@Article{RosascoMariMartPere:2011:CaMoPa,
author = "Rosasco, Franklin Velarde and Mariani, Rauda L{\'u}cia and
Martins, Maria Paulete Pereira and Pereira, Enio Bueno",
affiliation = "{} and {} and {Instituto Nacional de Pesquisas Espaciais (INPE)}
and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Caracteriza{\c{c}}{\~a}o morfol{\'o}gica de part{\'{\i}}culas
na atmosfera de S{\~a}o Jos{\'e} dos Campos SP, utilizando
microscopia eletr{\^o}nica de varredura (MEV)",
journal = "Geochimica Brasiliensis",
year = "2011",
volume = "25",
number = "1",
pages = "25--33",
note = "Setores de Atividade: Outras atividades profissionais,
cient{\'{\i}}ficas e t{\'e}cnicas.",
keywords = "aerossol black carbon, composi{\c{c}}{\~a}o qu{\'{\i}}mica,
morfologia, dispers{\~a}o, black carbon aerosol, chemical
composition, morphology, scatter.",
abstract = "O estudo trata da caracteriza{\c{c}}{\~a}o morfol{\'o}gica do
aerossol Black Carbon (BC) coletado durante os meses de
mar{\c{c}}o a novembro de 2008 num ponto de monitoramento em
S{\~a}o Jos{\'e} dos Campos-SP. O aerossol BC {\'e} um
particulado inerte na atmosfera, por{\'e}m, devido {\`a} sua
porosidade e natureza adsortiva, atua como superf{\'{\i}}cie
ativa de algumas rea{\c{c}}{\~o}es qu{\'{\i}}micas
heterog{\^e}neas, podendo estar saturado com esp{\'e}cies
t{\'o}xicas ou carcinog{\^e}nicas. Assim, aeross{\'o}is de BC
podem representar um perigo para a sa{\'u}de p{\'u}blica,
al{\'e}m de serem considerados o segundo maior contribuinte para
o aquecimento global, em termos de sua for{\c{c}}ante radiativa
direta. A t{\'e}cnica utilizada foi a Microscopia Eletr{\^o}nica
de Varredura (MEV) associada {\`a} Espectroscopia de Energia
Dispersiva de raios X (EDX). Essa t{\'e}cnica tamb{\'e}m permite
a an{\'a}lise qualitativa da composi{\c{c}}{\~a}o elementar das
part{\'{\i}}culas. A partir de classifica{\c{c}}{\~a}o, por
semelhan{\c{c}}a morfol{\'o}gica, foram identificados 6 grupos
distintos de part{\'{\i}}culas: um grupo de part{\'{\i}}culas
produzidas por combust{\~a}o de motores; outro de
part{\'{\i}}culas procedentes da ressuspens{\~a}o do solo;
grupo de part{\'{\i}}culas da queima de biomassa; de
part{\'{\i}}culas de fuligem industrial e mais dois grupos com
morfologia e composi{\c{c}}{\~a}o qu{\'{\i}}mica semelhantes e
espec{\'{\i}}ficos da regi{\~a}o. As principais fontes
identificadas foram de combust{\~a}o de motores e
ressuspens{\~a}o do solo, por{\'e}m com influ{\^e}ncias de
outras fontes naturais e antr{\'o}picas. ABSTRACT: The study
deals with the morphological characterization of aerosol Black
Carbon (BC) collected during the months from March to November
2008 in a monitoring point in Sao Jose dos Campos, State of
S{\~a}o Paulo, southern Brazil. The BC aerosol particles is an
inert in the atmosphere, but due to its porosity and adsorptive
nature acts as the active surface of some heterogeneous chemical
reactions, which may be saturated with toxic or carcinogenic
species. Thus, aerosol BC may represents a danger to public
health, besides being considered the second largest contributor to
global warming, in terms of their direct radioactive forcing. The
technique used was electron microscopy (SEM) associated with
Energy Dispersive Spectroscopy (EDS). This technique also allows
the quantitative analysis of elemental composition of the
particles. From the classification by morphological similarity, we
identified six distinct groups of particles: a group produced by
combustion engines, other particles coming from resuspension of
soil; group of particles from biomass burning, soot particles from
industrial and two groups with similar morphology and chemical
composition and specific to the region. The main sources were
identified combustion engines and resuspension of soil, but with
influences of other natural and anthropogenic sources.",
issn = "0102-9800",
label = "lattes: 0638551133292550 4 RosascoMariMartPere:2012:CaMoPa",
language = "pt",
targetfile = "329-1319-1-PB.pdf",
url = "http://www.geobrasiliensis.org.br/ojs/index.php/geobrasiliensis/issue/view/48",
urlaccessdate = "30 abr. 2024"
}