scholarly journals Review for Li et al.: Morphology, mixing state, and hygroscopicity of primary biological aerosol particles from a Chinese boreal forest

2019 ◽  
Author(s):  
Anonymous
2019 ◽  
Author(s):  
Weijun Li ◽  
Lei Liu ◽  
Qi Yuan ◽  
Liang Xu ◽  
Yanhong Zhu ◽  
...  

Abstract. Biological aerosols play an important role in atmospheric chemistry, clouds, climate, and public health. Here, we studied the morphology and composition of primary biological aerosol particles (PBAPs) collected in the Lesser Khingan Mountain boreal forest of China in summertime using transmission electron microscopy and scanning electron microscopy. Of all detected particles > 100 nm in diameter, 13 % by number were identified as PBAPs. In addition, 57 % of the PBAPs were identified as bacteria, followed by brochosomes (24 %) and fungi (19 %). The dominant size of bacteria was 1–4 μm, fungi was 2–4 μm, and brochosomes was 300–500 nm. The number size distribution of PBAPs coupled with the mass concentrations of PM2.5 and PM10 were used to estimate the total mass concentration of PBAPs, which is approximately 1.9 μg m−3 and accounts for 47 % of the in situ PM2.5–10 mass. C, N, O, P, K, and Si are detected in all PBAP particles, and P represented a major marker to identify PBAPs. Moreover, there is a higher frequency and concentration of PBAPs at night compared with day. Bacterial and fungal particles displayed weak hygroscopicity with a growth factor of ~ 1.09 at RH = 94 %. Electron microscopy shows that approximately 20 % of the bacterial particles were internally mixed with metal, mineral dust, and inorganic salts in the boreal forest air. This work provides a database for both further understanding physicochemical state of individual PBAP particles from natural sources and expanding the scope of atmospheric implications.


Author(s):  
Jose Ruiz-Jimenez ◽  
Magdalena Okuljar ◽  
Outi-Maaria Sietiö ◽  
Giorgia Demaria ◽  
Thanaporn Liangsupree ◽  
...  

Indoor Air ◽  
2018 ◽  
Vol 28 (4) ◽  
pp. 559-571 ◽  
Author(s):  
Y. Tian ◽  
Y. Liu ◽  
P. K. Misztal ◽  
J. Xiong ◽  
C. M. Arata ◽  
...  

2018 ◽  
Vol 18 (20) ◽  
pp. 15437-15450 ◽  
Author(s):  
Matthias Hummel ◽  
Corinna Hoose ◽  
Bernhard Pummer ◽  
Caroline Schaupp ◽  
Janine Fröhlich-Nowoisky ◽  
...  

Abstract. Primary ice formation, which is an important process for mixed-phase clouds with an impact on their lifetime, radiative balance, and hence the climate, strongly depends on the availability of ice-nucleating particles (INPs). Supercooled droplets within these clouds remain liquid until an INP immersed in or colliding with the droplet reaches its activation temperature. Only a few aerosol particles are acting as INPs and the freezing efficiency varies among them. Thus, the fraction of supercooled water in the cloud depends on the specific properties and concentrations of the INPs. Primary biological aerosol particles (PBAPs) have been identified as very efficient INPs at high subzero temperatures, but their very low atmospheric concentrations make it difficult to quantify their impact on clouds. Here we use the regional atmospheric model COSMO–ART to simulate the heterogeneous ice nucleation by PBAPs during a 1-week case study on a domain covering Europe. We focus on three highly ice-nucleation-active PBAP species, Pseudomonas syringae bacteria cells and spores from the fungi Cladosporium sp. and Mortierella alpina. PBAP emissions are parameterized in order to represent the entirety of bacteria and fungal spores in the atmosphere. Thus, only parts of the simulated PBAPs are assumed to act as INPs. The ice nucleation parameterizations are specific for the three selected species and are based on a deterministic approach. The PBAP concentrations simulated in this study are within the range of previously reported results from other modeling studies and atmospheric measurements. Two regimes of PBAP INP concentrations are identified: a temperature-limited and a PBAP-limited regime, which occur at temperatures above and below a maximal concentration at around −10 ∘C, respectively. In an ensemble of control and disturbed simulations, the change in the average ice crystal concentration by biological INPs is not statistically significant, suggesting that PBAPs have no significant influence on the average state of the cloud ice phase. However, if the cloud top temperature is below −15 ∘C, PBAP can influence the cloud ice phase and produce ice crystals in the absence of other INPs. Nevertheless, the number of produced ice crystals is very low and it has no influence on the modeled number of cloud droplets and hence the cloud structure.


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