Ventilation Perfusion Mismatching
At rest, alveolar
ventilation and pulmonary
blood flow are
similar, each being around 5 L/min. Ventilation (V- A) and perfusion (Q-
) may vary in different lung regions, but for optimal gas exchange they must be
matched.
Areas with high
perfusion need high
ventilation, and, ideally, local
ventilation-perfusion ratios (VA/Q) should
be close to 1. Ventilation-perfusion mismatching or inequality
is said to occur when regional VA/Q ratios vary, with many being
much greater or less than 1 (Fig. 14a). A right-to-left shunt from complete
collapse or consolidation of a region (Chapter 13) has VA/Q = 0, and can be viewed as
an extreme example of ventilation-perfusion mismatching.
At the other extreme, alveolar dead space from a
pulmonary embolus is a ventilated region without perfusion and VA/Q
= ∞. Regions where VA/Q is much greater than 1 have excessive
ventilation or dead space effect and blood from
them has a high Po2 and a low Pco2. Regions
with VA/Q much less than 1 behave qualitatively like shunts and are
sources of shunt effect or venous admixture. Blood draining them
has undergone some gas exchange, but Po2 is lower and Pco2
higher than normal. The effect on Po2 and O2
content draining different VA/Q regions both during air breathing
and during oxygen breathing is shown in Fig. 14a (lower panel).
Effect of the upright posture on perfusion,
ventilation and VA/Q (Fig. 14b)
Hydrostatic pressure in all vessels varies with vertical
height above or below the heart because of the weight of blood. On standing,
the increased pressure at the lung bases distends vessels, increasing f ow.
Pressures generated by the right side of the heart are low, and higher up the
lung vascular pressures in diastole may fall below alveolar pressure at the
venous end of the pulmonary capillary. In such regions, fl w is reduced and
determined by the difference between arterial and alveolar pressure. There may
be regions at the apices - especially in haemorrhage or positive-pressure
ventilation where alveolar pressure also exceeds pressure at the arterial end
of the pulmonary capillaries. The vessels collapse completely for part of each
cardiac cycle, giving low intermittent flow. The net result is a blood flow per
unit volume of lung tissue that falls progressively from base to apex.
Gravity also affects intrapleural pressure, which is
less negative at the base than at the apex. As a result, at functional residual
capacity, apical alveoli are more expanded with less capacity for further
expansion during inspiration than at the bases. Consequently, ventilation is
also higher at the base than at the apex. The effect of gravity on ventilation
is less marked than on perfusion and so VA/Q is higher at the apex
than at the base. In young people, the degree of mismatching is modest and has
little effect on blood gases because the regions with low VA/Q are still
ventilated enough to nearly saturate the blood passing through them with
oxygen. The scatter of ventilation-perfusion ratios increases with age and
contributes to the reduction in Pao2 seen in the
elderly.
Ventilation–perfusion matching in disease
Increased ventilation-perfusion mismatching is an
important cause of gas exchange problems in many respiratory diseases,
including asthma, chronic obstructive pulmonary disease (COPD), pneumonia and
pulmonary oedema. Regions of low VA/Q may arise when airways are
partly blocked by bronchoconstriction, inflammatio or secretions and high VA/Q
areas arise in emphysematous areas where capillaries are lost or pulmonary
emboli are partially blocking blood fl w. Hypoxic vasoconstriction (Chapter
13) helps reduce the severity of ventilation-perfusion mismatching by diverting
blood from regions with low VA/Q to regions that are better
ventilated.
Effect of ventilation–perfusion mismatching on
arterial blood gases
Blood emerging from areas with high VA/Q
might be expected to compensate for blood from areas with low VA/Q.
This is not the case, for two reasons (Fig. 14c). First, although Po2
will be increased in high VA/Q regions, oxygen content is raised
little, as blood is normally nearly saturated. Blood draining regions with low
VA/Q and low Po2 (especially if <8 kPa,
60 mmHg) will have significantl reduced oxygen content. In addition, these
areas contribute more blood than areas with high VA/Q, which are typically
caused by reduced perfusion. The net effect of mixing blood from areas with a
wide range of ventilation-perfusion ratios is a low arterial O2
content and Pao2. CO2 content is less
severely affected because the over ventilated areas do lose extra CO2 and
partly compensate for low VA/Q regions. Moreover, any abnormalities
of Pao2 and Paco2
will lead to a reflex increase in ventilation, which usually corrects or
overcorrects the raised Paco2 while being less
effective at raising Pao2. The fina arterial blood
gas picture, a low Pao2 and a normal or low Paco2,
is similar to that resulting from anatomical right-to-left shunts (Chapter 13).
One difference is that arterial hypoxia caused by
ventilation-perfusion mismatching improves much more with oxygen therapy than
that caused by a shunt. In a hypoxic patient with a pure shunt, the oxygen-enriched
air fails to reach the shunted blood. In VA/Q mismatching,
increased oxygen fraction can increase local Po2 in areas of
low VA/Q (Fig. 14a), giving rise to significan improvement in
arterial oxygen content and pressure.
Assessment of ventilation–perfusion mismatching
Regional ventilation and perfusion can be visualized by
inhalation and infusion of appropriate radioisotopes (Chapter 21). A simple but
useful index of the degree of mismatching is the difference between Po2
in gas-exchanging or 'ideal' alveoli and in arterial blood. Ideal alveolar Po2
can be calculated from the alveolar air equation (Fig. 14d). An
increased A–a Po2 gradient (A = alveolar Po2,
a =
arterial Po2) is usually caused by ventilation-perfusion
mismatching or anatomical right-to-left shunts. In healthy young people, there
is a small A-a gradient (<2 kPa) arising from the normal anatomical
right-to-left shunts, discussed in Chapter 13. The normal value for A-a
gradient increases with age and in a healthy 80-year-old may be as high as 5 kPa (38 mmHg).