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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National Institute of Polar Research
2002-06-01
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Series: | Antarctic Record |
Online Access: | http://doi.org/10.15094/00009213 |
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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 |
work_keys_str_mv |
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