scholarly journals Estimation of Mean Left Atrial Pressure From Transesophageal Pulsed Doppler Echocardiography of Pulmonary Venous Flow

1991 ◽  
Vol 7 (2) ◽  
pp. 104-104
Circulation ◽  
1990 ◽  
Vol 82 (4) ◽  
pp. 1127-1139 ◽  
Author(s):  
H F Kuecherer ◽  
I A Muhiudeen ◽  
F M Kusumoto ◽  
E Lee ◽  
L E Moulinier ◽  
...  

1993 ◽  
Vol 72 (14) ◽  
pp. 1089-1093 ◽  
Author(s):  
Akira Kisanuki ◽  
Kunihiko Shibata ◽  
Yutaka Otsuji ◽  
Ryuichi Kuroiwa ◽  
Takashi Murayarna ◽  
...  

1998 ◽  
Vol 21 (10) ◽  
pp. 753-758 ◽  
Author(s):  
Takashi Oki ◽  
Tomotsugu Tabata ◽  
Hirotsugu Yamada ◽  
Kazuyo Fukuda ◽  
Miho Abe ◽  
...  

1990 ◽  
Vol 70 (Supplement) ◽  
pp. S277
Author(s):  
I. A. Muhiudeen ◽  
H. F. Kuecherer ◽  
N. B. Schiller ◽  
M. K. Cahalan

Cardiology ◽  
1996 ◽  
Vol 87 (3) ◽  
pp. 224-229 ◽  
Author(s):  
Jer-Min Lin ◽  
Yi-Heng Li ◽  
Kwan-Lih Hsu ◽  
Juey-Jen Hwang ◽  
Yung-Zu Tseng

2000 ◽  
Vol 279 (2) ◽  
pp. H594-H600 ◽  
Author(s):  
Michael S. Firstenberg ◽  
Neil L. Greenberg ◽  
Nicholas G. Smedira ◽  
David L. Prior ◽  
Gregory M. Scalia ◽  
...  

The simplified Bernoulli equation relates fluid convective energy derived from flow velocities to a pressure gradient and is commonly used in clinical echocardiography to determine pressure differences across stenotic orifices. Its application to pulmonary venous flow has not been described in humans. Twelve patients undergoing cardiac surgery had simultaneous high-fidelity pulmonary venous and left atrial pressure measurements and pulmonary venous pulsed Doppler echocardiography performed. Convective gradients for the systolic (S), diastolic (D), and atrial reversal (AR) phases of pulmonary venous flow were determined using the simplified Bernoulli equation and correlated with measured actual pressure differences. A linear relationship was observed between the convective ( y) and actual ( x) pressure differences for the S ( y = 0.23 x + 0.0074, r = 0.82) and D ( y = 0.22 x + 0.092, r = 0.81) waves, but not for the AR wave ( y = 0.030 x + 0.13, r = 0.10). Numerical modeling resulted in similar slopes for the S ( y = 0.200 x − 0.127, r = 0.97), D ( y = 0.247 x − 0.354, r= 0.99), and AR ( y = 0.087 x − 0.083, r = 0.96) waves. Consistent with numerical modeling, the convective term strongly correlates with but significantly underestimates actual gradient because of large inertial forces.


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