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In Fig. 3c, jetting initiation time is the time it takes to observe the first aerosol dispersion after the droplet reaches the maximum diameter after impact.
We report here the first aerosol shock tube ignition delay time measurements of n-dodecane/O2/argon and JP-7/O2/argon mixtures.
Atmospheric aerosol alters the Earth's climate by absorbing and scattering radiation (the direct radiative effect, DRE) and through altering the albedo of clouds (the first aerosol indirect effect, AIE 11.
In fact, administration of an anti-IL-10 receptor monoclonal antibody before the first aerosol OVA challenge completely abolished the therapeutic effect (Figure 9C).
Tracheal aspirates were collected on day 3 after the first aerosol and during the following 24 hours.
The same patients were crossed-over to receive the alternate saline or albuterol treatment 6 hours after the first aerosol administration.
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A Fast Integrated Mobility Spectrometer (FIMS) has been developed for sub-second aerosol size distribution measurements based on the description presented in the preceding paper (Paper I).
Thus, MyD88−/−NOD mice immunized with OVA died (with asphyxia) within few hours following the first or the second aerosol challenge with OVA as compared to wild-type MyD88 sufficient NOD mice which regularly survived the three challenges (Figure 5A).
The entire procedure was repeated in 6 hours, with the second aerosol (either saline or albuterol) treatment.
The first period (H1 to H6) corresponds to the first six hours following the first day 3 aerosol, the second (H7 to H12) to the next six hours (before the second aerosol of the day), the third (H13 to H18) to the six hours following the second day 3 nebulization, and the fourth (H19 to H24) to the last six hours of the day, before the next aerosol.
First, higher aerosol concentrations should amplify the sky glow (particularly on cloud free nights), as aerosols increase the chance that light is scattered back to Earth.
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