Atmospheric formation of NO from N 2 (A³Σ)
The reaction between N 2 (A³Σ) and O(³P) contributes to the production of O(¹S) in auroras. It is argued here that the other possible products for the reaction, NO(X²π) + N(²D, 4 S) also may be significant and have an important impact upon odd nitrogen chemistry in the auroral E‐region and perhaps e...
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| Veröffentlicht in: | Geophysical research letters 1976-06, Vol.3 (6), p.335-337 |
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| container_title | Geophysical research letters |
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| creator | Swider, William |
| description | The reaction between N
2
(A³Σ) and O(³P) contributes to the production of O(¹S) in auroras. It is argued here that the other possible products for the reaction, NO(X²π) + N(²D,
4
S) also may be significant and have an important impact upon odd nitrogen chemistry in the auroral E‐region and perhaps even the quiet daytime E‐region which is formed in part by ionization created by energetic electrons liberated by the absorption of solar X‐rays. The reaction between N
2
(A³Σ) and O
2
(X³Σ), which has been suggested as leading to N
2
O formation, is discussed. |
| doi_str_mv | 10.1029/GL003i006p00335 |
| format | Article |
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2
(A³Σ) and O(³P) contributes to the production of O(¹S) in auroras. It is argued here that the other possible products for the reaction, NO(X²π) + N(²D,
4
S) also may be significant and have an important impact upon odd nitrogen chemistry in the auroral E‐region and perhaps even the quiet daytime E‐region which is formed in part by ionization created by energetic electrons liberated by the absorption of solar X‐rays. The reaction between N
2
(A³Σ) and O
2
(X³Σ), which has been suggested as leading to N
2
O formation, is discussed.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/GL003i006p00335</identifier><language>eng</language><ispartof>Geophysical research letters, 1976-06, Vol.3 (6), p.335-337</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c865-f86e00fdef1830d726c1c684b996e937cf54d7d9728e3cc910e831d421188b043</citedby><cites>FETCH-LOGICAL-c865-f86e00fdef1830d726c1c684b996e937cf54d7d9728e3cc910e831d421188b043</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Swider, William</creatorcontrib><title>Atmospheric formation of NO from N 2 (A³Σ)</title><title>Geophysical research letters</title><description>The reaction between N
2
(A³Σ) and O(³P) contributes to the production of O(¹S) in auroras. It is argued here that the other possible products for the reaction, NO(X²π) + N(²D,
4
S) also may be significant and have an important impact upon odd nitrogen chemistry in the auroral E‐region and perhaps even the quiet daytime E‐region which is formed in part by ionization created by energetic electrons liberated by the absorption of solar X‐rays. The reaction between N
2
(A³Σ) and O
2
(X³Σ), which has been suggested as leading to N
2
O formation, is discussed.</description><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1976</creationdate><recordtype>article</recordtype><recordid>eNpdj7tOwzAYRq0KpIbC3NUjSIT-v-34MkYVFKSoXbpHqS8iFcGR3YXn4RF4Ax6AZyIIJqbzDZ-OdAhZItwhMLPaNAC8B5DjRF7NSIFGiFIDqDNSAJhpMyXn5CLnI0wf4FiQ2_o0xDw--9RbGmIaulMfX2kMdLujIcWBbimj1_Xnx9f7zSU5D91L9ld_XJD9w_1-_Vg2u83Tum5Kq2VVBi09QHA-oObgFJMWrdTiYIz0hisbKuGUM4ppz601CF5zdIIhan0AwRdk9au1KeacfGjH1A9demsR2p_W9l8r_wYKmEWW</recordid><startdate>197606</startdate><enddate>197606</enddate><creator>Swider, William</creator><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>197606</creationdate><title>Atmospheric formation of NO from N 2 (A³Σ)</title><author>Swider, William</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c865-f86e00fdef1830d726c1c684b996e937cf54d7d9728e3cc910e831d421188b043</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1976</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Swider, William</creatorcontrib><collection>CrossRef</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Swider, William</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Atmospheric formation of NO from N 2 (A³Σ)</atitle><jtitle>Geophysical research letters</jtitle><date>1976-06</date><risdate>1976</risdate><volume>3</volume><issue>6</issue><spage>335</spage><epage>337</epage><pages>335-337</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>The reaction between N
2
(A³Σ) and O(³P) contributes to the production of O(¹S) in auroras. It is argued here that the other possible products for the reaction, NO(X²π) + N(²D,
4
S) also may be significant and have an important impact upon odd nitrogen chemistry in the auroral E‐region and perhaps even the quiet daytime E‐region which is formed in part by ionization created by energetic electrons liberated by the absorption of solar X‐rays. The reaction between N
2
(A³Σ) and O
2
(X³Σ), which has been suggested as leading to N
2
O formation, is discussed.</abstract><doi>10.1029/GL003i006p00335</doi><tpages>3</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0094-8276 |
| ispartof | Geophysical research letters, 1976-06, Vol.3 (6), p.335-337 |
| issn | 0094-8276 1944-8007 |
| language | eng |
| recordid | cdi_crossref_primary_10_1029_GL003i006p00335 |
| source | Wiley Online Library Journals Frontfile Complete |
| title | Atmospheric formation of NO from N 2 (A³Σ) |
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