2010
DOI: 10.1016/j.jviromet.2009.12.004
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A mathematical model for predicting the viability of airborne viruses

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Cited by 26 publications
(30 citation statements)
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“…Efflorescence or crystallization of NaCl, a major component of respiratory droplets, due to loss of water is expected to occur between 40–50% RH [24]. According to our results, between 10–40% RH, D eq / D i varies by only 3.7% (0.402–0.417); in comparison, between 50–90% RH, the ratio varies by 21.7% (0.424–0.516).…”
Section: Resultssupporting
confidence: 45%
“…Efflorescence or crystallization of NaCl, a major component of respiratory droplets, due to loss of water is expected to occur between 40–50% RH [24]. According to our results, between 10–40% RH, D eq / D i varies by only 3.7% (0.402–0.417); in comparison, between 50–90% RH, the ratio varies by 21.7% (0.424–0.516).…”
Section: Resultssupporting
confidence: 45%
“…According to Posada et al (2010), the inactivation rate of viruses in an aerosol can be described by:…”
Section: Virusesmentioning
confidence: 99%
“…As evaporation proceeds, the water vapor pressure at the surface, which is proportional to the molar fraction of water in the aerosol (Raoult's Law), decreases because water is lost to evaporation while solutes such as salts and proteins remain. Evaporation ceases when the vapor pressure at the aerosol's surface is reduced to that of ambient air, a point at which the water activity of the aerosol equals the ambient RH (42). The extent to which an aerosol evaporates depends on its solute content and RH, and the final size can be calculated using mathematical models based on thermodynamics and fluid mechanics (32,39,44).…”
Section: Rh Evaporation and Water Activitymentioning
confidence: 99%