Pulmonary Function Tests and Alveolar Ventilation: Introductory Human Physiology
Pulmonary Function Tests and Alveolar Ventilation: Introductory Human Physiology
Pulmonary Function Tests and Alveolar Ventilation: Introductory Human Physiology
In a steady state, the amount of O2 that is consumed by the cells per unit time is equal
to the amount of O2 added to the blood in the lungs during the same time period.
Likewise the rate at which CO2 is generated by the cells is equal to the rate at which
CO2 leaves the blood in the lungs and is exhaled.
A second set of gradients must exist at the tissue-blood interface. Here the amount of
O2 consumed by cells and CO2 produced are not necessarily identical and depend on
the fuel source consumed. The ratio of CO2 produced to O2 consumed is called the
respiratory quotient (RQ). For a mixed diet, 8 molecules of CO2 are produced for
every 10 molecules of O2 consumed (i.e., RQ = 0.8). For a diet composed of
carbohydrates, the RQ is 1.0. For a diet of fat, the RQ is 0.7.
Introductory Human Physiology ©copyright Jennifer Carbrey & Emma Jakoi
Minute ventilation = VE = TV x f
However, because of the anatomical dead space (VD), not all of this entering air is
available for exchange with the blood . Recall that the conducting airway (anatomical
dead space) has a volume of ~150 ml. If 450 ml of fresh air is inspired, the first gas to
reach the respiratory zone comes from this anatomical dead space (150 ml). Then 300
ml of fresh gas reaches the respiratory zone and the last 150 ml of inspired gas remains
in the dead space. Thus, the total amount of fresh air reaching the alveoli during each
inspiration equals the tidal volume minus the volume of the anatomical dead space:
Alveolar ventilation (VA) is the total volume of fresh air entering the alveoli per minute.
It is calculated as:
When evaluating the efficiency of ventilation, one should focus on the alveolar
ventilation not minute ventilation.
For example, in the table below, Subjects A and B have the same minute ventilation (VE
= 6 L) but very different alveolar ventilations (VA). Subject A has no alveolar ventilation
and would be become unconscious in a few minutes but Subject B is breathing
normally.
Subject TV f VE VD VA
A 150ml 40 6000ml 150ml 0
B 500ml 12 6000ml 150ml 4200ml
One other important point shown in the table above is that the depth of breathing (TV)
is far more effective in elevating the alveolar ventilation than an increase in ventilation
rate (f). This is because for each tidal breath a fixed volume is dead space. As tidal
volume decreases, the fraction going to dead space increases. The respiratory system
will respond to O2 need (as in exercise) by reflexively increasing ventilation by
increasing the depth of breathing.
The anatomical dead space is not the only type of dead space in the lung. Some fresh
air is not used for gas exchange even though it reaches the alveoli because some
alveoli may have little or no blood supply (i.e., blood perfusion). This volume of air is
called alveolar dead space. In normal individuals this is quite small but may be large in
Introductory Human Physiology ©copyright Jennifer Carbrey & Emma Jakoi
several kinds of lung disease. As we will discuss later, a mismatch in ventilation and
blood perfusion is minimized by local mechanisms that match air and blood flow. The
sum of the anatomical dead space and alveolar dead space is the physiologic
dead space.
PX = Patm x FX
Where, Patm is the atmospheric pressure (at sea level = 760 mm Hg), and FX is the
fractional concentration of gas X.
Atmospheric air contains mostly nitrogen (79%) and oxygen (21% O2) with trace
amounts of CO2 and other gases. Air also contains water vapor. At sea level, water
vapor is 47 mm Hg. For simplicity, respiratory physiologists and physicians generally
assume that room air is always dry. Since 21% of dry room air is oxygen, the fraction
of O2 in inspired air (FiO2) is:
When inspired, the room air is warmed to 37oC and becomes humidified as it passes
through the nasal passages. The water vaporizes into the air until the P H2O= 47 mm Hg.
What this means is that only 760 - 47 mm Hg or 713mm Hg is available for other gases
besides water. Therefore,