2006
DOI: 10.1039/b518088k
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VUV spectroscopy and photo-processing of astrochemical ices: an experimental study

Abstract: In order to understand much of the chemistry that underpins astronomical phenomena (e.g. star and planet formation) it is essential to probe the physico-chemistry of ice surfaces under astronomical conditions. The physical properties and chemical reactivity of such icy surfaces depends upon its morphology. Thus it is necessary to explore how the morphology of astrochemical ices is influenced by their local environment (e.g. temperature and pressure) and the mechanisms by which they are processed. In this paper… Show more

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Cited by 107 publications
(171 citation statements)
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“…Error margins corresponding to the values in the second and third column are ±0.4 nm and ±0.03 eV. The peak positions agree with previous works, see Mason et al (2006), Lu et al (2005), and Brith & Schnepp (1965). Table 4.…”
Section: Solid Carbon Monoxidesupporting
confidence: 77%
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“…Error margins corresponding to the values in the second and third column are ±0.4 nm and ±0.03 eV. The peak positions agree with previous works, see Mason et al (2006), Lu et al (2005), and Brith & Schnepp (1965). Table 4.…”
Section: Solid Carbon Monoxidesupporting
confidence: 77%
“…Figure 3 displays the CO fourth positive band system; it is attributed to the A 1 Π ← X 1 Σ + system. Table 3 summarizes the transition, band position, and area of each feature at 8 K. We were able to observe twelve bands identified as (0, 0) to (11,0) where the (0, 0), (1, 0), and (2, 0) bands present a Davydov splitting, in agreement with Mason et al (2006), Lu et al (2005), and Brith & Schnepp (1965). Like Mason et al (2006), we were unable to observe the (12, 0) transition reported by Brith & Schnepp (1965) and Lu et al (2005), because of the low intensity Fig.…”
Section: Solid Carbon Monoxidesupporting
confidence: 67%
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“…In our experiments molecular oxygen was deposited at a pressure of 1 × 10 −7 mbar onto a cold CaF 2 window, kept at ∼25 K, for different exposure times (15, 20, 25 and 32 second) and VUV spectra were recorded. The feature peaking at 180 nm was assigned to the (O 2 ) 2 , dimer (Mason et al 2006). The band was very weak when using thin O 2 ice layers but grew in intensity with increased deposition to form a thick O 2 ice (Figure 1).…”
Section: Oxygen Dimermentioning
confidence: 99%