relevant for studies of early atmospheric chemistry and potential prebiotic reactions. We developed an experimental setup to investigate VL in varying atmospheres. We present the first experiments of laboratory discharges in particle-laden jets in varying atmospheric conditions. The new experimental setup is a mobile fragmentation bomb erupting into a gas-tight particle collector tank. This setup enables the testing of different atmospheric conditions, changes in the carrier gas of the jet, changes in the pressure within the tank, monitoring of the jet behaviour, and sampling of the atmosphere together with the decompressed solid materials. We find that the number and magnitude of near-vent electrical discharge events are similar in CO2-CO and air atmospheres.
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- Award ID(s):
- 2042173
- PAR ID:
- 10538591
- Publisher / Repository:
- Presses Universitaires de Strasbourg
- Date Published:
- Journal Name:
- Volcanica
- Volume:
- 6
- Issue:
- 2
- ISSN:
- 2610-3540
- Page Range / eLocation ID:
- 437 to 445
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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