Chemical Characterization of Airborne Particulate Matter in Ambient Air of Nagoya, Japan, as Studied by the Multielement Determination with ICP-AES and ICP-MS

The multielement determination of PM10 (airborne particulate matter smaller than 10 µm) samples, which was collected by a high volume air sampler at the urban site of Nagoya City, was carried out by inductively coupled plasma atomic emission spectrometry (ICP-AES) and inductively coupled plasma mass...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Analytical Sciences 2007, Vol.23(2), pp.207-213
Hauptverfasser: FUKAI, Taku, KOBAYASHI, Tatsuya, SAKAGUCHI, Masahiro, AOKI, Masanori, SAITO, Tsuyoshi, FUJIMORI, Eiji, HARAGUCHI, Hiroki
Format: Artikel
Sprache:eng
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:The multielement determination of PM10 (airborne particulate matter smaller than 10 µm) samples, which was collected by a high volume air sampler at the urban site of Nagoya City, was carried out by inductively coupled plasma atomic emission spectrometry (ICP-AES) and inductively coupled plasma mass spectrometry (ICP-MS). The present analytical method was validated by analyzing urban particulate matter standard reference material of NIST SRM 1648. The analytical data for ca. 30 elements in PM10 samples collected during a period from 8 September to 9 October, 2003, were obtained in the concentration range from sub-µg g-1 to several-10 mg g-1, but the data for 18 elements among ca. 30 elements were available for the characterization of PM10 samples in ambient air, because of problems caused by the filter blanks. Then, the trends concerning the distributions of diverse elements in PM10 samples were analyzed based on the enrichment factors and size distribution factors. The lithophile and siderophile elements were distributed more than 50% in coarse particle fraction (>2.1 µm), which was derived mainly from natural sources, such as soils and crustal minerals. On the other hand, chalcophile elements were distributed more than 50% in fine particle fraction (
ISSN:0910-6340
1348-2246
DOI:10.2116/analsci.23.207