Department of Medicine, University of California, San Diego, La Jolla, California 92093-0623, USA.
J Appl Physiol (1985). 2013 Aug 15;115(4):546-55. doi: 10.1152/japplphysiol.01520.2012. Epub 2013 Jun 6.
Lung deposition of >0.5-μm particles is strongly influenced by gravitational sedimentation, with deposition being reduced in microgravity (μG) compared with normal gravity (1G). Gravity not only affects total deposition, but may also alter regional deposition. Using gamma scintigraphy, we measured the distribution of regional deposition and retention of radiolabeled particles ((99m)Tc-labeled sulfur colloid, 5-μm diameter) in five healthy volunteers. Particles were inhaled in a controlled fashion (0.5 l/s, 15 breaths/min) during multiple periods of μG aboard the National Aeronautics and Space Administration Microgravity Research Aircraft and in 1G. In both cases, deposition scans were obtained immediately postinhalation and at 1 h 30 min, 4 h, and 22 h postinhalation. Regional deposition was characterized by the central-to-peripheral ratio and by the skew of the distribution of deposited particles on scans acquired directly postinhalation. Relative distribution of deposition between the airways and the alveolar region was derived from data acquired at the various time points. Compared with inhalation in 1G, subjects show an increase in central-to-peripheral ratio (P = 0.043), skew (P = 0.043), and tracheobronchial deposition (P < 0.001) when particles were inhaled in μG. The absence of gravity caused fewer particles to deposit in the lung periphery than in the central region where deposition occurred mainly in the airways in μG. Furthermore, the increased skew observed in μG likely illustrates the presence of localized areas of deposition, i.e., "hot spots", resulting from inertial impaction. In conclusion, gravity has a significant effect on deposition patterns of coarse particles, with most of deposition occurring in the alveolar region in 1G but in the large airways in μG.
大于 0.5 微米的颗粒在肺部的沉积强烈受到重力沉降的影响,在微重力(μG)下的沉积量比正常重力(1G)下的沉积量要少。重力不仅影响总沉积量,还可能改变区域沉积。我们使用伽马闪烁法测量了 5 名健康志愿者吸入放射性标记颗粒((99m)Tc 标记的硫胶体,直径 5μm)后的局部沉积和保留情况。颗粒在受控的条件下以 0.5 l/s、15 次呼吸/分钟的速度吸入,吸入过程分别在 NASA 微重力研究飞机上的μG 条件下和 1G 条件下进行。在这两种情况下,吸入后立即和吸入后 1 小时 30 分钟、4 小时和 22 小时进行沉积扫描。局部沉积情况由中央到外周的比值和直接吸入后扫描时沉积颗粒的分布偏度来描述。从各个时间点获取的数据推导出了沉积在气道和肺泡区域之间的相对分布。与在 1G 条件下的吸入相比,在μG 条件下吸入时,受试者的中央到外周的比值(P = 0.043)、偏度(P = 0.043)和气管支气管沉积(P < 0.001)增加。在没有重力的情况下,与中央区域相比,较少的颗粒沉积在肺部外周,而在μG 中,主要在气道中发生的沉积则集中在中央区域。此外,在μG 中观察到的偏度增加可能表明存在局部沉积区域,即“热点”,这是由于惯性冲击造成的。总之,重力对粗颗粒的沉积模式有显著影响,在 1G 条件下,大部分沉积发生在肺泡区域,而在μG 条件下,大部分沉积发生在大气道。