TY - JOUR
T1 - Characterization and source apportionment of aerosol light extinction in Chengdu, southwest China
AU - Tao, Jun
AU - Zhang, Leiming
AU - Cao, Junji
AU - Hsu, Shih Chieh
AU - Xia, Xiangao
AU - Zhang, Zhisheng
AU - Lin, Zejian
AU - Cheng, Tiantao
AU - Zhang, Renjian
PY - 2014/10
Y1 - 2014/10
N2 - To investigate aerosol properties in the Sichuan Basin of China, field aerosol sampling was carried out in Chengdu, China during four one-month periods, each in a different season in 2011. Aerosol scattering coefficient (bsp) at dry (RH<40%) and wet (40%ap) were measured. Additionally, daily PM2.5 and PM10 samples were also collected. PM2.5 samples were subject to chemical analysis for various chemical components including major water-soluble ions, organic and elemental carbon (OC and EC), trace elements, as well as anhydrosugar Levoglucosan (LG) and Mannosan (MN). A multiple linear regression analysis was applied to the measured dry bsp against (NH4)2SO4, NH4NO3, organic mass (OM), fine soil (FS), and coarse mass (CM, PM2.5-10), and to the measured bap against EC in all the four seasons to evaluate the impact of individual chemical components of PM2.5 and CM on aerosol light extinction (bext=bsp+bap). Mass scattering efficiency (MSE) and mass absorption efficiency (MAE) of the individual chemical components of PM2.5 were estimated based on seasonal regression equations and were then used for estimating bext. The annual bsp, bap and single scattering albedo (SSA) at dry conditions were 456±237Mm-1, 96±48Mm-1 and 0.82±0.05, respectively. The annual average bsp at ambient conditions estimated through hygroscopic curve of aerosol (f(RH)) was 763±415Mm-1, which was 1.7 times of the dry bsp. The annual average SSA at ambient conditions also increased to 0.88±0.04. The estimated dry bext was only 2±9% higher than the measurements and the estimated ambient bext from individual chemical components was only 1±10% lower, on an annual basis, than that estimated from using f(RH). Secondary inorganic aerosols, coal combustion, biomass burning, iron and steel industry, Mo-related industry, soil dust, and CM to bext were estimated to account for 41±19%, 18±12%, 14±13%, 13±11%, 5±4%, 5±7% and 4±3%, respectively, of the estimated ambient bext.
AB - To investigate aerosol properties in the Sichuan Basin of China, field aerosol sampling was carried out in Chengdu, China during four one-month periods, each in a different season in 2011. Aerosol scattering coefficient (bsp) at dry (RH<40%) and wet (40%ap) were measured. Additionally, daily PM2.5 and PM10 samples were also collected. PM2.5 samples were subject to chemical analysis for various chemical components including major water-soluble ions, organic and elemental carbon (OC and EC), trace elements, as well as anhydrosugar Levoglucosan (LG) and Mannosan (MN). A multiple linear regression analysis was applied to the measured dry bsp against (NH4)2SO4, NH4NO3, organic mass (OM), fine soil (FS), and coarse mass (CM, PM2.5-10), and to the measured bap against EC in all the four seasons to evaluate the impact of individual chemical components of PM2.5 and CM on aerosol light extinction (bext=bsp+bap). Mass scattering efficiency (MSE) and mass absorption efficiency (MAE) of the individual chemical components of PM2.5 were estimated based on seasonal regression equations and were then used for estimating bext. The annual bsp, bap and single scattering albedo (SSA) at dry conditions were 456±237Mm-1, 96±48Mm-1 and 0.82±0.05, respectively. The annual average bsp at ambient conditions estimated through hygroscopic curve of aerosol (f(RH)) was 763±415Mm-1, which was 1.7 times of the dry bsp. The annual average SSA at ambient conditions also increased to 0.88±0.04. The estimated dry bext was only 2±9% higher than the measurements and the estimated ambient bext from individual chemical components was only 1±10% lower, on an annual basis, than that estimated from using f(RH). Secondary inorganic aerosols, coal combustion, biomass burning, iron and steel industry, Mo-related industry, soil dust, and CM to bext were estimated to account for 41±19%, 18±12%, 14±13%, 13±11%, 5±4%, 5±7% and 4±3%, respectively, of the estimated ambient bext.
KW - Aerosol absorption coefficient
KW - Aerosol scattering coefficient
KW - Hygroscopic growth
KW - Urban aerosols
UR - https://www.scopus.com/pages/publications/84904113434
U2 - 10.1016/j.atmosenv.2014.07.017
DO - 10.1016/j.atmosenv.2014.07.017
M3 - 文章
AN - SCOPUS:84904113434
SN - 1352-2310
VL - 95
SP - 552
EP - 562
JO - Atmospheric Environment
JF - Atmospheric Environment
ER -