2015
DOI: 10.1016/j.jastp.2015.01.010
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The uptake of HNO3 on meteoric smoke analogues

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Cited by 23 publications
(26 citation statements)
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References 34 publications
(51 reference statements)
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“…Samples of the Allende (CV3) (Clarke, et al, 1971), Murchison (CM2) (Fuchs, et al, 1973) Fe(SO4)2(NH4)2 (Sigma-Aldrich) and Na4SiO4 (Alfa Aesar) (Frankland, et al, 2015). Solutions 207 immediately turn blue when Fe is present but otherwise are colourless.…”
Section: Meteoritic Materials 178mentioning
confidence: 99%
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“…Samples of the Allende (CV3) (Clarke, et al, 1971), Murchison (CM2) (Fuchs, et al, 1973) Fe(SO4)2(NH4)2 (Sigma-Aldrich) and Na4SiO4 (Alfa Aesar) (Frankland, et al, 2015). Solutions 207 immediately turn blue when Fe is present but otherwise are colourless.…”
Section: Meteoritic Materials 178mentioning
confidence: 99%
“…given system, however this large upper limit allows measurement of processes which are 492 relatively slow (Frankland, et al, 2015). The question of available surface area is also 493 pertinent in the environment, since fractal or dendritic particles are often represented as 494 spheres for reasons of computation efficiency (Saunders, et al, 2007).…”
Section: Surface Area and Morphology 473mentioning
confidence: 99%
“…Note that the laboratory measurement was made at 181 K, and the temperature dependence of could not be measured at lower temperatures using the flow tube system. Since uptake coefficients typically have negative temperature dependences (see discussion in Frankland et al (2015)), is probably higher in T below 300 km (Flasar et al, 2005), and so the rate of uptake should be a lower limit. The uptake of C2H2 was restricted to sub-monolayer coverage (i.e.…”
Section: Heterogeneous Chemical Kineticsmentioning
confidence: 99%
“…Balloon-borne mass spectrometry measurements show unexpectedly low H 2 SO 4 concentrations above 40 km (Arijs et al 1985), which can be explained if the uptake coefficient for H 2 SO 4 on MSPs is greater than 0.01 (Saunders et al 2012). Frankland et al (2015) used a laboratory measurement of the uptake coefficient of HNO 3 on MSP analogue particles to show that heterogeneous removal on MSPs in the winter polar vortex between 30 and 60 km should provide an important sink for HNO 3 . Similarly, heterogeneous uptake of the HO 2 radical on MSPs, which is sensitive to the fraction of Fe in the particles, should significantly alter the general radical chemistry of the nighttime polar vortex (James et al 2017b).…”
Section: Earthmentioning
confidence: 99%