Transient Spark Discharge and Ozone-Driven Nitrogen Fixation to Water

dc.bibliographicCitation.firstPage1741
dc.bibliographicCitation.issue6
dc.bibliographicCitation.journalTitlePlasma Chemistry and Plasma Processing
dc.bibliographicCitation.lastPage1762
dc.bibliographicCitation.volume45
dc.contributor.authorPareek, Pankaj
dc.contributor.authorSelvaraj, Gokul
dc.contributor.authorHensel, Karol
dc.contributor.authorJanda, Mário
dc.date.accessioned2026-02-26T12:44:55Z
dc.date.available2026-02-26T12:44:55Z
dc.date.issued2025
dc.description.abstractFixation of nitrogen and the generation of plasma-activated water are currently a significant focus within the low-temperature plasma research community. This study examines the enhancement of nitrogen fixation in water, by converting the weakly soluble nitrogen oxides (NO and NO₂) generated by transient spark (TS) to highly soluble dinitrogen pentoxide (N<inf>2</inf>​O<inf>5</inf>​) and nitric acid (HNO<inf>3</inf>​) in the gas phase. This is achieved by mixing ozone (O<inf>3</inf>) with air that has been treated by a TS discharge. Without O<inf>3</inf>, only nitrite ions (NO<inf>2</inf><sup>−</sup>)​ are detected in the water, formed primarily due to reaction between solvated NO and NO<inf>2</inf>. With addition of O<inf>3</inf> (400 ppm), the composition of species in water significantly changes depending on the initial NO/O<inf>3</inf> ratio. An excess of O<inf>3</inf> enables formation of N<inf>2</inf>​O<inf>5</inf>​ and HNO<inf>3</inf>​ in the gas and a high concentration of nitrate ions (NO<inf>3</inf><sup>−</sup>​) in the water. With an excess of NO, the dominant gas phase product is NO<inf>2</inf> and a mixture of NO<inf>2</inf><sup>−</sup> and NO<inf>3</inf><sup>−</sup> is formed in the water by reaction between solvated NO<inf>2</inf> molecules. Despite the additional energy required for O<inf>3</inf>​ generation, the overall energy efficiency for the formation of NOx​<sup>−</sup> (NO<inf>2</inf><sup>−</sup>​ + NO<inf>3</inf><sup>−</sup>​) in the water increases fourfold, when enough N<inf>2</inf>O<inf>5</inf> is formed. Further improvements are possible by optimizing the use of O<inf>3</inf>​ and ensuring all N<inf>2</inf>​O<inf>5</inf>​ is captured from the gas phase.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/31502
dc.identifier.urihttps://doi.org/10.34657/30571
dc.language.isoeng
dc.publisherDordrecht : Springer Science + Business Media B.V.
dc.relation.doihttps://doi.org/10.1007/s11090-025-10604-w
dc.relation.essn1572-8986
dc.relation.issn0272-4324
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subject.ddc540
dc.subject.otherIn-situ UV/Vis absorption spectroscopyeng
dc.subject.otherNitrogen fixationeng
dc.subject.otherOzoneeng
dc.subject.otherTransient sparkeng
dc.subject.otherLTP researcheng
dc.titleTransient Spark Discharge and Ozone-Driven Nitrogen Fixation to Watereng
dc.typeArticle
tib.accessRightsopenAccess

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