Aerosols and Viruses - COVID-19
Floating aerosols, a suspension of fine solid particles or liquid droplets in air or another gas, might contain viruses like the Covid-19.
The Nebulizer unit spreads the Biolight water - ASANTO detergent solution into the closed space.
The absolute humidity increases to a certain extent. The floating aerosol liquid droplets grow, become heavier and sink towards the ground, thereby reducing the direct potential infectious respiratory working of a virus like Covid-19.
Biolight energizes the air humidity and the virus is eliminated by the ASANTO solution.
comfortandmore recommends any quality micro-process-controlled humidifier
like a Solis Ultrasonic Pure Type 7217.
COVID-19 Viral Entry. “The Science of humidity of a parcel of air”
SARS-CoV-2 can enter the human body by inhaled respiratory aerosols and droplets containing viral particles, and by contact with contaminated surfaces, although the importance of this second possible mode of infection has not been established. SARS-CoV-2 particles have been shown to be stable and remain infectious for hours in aerosols or even days on surfaces (van Doremalen N, Bushmaker T, Morris DH, Holbrook MG, Gamble A, Williamson BN, et al. Aerosol and surface stability of SARS-CoV-2 as compared with SARS-CoV-1. N Engl J Med. (2020) 382:1564–67. doi: 10.1056/NEJMc2004973)
https://www.frontiersin.org/articles/10.3389/fimmu.2020.01131/full?utm_campaign=ba-cov-sci-fimmu-lessons-learned&utm_medium=cvlp&utm_source=fweb
Aerosols are approx. 5 μm (micron, 10−6 meter). An aerosol (abbreviation of "aero-solution") is a suspension of fine solid particles or liquid droplets in air or another gas. Examples of natural aerosols are fog, mist, dust, forest exudates and geyser steam. Examples of anthropogenic (means: caused by human being) aerosols are particulate air pollutants and smoke. The amount of water vapor needed to achieve saturation increases as the temperature increases. As the temperature of a parcel of air decreases it will eventually reach the saturation point without adding or losing water mass. The amount of water vapor contained within a parcel of air can vary significantly. For example, a parcel of air near saturation may contain 28 grams of water per cubic metre of air at 30 °C, but only 8 grams of water per cubic metre of air at 8 °C.
