Variations in gravity [head-to-foot acceleration (G(z))] induce hemodynamic
alterations as a consequence of changes in hydrostatic pressure gradients.
To estimate the contribution of the lower limbs to blood pooling or shifti
ng during the different gravity phases of a parabolic flight, we measured i
nstantaneous thigh and calf girths by using strain-gauge plethysmography in
five healthy volunteers. From these circumferential measurements, segmenta
l leg volumes were calculated at 1, 1.7, and 0 G(z). During hypergravity, l
eg segment volumes increased by 0.9% for the thigh (P < 0.001) and 0.5% for
the calf(P < 0.001) relative to 1-G(z) conditions. After sudden exposure t
o microgravity following hypergravity, leg segment volumes were reduced by
3.5% for the thigh (P < 0.001) and 2.5% for the calf (P < 0.001) relative t
o 1.7-G(z) conditions. Changes were more pronounced at the upper part of th
e leg. Extrapolation to the whole lower limb yielded an estimated 60-ml inc
rease in leg volume at the end of the hypergravity phase and a subsequent 2
25-ml decrease during microgravity. Although quantitatively less than previ
ous estimations, these blood shifts may participate in the hemodynamic alte
rations observed during hypergravity and weightlessness.