scholarly journals Personal exposures and indoor, residential outdoor, and urban background levels of fine particle trace elements in the general population

2006 ◽  
Vol 8 (5) ◽  
pp. 543-551 ◽  
Author(s):  
Peter Molnár ◽  
Sandra Johannesson ◽  
Johan Boman ◽  
Lars Barregård ◽  
Gerd Sällsten
2017 ◽  
Vol 25 ◽  
pp. 1-10 ◽  
Author(s):  
Mira Aničić Urošević ◽  
Gordana Vuković ◽  
Petar Jovanović ◽  
Milorad Vujičić ◽  
Aneta Sabovljević ◽  
...  

RADIOISOTOPES ◽  
1998 ◽  
Vol 47 (1) ◽  
pp. 46-55 ◽  
Author(s):  
Akito TSUMURA ◽  
Shin-ichi YAMASAKI

2020 ◽  
Vol 719 ◽  
pp. 134427
Author(s):  
Anja Stajnko ◽  
Rustam Tuhvatshin ◽  
Gulbarchin Suranova ◽  
Darja Mazej ◽  
Zdenka Šlejkovec ◽  
...  

2005 ◽  
Vol 15 (03n04) ◽  
pp. 233-239 ◽  
Author(s):  
EDUARD STELCER ◽  
OLGA HAWAS ◽  
DAVID COHEN ◽  
ADAM SARBUTT ◽  
DAVID BUTTON

Since 1991 ANSTO's ion beam analysis (IBA) laboratory has been sampling fine atmospheric particles every Wednesday and Sunday at urban and rural sites in New South Wales. Multi-elemental accelerator-based IBA techniques were used to characterise major components and significant trace elements with minimum detectable limits close to 1 ng/m3. Observed mass concentrations will be compared with air quality US EPA standards and proposed Australian fine particle NEPM guidelines. Trace elements strongly associated with source fingerprints responsible for high air pollution will also be discussed in this paper.


1996 ◽  
Vol 27 ◽  
pp. S31-S32 ◽  
Author(s):  
P.F. Caffrey ◽  
A.E. Suarez ◽  
J.M. Ondov ◽  
M. Han

1980 ◽  
Vol 60 (4) ◽  
pp. 763-771 ◽  
Author(s):  
M. J. DUDAS ◽  
S. PAWLUK

Background levels of As, Cd, Co, Cu, Pb, and Zn in Chernozemic and Luvisolic soils from Alberta were established and are similar to the average terrestrial abundances in shale and granite. Redistribution of As, Cd, Co, Cu, and Zn within the solum was more pronounced in Luvisolic soils than in Chernozems. Partitioning of the six trace elements, determined by analysis of particle size separates, was unique for each element. Copper and zinc were more uniformly enriched in clay separates than were the other four trace elements. Differences in the content of trace elements within and among soils arise not only from textural variation, but also from large variations in the quantity of trace elements within a specific particle size fraction.


2021 ◽  
Vol 2021 (1) ◽  
Author(s):  
Marta Gálvez Fernández ◽  
Francisco Sanchez Saez ◽  
Arce Domingo Relloso ◽  
Zulema Rodriguez Hernandez ◽  
Vannina Gonzalez Marrachelli ◽  
...  

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