Gas Diffusion

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Gas Diffusion

What is Diffusion?

Diffusion is the result of high-speed random motion of gas or liquid molecules. For example, if the number of molecules present in area A is greater than in area B, mathematical probability dictates that more molecules will move from A to B than from B to A. This net movement of molecules from high to low concentrations is called diffusion. Diffusion in the above-mentioned example continues until the molecules are evenly distributed such that the number of molecules moving from A to B and from B to A is the same. This state is called equilibrium.

The high-speed random impacts of atmospheric air molecules on solid surfaces create the atmosphere’s pressure. Air is a gas mixture; the contribution that each gas makes to the atmospheric pressure is proportional to the number of its molecules present (i.e., each gas exerts its own partial pressure, as explained in Chapter 4). A gas diffuses from one point to another when there are differences in its partial pressures within the mixture; the direction of diffusion is always from high to low partial pressure. When no partial pressure difference exists for any gas throughout the mixture, equilibrium is present. Individual gas partial pressure differences are called diffusion gradients. During diffusion, each gas in a mixture moves according to its own diffusion gradient. That is, two different gases may simultaneously diffuse in opposite directions because of oppositely oriented partial pressure gradients. This occurs for oxygen (O2) and carbon dioxide (CO2) across the alveolar capillary membrane (Figure 7-1).

Diffusion is not the same as bulk gas flow, in which a large pressure gradient causes all molecules of all gases to move together in one direction. An example of bulk gas flow is ventilation, in which mouth and alveolar pressure differences cause gas to move in and out of the lungs. In terminal airways and alveoli, random molecular diffusion is the main mechanism whereby gas molecules reach the alveolar surface.

Diffusion Gradients of Respiratory Gases

Figure 7-2 illustrates diffusion gradients between alveolar gas and blood and between blood and body tissues. Inspired air contains about 21% O2 and essentially no CO2. Inspired oxygen partial pressure (PIO2) is about 160 mm Hg, as the following calculation shows:

Conducting airway PO2 is lower than the air’s PO2 because gas in the lung is 100% saturated with water vapor. At body temperature, the partial pressure of water vapor in the lung (PH2O) is 47 mm Hg. PO2 in conducting airways is about 150 mm Hg, as the following calculation shows:

Alveolar PO2 (PAO2) is lower still because CO2 diffuses into the alveoli, diluting incoming O2 and lowering PAO2 to about 100 mm Hg. (Calculation of PAO2 is discussed in the next section.)

The diffusion gradient between alveolar gas and mixed venous blood is much larger for O2 than it is for CO2 (60 mm Hg vs. 6 mm Hg), as shown in Figure 7-2. At rest, these diffusion gradients transfer about 250 mL of O2 into the blood and 200 mL of CO2 into the alveoli each minute. By the time blood leaves the alveolar capillary, the PO2 and PCO2 of the blood have reached equilibrium with alveolar gases, even during exercise when blood flows very rapidly through the capillary. PO2 of blood entering the left atrium is never as high as PO2 of blood leaving the pulmonary capillaries (see Figure 7-2) because a small amount of deoxygenated bronchial venous blood mixes with capillary blood; this constitutes a normal anatomical shunt. Anatomical shunt is mostly responsible for the normal P(A-a)O2 (alveolar-to-arterial oxygen pressure difference). Left atrial blood normally flows unaltered into the systemic arteries.

Alveolar Air Equation

The sum of all gas pressures at any point in the lung must equal 760 mm Hg at sea level. When air—which is CO2-free—is inspired and enters the alveoli, its PCO2 immediately increases to 40 mm Hg as it mixes with the CO2 present in the alveoli; because the sum of all alveolar gas pressures is constant (760 mm Hg), the inspired air PO2 decreases by about 40 mm Hg. If the amount of O2 diffusing out of alveoli into the blood each minute were exactly equal to the amount of CO2 diffusing

from the blood into alveoli each minute, PAO2 would be calculated by simply subtracting alveolar PCO2 (normally 40 mm Hg) from the result of equation 2. However, O2 diffuses out of the alveolus at a greater rate than CO2 diffuses into the alveolus. At rest, pulmonary capillary blood removes about 250 mL per minute of O2 from the alveoli, replacing it with only 200 mL per minute of CO2. The ratio of alveolar CO2 excretion (V˙imageCO2) to blood oxygen uptake (V˙imageO2) is called the respiratory exchange ratio (R), and its value is normally about 0.8 (R=V˙CO2/V˙O2=200/250=0.8image).

When R is equal to 0.8, the CO2 diffusing into the alveolus replaces only 80% of the volume that O2 vacated when it diffused out of the alveolus. This uneven exchange causes the alveolar gas volume to shrink slightly, but alveolar gas pressure remains constant at 760 mm Hg. The shrinkage in alveolar volume concentrates the alveolar nitrogen molecules, which the alveolar air equation takes into account. This equation is known as the ideal alveolar air equation because it assumes the ventilation-to-blood flow ratios of each alveolus in the lung are identical, as the following calculation shows:

In this equation PIO2 equals FIO2 (760 − 47). FIO2 represents inspired oxygen concentration expressed as a decimal fraction. The bracketed part of equation 3 is a correcting factor that considers the effect of R on PAO2. When R equals 1, the correction factor equals 1 and does not need to be applied.

The term 1 − FIO2 is equal to the inspired nitrogen concentration. When R is less than 1, the effect is to increase nitrogen concentration, causing the bracketed term to increase to values greater than 1. In equation 3, if R = 0.8 and FIO2 = 0.21 (room air), the bracketed factor is equal to 1.2.

Examination of equation 3 shows that higher FIO2 values require progressively smaller correction factors; at 100% inspired oxygen (FIO2 = 1.0), no correction is needed. A sufficiently accurate equation for clinical use is a simplified form of equation 3 for patients breathing an FIO2 of 0.60 or less. This is shown as follows:1

For FIO2 values greater than 0.60, a sufficiently accurate clinical equation is as follows:1

In equations 4 and 5, PaCO2 is substituted for PACO2 because these two values are generally equal, unless the lungs have a high degree of alveolar dead space.

A normal PAO2 for a person breathing room air at sea level, with a PaCO2 equal to 40 mm Hg and an R equal to 0.8, is about 100 mm Hg (using equation 4). This is shown as follows:

PAO2=0.2093(76047)(40×1.2)

image

PAO2=149.248

image

PAO2=101.2

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Table 7-1 summarizes respiratory gas partial pressures at sea level in dry inspired air, humidified (tracheal) air, alveolar air, and mixed expired air. Expired gas PO2, PCO2, and PN2 differ from alveolar values because expired air contains dead space gas mixed with alveolar gas.

TABLE 7-1

Partial Pressures of Gases at Sea Level

  Dry Air Humidified Air Alveolar Air Expired Air
Gases mm Hg % mm Hg % mm Hg % mm Hg %
Nitrogen 600.2 78.98 563.4 74.09 569.0 74.9 566.0 74.5
Oxygen 159.5 20.98 149.3 19.67 104.0 13.6 120.0 15.7
Carbon dioxide 0.3 0.04 0.3 0.04 40.0 5.3 27.0 3.6
Water vapor 0.0 0.0 47.0 6.20 47.0 6.2 47.0 6.2

image

Modified from Seeley RR, Stephens TD, Tate P: Anatomy & physiology, ed 3, New York, 1995, McGraw-Hill.

Laws Governing Diffusion

Fick’s law summarizes the factors that determine the rate of gas diffusion through the alveolar capillary membrane. This is shown as follows:

V ˙gas=A×D×(P1P2)T

image

In this equation the following are represented:

V˙gasimage represents the volume of gas diffusing through the membrane per minute (mL per minute).

A represents the surface area of the membrane available for diffusion (cm2).

CLINICAL FOCUS 7-2   Using the Alveolar Air Equation: Effect of Hypoventilation on Alveolar Partial Pressure of Oxygen When Room Air is Breathed

A healthy 60-year-old woman was brought to the emergency department in a comatose state, breathing very shallowly. The family stated that she had taken an excess number of sleeping pills. Arterial blood gases obtained while she was breathing room air (fractional concentration of oxygen in inspired gas [FIO2] = 0.21) revealed arterial oxygen partial pressure (PaO2) of 55 mm Hg, partial pressure of carbon dioxide in arterial blood (PaCO2) of 70 mm Hg, and pH of 7.15. Normal PaCO2 is equal to 40 mm Hg. Her elevated PaCO2 is explained by her hypoventilation; she cannot remove CO2 from her lungs as rapidly as it diffuses in from the capillary blood. But why is her PaO2 reduced?

D represents the diffusion coefficient (D), or diffusivity, of a particular gas. It is directly proportional to the gas solubility (sol) but inversely proportional to the square root of the gas molecular weight (mw):

D solmw

image

This equation states that V˙gasimage increases if there are increases in the membrane surface area, gas diffusivity, or diffusion pressure gradient. The diffusion rate decreases if membrane thickness increases. Doubling the membrane surface area or diffusion pressure gradient doubles the overall diffusion rate; doubling the membrane thickness reduces the diffusion rate by half. Figure 7-3 illustrates the factors involved in Fick’s law.

Physical Gas Characteristics and Diffusion

O2 and CO2 diffuse through gaseous and liquid phases in the lung; the alveolar capillary membrane (see Figure 7-1) is a liquid barrier. Light gases diffuse more rapidly than heavier gases, and highly soluble gases diffuse through liquids more rapidly than less soluble gases. The rate of gas diffusion in the lung is inversely proportional to its molecular weight and directly proportional to its solubility; the diffusion coefficient in Fick’s law is derived from these two factors. Specifically, the gas diffusion rate is inversely proportional to the square root of its gram molecular weight (gmw) (Graham’s law). Relative rates of diffusion for O2 (molecular weight = 32) and CO2 (molecular weight = 44) in a gaseous medium are as follows:

O2 rateCO2 rate=gmwCO2gmwO2=4432=6.635.66=1.171.0

image

Because O2 is a lighter molecule, it diffuses through a gas medium 1.17 times faster than CO2.

Conversely, CO2 is much more soluble in water than O2Henry’s law states that the amount of gas dissolving in a liquid is directly proportional to the gas partial pressure. At body temperature (37° C) and 760 mm Hg pressure, 0.592 mL of CO2 and 0.0244 mL of O2 dissolve in 1 mL of water. CO2 is about 24 times more soluble than O2, as the following equation shows:

CO2 solO2 sol=0.5920.0244=24.31.0

image

Combining Graham’s law and Henry’s law, CO2 diffuses across the alveolar capillary membrane about 20 times faster than O2. This is shown as follows:

CO2 rateO2 rate=3244×0.5920.0244=3.350.16=20.7

image

For this reason, alveolar capillary membrane defects limit O2 diffusion long before they limit CO2 diffusion. In a practical clinical sense, the alveolar capillary membrane never limits outward diffusion of CO2 from blood to alveoli. Discussion of diffusion in this chapter is therefore primarily focused on O2 diffusion.

Limitations of Oxygen Diffusion

Factors influencing the rate of O2 transfer across the alveolar capillary membrane include (1) the partial pressure gradient across the membrane, (2) the diffusion path length, and (3) the membrane surface area. (All factors are included in Fick’s law of diffusion.)

Effects of the Partial Pressure Gradient and Capillary Blood Transit Time on Gas Equilibrium

At a resting cardiac output, a red blood cell spends about 0.75 second traveling through the pulmonary capillary. Normally, the equilibrium between alveolar gas and capillary blood PO2 occurs within 0.25 second, or about one third of the distance through the capillary (Figure 7-4, dark curved line). The time to reach equilibrium may be prolonged if alveolar capillary membranes are thickened (light curved line in Figure 7-4). Even so, equilibrium is virtually always achieved at rest. The rate of diffusion is rapid at first when the partial pressure gradient across the alveolar capillary membrane is greatest. The diffusion rate continuously slows as the partial pressure gradient diminishes (notice the shape of the PO2 curve [dark line] in Figure 7-4) until diffusion completely ceases at equilibrium. Thus, during the last two thirds of travel through the pulmonary capillary, no diffusion normally occurs.

Even when capillary transit time is shortened to 0.25 second by a high blood flow rate during exercise, complete O2 equilibrium normally occurs between alveolar gas and end-capillary blood; it simply occurs at some point farther along the capillary path. In such a situation, the number of O2 molecules transferred into the blood each minute is greatly increased because the greater rate of blood flow takes up more O2 molecules from the alveoli each minute. Another reason exercise increases the number of O2 molecules transferred each minute is that previously nonperfused capillaries are recruited, which increases the surface area for diffusion.

If a healthy person exercises vigorously at a high altitude, where atmospheric PO2 is very low, the O2 diffusion gradient may be so low that O2 cannot diffuse across the alveolar capillary membrane fast enough to establish equilibrium during the shortened capillary transit time. Alternatively, if disease thickens the alveolar capillary membrane, the diffusion rate across the membrane may be slowed enough to prevent complete O2 equilibrium by the time blood leaves the capillary. In the clinical setting, this situation rarely occurs at rest, even in severe lung disease.2 However, exercise immediately exposes the diffusion abnormality problem because it shortens the blood’s transit time through the capillary, making it likely that alveolar and capillary O2 equilibrium never occurs (Figure 7-5). Patients with thickened alveolar capillary membranes are most likely to show evidence of O2 diffusion impairment during exercise.3

Perfusion and Diffusion Limitations to Oxygen Transfer

Figure 7-4 shows that diffusion normally stops when O2 equilibrium is reached between the alveolus and capillary, which occurs long before the blood travels the length of the capillary. If blood flow (perfusion) increases, more O2 leaves the lung each minute because the O2-saturated blood moves out of the capillary more quickly, which means deoxygenated blood enters more quickly to take up more O2. Therefore the O2 diffusion rate through the alveolar-capillary membrane is normally perfusion limited (see Figure 7-4); that is, a change in blood flow rate alters the number of O2 molecules that cross the alveolar-capillary membrane each minute. If O2 equilibrium between the alveolus and capillary never occurs because of thickened membranes, O2 transfer is truly diffusion limited. In such an instance, it is the alveolar capillary membrane, not blood flow rate, that influences the O2 transfer rate (see Figure 7-5).

If one wishes to evaluate the extent to which the alveolar capillary membrane itself impedes the diffusion rate (milliliters per minute of O2 transfer per millimeters of mercury pressure gradient), one should not measure the O2 diffusion rate because it is affected by blood flow rate. Instead, one should measure the diffusion rate of a gas that never reaches equilibrium between alveolar gas and capillary blood, even in resting conditions. In other words, the blood’s capacity for this gas should be so great that the gas cannot diffuse across the membrane fast enough to saturate the blood to capacity before it leaves the capillary. For such a gas, the only factor that limits diffusion is the resistance of the alveolar capillary membrane itself. Carbon monoxide (CO) is the ideal gas for this kind of measurement because blood can absorb it at a greater rate than CO can diffuse across the alveolar capillary membrane, even under resting conditions. For this reason, CO is always diffusion limited. Figure 7-6 illustrates the diffusion-limited characteristics of CO. All events that are illustrated in Figure 7-6 occur at rest; increased blood flow cannot result in greater CO uptake because CO is already diffusing through the alveolar-capillary membrane at its maximum rate. For this reason, CO is commonly used in pulmonary function laboratories to evaluate the lung’s true diffusion capacity.

Hemoglobin in the blood makes O2 and CO much more soluble in whole blood than they are in the alveolar-capillary membrane fluid or the blood plasma. In contrast, a gas such as nitrous oxide (N2O), highly soluble in the alveolar-capillary membrane and plasma, does not chemically bind with hemoglobin; its solubility in whole blood is much less than that of CO or O2. If N2O is inhaled, the pulmonary capillary blood reaches its maximum capacity for N2O almost instantly (Figure 7-7). N2O partial pressures across the alveolar capillary membrane reach equilibrium in the first one twentieth of the distance along the capillary.

Increased blood flow causes N2O-saturated blood to exit the capillary sooner, allowing more mixed venous blood to enter and take up alveolar N2O. Thus, diffusion of N2O in the lung is strictly perfusion limited. This characteristic makes N2O an ideal test gas to measure pulmonary blood flow.

O2 diffusion is normally perfusion limited because it equilibrates across the alveolar capillary membrane long before blood leaves the capillary; increased blood flow increases the amount of O2 taken up from the alveolus. Exercise increases blood flow and may cause O2 to become diffusion limited if the alveolar capillary membrane is thickened.

Diffusion Path Length

The distance for diffusion includes the entire path length from alveolar gas to the hemoglobin in the red blood cell. It was originally thought that the alveolar capillary membrane was the only important rate-limiting barrier to diffusion; it is now known that the red blood cell membrane and rate of O2 combined with hemoglobin limit the lung’s O2 uptake to the same extent as the alveolar-capillary membrane.4 The total diffusion path distance is normally less than 0.1 µ and includes the following (see Figure 7-1): (1) surfactant layer that is lining the alveolar surface, (2) alveolar epithelium, (3) basement membrane of the alveolar epithelium, (4) extremely thin interstitial space, (5) basement membrane of the capillary endothelium, (6) capillary endothelium, (7) plasma, (8) red blood cell membrane, and (9) intracellular fluid bathing the hemoglobin molecule.

Various abnormal conditions can increase the diffusion path length, including the following: (1) fibrotic thickening of alveolar and capillary walls; (2) interstitial edema fluid, separating alveolar and capillary membranes; (3) fluid in the alveoli; (4) interstitial fibrotic processes that thicken the interstitial space; and (5) dilated, engorged capillaries, which allow red blood cells to flow side by side. Abnormalities that increase the distance for diffusion are rarely the cause of decreased end-capillary or arterial PO2 at rest. The major cause of resting hypoxemia in these patients is a mismatch between ventilation and blood flow.2 That is, the processes that increase diffusion distance generally decrease lung compliance, which decreases ventilation in these areas. Blood perfusing these underventilated areas tends to be inadequately oxygenated.

Diffusion Surface Area

Diffusion surface area is the total area of contact between ventilated alveoli and perfused capillaries. A decrease in the number of open, perfused capillaries or in the number of open, ventilated alveoli decreases the diffusion surface area and the lung’s diffusion capacity. In such instances, diffusion capacity is decreased, although the diffusion path length may be normal at all points. For example, emphysema destroys alveolar walls and their associated capillaries, which decreases the diffusion surface area. Although the diffusion path length is not thickened at any point, overall diffusion rate is decreased because much of the functional gas-exchange surface area is lost.

Measuring Diffusion Capacity

General Principles

A diffusion-limited test gas such as CO is used to measure the diffusion capacity of the lung. As clinically performed, the single breath CO diffusion test measures the amount (in milliliters) of CO that diffuses out of the lung into the pulmonary capillaries during a 10-second breath-holding period after first inhaling a known concentration of CO. The average diffusion pressure gradient also must be calculated during the breath-holding period, that is, mean PACO − mean capillary PCO. (Partial pressure of CO in the capillary blood is denoted by the symbol PćCO). The theoretical formula for the diffusion capacity of the lung for CO (DLCO) is as follows:

DLCO=millilitersofCOtransferredtothebloodperminutemeanPACOmeancapillaryPćCO

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Normal Values

Normal DLCO values in healthy individuals vary considerably depending on age, body size, and body position as explained in subsequent sections. A large cross-sectional study of healthy, never-smoking adult men and women in the United States yielded a mean DLCO of 26.4 mL/min/mm Hg (single breath testing method).5 The mean DLCO was about 33 mL/min/mm Hg in men and about 24 mL/min/mm Hg in women. The diffusion capacity of the lung for oxygen (DLO2) is obtained by multiplying DLCO by 1.23. A mean DLCO of 26 mL/min/mm Hg yields a normal DLO2 of about 32 mL/min/mm Hg. It may seem odd that DLO2 is greater than DLCO, considering the much greater affinity of hemoglobin for CO than O2. This peculiarity is explained by the fact that O2 is more soluble than CO in the alveolar capillary membrane and the plasma and diffuses more rapidly. The fact that hemoglobin has 210 times greater affinity for CO than O2 simply means that at a given partial pressure (PCO or PO2), the hemoglobin carries more CO than O2. This fact is unrelated to O2 and CO diffusion rate across the alveolar capillary membrane, which is determined by molecular weight and solubility coefficients.

Factors Affecting Measured Carbon Monoxide Diffusion in the Lung

Body Size

DLCO increases with body size. Larger lungs have a greater absolute DLCO than smaller lungs because they have a greater gas-exchange surface area.

Body Position

DLCO is 15% to 20% greater in supine than in standing positions.4 This is probably because gravitational effects decrease pulmonary blood volume in the standing position.

CLINICAL FOCUS 7-3   Technique for Measuring Carbon Monoxide Diffusion in the Lung

When measuring the carbon monoxide diffusion in the lung (DLCO), a volume of gas equal to vital capacity containing about 0.3% CO is inhaled through a tube attached to a spirometer. This means the patient first exhales forcefully to the residual volume (RV), then inhales the CO gas mixture maximally to total lung capacity (TLC). This breath is held at TLC for 10 seconds, after which the vital capacity is forcefully exhaled back to the RV level. As the exhalation approaches RV, a gas sample from the exhaled stream is collected in a small balloon by opening a valve in the apparatus. This gas represents the composition of alveolar gas. The amount of CO that diffused into the blood is calculated by analyzing the alveolar gas sample for CO and comparing it with the calculated initial alveolar CO concentration. (The amount diffusing in 10 seconds is multiplied by 6 to obtain the amount diffusing in 1 minute.) The spirometer’s microprocessor performs a complicated calculation of the average CO diffusion gradient over the 10-second breath-holding interval. The calculation is complicated because it is not simply the average of beginning and final PCO diffusion gradients but the average of an infinite number of continuously changing pressure gradients occurring over 10 seconds. The pressure gradient driving CO diffusion changes continuously as pressures between alveolus and capillary approach equilibrium. This means the CO diffusion rate changes continuously over the 10-second breath-hold period as well. (Note the changing pressure gradient examples in Figure 7-6.) The microprocessor calculates the average diffusion rate in units of milliliters per minute per millimeter of mercury (mL/min/mm Hg).

Alveolar Partial Pressure of Carbon Monoxide

Heavy smokers already have CO in their mixed venous blood. The presence of CO in mixed venous blood lowers the diffusion pressure gradient across the alveolar-capillary membrane and slows the diffusion rate.

Pulmonary Diseases

Box 7-1 lists conditions that decrease diffusion capacity. DLCO is useful in differentiating emphysema from other obstructive diseases not associated with destroyed alveolar architecture, such as chronic bronchitis and asthma. Asthma is often associated with an increased DLCO. An explanation may be that high inspiratory resistance created by narrowed airways increases negative intrathoracic pressure during maximal inspiration of the test gas, which increases the gas diffusion pressure gradient and the blood flow in lung apices.6

Clinical Use of Carbon Monoxide Diffusion in the Lung

The DLCO test assesses the extent to which the alveolar capillary membrane is a barrier to gas diffusion. Because O2 equilibrium normally occurs before blood traverses one third of the

pulmonary capillary distance, a 50% reduction in DLCO can exist without affecting end-capillary and arterial PO2. In this sense, the DLCO test is more sensitive than the PaO2 to potential O2 transfer problems (i.e., as disease progresses, DLCO becomes abnormal before PaO2). Impairment of diffusion across the alveolar capillary membrane is only one mechanism that can cause arterial hypoxemia. Many factors decrease PaO2 without affecting the diffusion path length or membrane surface area, such as ventilation–blood flow mismatches. The DLCO test can help clarify the mechanism of arterial hypoxemia; if DLCO is normal, diffusion impairment cannot be a contributing factor.