Chia-Li Chen
University of California, San Diego
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Featured researches published by Chia-Li Chen.
Aerosol Science and Technology | 2017
Derek J. Price; Chia-Li Chen; Lynn M. Russell; Maryam A. Lamjiri; Raghu Betha; Kevin J. Sanchez; Jun Liu; Alex K. Y. Lee; David R. Cocker
ABSTRACT The aerosol particle emissions from R/V Robert Gordon Sproul were measured during two 5-day research cruises (29 September–3 October 2014; 4–7 and 26–28 September 2015) at four engine speeds (1600 rpm, 1300 rpm, 1000 rpm, and 700 rpm) to characterize the emissions under different engine conditions for ultra low sulfur diesel (ULSD) and hydrogenation derived renewable diesel (HDRD) fuels. Organic aerosol composition and mass distribution were measured on the aft deck of the vessel directly behind the exhaust stack to intercept the ship plume. The ship emissions for both fuels were composed of alkane-like compounds (H/C = 1.94 ± 0.003, O/C = 0.04 ± 0.001, CnH2n) with mass spectral fragmentation patterns consistent with hydrocarbon-like organic aerosol (HOA). Single-particle mass spectra from emissions for both fuels showed two distinct HOA compositions, with one HOA type containing more saturated alkane fragments (CnH2n+1) and the other HOA type containing more monounsaturated fragments (CnH2n−1). The particles dominated by the CnH2n−1 fragment series are similar to mass spectra previously associated with cooking emissions. More cooking-type organic particles were observed in the ship emissions for HDRD than for ULSD (45% and 38%, respectively). Changes in the plume aerosol composition due to photochemical aging in the atmosphere were also characterized. The higher fraction of alkene or aromatic (CnH2n−m, m ≥ 3) fragments in aged compared to fresh plume emissions suggest that some of the semivolatile alkane-like components partition back to the vapor phase as dilution increases, while alkene or aromatic hydrocarbons contribute more mass to the particle phase due to continuing photochemical oxidation and subsequent condensation from the vapor phase. Copyright
Aerosol Science and Technology | 2017
Raghu Betha; Lynn M. Russell; Kevin J. Sanchez; Jun Liu; Derek J. Price; Maryam A. Lamjiri; Chia-Li Chen; Xiaobi M. Kuang; Gisele O. da Rocha; Suzanne E. Paulson; J. Wayne Miller; David R. Cocker
ABSTRACT Gas and particle emissions from R/V Robert Gordon Sproul were measured for ultra low sulfur diesel (ULSD) and hydrogenation derived renewable diesel (HDRD) during dedicated aerosol measurement cruises in 2014 (29 September–3 October) and 2015 (4–7 and 26–28 September). CO, CO2, and NOX were measured directly from the starboard stack from the 2-stroke, small bore, high speed engine, while number and mass size distributions for both particles and black carbon (BC) were measured by intercepting the ship plume. Measurements at constant engine speeds (1600 rpm, 1300 rpm, 1000 rpm, and 700 rpm) had emission factors of CO () and NOX that were lower by 20% and 13%, respectively, for HDRD compared to ULSD at 700 rpm. However, at 1600 rpm, and were within one standard deviation for both ULSD (: 4.0 ± 0.1 g [kg-fuel]−1; : 51 ± 0.8 g [kg-fuel]−1) and HDRD (: 3.9 ± 0.2 g [kg-fuel]−1; : 51 ± 2 g [kg-fuel]−1). HDRD emission factors of particle number and mass concentrations were higher than ULSD by 46% to 107% and 36% to 150%, respectively, at 1600, 1300, and 1000 rpm, but the differences were smaller than the cycle-to-cycle variability at 700 rpm. BC mass emission factors were nearly 200% larger for 700, 1000, and 1300 rpm for HDRD compared to ULSD, but the mass differences were smaller than cycle-to-cycle variability at 1600 rpm. BC mass size distributions showed that the peak diameter of the BC mass mode for ULSD (∼120 nm) is about 20 nm larger than for HDRD (∼100 nm), even though the particle mass and number size distributions are quite similar. Copyright
Scientific Reports | 2018
Kevin J. Sanchez; Chia-Li Chen; Lynn M. Russell; Raghu Betha; Jun Liu; Derek J. Price; Paola Massoli; Luke D. Ziemba; Ewan Crosbie; Richard Moore; Markus Müller; Sven A. Schiller; Armin Wisthaler; Alex K. Y. Lee; Patricia K. Quinn; Timothy S. Bates; Jack Porter; Thomas G. Bell; Eric S. Saltzman; Robert D. Vaillancourt; Michael J. Behrenfeld
Biogenic sources contribute to cloud condensation nuclei (CCN) in the clean marine atmosphere, but few measurements exist to constrain climate model simulations of their importance. The chemical composition of individual atmospheric aerosol particles showed two types of sulfate-containing particles in clean marine air masses in addition to mass-based Estimated Salt particles. Both types of sulfate particles lack combustion tracers and correlate, for some conditions, to atmospheric or seawater dimethyl sulfide (DMS) concentrations, which means their source was largely biogenic. The first type is identified as New Sulfate because their large sulfate mass fraction (63% sulfate) and association with entrainment conditions means they could have formed by nucleation in the free troposphere. The second type is Added Sulfate particles (38% sulfate), because they are preexisting particles onto which additional sulfate condensed. New Sulfate particles accounted for 31% (7 cm−3) and 33% (36 cm−3) CCN at 0.1% supersaturation in late-autumn and late-spring, respectively, whereas sea spray provided 55% (13 cm−3) in late-autumn but only 4% (4 cm−3) in late-spring. Our results show a clear seasonal difference in the marine CCN budget, which illustrates how important phytoplankton-produced DMS emissions are for CCN in the North Atlantic.
Journal of Geophysical Research | 2018
Sonya Collier; Leah R. Williams; Timothy B. Onasch; Christopher D. Cappa; Xiaolu Zhang; Lynn M. Russell; Chia-Li Chen; Kevin J. Sanchez; Douglas R. Worsnop; Qi Zhang
Inorganic and organic coatings on black carbon (BC) particles can enhance light absorption and affect atmospheric lifetimes of BC-containing particles and thus have significant implications for climate. To study the physical and chemical characteristics of atmospheric BC and BC-associated coatings, a soot-particle aerosol mass spectrometer (SP-AMS) was deployed during the winter of 2014-2015 in Fresno, a city located in the San Joaquin Valley of California, to selectively analyze BC-containing particles. Comparing SP-AMS measurements to those from the collocated single particle soot photometer (SP2) and high resolution aerosol mass spectrometer (HR-AMS), we found that 17% of total submicrometer aerosol mass was associated with BC-containing particles, suggesting that a majority of the fine particles in Fresno contained no BC. Most BC-containing particles appeared to be associated with residential wood burning and vehicular traffic. These particles typically had a bulk-average mass ratio of coating-to-BC (Rcoat/rBC) less than 2. However, during periods of persistent fog larger Rcoat/rBC values were observed, with the coatings primarily composed of secondary inorganic and organic components that likely resulted from aqueous-phase processing. Specifically, compared to periods with less fog, the BC coating increased in concentration and contained a larger fraction of nitrate and oxidized organic matter. The size distributions of BC and associated organic coating were generally centered around 300 nm in vacuum aerodynamic diameter. However, during foggy periods BC had an additional peak at ~ 400 nm and organics and nitrate displayed a prominent mode in the accumulation size range.
Journal of Environmental Sciences-china | 2017
Nicholas Gysel; William A. Welch; Chia-Li Chen; Poornima Dixit; David R. Cocker; Georgios Karavalakis
This study assessed the effectiveness of three novel control technologies for particulate matter (PM) and volatile organic compound (VOC) removal from commercial meat cooking operations. All experiments were conducted using standardized procedures at University of California, Riversides commercial test cooking facility. PM mass emissions collected using South Coast Air Quality Management District (SCAQMD) Method 5.1, as well as a dilution tunnel-based PM method showed statistically significantly reductions for each control technology when compared to baseline testing (i.e., without a catalyst). Overall, particle number emissions decreased with the use of control technologies, with the exception of control technology 2 (CT2), which is a grease removal technology based on boundary layer momentum transfer (BLMT) theory. Particle size distributions were unimodal with CT2 resulting in higher particle number populations at lower particle diameters. Organic carbon was the dominant PM component (>99%) for all experiments. Formaldehyde and acetaldehyde were the most abundant carbonyl compounds and showed reductions with the application of the control technologies. Some reductions in mono-aromatic VOCs were also observed with CT2 and the electrostatic precipitator (ESP) CT3 compared to the baseline testing.
Atmospheric Chemistry and Physics | 2012
Shunsuke Nakao; Yingdi Liu; Ping Tang; Chia-Li Chen; Jingsong Zhang; David R. Cocker
Atmospheric Environment | 2016
Chia-Li Chen; Mary Kacarab; Ping Tang; David R. Cocker
Atmospheric Chemistry and Physics | 2016
Lijie Li; Ping Tang; Shunsuke Nakao; Chia-Li Chen; David R. Cocker
Atmospheric Chemistry and Physics | 2011
Shunsuke Nakao; Yingdi Liu; Ping Tang; Chia-Li Chen; Jingsong Zhang; David R. Cocker
Atmospheric Environment | 2018
Weihua Li; Lijie Li; Chia-Li Chen; Mary Kacarab; Weihan Peng; Derek Price; Jin Xu; David R. Cocker