期刊
ACS CENTRAL SCIENCE
卷 7, 期 1, 页码 200-209出版社
AMER CHEMICAL SOC
DOI: 10.1021/acscentsci.0c01522
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资金
- University of Bristol
- Elizabeth Blackwell Institute for Health Research
- Natural Environment Research Council [NE/P018459/1]
- European Research Council [ERC-COG: 648239]
- NERC [NE/P018459/1] Funding Source: UKRI
Aerosols and droplets expelled during respiratory events are crucial in transmitting pathogens, but there are uncertainties in understanding the microphysics of aerosol droplets. Research shows that sedimentation outcomes vary in sensitivity to composition and environmental conditions based on droplet size, with evaporation process nature playing a key role in influencing the outcome.
Aerosols and droplets from expiratory events play an integral role in transmitting pathogens such as SARS-CoV-2 from an infected individual to a susceptible host. However, there remain significant uncertainties in our understanding of the aerosol droplet microphysics occurring during drying and sedimentation and the effect on the sedimentation outcomes. Here, we apply a new treatment for the microphysical behavior of respiratory fluid droplets to a droplet evaporation/sedimentation model and assess the impact on sedimentation distance, time scale, and particle phase. Above a 100 mu m initial diameter, the sedimentation outcome for a respiratory droplet is insensitive to composition and ambient conditions. Below 100 mu m, and particularly below 80 mu m, the increased settling time allows the exact nature of the evaporation process to play a significant role in influencing the sedimentation outcome. For this size range, an incorrect treatment of the droplet composition, or imprecise use of RH or temperature, can lead to large discrepancies in sedimentation distance (with representative values >1 m, >2 m, and >2 m, respectively). Additionally, a respiratory droplet is likely to undergo a phase change prior to sedimenting if initially <100 mu m in diameter, provided that the RH is below the measured phase change RH. Calculations of the potential exposure versus distance from the infected source show that the volume fraction of the initial respiratory droplet distribution, in this size range, which remains elevated above 1 m decreases from 1 at 1 m to 0.125 at 2 m.
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