Respiratory Physiology



Respiratory Physiology


Frank L. Powell

Gregory P. Heldt

Gabriel G. Haddad





PULMONARY GAS EXCHANGE

Pulmonary gas exchange describes the process of O2 uptake and CO2 elimination by the lungs to supply the metabolic demands of the body. This section of the chapter focuses on pulmonary gas exchange and how the lungs load adequate O2 into the blood to meet tissue O2 demand. It also covers the physiology of O2 and CO2 transport by the cardiovascular system and tissue gas exchange. Understanding pulmonary and tissue gas exchange also requires understanding O2 and CO2 blood dissociation curves. The general principles of respiratory physiology have been developed primarily in adults but the same principles apply to patients of any age. This chapter explains the general principles and highlights unique applications in pediatric and neonatal cases.

Normal O2 values are shown as a so-called oxygen cascade in Figure 43.1 as partial pressures (PO2) that can be measured in gas, blood, and tissue samples from a resting adult at sea level. Partial pressure (Px) is calculated as the fraction of the total barometric pressure (Pbar) occupied by a given gas species:

Px = Fx × (Pbar)

where Fx is the fractional concentration of gas “x” in a dry gas sample. Partial pressure is expressed in units of torr (1 torr = 1 mm Hg) or SI units of kilo Pascals (1 kPa = 7.5 mm Hg) in physiology.

The PO2 decreases at every step in the O2 cascade. The PO2 drop between dry room air and inspired gas in the trachea (PIO2) is due to humidification. Gas in the airways is saturated with water vapor at body temperature so that the total gas pressure available for O2 and CO2 inside the body is reduced. The water vapor pressure is 47 mm Hg at 37°C and 100% saturation. For a normal barometric pressure of 760 mm Hg at sea level:

PO2 in dry ambient air = 0.21 × 760 mm Hg = 160 mm Hg

PIO2 in the airways = 0.21 × (760 – 47) mm Hg = 150 mm Hg

Further decreases in PO2 along the O2 cascade are explained by the physiology of gas exchange. The large drop in PO2 between inspired and alveolar gas is a function of ventilation. Diffusion across the blood-gas barrier and other factors, such as shunts and the mismatching of ventilation and pulmonary blood flow, explains the relatively small decrease in PO2 between
alveolar gas and arterial blood. The circulation and O2 diffusion from capillaries to tissues cause the large decreases in PO2 between arterial and venous blood, and between blood and mitochondria in the tissues.






FIGURE 43.1. The “oxygen cascade” in a healthy subject breathing room air at sea level shows the pattern of PO2 decrease between the different steps of O2 transport. The difference between alveolar and arterial PO2 occurs because of pulmonary gas exchange limitations. (From Powell FL. Pulmonary gas exchange. In: Johnson LR, ed. Essential Medical Physiology. 3rd ed. Boston, MA: Elsevier/Academic Press, 2003, with permission.)

To quantify respiratory physiology for clinical diagnosis and research, standard symbols and conventions for reporting volumes and concentrations have been adopted. Table 43.1 describes these symbols and gives examples of how they are used. Conditions of standard temperature and pressure and dry (STPD) are used for volumes of O2 or CO2 (e.g., metabolic rate, [V with dot above]O2) while body temperate and pressure saturated (BTPS) conditions are used to report lung volumes and ventilation (e.g., expired ventilation, [V with dot above]E2). For a normal pressure of 760 mm Hg and 37°C body temperature, VBTPS = 1.21 × VSTPD. Often, volumes are measured at ambient temperature and pressure, saturated conditions (VATPS) and at 760 mm Hg and 20°C, VBTPS = 1.086 × VATPS and VSTPD = 0.885 × VATPS.

Quantitative models of gas exchange are useful for diagnosing pulmonary disease. Generally, these models are based on the principle of conservation of mass, or mass balance, and they assume a steady state. Steady state means an equal and constant rate of gas transport at each step in the O2 cascade, but it does not necessarily imply resting conditions. O2 transport can be elevated but still equal at every step in the O2 cascade (e.g., during steady-state exercise). However, nonsteady-state conditions occur frequently (e.g., at the onset of exercise or in acute respiratory distress).

In an “ideal” model of alveolar gas exchange, arterial blood equilibrates with alveolar gas; therefore, the ideal alveolararterial PO2 difference equals zero. In reality, the alveolararterial PO2 difference exceeds zero, even in health (Fig. 43.1). Several factors, called gas-exchange limitations, increase the alveolar-arterial PO2 difference. Gas-exchange limitations do not necessarily affect O2 consumption at rest, but they can lower maximal O2 consumption and decrease PO2 values along the O2 cascade in a steady state. The alveolar-arterial Po2 difference is useful for diagnosing O2 exchange limitations because different limitations respond differently to simple tests such as O2 breathing.








TABLE 43.1 SYMBOLS IN RESPIRATORY PHYSIOLOGY










































































































Primary variables (and units)


C


Concentration or content (mL/dL or mmol/L)


D


Diffusing capacity [mL O2/(min × mm Hg)]


F


Fractional concentration in dry gas (dimensionless)


P


Gas pressure or partial pressure (cm H2O or mm Hg)


[Q with dot above]


Blood flow or perfusion (L/min)


R


Respiratory exchange ratio (dimensionless)


T


Temperature (°C)


V


Gas volume (L or mL)


[Q with dot above]


Ventilation (L/min)


Modifying symbols


A


Alveolar gas


B


Barometric


DS


Dead space gas


E


Expired gas


E


Mixed-expired gas


I


Inspired gas


L


Lung or transpulmonary


T


Tidal gas


aw


Airway


w


Chest wall


es


Esophageal


pl


Intrapleural


rs


Transrespiratory system (total system)


a


Arterial blood


b


Blood (general)


c


Capillary blood


c′


End-capillary blood


t


Tissue


v


Venous blood


[v with bar above]


Mixed-venous blood


Examples


PAO2 = Partial pressure of O2 in alveolar gas


PaO2 = Partial pressure of O2 in arterial blood


F[ε with bar above]CO2 = Fraction of CO2 in dry mixed, expired gas


[V with dot above] = O2 consumption per unit time


[V with dot above]A = Ventilation of the alveoli per unit time



Oxygen in Blood

The O2 carriage by blood affects both O2 uptake in the lungs and delivery in the tissues, so it is considered first. Blood-O2 equilibrium curves (O2 dissociation curves) quantify O2 carriage as graphs of concentration versus partial pressure. It is necessary to consider both partial pressure and concentration because partial-pressure gradients drive diffusive gas transport in lungs and tissues, but concentration differences determine convective gas transport rates in lungs and the circulation (see the section, Cardiovascular and Tissue Oxygen Transport).

This topic would be much simpler to explain and understand if O2 was physiologically inert and occurred in blood only as physically dissolved gas. There is a linear relationship between the concentration and partial pressure of a gas that is physically dissolved in a liquid according to Henry’s law (C = α P, where α = solubility). However, O2 also enters into chemical reactions with blood that result in a more
complicated, nonlinear relationship (Fig. 43.2) but this shape is essential for life as we know it. The normal O2 concentration in arterial blood (CaO2) is ˜20 mL/dL but only 0.3 mL / dL is physically dissolved (note the usual units for O2 and CO2 concentration in blood are mL/dL, also called volume %, and 1 mL/dL ≈ 0.45 mmol/L for ideal gases). If arterial blood only contained dissolved O2, then cardiac output would have to be 100 L/min to deliver enough O2 to the tissues for a normal adult metabolic rate of 300 mL O2/min!






FIGURE 43.2. Standard human O2-blood equilibrium (or dissociation) curve at pH = 7.4, PCO2 = 40 mm Hg, and 37°C. Left ordinate shows O2 saturation of hemoglobin (Hb) available for O2 binding; right ordinate shows absolute O2 concentration in blood. Most O2 is bound to hemoglobin, and dissolved O2 contributes very little to total O2 concentration. (From Powell FL. Oxygen and CO2 transport in the blood. In: Johnson LR, ed. Essential Medical Physiology. 3rd ed. Boston, MA: Elsevier/Academic Press, 2003, with permission.)


Hemoglobin

Hemoglobin (Hb) is responsible for this dramatic increase in blood’s O2-carrying capacity. Hb consists of four polypeptide chains, each with a heme (iron-containing) protein that can bind O2 with iron in the ferrous (Fe2+) form. Methemoglobin results when iron is in the ferric form (Fe3+) and cannot bind O2. Small amounts of methemoglobin normally occur in blood and slightly reduce the amount of O2 that can be bound to Hb. One gram of pure adult Hb can bind 1.39 mL of O2 when fully saturated, but methemoglobin reduces this value to 1.34-1.36. The cellular packaging of Hb is important for the biophysics of the microcirculation, and it provides physiologic control of O2 binding through cellular changes in the Hb microenvironment.

The four subunits of Hb include two α– and two β-chains, and variations in the amino acid sequence of these polypeptides explain the differences in Hb-O2 affinity between species and at different stages of development. The threedimensional shape of an Hb molecule, which is determined by the allosteric interactions of its four subunits, causes the O2-equilibrium curve to be S-shaped, or sigmoidal (Fig. 43.2). O2-equilibrium curves for individual α– and β-chains are not sigmoidal but simple convex curves similar to the O2-equilibrium curve for myoglobin. Myoglobin occurs in muscle and has only a single polypeptide chain with one heme group. The sigmoidal shape of the O2-Hb equilibrium curve facilitates O2 loading into blood in the lungs and O2 unloading from blood in the tissues.


Blood-Oxygen Equilibrium Curves

The two forms of the O2 equilibrium curve are shown in Figure 43.2: (a) saturation of Hb with O2 (SO2) versus PO2, and (b) O2 concentration in blood (CO2) versus PO2. Saturation quantifies the amount of O2 in blood as the percentage of the total Hb sites available for binding O2 that actually bind O2 at a given PO2. Therefore, saturation equilibrium curves are independent of Hb concentration in blood. In contrast, concentration curves quantify the absolute amount of O2 in a volume of blood with a given PO2, and they depend on the amount of Hb available.

O2 capacity (O2cap) is defined as the O2 concentration in blood when Hb is 100% saturated with O2. Pure Hb binds 1.39 mL O2/g Hb. Figure 43.2 illustrates that the O2cap for normal blood with Hb concentration of 15 g/dL is 20.85 mL/ dL (1.39 × 15). Physically dissolved also contributes a small amount to O2 concentration. Therefore, total O2 concentration in blood (in mL O2/dL blood) is calculated as:

Co2 = (O2cap × [So2/100]) + (0.003 × PO2)

where O2cap is the O2 capacity, So2 the saturation, and 0.003 is the physical solubility for O2 in blood in (mL/dL)/mm Hg.

The shape of the O2-Hb equilibrium curves is complex and can be generated only experimentally or by sophisticated mathematical algorithms. However, remembering only four points on the normal adult curve allows one to solve many common problems of O2 transport:

a. PO2 = 0 mm Hg, SO2 = 0% (the origin of the curve)

b. PO2 = 100 mm Hg, SO2 = 98% (normal arterial blood, which is almost fully saturated)

c. PO2 = 40 mm Hg, SO2 = 75% (normal mixed-venous blood)

d. PO2 = 26 mm Hg, SO2 = 50% (i.e., P50)

The P50 quantifies the affinity of Hb for O2 as the PO2 at 50% saturation under standard conditions of partial pressure of CO2 (PCO2) = 40 mm Hg, pH = 7.4, and 37°C. P50 is only 20 mm Hg in the human fetus, as discussed below. A decrease in P50 indicates an increase in O2 affinity because SO2 or CO2 is greater for a given PO2.


Modulation of Blood-Oxygen Equilibrium Curves

The O2-equilibrium curve can be physiologically modulated in three ways: (a) the vertical height of the concentration curve (but not the saturation curve) can change, indicating a change in O2cap, (b) the horizontal position of saturation and concentration curves can change, indicating a change in Hb-O2 affinity, and (c) the shape of saturation and concentration curves can change, indicating a change in the chemical reaction between O2 and Hb. The maximum height of the saturation curve cannot change by definition; the maximum is always 100% when O2 is bound to all available Hb sites. However, changes in Hb concentration [Hb] will change the maximum height of the concentration curve, according to the relationship between O2cap and [Hb] as described previously. Mean corpuscular Hb concentration (MCHC) quantifies [Hb] in red blood cells and hematocrit (Hct) quantifies the percentage of blood volume that is red blood cells. Therefore, [Hb], in g/dL of blood, depends on both of these factors:

[Hb] = MCHC. Hct

Typical adult values of MCHC = 0.33, Hct = 45%, and [Hb] = 15 g/dL are used in Figure 43.2, which shows normal CaO2 = 20 mL/dL and that CaO2 = 15 mL/dL in mixed-venous blood (C[V with bar above]oxygen). If [Hb] decreases, for example with decreased Hct in anemia, O2cap and concentration decrease at any given PO2. The O2cap increases when [Hb] increases
by the stimulation of red blood cell production in bone marrow by the hormone erythropoietin or by transfusion. Erythropoietin transcription is regulated by hypoxia-inducible factors (HIF-1 and 2) released from cells in the kidneys in response to decreases in arterial O2 levels. Polycythemia (increased Hct) occurs with chronic hypoxemia in healthy people (e.g., during acclimatization to altitude) and with disease.

The horizontal position of the Hb-O2 equilibrium curves reflects the affinity of Hb for O2, and changes in horizontal position are quantified as changes in P50. A decrease in P50 is referred to as a left shift of the equilibrium curve and indicates increased Hb-O2 affinity; SO2 or CO2 is increased for a given PO2. Similarly, increased P50, or a right shift, reflects decreased Hb-O2 affinity. The three most important physiologic variables that can modulate P50—pH, PCO2, and temperature—are shown in Figure 43.3.

The Bohr effect describes changes in P50 with changes in blood PCO2 and pH. Decreased PCO2 causes Hb-O2 affinity to increase (decreased P50), and increased PCO2 causes Hb-O2 affinity to decrease (increased P50). As described later, pH decreases when PCO2 increases and vice versa, and pH changes explain most of the Bohr effect with PCO2 changes in blood. Hydrogen (H+) binds to histidine residues in Hb molecules, thereby changing the conformation of Hb and the ability of heme sites to bind O2. However, CO2 also has a small, independent effect on Hb-O2 affinity if pH is held constant. The physiologic advantage of the Bohr effect is that it facilitates loading in the lungs, where CO2 is low and pH is high. In the tissues, the opposite occurs, and increased CO2 causes pH to decrease and facilitates O2 unloading from Hb to the tissues. The effect of temperature on Hb-O2 affinity also has physiologic advantages. Warm temperatures in intensely exercising muscles will increase P50 and decrease Hb-O2 affinity to facilitate O2 unloading to tissues.

A physiologic O2-blood equilibrium curve can be defined as the curve that shows the change in blood O2 concentration when PO2 decreases from arterial to venous levels in the tissues or increases in the opposite direction in the lungs. The increase in PCO2, decrease in pH, and potential increase in temperature between arterial and venous points make the physiologic curve steeper than individual curves (Fig. 43.3). This is an advantage for gas exchange because it increases the change in O2 concentration for a given change in PO2, thereby increasing O2 uptake or delivery (see the section, Cardiovascular and Tissue Oxygen Transport).






FIGURE 43.3. Effects of pH and PCO2 (i.e., Bohr effect) and temperature on the position of the O2-hemoglobin (HbO2) equilibrium curve. The “physiological” curve connects the arterial (a) and mixed-venous points ([v with bar above]), so that the in vivo curve is steeper than the standard curve at pH = 7.4 (green). (From Powell FL. Oxygen and CO2 transport in the blood. In: Johnson LR, ed. Essential Medical Physiology. 3rd ed. Boston, MA: Elsevier/Academic Press, 2003, with permission.)

Hb-O2 affinity is also affected by organic phosphates, with 2,3-diphosphoglycerate (2,3-DPG) being most important in humans. 2,3-DPG is produced during glycolysis in red blood cells and increases P50 by interacting with Hb β-chains to decrease their O2-binding affinity. Physiologic stimuli that lead to enhanced O2 delivery (e.g., chronic decreases in blood PO2 levels) typically increase the concentration of 2,3-DPG and promote O2 delivery to tissues. In blood stored in blood banks, 2,3-DPG is generally decreased, and the increased Hb-O2 affinity can lead to problems in O2 delivery after blood transfusion.

Carbon monoxide (CO) is a deadly gas that also modulates the Hb-O2 dissociation curve by changing the shape and position of concentration or saturation curves. The affinity of Hb for CO is 240 times greater than it is for O2, so even very small amounts of CO greatly reduce the capacity for Hb to bind O2—that is, the O2cap. However, CO also decreases the P50 and makes the Hb-O2 curve less sigmoidal. CO causes a left shift of the curve by altering the ability of the Hb molecule to bind O2; therefore, blood O2 concentration remains high until Po2 decreases to very low levels, which impairs O2 unloading from blood to tissues. CO poisoning also has direct effects on cellular cytochromes, which contribute to its deadliness. CO is particularly dangerous because it is colorless and odorless, and the decrease it causes in arterial O2 concentration is not sensed by respiratory control systems, which respond only to O2 partial pressure, as explained in the Respiratory Control section. Hyperbaric O2 exposure is used to treat CO poisoning because only very high Po2 levels are effective at competing with CO for Hb-binding sites and driving CO out of the blood.


Oxygen Transport in Fetal Blood

The normal human fetus is exposed to a level of O2 that would be considered severe hypoxia in adults, similar to the levels experienced on the summit of Mt. Everest! This is possible not only because the fetus is less sensitive to hypoxia than adults, but also because of fetal Hb (HbF). HbF has a P50 of 20 torr, compared to 26 torr for adults, thus facilitating O2 transfer to the fetus in the placenta (Fig. 43.4). HbF is gradually replaced by adult Hb in the first year. O2 delivery across the placenta is ˜8 mL O2/min/kg of fetal mass, which is approximately twice the rate for an adult, but blood O2 stores in the fetus are sufficient for only a few minutes of metabolism. O2 delivery across the placenta is limited by blood flow and PO2 levels in the mother and fetus, but not by diffusion. For example, decreasing maternal PaO2 below 70 torr can reduce placental O2 transfer. Increasing maternal PaO2 to 600 torr, with O2 breathing, can increase fetal umbilical O2 tensions by 3-5 torr, which can be important if the fetus is suffering any hypoxic stress. Both the left shift of fetal versus adult O2-Hb equilibrium curves and the high fetal O2 capacity facilitate O2 unloading from the mother to the fetus (Fig. 43.4). It is also significant that O2 capacity is decreased in the mother near term (11.5 vs. 14 g/dL Hb). The Bohr effect also contributes to placental O2 transport, as pH decreases from 7.42 in the maternal artery to 7.35 in the maternal vein.


Carbon Dioxide in Blood

The general principles of CO2 transport by blood are similar to those for O2, i.e., blood carries much more CO2 than would be possible if it was only physically dissolved, and the CO2-blood equilibrium curve is modulated by physiologic factors. In addition, CO2 carriage by blood has important effects on acid-base balance.

CO2-blood equilibrium (or dissociation) curves are nonlinear, but they have a different shape and position than
O2-blood equilibrium curves. Blood holds more CO2 than O2, in part because CO2 is carried by blood in three forms (Fig. 43.5). Also, the CO2-blood equilibrium curve is steeper than the O2 curve, resulting in a smaller range of PCO2 values in the body, compared with the range of PO2 values, although the differences between arterial and venous concentrations are similar for CO2 and O2 (˜5 mL/dL of blood). The resulting physiologic CO2 dissociation curve between the arterial and venous points is much more linear than the physiologic O2 dissociation curve (Fig. 43.5).






FIGURE 43.4. Oxygen-hemoglobin equilibrium curves for maternal and fetal hemoglobin. A: When PO2 equilibrates between the fetal and maternal circulations, O2 saturation is increased by 10% or more because of the lower P50 in fetal hemoglobin. B: Higher O2 capacity of fetal compared to maternal blood further increases the amount of O2 in blood for a given PO2 and saturation. A, maternal arterial, V, maternal venous; a′, umbilical (maternal) arterial; v′, umbilical (maternal) venous; a, fetal arterial; v, fetal venous. (From Powell FL. Pulmonary gas exchange. In: Johnson LR, ed. Essential Medical Physiology. 3rd ed. Boston, MA: Elsevier Academic Press, 2003, with permission.)


Carbon Dioxide and Blood Acid-Base

Physically dissolved CO2 is a function of CO2 solubility in plasma, which is 0.067 mL/(dL mm Hg) and 20 times more soluble than O2. Still, dissolved CO2 contributes only ˜5% of total CO2 concentration in arterial blood.

Carbamino compounds comprise the second form of blood CO2. These compounds occur when CO2 combines with amine groups in blood proteins, especially with the globin of Hb. However, this chemical combination between CO2 and Hb is much less important than Hb-O2 binding; therefore carbamino compounds comprise only 5% of the total CO2 in arterial blood.

Bicarbonate ion HCO3 is the most important form of CO2 carriage in blood. CO2 combines with water to form carbonic acid, and this dissociates to HCO3 and H+:

CO2 + H2O ↔ H2CO3 + HCO3 + H+

Carbonic anhydrase is the enzyme that catalyzes this reaction, making it almost instantaneous. Carbonic anhydrase occurs mainly in red blood cells, but it also occurs on pulmonary capillary endothelial cells and accelerates the reaction in plasma in the lungs. The uncatalyzed reaction will occur in any aqueous medium, but at a much slower rate, requiring >4 minutes for equilibrium. The rapid conversion of CO2 to bicarbonate results in ˜90% of the CO2 in arterial blood that is carried in that form and has important implications for acid-base balance.

Figure 43.6 shows the carbonic acid reactions in plasma and red blood cells and illustrates important ion fluxes that occur with CO2 transport in blood. CO2 rapidly enters red blood cells from the plasma because it is soluble in cell membranes. Carbonic anhydrase catalyzes the rapid formation of HCO.3 and H+ in the cells and an electrically neutral bicarbonate-chloride exchanger moves some of this HCO3 out of
the cell. The chloride shift (Hamburger shift) is an increased intracellular chloride level with increased CO2, or vice versa. The H+ produced from CO2 reacts with Hb and affects both the O2 equilibrium curve (Bohr effect) and CO2 equilibrium curve, as described next.






FIGURE 43.5. CO2-blood equilibrium curve shown on same graph with O2 equilibrium curve. Differences between the curves result in higher CO2 concentrations in the blood and smaller PCO2 differences between arterial (a) and venous ([v with bar above]) blood. Hemoglobin-O2 saturation affects the position of the CO2 equilibrium curve (i.e., Haldane effect). (From Powell FL. Oxygen and CO2 transport in the blood. In: Johnson LR, ed. Essential Medical Physiology. 3rd ed. Boston, MA: Elsevier/Academic Press, 2003, with permission.)






FIGURE 43.6. CO2 and O2 reactions in blood and tissues; the opposite reactions occur in the lungs. CA, carbonic anhydrase; HHb, protonated hemoglobin. (From Powell FL. Oxygen and CO2 transport in the blood. In: Johnson LR, ed. Essential Medical Physiology. 3rd ed. Boston, MA: Elsevier/Academic Press, 2003, with permission.)


Modulation of Blood-Carbon Dioxide Equilibrium Curves

Hb-O2 saturation is the major factor affecting the position of the CO2 equilibrium curve. The Haldane effect increases CO2 concentration when blood is deoxygenated or decreases CO2 concentration when blood is oxygenated at any given PCO2 (Fig. 43.5). The Haldane effect is actually another view of the same molecular mechanism that causes the Bohr effect on the O2 equilibrium curve (described previously). H+ ions from CO2 can be thought of as competing with O2 for Hb binding. Hence, increasing O2 decreases the affinity of Hb for H+ and blood CO2 concentration (Haldane effect), and increased [H+] decreases the affinity of Hb for O2 (Bohr effect). These interactions are summarized in Figure 43.6.

The Haldane effect promotes unloading of CO2 in the lungs when blood is oxygenated and CO2 loading in the blood when O2 is released to tissues. The Haldane effect also results in a steeper physiologic CO2-blood equilibrium curve (see Fig. 43.5), which has the physiologic advantage of increasing CO2 concentration differences for a given PCO2 difference.


Alveolar Ventilation and Alveolar PO2

Ventilation is the first step in the O2 cascade, and the level of alveolar ventilation [V with dot above]A is the most important factor determining arterial PO2 for any given PIO2 and level of O2 consumption ([V with dot above]O2) in healthy lungs. Total expired ventilation can be measured with a pneumotachometer or spirometer as the product of the volume of each breath, or tidal volume (VT), and respiratory frequency (fR):

[V with dot above]E = VT × fR

However, all the tidal volume is not effective for gas exchange because the lung consists of a conducting zone, which does not exchange gas, and a respiratory zone, in which all gas exchange occurs. The conducting zone includes the conducting airways from the trachea to the terminal bronchioles, which occur at the 16th order of bronchial branching. The gas volume of the conducting zone equals the anatomic dead space. The respiratory zone comprises the rest of the lung from the 17th to 23rd orders of bronchial branching (i.e., respiratory bronchioles to alveolar sacs), and all gas exchange occurs there. With 23 orders of bronchial branching, total cross-sectional area of the airways in distal parts of the lung is greatly increased; therefore, the respiratory zone comprises most of the lung volume. For example, a normal adult will have a total lung capacity (TLC) of 6 L but an anatomic dead space of only 175 mL (˜1 mL per pound of body weight).

[V with dot above]A is the difference between total ventilation and dead space ventilation, and it is the effective conductance for pulmonary gas exchange. Total ventilation is not effective for gas exchange because part of the inspired tidal volume remains in the anatomic dead space (VDS). [V with dot above]A can be determined using the Fick principle, which is a physiologic version of the principle of conservation of mass that describes gas transport by convection or bulk flow of air or blood. The Fick principle states that the amount of gas consumed or produced by an organ is the difference between the amount of the substance that enters the organ and the amount that leaves the organ. The formula for CO2 elimination from the lungs ([V with dot above]CO2) is:

([V with dot above]CO2) = ([V with dot above]A FACO2) – ([V with dot above]I FICO2)

[V with dot above]CO2 is the difference between the CO2 expired from the alveoli, and the amount of CO2 inspired to the alveoli. Fico2 is essentially zero; therefore, the equation can be simplified and rearranged to the alveolar ventilation equation:

[V with dot above]A = ([V with dot above]CO2/PACO2)K

where [V with dot above]A is expressed at body temperature and pressure saturated (i.e., LBTPS/minute), [V with dot above]CO2 is expressed at standard temperature and pressure dry (i.e., mLSTPD/minute), PACO2 is substituted for FACO2, and K is a constant (0.863).

In practice, arterial PCO2 (PaCO2) is substituted for alveolar PCO2 (PACO2) because the two values are equal in normal lungs, and an arterial blood sample is usually taken to evaluate gas exchange.


Alveolar Ventilation Equation Predicts Alveolar PCO2

Rearranging the alveolar ventilation equation shows how [V with dot above]A and PACO2 (or PACO2) are inversely related for any given metabolic rate:

PACO2 = ([V with dot above]CO2/[V with dot above]A)K

Hence, if [V with dot above]A is doubled, PACO2 is halved, regardless of the exact values for either variable. Hyperventilation is defined by a decrease in PaCO2 from the normal value, implying excess [V with dot above]A for a given [V with dot above]CO2. Hypoventilation is defined by an increase in PaCO2, and this occurs when [V with dot above]A is lower than normal for a given [V with dot above]CO2.

As explained previously, [V with dot above]A is reduced from total ventilation by the amount of the dead space:

[V with dot above]A = fR ([V with dot above]T – [V with dot above]DS)

Although anatomic dead space can be measured with gas analyzers and flow meters, it is more clinically relevant to estimate physiologic dead space, which is also called Bohr dead space. Physiologic dead space includes all “wasted ventilation” and can exceed anatomic dead space, as described next. Physiologic dead space can be calculated from another rearrangement of the Fick principle applied to CO2 elimination by the lungs as:

VDS/VT = (PACO2 – PĒCO2)/PACO2

where PeĒCO2 = mixed-expired PCO2 that is measured by collecting all expired gas in a bag or a spirometer and includes gas exhaled from the alveoli and dead space. In practice, arterial PCO2 is substituted for alveolar PCO2 because it is easily measured.



Alveolar Gas Equation Predicts Alveolar PO2

Alveolar PO2 (PAO2) can be predicted from the alveolar gas equation that models an “ideal lung” with only physiologic dead space:

PAO2 = PIO2 – (PACO2/R) + F

where PIO2 is inspired PO2, PACO2 is alveolar PCO2, R is the respiratory exchange ratio, and F is a constant that can be ignored under normal conditions (F = PACO2 × FIO2 [1 – R]/R and increases PAO2 only 2 mm Hg at normal O2 and CO2 levels).

In practice, arterial PCO2 is substituted for alveolar PCO2 because PaCO2 = PaCO2 in normal lungs and arterial samples are easily obtained. The alveolar gas equation is only valid if inspired PCO2 = 0, which is a reasonable assumption for room air breathing.

The respiratory exchange ratio (R) is the ratio of uptake to CO2 elimination by the lungs:

R = [V with dot above]CO2/[V with dot above]O2

Under steady-state conditions, R equals the respiratory quotient (RQ), which is the ratio of CO2 production to O2 consumption in metabolizing tissues. RQ averages 0.8 on a normal, mixed, adult diet, but it can range from 0.67 to 1, depending on the relative amounts of fat, protein, and carbohydrate being metabolized. R can exceed this range in nonsteady states, for example, when R exceeds 1 during hyperventilation. CO2 stores in the body are much greater than O2 stores because of bicarbonate in blood and tissues. R can increase because it takes longer to wash out the CO2 stores than it does to charge up the much smaller O2 stores in the body.

Substituting normal adult values in the alveolar gas equation predicts that PAO2 = 100 mm Hg in breathing room air (PAO2 = 150 – 40/0.8). Increases in [V with dot above]A (hyperventilation) increases PAO2 by decreasing PACO2, whereas decreases in [V with dot above]A (hypoventilation) decreases PAO2. Why ideal alveolar PO2 is greater than measured arterial PO2 is explained in the next section.


Permissive Hypercapnia

Respiratory disease, and especially hypoventilation, is characterized by changes in blood gas homeostasis, namely, hypoxia and hypercapnia. Often, the only treatment that can be used is mechanical ventilation until the disease is resolved. While mechanical ventilation may be a lifesaver in certain conditions, this treatment can also injure the lungs with barotrauma. Epidemiologic data in the 1980s and 1990s showed that “permitting” an increase in PaCO2 without imposing mechanical ventilation, or delaying mechanical ventilation, might have beneficial effects. Both animal and human studies have shown that therapeutic hypercapnia attenuates various measures of lung injury. For example, 8% CO2 increases expression of genes encoding surfactant-associated proteins A and B, which contribute to host defense mechanisms in the lung.

In pediatrics, questions about this strategy have focused on bronchopulmonary dysplasia (BPD) in infants after prematurity. Higher PaCO2 values are associated with lower BPD rates and large population-based studies in premature neonates show decreased BPD and death with permissive hypercapnia used before or during intubation and mechanical ventilation. Permissive hypercapnia also increased survival in neonates who have congenital diaphragmatic hernia. However, experiments in animal and human cell cultures also suggest some undesirable effects of elevated CO2, such as suppressed immune function, increased oxidative lung injury, and impaired alveolar repair with potentiated tissue nitration. Summarizing, permissive hypercapnia is a ventilatory strategy that may reduce injury to the developing lung through a variety of mechanisms. Considering all of the evidence to date, permissive hypercapnia appears to be safe and beneficial in neonates subject to barotraumas.


Diffusion

Diffusion of O2 from alveoli to pulmonary capillary blood is the next step in the O2 cascade after alveolar ventilation. It is important to note that blood leaving the pulmonary capillaries is in equilibrium with alveolar gas in healthy lungs under normal resting conditions. Hence, the small decreases between PAO2 and PaO2 shown in Figure 43.1 are not caused by diffusion but by ventilation-perfusion mismatching in healthy lungs under normal conditions, as described in the next section.

O2 moves from the alveoli to pulmonary capillary blood barrier according to Fick’s first law of diffusion:

[V with dot above]O2 = ΔPO2 × DO2

ΔPO2 is the average Po2 gradient across the blood-gas barrier and DO2 is a “diffusing capacity” for O2 across the barrier.

Diffusion of a gas always occurs down a partial-pressure gradient, for example, from alveolar gas to pulmonary blood. Some readers may find it helpful to note the analogy between Fick’s law for O2 flux and Ohm’s law for the flow of electrons (current = voltage/resistance). [V with dot above]O2 is analogous to current, and ΔPo2 is analogous to the potential energy difference of voltage. However, Do2 is analogous to a conductance, which is the inverse of resistance (current = voltage × conductance). Flux can be increased either by increasing the Po2 gradient or increasing the conductance (DO2).

Do2 depends on both the molecular properties of the gas and the geometric properties of that membrane:

Do2 = (solubility/MW) O2 (area/thickness)membrane

Solubility is important because gas molecules must “dissolve” in a membrane before they can diffuse across it, and once dissolved, low-molecular-weight (MW) molecules move more quickly by the random motions of diffusion. Large surface areas increase the probability that an O2

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Jun 4, 2016 | Posted by in CRITICAL CARE | Comments Off on Respiratory Physiology

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