2015
DOI: 10.1016/j.atmosres.2015.01.023
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δ15N–NH4+ variations of rainwater: Application of the Rayleigh model

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Cited by 16 publications
(3 citation statements)
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“…2.2) with 6 h sampling intervals that included 00: 30-06:30, 06:30-12:30, 12:30-18:30, and 18:30-00:30 LT during summer (9 to 18 August 2017) and 00:00-06:00, 06:00-12:00, 12:00-18:00, and 18:00-00:00 LT during winter (21 January to 1 February 2018). During the sampling periods, NH x collections were not conducted during precipitation periods (or forecasted precipitation periods) due to the potential role of wet scavenging to alter δ 15 N(NH 3 ) (Xiao et al, 2015). NH 3 was also collected using a passive sampler (ALPHA), in which NH 3 diffuses through a PTFE membrane and accumulates on an acid-coated (5 % citric acid (w/v) in water) cellulose filter (Albet, grade 604, 24 mm diameter) housed in a protective case.…”
Section: Introductionmentioning
confidence: 99%
“…2.2) with 6 h sampling intervals that included 00: 30-06:30, 06:30-12:30, 12:30-18:30, and 18:30-00:30 LT during summer (9 to 18 August 2017) and 00:00-06:00, 06:00-12:00, 12:00-18:00, and 18:00-00:00 LT during winter (21 January to 1 February 2018). During the sampling periods, NH x collections were not conducted during precipitation periods (or forecasted precipitation periods) due to the potential role of wet scavenging to alter δ 15 N(NH 3 ) (Xiao et al, 2015). NH 3 was also collected using a passive sampler (ALPHA), in which NH 3 diffuses through a PTFE membrane and accumulates on an acid-coated (5 % citric acid (w/v) in water) cellulose filter (Albet, grade 604, 24 mm diameter) housed in a protective case.…”
Section: Introductionmentioning
confidence: 99%
“…Bulk-deposited NH 4 + mainly derives from below-cloud scavenging of gaseous NH 3 from local emissions and the regional transported particulate NH 4 + (aq) and liquid NH 4 + (l) in-cloud scavenging. , Raindrops primarily absorb gaseous NH 3 below clouds during high precipitation in the summer when the aerosol NH 4 + concentration is low. The scavenging of gaseous NH 3 in rain largely tends to have isotope exchange reactions in NH 3(gas) /NH 3(aq) and NH 3(gas) /NH 4 + (aq) equilibrium, which results in bulk-deposited NH 4 + enriched in 15 N relative to gaseous NH 3 . Thus, the local NH 3 emission sources dominate the contribution to bulk-deposited nitrogen in the below-cloud scavenging process, due to the distinction in scavenging coefficients of gaseous NH 3 and NH 4 + particles. Moreover, there will be significant nitrogen isotope fractionation during mostly in-cloud and below-cloud procedures during the precipitation stage, which can change the initial isotope values of atmospheric nitrogen emission sources to some extent.…”
Section: Resultsmentioning
confidence: 99%
“…to February 1, 2018). During the sampling periods, NHx collections were not conducted during precipitation periods (or 155 forecasted precipitation periods) due to the potential role of wet scavenging to alter δ 15 N(NH3) (Xiao et al, 2015). The sampling cartridges were mounted on the roof (~3.85 m above ground) of the air monitoring station on the underside of a weatherproof shelter.…”
Section: Near-highway Measurements (Providence Ri Usa)mentioning
confidence: 99%