关于全身动脉中储层-过量分离的机制及其对脉搏波分析的意义。

Jordi Alastruey
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引用次数: 39

摘要

有研究将系统动脉压力波形p分成储层p(r)和多余p(exc)分量,p = p(r) + p(exc),以改进脉冲波分析,利用风帆模型计算储层压力。然而,这种分离的机制以及p(r)和p(exc)的物理意义尚未确定。他们在这里研究使用时域,无粘和线性一维(1-D)方程的血液流动弹性血管。这些方程在55个较大的人体动脉分布模型中的解表明,使用二元风帆模型计算的p(r)与空间无关,并且可以很好地近似于动脉网络的顺性加权空间平均压力。当动脉连接处与前向行波的传播匹配良好时,使用三元素风筒模型计算的p(r)在收缩期和舒张期早期依赖于空间,由来自末端(外周)反射部位的所有反射波组成,而p(exc)是其余波的总和,这些波是通过传播左心室血流射血而获得的,没有任何外周反射。此外,本文还提出了在任意位置同时测量压力和流量所产生的储层和超压的新定义。它们为脉冲波分析提供了有价值的信息,并克服了当前二元和三元风帆模型计算p(r)的局限性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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On the mechanics underlying the reservoir-excess separation in systemic arteries and their implications for pulse wave analysis.

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).

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