Influence of gravity on pulmonary venous flow velocity patterns: Analysis of left and right pulmonary venous flow velocities in left and right decubitus positions
C. Izumi et al., Influence of gravity on pulmonary venous flow velocity patterns: Analysis of left and right pulmonary venous flow velocities in left and right decubitus positions, AM HEART J, 137(3), 1999, pp. 419-426
Citations number
14
Categorie Soggetti
Cardiovascular & Respiratory Systems","Cardiovascular & Hematology Research
Background The pulmonary venous flow signal measured by transesophageal ech
ocardiography is generally recorded from the left upper pulmonary vein in t
he left lateral decubitus position, whereas that by transthoracic echocardi
ography is from the right upper pulmonary vein in the left semi-lateral dec
ubitus position. The purpose of this study was to evaluate the influence of
the postural change on the peak flow velocities of the left and right pulm
onary veins and whether the parameters of the left and right pulmonary veno
us flow can be used interchangeably
Methods and Results The study group consisted of 37 patients with normal le
ft ventricular filling pressure and in whom the systolic forward flow signa
ls From both pulmonary veins recorded in the left and right lateral decubit
us positions were clear enough to differentiate as biphasic. The peak early
systolic (peak S1) and diastolic velocities were significantly increased w
hen the pulmonary vein was on the recumbent subject's upper side, whereas t
he peak late systolic velocity (peak S2) was significantly increased when t
he pulmonary vein was on the recumbent subject's lower side. The peak S1 wa
s higher than the peak S2 when the pulmonary vein was on the recumbent subj
ect's upper side, whereas the reverse relation was seen when the pulmonary
vein was on the recumbent subject's lower side.
Conclusions We should take into consideration the body position and the sid
e on which the pulmonary vein is situated in evaluating the peak flow veloc
ities of the pulmonary veins.