Pulmonary diffusing capacity and capillary blood volume in aging dogs.

Single-breath carbon monoxide diffusing capacity (DLco), pulmonary capillary blood volume (Vc), and membrane diffusing capacity (Dm) were measured in 24 beagle dogs aged 289-3,882 days. DLco and Vc were a function of age and alveolar volume (Va). Vc decreased with age resulting in changes in DLco. Changes in Vc may have been due to pulmonary morphological changes or to an exaggerated decrease in pulmonary blood flow in old dogs in response to 20-30 cmH-2O transpulmonary pressure. There was no age-related change in Dm.     

Pulmonary diffusing capacity and pulmonary capillary blood volume during parabolic flights

Vaïda, Pierre, Christian Kays, Daniel Rivière,Pierre Téchoueyres, and Jean-Luc Lachaud.Pulmonary diffusing capacity and pulmonary capillary blood volumeduring parabolic flights. J. Appl.Physiol. 82(4): 1091-1097, 1997.Data from theSpacelab Life Sciences-1 (SLS-1) mission have shown sustained butmoderate increase in pulmonary diffusing capacity(DL). Because of the occupational constraints of the mission, data were only obtained after24 h of exposure to microgravity. Parabolic flights are often used tostudy some effects of microgravity, and we measured changes inDL occurring at the very onsetof weightlessness. Measurements ofDL, membrane diffusing capacity,and pulmonary capillary blood volume were made in 10 male subjectsduring the 20-s 0-G phases of parabolic flights performed by the"zero-G" Caravelle aircraft. Using the standardized single-breathtechnique, we measuredDL for CO andnitric oxide simultaneously. We found significant increases inDL for CO (62%),in membrane diffusing capacity for CO (47%), inDL for nitric oxide (47%), andin pulmonary capillary blood volume (71%). We conclude that majorchanges in the alveolar membrane gas transfers and in the pulmonarycapillary bed occur at the very onset of microgravity. Because thesechanges are much greater than those reported during sustainedmicrogravity, the effects of rapid transition from hypergravity tomicrogravity during parabolic flights remain questionable.

     

Pulmonary capillary recruitment during airway hypoxia in the dog.

To study the effect of hypoxia on the pulmonary capillaries, windows were inserted in the chest wall of 9 pentobarbital-anesthetized dogs. A microscope with an image-superimposing device was used to make drawings of the perfused capillaries. Summed lengths of individual perfused capillaries in the drawing were determined with a map-measuring tool. Total capillary length was constant between PaO2 of 160 and 70 Torr. As PaO2 fell below 70 Torr, recruitment of previously unperfused capillaries occurred in every case; at PaO2 of 40 Torr, the total length of perfused capillaries was about 4 times greater than during normoxia. There was no correlation between the recruitment of capillaries and alterations in left atrial pressure, only a weak correlation with cardiac output changes, but a very strong correlation with increased pulmonary artery pressure. This implies that recruitment was probably caused by vasoconstriction within the lung.     

Pulmonary capillary blood volume and membrane conductance in Andeans and lowlanders at high altitude: A cross-sectional study

Lung carbon monoxide (CO) transfer and pulmonary capillary blood volume (Vc) at high altitudes have been reported as being higher in native highlanders compared to acclimatised lowlanders but large discrepancies appears between the studies. This finding raises the question of whether hypoxia induces pulmonary angiogenesis.Eighteen highlanders living in Bolivia and 16 European lowlander volunteers were studied. The latter were studied both at sea level and after acclimatisation to high altitude. Membrane conductance (Dm_CO) and Vc, corrected for the haemoglobin concentration (Vc_cor), were calculated using the NO/CO transfer technique. Pulmonary arterial pressure and left atrial pressures were estimated using echocardiography.Highlanders exhibited significantly higher NO and CO transfer than acclimatised lowlanders, with Vc_cor/VA and Dm_CO/VA being 49 and 17% greater (VA: alveolar volume) in highlanders, respectively. In acclimatised lowlanders, Dm_CO and Dm_CO/VA values were lower at high altitudes than at sea level. Echocardiographic estimates of cardiac output and pulmonary arterial pressure were significantly elevated at high altitudes as compared to sea level.The decrease in Dm_CO in lowlanders might be due to altered gas transport in the airways due to the low density of air at high altitudes. The disproportionate increase in Vc in Andeans compared to the change in Dm_CO suggests that the recruitment of capillaries is associated with a thickening of the blood capillary sheet. Since there was no correlation between the increase in Vc and the slight alterations in haemodynamics, this data suggests that chronic hypoxia might stimulate pulmonary angiogenesis in Andeans who live at high altitudes.