Kanner R E, Crapo R O
Am Rev Respir Dis. 1986 Apr;133(4):676-8. doi: 10.1164/arrd.1986.133.4.676.
The effects of alveolar oxygen tension (PAO2) on the single-breath carbon monoxide diffusing capacity (DLCO) were quantified and a factor was derived to accommodate for differences in PAO2 over commonly encountered altitudes and/or varying concentrations of oxygen in the test gas mixture (FIO2) We performed duplicate measurements of DLCO in 7 normal subjects with 6 different oxygen fractions (0.176, 0.196, 0.211, 0.22, 0.25, and 0.27). The PAO2 for each test was measured as the PO2 in the alveolar gas sample bag. DLCO varied inversely with PAO2 and changed by 0.35% for each mmHg change in PAO2 (r = -0.62, p less than 0.001). At an FIO2 of 0.25, PAO2 varied between subjects and was highly correlated with each subject's residual volume to total lung capacity ratio (r = -0.84, p less than 0.001). We suggest that laboratories can adjust the measured DLCO when PAO2 is not congruent to 120 mmHg by the following formula: DLCO (corrected = DLCO (measured) x [1.0 + 0.0035 (PAO2 - 120)].
对肺泡氧分压(PAO2)对单次呼吸一氧化碳弥散量(DLCO)的影响进行了量化,并推导出一个因子,以适应常见海拔高度下PAO2的差异和/或测试气体混合物中氧气浓度(FIO2)的变化。我们对7名正常受试者进行了重复测量,使用6种不同的氧分数(0.176、0.196、0.211、0.22、0.25和0.27)测量DLCO。每次测试的PAO2作为肺泡气样本袋中的PO2进行测量。DLCO与PAO2呈反比变化,PAO2每变化1 mmHg,DLCO变化0.35%(r = -0.62,p < 0.001)。在FIO2为0.25时,PAO2在受试者之间存在差异,并且与每个受试者的残气量与肺总量之比高度相关(r = -0.84,p < 0.001)。我们建议,当PAO2不等于120 mmHg时,实验室可以通过以下公式调整测量的DLCO:DLCO(校正后)= DLCO(测量值)×[1.0 + 0.0035(PAO2 - 120)] 。