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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
1

The mechanism of the oxygen airglow

Stott, Ian Peter January 1987 (has links)
It is well known that the atmosphere of the earth emits a glow throughout the night. The major contribution to this nightglow was first observed in 1901 and was later shown to be due to the transition: O(<SUP>1</SUP>S) → O(^1D) +<i>hv</i>. After many years of controversy, the accepted method for the production of the O(^1S) at a height around 100 km is the Barth mechanism: O(<SUP>3P) + O(<SUP>3P) + M →O <SUP>ast<SUB>2 + M </SUB></SUP>O<SUP>ast<SUB>2 + O(<SUP>3P) →O<SUB>2 + O(<SUP>1S)</SUB></SUP> Where O^ast_2 represents an excited species of oxygen. The precursor can be any of four possible states: O_2(<i>A</i>^3 Σ+_u), O_2(<i>c</i>^1Σ-_u), O_2(<i>A'</i>^3Δu) and O_2(^5πg). All of these states have been proposed as the O(^1S) precursor at one time or another, but none conclusively. For a long time it has been realised that atmospheric measurements of O(^1S), its possible precursors and other relevant species, needs to be taken simultaneously. However up to now this has not been achieved in the laboratory. In the work described here, O(^1S) and the three precursors O_2(<i>A</i>^3Σ+_u), O_2(<i>A'</i>^3Δu) and O_2(<i>c</i>^1Σ-_u) were observed in a laboratory fast flow system. A new method is described whereby upon the addition of a quencher to the system each species can be tested to see if it could be acting as the Barth precursor to O(^1S). Three different quenchers were added in turn; CO_2, SF_6 and O_2. The results gained lead to the conclusion that O_2(<i>c</i>^1Σ-_u), O_2(<i>A'</i>^3Δu) and O_2(<i>A</i>^3Σ+_u)(vleq4) cannot be acting as a O(^1S) precursor, and that O_2(<i>A</i>^3Σ+_u)(vgeq5) is able to do so. The absolute concentrations of O_2(A^3Σ+_u), O(^1S) and O(^3P) were measured and the results compared with the values of these quantities found at a height of 97 km in the earths atmosphere. This comparison shows that O_2(<i>A</i>^3Σ+_u)(vgeq5) can account for all the O(^1S) production at that height at night. The thesis concludes with a discussion of the application of the same method to the determination of the precursors for some of the excited species of O_2.

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