Transient Spark Discharge and Ozone-Driven Nitrogen Fixation to Water
| dc.bibliographicCitation.firstPage | 1741 | |
| dc.bibliographicCitation.issue | 6 | |
| dc.bibliographicCitation.journalTitle | Plasma Chemistry and Plasma Processing | |
| dc.bibliographicCitation.lastPage | 1762 | |
| dc.bibliographicCitation.volume | 45 | |
| dc.contributor.author | Pareek, Pankaj | |
| dc.contributor.author | Selvaraj, Gokul | |
| dc.contributor.author | Hensel, Karol | |
| dc.contributor.author | Janda, Mário | |
| dc.date.accessioned | 2026-02-26T12:44:55Z | |
| dc.date.available | 2026-02-26T12:44:55Z | |
| dc.date.issued | 2025 | |
| dc.description.abstract | Fixation 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.version | publishedVersion | eng |
| dc.identifier.uri | https://oa.tib.eu/renate/handle/123456789/31502 | |
| dc.identifier.uri | https://doi.org/10.34657/30571 | |
| dc.language.iso | eng | |
| dc.publisher | Dordrecht : Springer Science + Business Media B.V. | |
| dc.relation.doi | https://doi.org/10.1007/s11090-025-10604-w | |
| dc.relation.essn | 1572-8986 | |
| dc.relation.issn | 0272-4324 | |
| dc.rights.license | CC BY 4.0 Unported | |
| dc.rights.uri | https://creativecommons.org/licenses/by/4.0 | |
| dc.subject.ddc | 540 | |
| dc.subject.other | In-situ UV/Vis absorption spectroscopy | eng |
| dc.subject.other | Nitrogen fixation | eng |
| dc.subject.other | Ozone | eng |
| dc.subject.other | Transient spark | eng |
| dc.subject.other | LTP research | eng |
| dc.title | Transient Spark Discharge and Ozone-Driven Nitrogen Fixation to Water | eng |
| dc.type | Article | |
| tib.accessRights | openAccess |
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