Darquenne, Chantal, Manuel Paiva, and G. Kim Prisk. Effect of gravity on aerosol dispersion and deposition in the human lung after periods of breath holding. J Appl Physiol 89: 1787-1792, 2000.-To determine the extent of the role that gravity plays in dispersion and deposition during breath holds, we performed aerosol bolus inhalations of 1-m-diameter particles followed by breath holds of various lengths on four subjects on the ground (1G) and during short periods of microgravity (G). Boluses of ϳ70 ml were inhaled to penetration volumes (V p ) of 150 and 500 ml, at a constant flow rate of ϳ0.45 l/s. Aerosol concentration and flow rate were continuously measured at the mouth. Aerosol deposition and dispersion were calculated from these data. Deposition was independent of breath-hold time at both V p in G, whereas, in 1G, deposition increased with increasing breath hold time. At V p ϭ 150 ml, dispersion was similar at both gravity levels and increased with breath hold time. At V p ϭ 500 ml, dispersion in 1G was always significantly higher than in G. The data provide direct evidence that gravitational sedimentation is the main mechanism of deposition and dispersion during breath holds. The data also suggest that cardiogenic mixing and turbulent mixing contribute to deposition and dispersion at shallow V p . aerosol bolus; cardiogenic mixing AEROSOL BOLUS INHALATIONS have largely been used to study deposition and mixing processes in specific volumetric regions of the lung (3,4,13,19). Particles are transported in the respiratory tract by the carrier gas, and they deviate from the streamlines mainly by diffusion, sedimentation, and inertia. Of these mechanisms, sedimentation is the only mechanism that is directly affected by a change in the gravity (G) level. The deposition and dispersion of aerosol boluses inhaled in microgravity (G) therefore differ from those inhaled in normal gravity (1G) because sedimentation plays a role in these processes. This has been shown by our group in previous studies (7,8), in which aerosol bolus inhalations with no breath hold before the subsequent exhalation were performed in G, 1G, and 1.6G. In these studies, both aerosol deposition (DE) and dispersion (H) increased with increasing G level, and this effect was more pronounced in the alveolar region of the lung than in the large airways.In the present study, we performed bolus inhalations of 1-m-diameter particles, followed by breath holds of various lengths, up to 5 s. The tests were performed on the ground (1G) and during short periods of G aboard the NASA Microgravity Research Aircraft, to determine the extent of the role that gravity plays in DE and H during breath holds. We show that gravitational sedimentation is the principal mechanism of DE during breath holding. The data also suggest that cardiogenic mixing contributes to DE and H and that the effect is larger in the central airways than in the alveolar region.
METHODS
Equipment.Aerosol bolus data were collected with the same equipment used in previous studies (7,8). The eq...