scholarly journals Measurements of particle masses of inorganic salt particles for calibration of cloud condensation nuclei counters

2009 ◽  
Vol 9 (1) ◽  
pp. 4653-4689 ◽  
Author(s):  
M. Kuwata ◽  
Y. Kondo
Keyword(s):  
Inorganic Salt ◽  
Cloud Condensation Nuclei ◽  
Input Parameter ◽  
Pitzer Model ◽  
Particle Mass ◽  
Mass Analyzer ◽  
Differential Mobility ◽  
Shape Factors ◽  
Critical Supersaturation ◽  
Dynamic Shape

Abstract. We measured the mobility equivalent critical dry diameter for CCN activation (dcme) and the particle mass of size-selected (NH4)2SO4 and NaCl particles to calibrate a CCN counter (CCNC) precisely. The CCNC was operated downstream of a differential mobility analyzer (DMA) for the measurement of dcme. The particle mass was measured using an aerosol particle mass analyzer (APM) operated downstream of the DMA. The measurement of particle mass was conducted for 50–150-nm particles. Effective densities (ρeff) of (NH4)2SO4 particles were 1.67–1.75 g cm−3, which correspond to the dynamic shape factors (χ) of 1.01–1.04. This shows that (NH4)2SO4 particles are not completely spherical. In the case of NaCl particles, ρeff was 1.75–1.99 g cm−3 and χ was 1.05–1.14, demonstrating that their particle shape was non-spherical. Using these experimental data, the volume equivalent critical dry diameter (dcve) was calculated, and it was used as an input parameter for calculations of critical supersaturation (S). Several thermodynamics models were used for the calculation of water activity. When the Pitzer model was employed for the calculations, the critical S calculated for (NH4)2SO4 and NaCl agreed to well within the uncertainty of 2% (relative). This result demonstrates that the use of the Pitzer model for the calibration of CCNCs gives the most probable value of S.

scholarly journals Measurements of particle masses of inorganic salt particles for calibration of cloud condensation nuclei counters

2009 ◽  
Vol 9 (16) ◽  
pp. 5921-5932 ◽  
Author(s):  
M. Kuwata ◽  
Y. Kondo
Keyword(s):  
Inorganic Salt ◽  
Cloud Condensation Nuclei ◽  
Input Parameter ◽  
Pitzer Model ◽  
Particle Mass ◽  
Mass Analyzer ◽  
Condensation Nuclei ◽  
Shape Factors ◽  
Critical Supersaturation ◽  
Dynamic Shape

Abstract. We measured the mobility equivalent critical dry diameter for cloud condensation nuclei (CCN) activation (dc_me) and the particle mass of size-selected (NH4)2SO4 and NaCl particles to calibrate a CCN counter (CCNC) precisely. The CCNC was operated downstream of a differential mobility analyzer (DMA) for the measurement of dc_me. The particle mass was measured using an aerosol particle mass analyzer (APM) operated downstream of the DMA. The measurement of particle mass was conducted for 50–150-nm particles. Effective densities (ρeff) of (NH4)2SO4 particles were 1.67–1.75 g cm−3, which correspond to dynamic shape factors (χ) of 1.01–1.04. This shows that (NH4)2SO4 particles are not completely spherical. In the case of NaCl particles, ρeff was 1.75–1.99 g cm−3 and χ was 1.05–1.14, demonstrating that the particle shape was non-spherical. Using these experimental data, the volume equivalent critical dry diameter (dc_ve) was calculated, and it was used as an input parameter for calculations of critical supersaturation (S). Several thermodynamics models were used for the calculation of water activity. When the Pitzer model was employed for the calculations, the critical S calculated for (NH4)2SO4 and NaCl agreed to well within the uncertainty of 2% (relative). This result demonstrates that the use of the Pitzer model for the calibration of CCNCs gives the most accurate value of S.

scholarly journals Tandem configuration of differential mobility and centrifugal particle mass analyzers for investigating aerosol hygroscopic properties

2016 ◽  
Author(s):  
Sergey S. Vlasenko ◽  
Hang Su ◽  
Ulrich Pöschl ◽  
Meinrat O. Andreae ◽  
Eugene F. Mikhailov
Keyword(s):  
Water Uptake ◽  
Aerosol Particles ◽  
Interaction Model ◽  
Particle Morphology ◽  
Particle Mass ◽  
Submicron Particles ◽  
Mass Analyzer ◽  
Hygroscopic Growth ◽  
Differential Mobility ◽  
Hygroscopic Properties

Abstract. A tandem arrangement of Differential Mobility Analyzer and Humidified Centrifugal Particle Mass Analyzer (DMA-HCPMA) was developed to measure the deliquescence and efflorescence thresholds and the water uptake of submicron particles over the relative humidity (RH) range from 10 % to 95 %. The hygroscopic growth curves obtained for Ammonium sulfate and sodium chloride test aerosols are consistent with thermodynamic model predictions and literature data. The DMA-HCPMA system was applied to measure the hygroscopic properties of urban aerosol particles, and the kappa mass interaction model (KIM) was used to characterize and parameterize the concentration-dependent water uptake observed in the 50–95 % RH range. For DMA-selected 160 nm dry particles (mass of 3.5 fg), we obtained a volume-based hygroscopicity parameter κv ≈ 0.2, which is consistent with literature data for freshly emitted urban aerosols. Overall, our results show that the DMA-HCPMA system can be used to measure size-resolved mass growth factors of atmospheric aerosol particles upon hydration and dehydration up to 95 % RH. The direct measurements of humidified particle mass allow avoiding complications that occur in the commonly used mobility-diameter-based HTDMA technique due to poorly defined particle morphology and density.

scholarly journals Experimentally measured morphology of biomass burning aerosol and its impacts on CCN ability

2014 ◽  
Vol 14 (9) ◽  
pp. 12555-12589
Author(s):  
M. Giordano ◽  
C. Espinoza ◽  
A. Asa-Awuku
Keyword(s):  
Biomass Burning ◽  
Cloud Condensation Nuclei ◽  
Morphological Characteristics ◽  
Particle Morphology ◽  
Morphological Data ◽  
Environmental Research ◽  
Mass Analyzer ◽  
Condensation Nuclei ◽  
Biomass Burning Aerosol ◽  
Dynamic Shape

Abstract. This study examines the morphological properties of freshly emitted and atmospherically aged aerosols from biomass burning. The impacts of particle morphology assumptions on hygroscopic predictions are examined. Chamber experiments were conducted at the UC-Riverside Center for Environmental Research and Technology (CE-CERT) Atmospheric Processes Lab using two biomass fuel sources, manzanita and chamise. Morphological data was obtained through the use of an aerosol particle mass analyzer (APM), scanning mobility particle sizer (SMPS) system and transmission electron microscopy (TEM). Data from these instruments was used to calculate both a dynamic shape factor and a fractal-like dimension for the biomass burning emissions. This data was then used with κ-Köhler theory to adjust the calculated hygroscopicity for experimentally determined morphological characteristics of the aerosol. Laboratory measurement of biomass burning aerosol from two chaparral fuels show that particles are non-spherical with dynamic shape factors greater than 1.15 for aerosol sizes relevant to cloud condensation nuclei (CCN) activation. Accounting for particle morphology can shift the hygroscopicity parameter κ by 0.15 or more. To our knowledge, this work provides the first laboratory chamber measurements of morphological characteristics for biomass burning cloud condensation nuclei and provides experimental particle shape evidence to support the variation in reported hygroscopicities of the complex aerosol.

scholarly journals Experimentally measured morphology of biomass burning aerosol and its impacts on CCN ability

2015 ◽  
Vol 15 (4) ◽  
pp. 1807-1821 ◽  
Author(s):  
M. Giordano ◽  
C. Espinoza ◽  
A. Asa-Awuku
Keyword(s):  
Biomass Burning ◽  
Cloud Condensation Nuclei ◽  
Morphological Characteristics ◽  
Particle Morphology ◽  
Morphological Data ◽  
Environmental Research ◽  
Mass Analyzer ◽  
Condensation Nuclei ◽  
Biomass Burning Aerosol ◽  
Dynamic Shape

Abstract. This study examines the morphological properties of freshly emitted and atmospherically aged aerosols from biomass burning. The impacts of particle morphology assumptions on hygroscopic predictions are examined. Chamber experiments were conducted at the University of California, Riverside, Center for Environmental Research and Technology (CE-CERT) atmospheric processes lab using two biomass fuel sources: manzanita and chamise. Morphological data was obtained through the use of an aerosol particle mass analyzer (APM), scanning mobility particle sizer (SMPS) system and transmission electron microscope (TEM). Data from these instruments was used to calculate both a dynamic shape factor and a fractal-like dimension for the biomass burning emissions. This data was then used with κ-Köhler theory to adjust the calculated hygroscopicity for experimentally determined morphological characteristics of the aerosol. Laboratory measurement of biomass burning aerosol from two chaparral fuels show that particles are nonspherical with dynamic shape factors greater than 1.15 for aerosol sizes relevant to cloud condensation nuclei (CCN) activation. Accounting for particle morphology can shift the hygroscopicity parameter by 0.15 or more. To our knowledge, this work provides the first laboratory chamber measurements of morphological characteristics for biomass burning cloud condensation nuclei and provides experimental particle shape evidence to support the variation in reported hygroscopicities of the complex aerosol.

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