posted on 2006-02-15, 00:00authored byYann Batonneau, Sophie Sobanska, Jacky Laureyns, Claude Bremard
Particulate matter with aerodynamic diameters of <1,
1−2.5, and 2.5−10 μm were collected during two seasons
in two urban zones situated northeast and southwest,
respectively, of a lead/zinc smelter located in a former
mining region of northern France. We demonstrate the
effectiveness of the combined use of computer-controlled
Raman mapping and multivariate curve resolution (MCR)
of the Raman images to determine heterogeneous chemistry
at the level of aerosol particle. The resulting molecular
images of major species were found to be in accurate
agreement with elemental images obtained by WDS X-ray-mapping. Environmental SEM was very useful to localize
spare metal-rich particles before Raman mapping. Some spare
particles containing pyromorphite (Pb<sub>5</sub>(PO<sub>4</sub>)<sub>3</sub>OH) and
franklinite (Zn<i><sub>x</sub></i>Fe<sub>3</sub><sub>-</sub><i><sub>x</sub></i>O<sub>4</sub>) mixed with mineral dust were
detected at the northeast (NE) sampling site, when the
wind was blowing from the west (W) sector. These particles
were probably suspended in the troposphere by the
action of wind or by mechanical disturbance of polluted
top soils<i>.</i> The most abundantly encountered particles in the
10−2.5 and 2.5−1 μm fractions were found to be
aggregates of NaCl, CaCO<sub>3</sub>, CaSO<sub>4</sub>·2H<sub>2</sub>O, CaMg(CO<sub>3</sub>)<sub>2</sub>,
SiO<sub>2</sub>, feldspar, clay minerals, α-Fe<sub>2</sub>O<sub>3</sub>, NaNO<sub>3</sub>, and Ca(NO<sub>3</sub>)<sub>2</sub>·4H<sub>2</sub>O. Black carbon and (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> particles were observed
predominantly in the finest fraction. It was not rare to
detect Pb and Zn-rich particles in the 10−2.5 and 2.5−1
μm fractions collected at the southwest (SW) sampling site,
when the wind was blowing from the NE sector. Most of
these mixed particles probably result from the aggregation
between PbSO<sub>4</sub>, PbO·PbSO<sub>4</sub>, and ZnS particles emitted
by the smelters and hydroscopic mineral dust during transport
in the troposphere.