1994
DOI: 10.1016/1352-2310(94)90119-8
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Observation on great dun fell of the pathways by which oxides of nitrogen are converted to nitrate

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1994
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Cited by 17 publications
(2 citation statements)
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“…Leaitch et al (1988) studied the dissolution of N 2 O 5 in cloud droplets by using a Lagrangian chemical model with winter conditions in northeastern region of the United States and compared the resulting NO 3 − content in cloud water with measured values. They showed that the mean production rate of HNO 3 via cloud scavenging is also much more efficient than homogeneous N 2 O 5 hydrolysis, which was observed by Colvile et al (1994) as well. The potential significance of N 2 O 5 uptake on fog droplets was demonstrated through measurements by Wood et al (2005), where the N 2 O 5 mixing ratio was well below the detection limit of the instrument (LIF) during nights of high RH (above 70%).…”
Section: Model Representation Of N 2 O 5 Uptakementioning
confidence: 76%
“…Leaitch et al (1988) studied the dissolution of N 2 O 5 in cloud droplets by using a Lagrangian chemical model with winter conditions in northeastern region of the United States and compared the resulting NO 3 − content in cloud water with measured values. They showed that the mean production rate of HNO 3 via cloud scavenging is also much more efficient than homogeneous N 2 O 5 hydrolysis, which was observed by Colvile et al (1994) as well. The potential significance of N 2 O 5 uptake on fog droplets was demonstrated through measurements by Wood et al (2005), where the N 2 O 5 mixing ratio was well below the detection limit of the instrument (LIF) during nights of high RH (above 70%).…”
Section: Model Representation Of N 2 O 5 Uptakementioning
confidence: 76%
“…The principal heterogenous NO x removal mechanism is via the hydrolysis of N 2 O 5 which is much slower in the gas phase. Field observations and laboratory studies support the efficient uptake of N 2 O 5 [17,18], with said studies measuring the reaction probability (γ) to be in the range of 0.01-1 for aqueous solutions such as H 2 SO 4 largely independent of aerosol composition [19]. Importantly, the timescale for N 2 O 5 removal on tropospheric aerosol is estimated to range from minutes in heavily polluted air, characterised by increased particle density and surface area, to hours in more remote regions [16].…”
Section: Introductionmentioning
confidence: 80%