DOES SYSTOLIC SUBEPICARDIAL PERFUSION COME FROM RETROGRADE SUBENDOCARDIAL FLOW

被引:52
作者
FLYNN, AE
COGGINS, DL
GOTO, M
ALDEA, GS
AUSTIN, RE
DOUCETTE, JW
HUSSEINI, W
HOFFMAN, JIE
机构
[1] UNIV CALIF SAN FRANCISCO, CARDIOVASC RES INST, BOX 0544, HSE 1403, SAN FRANCISCO, CA 94143 USA
[2] UNIV CALIF SAN FRANCISCO, DEPT SURG, SAN FRANCISCO, CA 94143 USA
[3] UNIV CALIF SAN FRANCISCO, DEPT PEDIAT, SAN FRANCISCO, CA 94143 USA
来源
AMERICAN JOURNAL OF PHYSIOLOGY | 1992年 / 262卷 / 06期
关键词
MODEL OF CORONARY BLOOD FLOW DISTRIBUTION; CARBOCHROMEN; ADENOSINE; DOPPLER VELOCIMETER; RADIOLABELED MICROSPHERES;
D O I
10.1152/ajpheart.1992.262.6.H1759
中图分类号
Q4 [生理学];
学科分类号
071003 ;
摘要
To examine the influence of cardiac contraction on systolic coronary flow and transmural blood flow distribution, we measured phasic blood flow velocity in distal extramural coronary arteries by Doppler velocimeter and regional myocardial blood flow by radiolabeled microspheres while the heart was beating and during prolonged diastoles in 12 dogs. A servo-controlled coronary perfusion circuit allowed mean coronary pressure to be selected and maintained during beating and diastolic conditions. In epicardial arteries just proximal to their entrance into the myocardium, blood flow was either negligible or reverse in direction during systole. When the heart was beating, subepicardial blood flow was 24.2 +/- 12.3% higher than during asystole (5.05 +/- 0.91 and 4.11 +/- 0.79 ml.min-1.g-1 for beating and prolonged diastoles, respectively; P < 0.01). In the subendocardium, flow was 49.8 +/- 14.7% lower in the beating condition than during prolonged diastoles (4.23 +/- 1.46 and 8.26 +/- 1.71 ml.min-1.g-1 for beating and asystole, respectively; P < 0.01). When heart rate was increased stepwise from 60 to 150 beats/min, subendocardial flow fell approximately linearly; flow to the superficial layer was relatively unaffected. In beating hearts, lowering mean left main coronary artery (LMCA) pressure from 80 to 50 mmHg resulted in more systolic reverse flow and a fall in inner-to-outer flow ratio from 0.82 +/- 0.18 to 0.66 +/- 0.34 (P < 0.05). Because mean LMCA pressure was held constant when the heart was stopped, differences in regional blood flow between beating and diastolic conditions were primarily due to cardiac contraction. Because little or no blood entered the myocardium from the extramural arteries during systole, we conclude that the decrease in subendocardial flow and the increase in subepicardial flow were caused by retrograde pumping of blood from the deep layer to the superficial layer of the left ventricle. Systolic retrograde flow to the subepicardium may help explain this layer's relative protection from ischemia.
引用
收藏
页码:H1759 / H1769
页数:11
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