1978
DOI: 10.1016/0301-0104(78)80033-0
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Dissociation patterns in N2O following electron impact

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Cited by 26 publications
(12 citation statements)
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“…Because of their long lifetimes, single particle detection of most metastable species is very difficult in the laboratory. Various attempts to detect oxygen metastables such as using Auger emission from a low work function surface (Gilpin andWelge 1971, Allcock andMcConkey 1978), using a chemi-ionization process (Stone et al 1976) or by detection of inelastically scattered electrons, all suffered from a lack of discrimination against other atomic or molecular species in addition to not being particularly sensitive. More recently laser or synchrotron-based techniques such as REMPI or VUV ionization have been used to monitor the production of specific fragments (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…Because of their long lifetimes, single particle detection of most metastable species is very difficult in the laboratory. Various attempts to detect oxygen metastables such as using Auger emission from a low work function surface (Gilpin andWelge 1971, Allcock andMcConkey 1978), using a chemi-ionization process (Stone et al 1976) or by detection of inelastically scattered electrons, all suffered from a lack of discrimination against other atomic or molecular species in addition to not being particularly sensitive. More recently laser or synchrotron-based techniques such as REMPI or VUV ionization have been used to monitor the production of specific fragments (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…It plays an important role in stratospheric photochemistry, particularly with regard to ozone, and in the overall global radiation budget (e.g., [1,2]). Because it is known to produce a wide range of metastable fragments upon dissociation (see [3,4]), N 2 O can be a very active species in any discharge situation. In the ground state it has a linear, asymmetric (N-N-O) configuration with a small (0.28 D) dipole moment.…”
Section: Introductionmentioning
confidence: 99%
“…Previous attempts to detect O( 1 S) by techniques such as Auger emission from a low work function surface (Alcock and McConkey, 1978;Gilpin and Welge, 1971), by a chemi-ionization process (Stone et al, 1976), or by detection of inelastically scattered electrons, were limited by a lack of sensitivity or suffered from poor discrimination against other metastable atomic or molecular species, such as O( 5 S), or ground state O( 3 P), and generally suffered from poor signal to background ratios. Optical methods to record emissions from the low lying oxygen metastables relied on buffering the metastable atoms from the walls using rare gases such as He, as used by McLennan and Shrum (1925) in their historic experiment or by lifetime shortening through excimer formation with high pressure Kr or Xe gases (Cooper et al, 1961;Cunningham and Clark, 1974;Herman and Herman, 1950;Huestis et al, 1975;Kenty et al, 1946;Simmons et al, 1979).…”
Section: Basic Concepts 21 Relevant Backgroundmentioning
confidence: 99%