Quantifying the dry deposition of reactive nitrogen and sulfur containing species in remote areas using a surrogate surface analysis approach

In this study, the fluxes of gaseous (HNO 3 and SO 2) and particulate (NO 3 − and SO 4 2−) species were measured using two recently developed surrogate surfaces, the water surface sampler (WSS) and the knife-edge surrogate surface (KSS). Sampling was conducted in Potsdam, NY, Solomons, MD, and at a...

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Veröffentlicht in:Atmospheric environment (1994) 2004-06, Vol.38 (17), p.2687-2697
Hauptverfasser: Raymond, Heather A, Yi, Seung-Muk, Moumen, Nadjoua, Han, YoungJi, Holsen, Thomas M
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container_end_page 2697
container_issue 17
container_start_page 2687
container_title Atmospheric environment (1994)
container_volume 38
creator Raymond, Heather A
Yi, Seung-Muk
Moumen, Nadjoua
Han, YoungJi
Holsen, Thomas M
description In this study, the fluxes of gaseous (HNO 3 and SO 2) and particulate (NO 3 − and SO 4 2−) species were measured using two recently developed surrogate surfaces, the water surface sampler (WSS) and the knife-edge surrogate surface (KSS). Sampling was conducted in Potsdam, NY, Solomons, MD, and at a farm in upstate NY intermittently between March 2000 and August 2001. The KSS contained both Nylasorb filters and greased Mylar disks. No statistical difference was found between measured total nitrate and sulfate deposition in side-by-side experiments with two WSSs. Average total nitrate fluxes measured with the WSS and Nylasorb filter on the KSS in Potsdam, Solomons, and at the farm were 3.6, 6.2, 2.9 mg m −2 day −1 and 2.5, 6.7, 2.3 mg m −2 day −1, respectively. Solomons had the highest total nitrate flux probably due to its proximity to large urban industrialized areas including Washington, DC, and Baltimore, MD. Average gaseous HNO 3 fluxes measured with the WSS and Nylasorb filter on the KSS in Potsdam, Solomons, and at the farm (calculated by subtracting the fraction of particles deposited to the Mylar disk from the total deposition to the WSS and Nylasorb filter) were 2.4, 4.9, 1.9 mg m −2 day −1 and 1.3, 5.6, 1.3 mg m −2 day −1, respectively. In Potsdam, total nitrate deposition to the WSS was greater than to the Nylasorb filter whereas in Solomons the opposite was true. This increased flux at Solomons may be because nitrate salts were formed on the surface of the Nylasorb filter by reaction of HNO 3 with previously deposited sea salt aerosols. Average p-NO 3 − fluxes to the greased Mylar for the three sampling sites were 1.3, 1.3, and 1.0 mg m −2 day −1. The measured SO 2 deposition velocity to the WSS in Potsdam and Solomons was 2.1 and 1.5 cm s −1, respectively, and agreed well with other studies. The deposition velocity for HNO 3 to the WSS measured in Potsdam (8.1 cm s −1) was greater than to the Nylasorb filter (4.6 cm s −1) whereas in Solomons the opposite was true (4.6 cm s −1 vs. 7.1 cm s −1).
doi_str_mv 10.1016/j.atmosenv.2004.02.011
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Sampling was conducted in Potsdam, NY, Solomons, MD, and at a farm in upstate NY intermittently between March 2000 and August 2001. The KSS contained both Nylasorb filters and greased Mylar disks. No statistical difference was found between measured total nitrate and sulfate deposition in side-by-side experiments with two WSSs. Average total nitrate fluxes measured with the WSS and Nylasorb filter on the KSS in Potsdam, Solomons, and at the farm were 3.6, 6.2, 2.9 mg m −2 day −1 and 2.5, 6.7, 2.3 mg m −2 day −1, respectively. Solomons had the highest total nitrate flux probably due to its proximity to large urban industrialized areas including Washington, DC, and Baltimore, MD. Average gaseous HNO 3 fluxes measured with the WSS and Nylasorb filter on the KSS in Potsdam, Solomons, and at the farm (calculated by subtracting the fraction of particles deposited to the Mylar disk from the total deposition to the WSS and Nylasorb filter) were 2.4, 4.9, 1.9 mg m −2 day −1 and 1.3, 5.6, 1.3 mg m −2 day −1, respectively. In Potsdam, total nitrate deposition to the WSS was greater than to the Nylasorb filter whereas in Solomons the opposite was true. This increased flux at Solomons may be because nitrate salts were formed on the surface of the Nylasorb filter by reaction of HNO 3 with previously deposited sea salt aerosols. Average p-NO 3 − fluxes to the greased Mylar for the three sampling sites were 1.3, 1.3, and 1.0 mg m −2 day −1. The measured SO 2 deposition velocity to the WSS in Potsdam and Solomons was 2.1 and 1.5 cm s −1, respectively, and agreed well with other studies. The deposition velocity for HNO 3 to the WSS measured in Potsdam (8.1 cm s −1) was greater than to the Nylasorb filter (4.6 cm s −1) whereas in Solomons the opposite was true (4.6 cm s −1 vs. 7.1 cm s −1).</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.atmosenv.2004.02.011</doi><tpages>11</tpages></addata></record>
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ispartof Atmospheric environment (1994), 2004-06, Vol.38 (17), p.2687-2697
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subjects Air. Soil. Water. Waste. Feeding
Applied sciences
Atmospheric pollution
Biological and medical sciences
Deposition velocity
Earth, ocean, space
Environment. Living conditions
Exact sciences and technology
External geophysics
Flux
KSS
Medical sciences
Meteorology
Nitrate
Nylasorb filter
Pollution
Public health. Hygiene
Public health. Hygiene-occupational medicine
Sulfate
WSS
title Quantifying the dry deposition of reactive nitrogen and sulfur containing species in remote areas using a surrogate surface analysis approach
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