6 research outputs found
Highly time-resolved chemical speciation and source apportionment of organic aerosol components in Delhi, India, using extractive electrospray ionization mass spectrometry
In recent years, the Indian capital city of Delhi has been impacted by very high levels of air pollution, especially during winter. Comprehensive knowledge of the composition and sources of the organic aerosol (OA), which constitutes a substantial fraction of total particulate mass (PM) in Delhi, is central to formulating effective public health policies. Previous source apportionment studies in Delhi identified key sources of primary OA (POA) and showed that secondary OA (SOA) played a major role but were unable to resolve specific SOA sources. We address the latter through the first field deployment of an extractive electrospray ionization time-of-flight mass spectrometer (EESI-TOF) in Delhi, together with a high-resolution aerosol mass spectrometer (AMS). Measurements were conducted during the winter of 2018/19, and positive matrix factorization (PMF) was used separately on AMS and EESI-TOF datasets to apportion the sources of OA. AMS PMF analysis yielded three primary and two secondary factors which were attributed to hydrocarbon-like OA (HOA), biomass burning OA (BBOA-1 and BBOA-2), more oxidized oxygenated OA (MO-OOA), and less oxidized oxygenated OA (LO-OOA). On average, 40 % of the total OA mass was apportioned to the secondary factors. The SOA contribution to total OA mass varied greatly between the daytime (76.8 %, 10:00–16:00 local time (LT)) and nighttime (31.0 %, 21:00–04:00 LT). The higher chemical resolution of EESI-TOF data allowed identification of individual SOA sources. The EESI-TOF PMF analysis in total yielded six factors, two of which were primary factors (primary biomass burning and cooking-related OA). The remaining four factors were predominantly of secondary origin: aromatic SOA, biogenic SOA, aged biomass burning SOA, and mixed urban SOA. Due to the uncertainties in the EESI-TOF ion sensitivities, mass concentrations of EESI-TOF SOA-dominated factors were related to the total AMS SOA (i.e. MO-OOA + LO-OOA) by multiple linear regression (MLR). Aromatic SOA was the major SOA component during the daytime, with a 55.2 % contribution to total SOA mass (42.4 % contribution to total OA). Its contribution to total SOA, however, decreased to 25.4 % (7.9 % of total OA) during the nighttime. This factor was attributed to the oxidation of light aromatic compounds emitted mostly from traffic. Biogenic SOA accounted for 18.4 % of total SOA mass (14.2 % of total OA) during the daytime and 36.1 % of total SOA mass (11.2 % of total OA) during the nighttime. Aged biomass burning and mixed urban SOA accounted for 15.2 % and 11.0 % of total SOA mass (11.7 % and 8.5 % of total OA mass), respectively, during the daytime and 15.4 % and 22.9 % of total SOA mass (4.8 % and 7.1 % of total OA mass), respectively, during the nighttime. A simple dilution–partitioning model was applied on all EESI-TOF factors to estimate the fraction of observed daytime concentrations resulting from local photochemical production (SOA) or emissions (POA). Aromatic SOA, aged biomass burning, and mixed urban SOA were all found to be dominated by local photochemical production, likely from the oxidation of locally emitted volatile organic compounds (VOCs). In contrast, biogenic SOA was related to the oxidation of diffuse regional emissions of isoprene and monoterpenes. The findings of this study show that in Delhi, the nighttime high concentrations are caused by POA emissions led by traffic and biomass burning and the daytime OA is dominated by SOA, with aromatic SOA accounting for the largest fraction. Because aromatic SOA is possibly more toxic than biogenic SOA and primary OA, its dominance during the daytime suggests an increased OA toxicity and health-related consequences for the general public.</p
Temporal Characteristics of Brown Carbon over the Central Indo-Gangetic Plain
Recent global models estimate that
light absorption by brown carbon
(BrC) in several regions of the world is ∼30–70% of
that due to black carbon (BC). It is, therefore, important to understand
its sources and characteristics on temporal and spatial scales. In
this study, we conducted semicontinuous measurements of water-soluble
organic carbon (WSOC) and BrC using particle-into-liquid sampler coupled
with a liquid waveguide capillary cell and total organic carbon analyzer
(PILS-LWCC-TOC) over Kanpur (26.5°N, 80.3°E, 142 m amsl)
during a winter season (December 2015 to February 2016). In addition,
mass concentrations of organic and inorganic aerosol and BC were also
measured. Diurnal variability in the absorption coefficient of BrC
at 365 nm (<i>b</i><sub>abs_365</sub>) showed higher values (35 ± 21 Mm<sup>–1</sup>) during late evening to early morning hours and was attributed to
primary emissions from biomass burning (BB) and fossil fuel burning
(FFB). The <i>b</i><sub>abs_365</sub> reduced by more than
80% as the day progressed, which was ascribed to photo bleaching/volatilization
of BrC and/or due to rising boundary layer height. Further, diurnal
variability in the ratios of <i>b</i><sub>abs_405</sub>/<i>b</i><sub>abs_365</sub> and <i>b</i><sub>abs_420</sub>/<i>b</i><sub>abs_365</sub> suggests that the BrC composition
was not uniform throughout a day. WSOC exhibited a strong correlation
with <i>b</i><sub>abs_365</sub> (slope = 1.22 ± 0.007, <i>r</i><sup>2</sup> = 0.70, <i>n</i> = 13 265,
intercept = −0.69 ± 0.17), suggesting the presence of
a significant but variable fraction of chromophores. Mass absorption
efficiency (MAE) values of WSOC ranged from 0.003 to 5.26 m<sup>2</sup> g<sup>–1</sup> (1.16 ± 0.60) during the study period.
Moderate correlation (<i>r</i><sup>2</sup> = 0.50, slope
= 1.58 ± 0.019, <i>n</i> = 6471) of <i>b</i><sub>abs_365</sub> was observed with the semivolatile oxygenated
organic aerosols (SV-OOA) fraction of BB resolved from positive matrix
factorization (PMF) analysis of organic mass spectral data obtained
from a high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS).
The low-volatility OOA (LV-OOA) fraction of BB had a similar correlation
to <i>b</i><sub>abs_365</sub> (<i>r</i><sup>2</sup> = 0.54, slope = 0.38 ± 0.004, <i>n</i> = 6471) but
appears to have a smaller contribution to the absorption
Real-time characterization and source apportionment of fine particulate matter in the Delhi megacity area during late winter
National Capital Region (NCR) encompassing New Delhi is one of the most polluted urban metropolitan areas in the world.
Real-time chemical characterization of fine particulate matter (PM1 and PM2.5) was carried out using three aerosol mass
spectrometers, two aethalometers, and one single particle soot photometer (SP2) at two sites in Delhi (urban) and one site located
~40 km downwind of Delhi, during January-March, 2018. The campaign mean PM2.5 (NR-PM2.5 + BC) concentrations at the two
urban sites were 153.8±109.4 μg.m-3 and 127.8±83.2 μg.m-3, respectively, whereas PM1 (NR-PM1 + BC) was 72.3 ± 44.0 μg.m-3
at the downwind site. PM2.5 particles were composed mostly of organics (43-44)% followed by chloride (14-17)%, ammonium
(9-11)%, nitrate (9%), sulfate (8-10)%, and black carbon (11-16)%, whereas PM1 particles were composed of 47% organics,
13% sulfate as well as ammonium, 11% nitrate as well as chloride, and 5% black carbon. Organic aerosol (OA) source
apportionment was done using positive matrix factorization (PMF), solved using an advanced multi-linear engine (ME-2) model.
Highly mass-resolved OA mass spectra at one urban and downwind site were factorized into three primary organic aerosol
(POA) factors including one traffic-related and two solid-fuel combustion (SFC), and three oxidized OA (OOA) factors.
Whereas unit mass resolution OA at the other urban site was factorized into two POA factors related to traffic and SFC, and one
OOA factor. OOA constituted a majority of the total OA mass (45-55)% with maximum contribution during afternoon hours
~(70-80)%. Significant differences in the absolute OOA concentration between the two urban sites indicated the influence of local emissions on the oxidized OA formation. Similar PM chemical composition, diurnal and temporal variations at the three
sites suggest similar type of sources affecting the particulate pollution in Delhi and adjoining cities, but variability in mass concentration suggest more local influence than regional