Laviolette M, Cormier Y
Respir Physiol. 1980 Sep;41(3):267-77. doi: 10.1016/0034-5687(80)90076-6.
To investigate the genesis of cardiogenic oscillations (C.O.) and the slopes of the single-breath nitrogen test, we studied ten healthy volunteers with a modified test. This test utilized incremental volumes of air from 10% to 100% vital capacity (VC) after a nitrogen washout with oxygen. Subjects exhaled to residual volume, inspired the air volume and completed a full inspiration with oxygen. C.O. and both slopes were positive with low air volumes and negative with a VC of air. The slope of phase IV showed a linear decrease with the increasing inspired air volume, and reached zero with an air volume of 38% VC. AT higher volumes it became progressively more negative. The slope of phase III and C.O. were highly positive with 10% to 50% VC air volume then subsequently decreased. The values for C.O. and the slope of phase III were significantly different (P < 0.001) from those of the slop of phase IV and the apex-base gradients predicted by the model of Milic-Emili et al. These results suggest that intraregional gradients are significantly involved in the genesis of C.O. and the slop of phase III.
为了研究心源性振荡(C.O.)的起源以及单次呼吸氮试验的斜率,我们采用改良试验对10名健康志愿者进行了研究。该试验在氧气洗出氮气后,使用从10%到100%肺活量(VC)递增的气量。受试者呼气至残气量,吸入该气量并完成一次用氧气的完全吸气。在气量较低时,C.O.和两个斜率均为正值,而在吸入气量达到肺活量时为负值。第四阶段的斜率随吸入气量增加呈线性下降,当吸入气量为肺活量的38%时降至零。在更高的气量时,其变得越来越负。第三阶段的斜率和C.O.在吸入气量为肺活量的10%至50%时为高度正值,随后下降。C.O.的值和第三阶段的斜率与米利奇 - 埃米利等人模型预测的第四阶段斜率和心尖 - 心底梯度的值有显著差异(P < 0.001)。这些结果表明,区域内梯度在心源性振荡的起源和第三阶段斜率中起重要作用。