Wintertime Overnight NOx Removal in a Southeastern United States Coal‐fired Power Plant Plume: A Model for Understanding Winter NOx Processing and its Implications.
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| Title: | Wintertime Overnight NO |
|---|---|
| Authors: | Fibiger, Dorothy L.1,2, McDuffie, Erin E.1,3, Dubé, William P.1,2, Aikin, Kenneth C.1,2, Lopez‐Hilfiker, Felipe D.4, Lee, Ben H.4, Green, Jaime R.5, Fiddler, Marc N.5, Holloway, John S.1, Ebben, Carlena6, Sparks, Tamara L.6, Wooldridge, Paul6,7, Weinheimer, Andrew J.8, Montzka, Denise D.8, Apel, Eric C.8, Hornbrook, Rebecca S.8, Hills, Alan J.8, Blake, Nicola J.9, DiGangi, Josh P.10, Wolfe, Glenn M.10,11 |
| Source: | Journal of Geophysical Research. Atmospheres. Jan2018, Vol. 123 Issue 2, p1412-1425. 14p. |
| Abstract: | Abstract: Nitric oxide (NO) is emitted in large quantities from coal‐burning power plants. During the day, the plumes from these sources are efficiently mixed into the boundary layer, while at night, they may remain concentrated due to limited vertical mixing during which they undergo horizontal fanning. At night, the degree to which NO is converted to HNO3 and therefore unable to participate in next‐day ozone (O3) formation depends on the mixing rate of the plume, the composition of power plant emissions, and the composition of the background atmosphere. In this study, we use observed plume intercepts from the Wintertime INvestigation of Transport, Emissions and Reactivity campaign to test sensitivity of overnight NOx removal to the N2O5 loss rate constant, plume mixing rate, background O3, and background levels of volatile organic compounds using a 2‐D box model of power plant plume transport and chemistry. The factor that exerted the greatest control over NOx removal was the loss rate constant of N2O5. At the lowest observed N2O5 loss rate constant, no other combination of conditions converts more than 10% of the initial NOx to HNO3. The other factors did not influence NOx removal to the same degree. [ABSTRACT FROM AUTHOR] |
| Copyright of Journal of Geophysical Research. Atmospheres is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.) | |
| Database: | GreenFILE |
| FullText | Text: Availability: 0 |
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| Header | DbId: 8gh DbLabel: GreenFILE An: 128109420 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: Wintertime Overnight NO<subscript><italic>x</italic></subscript> Removal in a Southeastern United States Coal‐fired Power Plant Plume: A Model for Understanding Winter NO<subscript><italic>x</italic></subscript> Processing and its Implications. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Fibiger%2C+Dorothy+L%2E%22">Fibiger, Dorothy L.</searchLink><relatesTo>1,2</relatesTo><br /><searchLink fieldCode="AR" term="%22McDuffie%2C+Erin+E%2E%22">McDuffie, Erin E.</searchLink><relatesTo>1,3</relatesTo><br /><searchLink fieldCode="AR" term="%22Dubé%2C+William+P%2E%22">Dubé, William P.</searchLink><relatesTo>1,2</relatesTo><br /><searchLink fieldCode="AR" term="%22Aikin%2C+Kenneth+C%2E%22">Aikin, Kenneth C.</searchLink><relatesTo>1,2</relatesTo><br /><searchLink fieldCode="AR" term="%22Lopez‐Hilfiker%2C+Felipe+D%2E%22">Lopez‐Hilfiker, Felipe D.</searchLink><relatesTo>4</relatesTo><br /><searchLink fieldCode="AR" term="%22Lee%2C+Ben+H%2E%22">Lee, Ben H.</searchLink><relatesTo>4</relatesTo><br /><searchLink fieldCode="AR" term="%22Green%2C+Jaime+R%2E%22">Green, Jaime R.</searchLink><relatesTo>5</relatesTo><br /><searchLink fieldCode="AR" term="%22Fiddler%2C+Marc+N%2E%22">Fiddler, Marc N.</searchLink><relatesTo>5</relatesTo><br /><searchLink fieldCode="AR" term="%22Holloway%2C+John+S%2E%22">Holloway, John S.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Ebben%2C+Carlena%22">Ebben, Carlena</searchLink><relatesTo>6</relatesTo><br /><searchLink fieldCode="AR" term="%22Sparks%2C+Tamara+L%2E%22">Sparks, Tamara L.</searchLink><relatesTo>6</relatesTo><br /><searchLink fieldCode="AR" term="%22Wooldridge%2C+Paul%22">Wooldridge, Paul</searchLink><relatesTo>6,7</relatesTo><br /><searchLink fieldCode="AR" term="%22Weinheimer%2C+Andrew+J%2E%22">Weinheimer, Andrew J.</searchLink><relatesTo>8</relatesTo><br /><searchLink fieldCode="AR" term="%22Montzka%2C+Denise+D%2E%22">Montzka, Denise D.</searchLink><relatesTo>8</relatesTo><br /><searchLink fieldCode="AR" term="%22Apel%2C+Eric+C%2E%22">Apel, Eric C.</searchLink><relatesTo>8</relatesTo><br /><searchLink fieldCode="AR" term="%22Hornbrook%2C+Rebecca+S%2E%22">Hornbrook, Rebecca S.</searchLink><relatesTo>8</relatesTo><br /><searchLink fieldCode="AR" term="%22Hills%2C+Alan+J%2E%22">Hills, Alan J.</searchLink><relatesTo>8</relatesTo><br /><searchLink fieldCode="AR" term="%22Blake%2C+Nicola+J%2E%22">Blake, Nicola J.</searchLink><relatesTo>9</relatesTo><br /><searchLink fieldCode="AR" term="%22DiGangi%2C+Josh+P%2E%22">DiGangi, Josh P.</searchLink><relatesTo>10</relatesTo><br /><searchLink fieldCode="AR" term="%22Wolfe%2C+Glenn+M%2E%22">Wolfe, Glenn M.</searchLink><relatesTo>10,11</relatesTo> – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Journal+of+Geophysical+Research%2E+Atmospheres%22">Journal of Geophysical Research. Atmospheres</searchLink>. Jan2018, Vol. 123 Issue 2, p1412-1425. 14p. – Name: Abstract Label: Abstract Group: Ab Data: Abstract: Nitric oxide (NO) is emitted in large quantities from coal‐burning power plants. During the day, the plumes from these sources are efficiently mixed into the boundary layer, while at night, they may remain concentrated due to limited vertical mixing during which they undergo horizontal fanning. At night, the degree to which NO is converted to HNO3 and therefore unable to participate in next‐day ozone (O3) formation depends on the mixing rate of the plume, the composition of power plant emissions, and the composition of the background atmosphere. In this study, we use observed plume intercepts from the Wintertime INvestigation of Transport, Emissions and Reactivity campaign to test sensitivity of overnight NOx removal to the N2O5 loss rate constant, plume mixing rate, background O3, and background levels of volatile organic compounds using a 2‐D box model of power plant plume transport and chemistry. The factor that exerted the greatest control over NOx removal was the loss rate constant of N2O5. At the lowest observed N2O5 loss rate constant, no other combination of conditions converts more than 10% of the initial NOx to HNO3. The other factors did not influence NOx removal to the same degree. [ABSTRACT FROM AUTHOR] – Name: AbstractSuppliedCopyright Label: Group: Ab Data: <i>Copyright of Journal of Geophysical Research. Atmospheres is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.) |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1002/2017JD027768 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 14 StartPage: 1412 Titles: – TitleFull: Wintertime Overnight NO<italic>x</italic> Removal in a Southeastern United States Coal‐fired Power Plant Plume: A Model for Understanding Winter NO<italic>x</italic> Processing and its Implications. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Fibiger, Dorothy L. – PersonEntity: Name: NameFull: McDuffie, Erin E. – PersonEntity: Name: NameFull: Dubé, William P. – PersonEntity: Name: NameFull: Aikin, Kenneth C. – PersonEntity: Name: NameFull: Lopez‐Hilfiker, Felipe D. – PersonEntity: Name: NameFull: Lee, Ben H. – PersonEntity: Name: NameFull: Green, Jaime R. – PersonEntity: Name: NameFull: Fiddler, Marc N. – PersonEntity: Name: NameFull: Holloway, John S. – PersonEntity: Name: NameFull: Ebben, Carlena – PersonEntity: Name: NameFull: Sparks, Tamara L. – PersonEntity: Name: NameFull: Wooldridge, Paul – PersonEntity: Name: NameFull: Weinheimer, Andrew J. – PersonEntity: Name: NameFull: Montzka, Denise D. – PersonEntity: Name: NameFull: Apel, Eric C. – PersonEntity: Name: NameFull: Hornbrook, Rebecca S. – PersonEntity: Name: NameFull: Hills, Alan J. – PersonEntity: Name: NameFull: Blake, Nicola J. – PersonEntity: Name: NameFull: DiGangi, Josh P. – PersonEntity: Name: NameFull: Wolfe, Glenn M. IsPartOfRelationships: – BibEntity: Dates: – D: 27 M: 01 Text: Jan2018 Type: published Y: 2018 Identifiers: – Type: issn-print Value: 2169897X Numbering: – Type: volume Value: 123 – Type: issue Value: 2 Titles: – TitleFull: Journal of Geophysical Research. Atmospheres Type: main |
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