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首页> 外文期刊>Cardiovascular engineering >On the mechanics underlying the reservoir-excess separation in systemic arteries and their implications for pulse wave analysis.
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On the mechanics underlying the reservoir-excess separation in systemic arteries and their implications for pulse wave analysis.

机译:关于系统性动脉过多储层分离的机理及其对脉搏波分析的意义。

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Several works have separated the pressure waveform p in systemic arteries into reservoir p(r) and excess p(exc) components, p = p(r) + p(exc), to improve pulse wave analysis, using windkessel models to calculate the reservoir pressure. However, the mechanics underlying this separation and the physical meaning of p(r) and p(exc) have not yet been established. They are studied here using the time-domain, inviscid and linear one-dimensional (1-D) equations of blood flow in elastic vessels. Solution of these equations in a distributed model of the 55 larger human arteries shows that p(r) calculated using a two-element windkessel model is space-independent and well approximated by the compliance-weighted space-average pressure of the arterial network. When arterial junctions are well-matched for the propagation of forward-travelling waves, p(r) calculated using a three-element windkessel model is space-dependent in systole and early diastole and is made of all the reflected waves originated at the terminal (peripheral) reflection sites, whereas p(exc) is the sum of the rest of the waves, which are obtained by propagating the left ventricular flow ejection without any peripheral reflection. In addition, new definitions of the reservoir and excess pressures from simultaneous pressure and flow measurements at an arbitrary location are proposed here. They provide valuable information for pulse wave analysis and overcome the limitations of the current two- and three-element windkessel models to calculate p(r).
机译:多项工作将全身动脉的压力波形p分为储层p(r)和多余的p(exc)分量p = p(r)+ p(exc),以改进脉搏波分析,使用windkessel模型计算储层压力。但是,尚未确定这种分离的机制以及p(r)和p(exc)的物理含义。在这里使用弹性血管中血流的时域,无粘性和线性一维(1-D)方程进行研究。在55个较大的人体动脉的分布式模型中对这些方程的求解表明,使用二元风向标模型计算的p(r)与空间无关,并且可以通过顺应加权的动脉网络平均空间压力很好地近似。当动脉交界点与向前行进波的传播完全匹配时,使用三元素风向标模型计算的p(r)在收缩期和早期舒张期与空间有关,并且由起源于末端的所有反射波组成( p(exc)是其余波的总和,这些波是通过传播左心室射流而无任何外围反射而获得的。此外,在此提出了新的储层定义以及在任意位置同时进行压力和流量测量得出的过压。它们为脉搏波分析提供了有价值的信息,并克服了当前两元素和三元素风帆模型计算p(r)的局限性。

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