P. Artaxo et al., ELEMENTAL COMPOSITION OF AEROSOL-PARTICLES FROM 2 ATMOSPHERIC MONITORING STATIONS IN THE AMAZON BASIN, Nuclear instruments & methods in physics research. Section B, Beam interactions with materials and atoms, 75(1-4), 1993, pp. 277-281
One key region for the study of processes that are changing the compos
ition of the global atmosphere is the Amazon Basin tropical rain fores
t. The high rate of deforestation nd biomass burning is emitting large
amounts of gases and fine-mode aerosol particles to the global atmosp
here. Two background monitoring stations are operating continuously me
asuring aerosol composition, at Cuiaba, and Serra do Navio. Fine- and
coarse-mode aerosol particles are being collected using stacked filter
units. Particle induced X-rav emission (PIXE) was used to measure con
centrations of up to 21 elements: Al, Si, P, S, Cl, K, Ca, Ti, V, Cr,
Mn, Fe, Ni, Cu, Zn, Se, Br, Rb, Sr, Zr, and Pb. The elemental composit
ion was measured at the new PIXE facility from the University of Sao P
aulo, using a dedicated 5SDH tandem Pelletron nuclear accelerator. Abs
olute principal factor analysis (APFA) has derived absolute elemental
source profiles. At the Serra do Navio sampling site a very clean back
ground aerosol is being observed. Biogenic aerosol dominates the fine-
mode mass concentration, with the presence of K, P, S, Cl, Zn, Br, and
FPM. Three components dominate the aerosol composition: soil dust par
ticles, the natural biogenic release by the forest, and a marine aeros
ol component. At the Cuiaba site, during the dry season, a strong comp
onent of biomass burning is observed. An aerosol mass concentration up
to 120 mug/m3 WaS measured. APFA showed three components: soil dust (
Al, Ca, Ti, Mn, Fe), biomass burning (soot, FPM, K, Cl) and natural bi
ogenic particles (K, S, Ca, Mn, Zn). The fine-mode biogenic component
of both sites shows remarkable similarities, although the two sampling
sites are 3000 km apart. Several essential plant nutrients like P, K,
S. Ca, Ni and others are transported in the atmosphere as a result of
biomass burning processes.