Airborne measurement of ionic components in aerosol particles during AAMP98

During the Arctic Airborne Measurement Program 1998 (AAMP 98), atmospheric aerosols were collected onto PTFE filters from the inlet of Gulfstream II through a diffuser installed in the cabin. During the sampling the number concentrations of aerosol particles with diameters larger than 0.3 µm were co...

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Main Authors: Sadamu Yamagata, Katsuhiro Shoji, Naoto Murao, Sachio Ohta
Format: Article
Language:English
Published: National Institute of Polar Research 2002-06-01
Series:Antarctic Record
Online Access:http://doi.org/10.15094/00009213
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spelling doaj-a423e41d9c524fd9a8080002acd720cd2020-11-24T23:09:10ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X2002-06-01461A16717610.15094/00009213Airborne measurement of ionic components in aerosol particles during AAMP98Sadamu Yamagata0Katsuhiro Shoji1Naoto Murao2Sachio Ohta3Division of Environment and Resource Engineering, Graduate School of Engineering, Hokkaido University/Division of Environment and Resource Engineering, Graduate School of Engineering, Hokkaido University/Division of Environment and Resource Engineering, Graduate School of Engineering, Hokkaido University/Division of Environment and Resource Engineering, Graduate School of Engineering, Hokkaido University/During the Arctic Airborne Measurement Program 1998 (AAMP 98), atmospheric aerosols were collected onto PTFE filters from the inlet of Gulfstream II through a diffuser installed in the cabin. During the sampling the number concentrations of aerosol particles with diameters larger than 0.3 µm were continuously monitored with an optical particle counter (OPC) connected to the diffuser in parallel to the filter sampling line. The data from the OPC were transferred by serial communication to a computer and recorded. The filter samples were brought back to the laboratory, then extracted with ion exchanged water and the concentrations of anions and cations were analyzed by ion chromato­graphy. Detected ions were as follows: Cl^-, N02^-, 1 , N03^-, SO4^2-, Na^+, NH4+, K^+, Mg^2+, Ca^2+. Even at high altitudes Cl^- and Ca^2+ were frequently detected, in addition to SO4^2- , which is known as a major ionic component in the stratosphere. http://doi.org/10.15094/00009213
collection DOAJ
language English
format Article
sources DOAJ
author Sadamu Yamagata
Katsuhiro Shoji
Naoto Murao
Sachio Ohta
spellingShingle Sadamu Yamagata
Katsuhiro Shoji
Naoto Murao
Sachio Ohta
Airborne measurement of ionic components in aerosol particles during AAMP98
Antarctic Record
author_facet Sadamu Yamagata
Katsuhiro Shoji
Naoto Murao
Sachio Ohta
author_sort Sadamu Yamagata
title Airborne measurement of ionic components in aerosol particles during AAMP98
title_short Airborne measurement of ionic components in aerosol particles during AAMP98
title_full Airborne measurement of ionic components in aerosol particles during AAMP98
title_fullStr Airborne measurement of ionic components in aerosol particles during AAMP98
title_full_unstemmed Airborne measurement of ionic components in aerosol particles during AAMP98
title_sort airborne measurement of ionic components in aerosol particles during aamp98
publisher National Institute of Polar Research
series Antarctic Record
issn 0085-7289
2432-079X
publishDate 2002-06-01
description During the Arctic Airborne Measurement Program 1998 (AAMP 98), atmospheric aerosols were collected onto PTFE filters from the inlet of Gulfstream II through a diffuser installed in the cabin. During the sampling the number concentrations of aerosol particles with diameters larger than 0.3 µm were continuously monitored with an optical particle counter (OPC) connected to the diffuser in parallel to the filter sampling line. The data from the OPC were transferred by serial communication to a computer and recorded. The filter samples were brought back to the laboratory, then extracted with ion exchanged water and the concentrations of anions and cations were analyzed by ion chromato­graphy. Detected ions were as follows: Cl^-, N02^-, 1 , N03^-, SO4^2-, Na^+, NH4+, K^+, Mg^2+, Ca^2+. Even at high altitudes Cl^- and Ca^2+ were frequently detected, in addition to SO4^2- , which is known as a major ionic component in the stratosphere.
url http://doi.org/10.15094/00009213
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