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Department of Physiology, University of Bonn, 53115 Bonn, Germany
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ABSTRACT |
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Heller, Hartmut, Gabi Fuchs, and Klaus-Dieter
Schuster. Pulmonary diffusing capacities for
oxygen-labeled CO2 and nitric oxide in rabbits.
J. Appl. Physiol. 84(2): 606-611, 1998.
We determined the pulmonary diffusing capacity
(DL) for
18O-labeled
CO2
(C18O2)
and nitric oxide (NO) to estimate the membrane component of the
respective gas conductances. Six anesthetized paralyzed rabbits were
ventilated by a computerized ventilatory servo system. Single-breath maneuvers were automatically performed by inflating the lungs with gas
mixtures containing 0.9%
C18O2
or 0.05% NO in nitrogen, with breath-holding periods ranging from 0 to
1 s for
C18O2
and from 2 to 8 s for NO. The alveolar partial pressures of C18O2
and NO were determined by using respiratory mass spectrometry. DL was calculated from gas
exchange during inflation, breath hold, and deflation. We obtained
values of 14.0 ± 1.1 and 2.2 ± 0.1 (mean value ± SD)
ml · mmHg
1 · min
1
for
DLC18O2
and DLNO,
respectively. The measured DLC18O2/DLNO
ratio was one-half that of the theoretically predicted value according
to Graham's law (6.3 ± 0.5 vs. 12, respectively).
Analyses of the several mechanisms influencing the determination of
DLC18O2
and DLNO
and their ratio are discussed. An underestimation of the membrane
diffusing component for CO2 is
considered the likely reason for the low
DLC18O2/DLNO
ratio obtained.
alveolar-capillary gas exchange; single-breath method
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INTRODUCTION |
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THE OVERALL PULMONARY diffusing capacity (DL) is commonly determined by using carbon monoxide (CO) as an indicator. According to Roughton and Forster (19), the overall conductance of the alveolar-capillary CO transfer (DLCO) can be partitioned
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(1) |
CO is the CO uptake conductance
of red blood cells per unit blood volume, and Vc is the pulmonary
capillary blood volume. DmCO can
be determined by using the results of
DLCO
measurements during hyperoxia and normoxia as well as
CO values derived from in vitro
studies. The DmCO data as reported
by Roughton and Forster are under debate at present. By using
morphometric techniques, Crapo et al. (5) found 10-fold higher values.
On the other hand, Hsia et al. (12) concluded from theoretical analyses
that the Roughton-Forster model provided reasonable estimates of
DmCO.
Apart from CO, two novel indicator gases have recently been introduced for estimating Dm: doubly labeled carbon dioxide (C18O2) and nitric oxide (NO). Both gases are assumed to be quickly eliminated by chemical reactions within the red blood cells: C18O2 because of isotopic exchange catalyzed by carbonic anhydrase (21) and NO by very rapid binding to hemoglobin, the reaction of which is 280 times faster than that of CO (4, 14). Therefore it is expected that the uptake of both gases is mainly limited by diffusion. Because the pathways of both gases include the alveolar-capillary membrane, the plasma layer, and the red blood cell membrane, as well as the mean diffusion distance within red blood cells to the point of reaction, overall DL of NO (DLNO) and C18O2 (DLC18O2) are similar but not identical with Dm, even when assuming that reaction rates of both gases are infinitely high.
Because the DLNO/DLCO ratios in humans (8, 13) and in dogs (14) were higher than the respective ratio of Krogh's diffusion constants, it has been concluded that DLNO indeed represents the membrane component DmNO. However, because the C18O2 uptake may be influenced by isotopic exchange reactions (16, 21) and NO may react with tissues (14, 26), the interpretation of DLC18O2 and DLNO determinations has remained uncertain.
To assess which of the two indicator gases yields the closer approximation to Dm, we performed measurements of DLC18O2 and DLNO on rabbits to study the uptake kinetics of both gases as well as the influences exerted by chemical reactions.
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METHODS |
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The experiments were carried out on six supine rabbits (mean body
weight, 3.15 kg; range, 2.8-3.3 kg) that were anesthetized with
pentobarbital sodium (19 mg · kg
1 · h
1
iv), paralyzed by alcuronium (0.09 mg · kg
1 · h
1
iv), endotracheally intubated (2.5-3 mm ID), and artificially ventilated by a computerized ventilatory servo system. The ventilator was designed to maintain steady mechanical ventilation and to enable
single-breath maneuvers.
Indicator gas mixtures and protocol of experiments. To avoid the formation of NO2 or its dimer N2O4 within the inspiratory gas and to facilitate the comparison of DLC18O2 and DLNO, two O2-free gas mixtures (containing 0.9% C18O2 in N2 and 0.05% NO in N2) were prepared and stored in gas-tight flexible aluminum bags. NO from the pure source was led through diluted KOH, subsequently collected with a KOH-containing syringe, and finally injected into the aluminum bag, which had been washed out repeatedly with N2. To avoid reaction with water, pure C18O2 was dried within a trap and led into a bag containing N2.
Before the single-breath maneuvers, pressure-volume curves were recorded. For this purpose, the lungs were inflated and deflated by definite volume steps, and the airway pressure was measured during short breath holds by a differential pressure transducer covering a range between
20 and +20
cmH2O. The residual volume (RV)
was defined as the resting lung volume attained at
20
cmH2O of airway pressure.
Because breath-holding periods of 0-3 s for
C18O2
(21) and 3-10 s for NO (2, 8, 13) are known to be suitable for
measuring the respective diffusing capacities, we had to
perform the
DLC18O2 and DLNO
determinations in separate experiments. Starting from RV,
the lungs were inflated by using 50 ml of the indicator gas mixtures.
After the breath-holding periods, up to 50 ml of total expired gas was
sampled by deflating the lungs via a spiral stainless steel tube (3.5 mm ID, length 5 m). The respective times for inflation and deflation
were set at 0.6 s for
C18O2
and at 1 s for NO. The gas stored within the tube was dried by
freezing. The alveolar sample was continuously sucked from the tube
into the inlet system of the mass spectrometer. RV was calculated from
the argon (Ar) dilution produced by inflating the lungs with the
Ar-free indicator gas mixtures. Anatomic and apparatus dead spaces were
determined in separate experiments by recording expirograms for
C18O2
and NO, and dead spaces were used to calculate the
effective inflation and deflation times (22).
Mass spectrometry. We used a respiratory magnetic sector mass spectrometer (M3; Varian MAT, Bremen, Germany) modified to measure isotopic ratios also (23). The relevant gases (NO, O2, CO2, Ar, and C18O2) were recorded, setting three ion collectors at the following mass-to-charge ratios (m/e): 30 for NO, 32 for O2, and 44 for CO2. We determined CO2 at the first plate of a double-ion collector set at m/e = 44. By repeatedly changing the accelerating voltage (peak jump), we detected C18O2 at the second plate of this double collector (m/e = 48). In the same way, Ar (m/e = 40) was measured at the CO2-44 ion collector. The signal-to-noise ratios for C18O2 and NO were 1,800:1 at 8,700 parts/million C18O2 and 325:1 at 500 parts/million NO. A particular feature of the analyzing procedure is that dry sample gas was repeatedly compared with a reference gas that differed only in its C18O2 or NO content. Drift errors and cross-talk effects were thereby avoided (7, 14), background of the mass peaks was subtracted, and C18O2 concentration was obtained in terms of the difference compared with natural abundance.
Calculations for DL. We used the alveolar partial pressures (PA) for C18O2 and NO (PAC18O2 and PANO, respectively) obtained from the end-tidal portion of the gas sample. These values were processed by performing the DLC18O2 and DLNO calculations on the basis of three equations defining gas transfer during inspiration, breath holding, and expiration, as previously described (22). DL was calculated by a trial-and-error approximation method. A detailed description of the underlying model and derivation of the equations is given elsewhere (22).
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RESULTS |
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A total of 63 single-breath experiments for C18O2 were carried out in six rabbits. The lung volume before inflation (RV) averaged 14.1 ± 1.8 (SD) ml, the lung volume after inflation was 64.1 ± 1.8 ml, dead space averaged 6.93 ± 0.9 ml, and static compliance was 2.23 ± 0.2 ml/cmH2O. The breath-holding periods ranged from 0 to 17 s. In Fig. 1, the ratio of the PAC18O2 at overall time t and time 0 (PAC18O2/PA0,C18O2) is related to the overall time (including inflation, breath holding, and deflation) for the C18O2 disappearance from alveolar gas. PA0,C18O2 (ranging between 6 and 7 Torr) was derived by calculating the dilution of inspired C18O2 within the alveolar volume. The 18O label was removed according to the relationship
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(2) |
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The coefficient 0.9965 was calculated as 1
0.0035, because a
reasonable extrapolation to time 0 from the measurements (Fig. 1) was not feasible. During the
initial phase (t <3 s), the ratio PAC18O2/PA0,C18O2
was reduced to <0.01. The
DLC18O2
was calculated from the fast component, as explained
previously (21, 22). The smallest
PAC18O2
values, measured during the slow phase, came close to 30 times the
level of natural abundance of 18O.
The NO results from 24 measurements are similarly illustrated as a plot of PANO/PA0,NO vs. t in Fig. 2. In each animal, the overall time available for NO removal was set at 4, 6, 8, and 10 s. During a time span of 10 s, >99% of the inhaled NO disappeared from the alveolar gas. Nonlinear regression analysis provided the following PANO/PA0,NO-to-time relationship
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(3) |
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The
DLC18O2
and DLNO
data from each animal are shown in Table 1.
The overall values (means ± SD) are 14.0 ± 1.1 ml · mmHg
1 · min
1
(for
DLC18O2;
n = 34) and 2.2 ± 0.1 ml · mmHg
1 · min
1
(for DLNO;
n = 24). The reproducibility,
determined as the coefficient of variation (SD/mean value) in each
animal, was 7.5% for
DLC18O2 and 4.4% for
DLNO.
Because of the ratio of RV-to-inspiratory volume (14/50 ml) in the
animals, the end-tidal PO2 values (as determined within the end-tidal portion of the alveolar gas sample) averaged 21 ± 3 Torr. The far right column of Table 1 contains the
DLC18O2/DLNO
ratios. The
DLC18O2/DLNO ratio averaged 6.3 ± 0.5 (±SD). There was no
significant correlation between the individual
DLNO or
DLC18O2
values and the
DLC18O2/DLNO
ratios.
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DISCUSSION |
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Critique of methods. The technique of applying 18O-labeled CO2 and NO for determinations of diffusing capacity has been analyzed previously (14, 21, 22). A serious problem was the high removal rate of both gases, in particular of C18O2. Therefore, we performed very short single-breath maneuvers and, instead of only considering breath holding (as usually applied for determining DLCO), the phases of inspiration and expiration were also taken into account. However, there was no significant difference between DL values obtained at different end-expiratory partial pressure levels and with different breath-holding times. This result indicates that the problem of calculating DL from very short single-breath experiments was reasonably solved by applying the three-equation solution (22). More than 99% of inspired C18O2 disappears from alveolar space within 3 s (Fig. 1). Thereafter, the small remaining residue is removed very slowly during a second phase. The first phase of label decay is assumed to be primarily caused by alveolar-capillary transfer of C18O2; however, the second phase is as yet poorly understood. A similar characteristic has been previously found in humans (22). In this paper, the phenomenon of slow label removal was assumed to be caused by admixtures regained from dead spaces or from the bicarbonate and water pools of the tissues lining the airways and alveoli. Nioka et al. (16) did not find this slow phase of label decay in rebreathing studies of C18O2 uptake performed on isolated buffer-perfused guinea pig lungs. This discrepancy could be caused by the fact that the sources of C18O2, which account for the effects in single-breath experiments, are unloaded during rebreathing. We determined the DLC18O2 from the fast phase of C18O2 removal, correcting the respective PAC18O2 values by subtracting the partial pressure of the remaining residues. The influence of pulmonary tissues was neglected. This may lead to errors in DLC18O2 determinations (21, 22) and is therefore briefly discussed below.
Comparison of DLC18O2 and DLNO determinations. C18O2 as well as NO have been applied for assessing Dm, the membrane component of DL (2, 8, 14, 21). The question arises which of the two indicator gases yields the closer approximation to Dm. This question cannot be answered by simply comparing the DL values.
According to the model of Roughton and Forster (19), DL represents a combination of two conductances: a membrane component Dm and a blood component (
· Vc; see Eq. 1). DL is
lower than Dm but approaches Dm for
· Vc
. The membrane component represents only a diffusion process.
Therefore, Dm values of different gases are expected to be related to
each other as are the respective Krogh's diffusion constants of the
diffusion pathways, including water and lipid layers. The same relation
should exist for
DLC18O2 and DLNO
when assuming that the corresponding reaction rates within red blood
cells are infinitely high. Unfortunately, data on lipid bilayers of the
alveolar-capillary membrane are unavailable to date. The ratio of
Krogh's diffusion constants for
C18O2
and NO, estimated from the product of the solubility constant ratio in
water
(
/
NO = 15.2; see Refs. 1 and 28) and the reciprocal square
roots in the respective molecular weights (
/
= 0.79), yields a value of 12, whereas the mean experimental
DL ratio was 6.3. Apart from the
possibility that the unknown solubilities of both gases in lipid
bilayers could contribute to this deviation, various other sources
could also account for it. We will analyze these in the following
section.
Factors affecting the
DLC18O2/DLNO
ratio.
The almost complete disappearance of
C18O2
is caused by isotopic exchange reactions that have been
described in detail in previous papers (16, 22). In brief,
C18O2
reacts with water,
H216O,
forming bicarbonate,
HC18O16O18O
.
During the back reaction, there is a one-third probability of regaining
C18O2
but a two-thirds probability for producing
C16O18O
and 18O-labeled water
(H218O). This
isotopic exchange occurs very quickly within the red blood cells
(because of high catalytic activity of carbonic anhydrase) and, to a
smaller extent, within pulmonary tissues. This means that the
18O label and thus, in a broader
sense, also
C18O2,
disappears into the large O2 pool
of body water, thereby reducing the back pressure of
C18O2
to very low values. Because
DLC18O2
is calculated by assuming the back pressure to be zero, it represents a
lower limit of
DmCO2
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(4) |
Influence of inhomogeneities. Determinations of DL are based on the assumption of functionally homogeneous lungs. By simulating rebreathing experiments in studies of the influences of various inhomogeneities, Meyer et al. (14) have shown that sufficiently large inhomogeneities can significantly affect the DLNO/DLCO ratio. Because single-breath experiments are supposed to be more strongly influenced by inhomogeneities, and the DLC18O2/DLNO ratio exceeds DLNO/DLCO by a factor of two, even larger effects could have affected our experiments. Therefore, we modeled single-breath maneuvers in a manner fairly similar to that described by Meyer et al., investigating unequal distributions of tidal volume, RV, DL, and combinations of these parameters for two parallel alveolar compartments. We obtained decreases in the effective DLC18O2/DLNO below the DLC18O2/DLNO values of a homogeneous lung for various types of inhomogeneities; these were most pronounced when DL values were distributed inhomogeneously. Distributing 80% of DL to the first compartment and 20% to the second compartment produced reductions of DLC18O2 by 56%, DLNO by 36%, and DLC18O2/DLNO by 31% compared with homogeneous conditions. Marked inhomogeneities thus have to be assumed to explain a significant deviation between DLC18O2/DLNO and Krogh's diffusion-constant ratio. Moreover, the inhomogeneities must have been of similar extent in all six rabbits studied; otherwise, we should have found a correlation between the interindividual DL values and the DL ratios. Therefore, we conclude that inhomogeneities of a parallel type could have exerted only a minor influence on the DLC18O2/DLNO ratio.
Stratified inhomogeneities, i.e., axial gas-mixing deficit inside the alveolar space, have also been discussed for many years as a possible limiting factor of pulmonary gas exchange. Some recent experimental studies (15, 20, 24) have provided evidence for the importance of stratified inhomogeneities. According to the simple model of Okubo and Piiper (17), and taking the overall conductance DL as being limited only by diffusion, DL is partitioned into two serially arranged conductances through
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(5) |
1 · min
1
and GSNO = 1.26 · GS,C18O2,
one obtains from Eq. 5, with our
experimental
DLC18O2 and
DLNO/DmC18O2 = 28 ml · mmHg
1 · min
1,
DmNO = 2.35 ml · mmHg
1 · min
1
and
DmC18O2/DmNO
12, a value that is in keeping with the Krogh diffusion-constant
ratio. A GS of such a
magnitude is not contradictory to the data gathered from the pertinent
literature. Qualitatively, the outcome is easily understood, because an
additional limitation of gas uptake brought about by stratification is
expected to predominantly influence the uptake of the gas with the
largest diffusing capacity, i.e.,
C18O2.
Because a certain amount of the deviation between
DmCO2 and DLC18O2
may be attributed to other (parallel inhomogeneity) factors, as
discussed above, an even smaller gap has to be closed by a higher
GS
(meaning less gas-phase diffusion resistance) to explain the
experimentally found
DLC18O2/DLNO ratio.
Influence of pulmonary tissues on DLNO determinations. Calculations of diffusing capacity depend on the alveolar distribution volume (VA), which was determined on the basis of the Ar dilution. Previous determinations by Meyer et al. (14), in rebreathing experiments on dogs, have shown that VA for NO exceeded VA for the poorly soluble gas He by up to 36%. They considered three major reasons as possibly accounting for the excess of the VA of NO over the VA of He.
Reversible absorption of NO by lung tissues is well known for gases with higher solubilities such as N2O or C2H2. However, the water-gas partition coefficient for NO is low 0.0292 (26). NO is a highly reactive molecule and is known to combine with a number of biochemical species. However, no data for a quantitative estimation are available. Irreversible binding of NO during the early part of the breathing maneuver could produce effects such as reversible absorption and cannot be easily evaluated. However, a dependence of DLNO on breath-hold duration, which was not found in our data, would then be predicted. Irreversible binding of NO throughout the experiment would constitute an apparent conductance in parallel with the true NO conductance gas to blood and DLNO would be overestimated. Reaction kinetics other than those of the first order should lead to a DLNO-to-breath-hold dependence that was not observed. But reaction of NO with tissues in proportion to partial pressure of NO would be indistinguishable from transport by alveolar-capillary NO diffusion. Spriestersbach et al. (26) perfused isolated rabbit lungs with Krebs-Henseleit buffer equilibrated with NO. The NO inflow was almost completely recovered within the expiratory gas flow, and to a minor extent in the outflow, suggesting that chemical reactions contribute little to NO elimination. In another series of experiments, the above authors admixed NO at various rates (31.4-2,500 nmol/min) to the inhaled gas flow (900 ml/min) and measured the appearance rate values within the buffer fluid of lung perfusion. Using their data, we could calculate the rate of NO disappearance by reaction and by dividing the data according to the estimated alveolar partial pressures of NO (PANO). Thus we obtained a "chemical conductance" (in ml · mmHg
1 · min
1)
of 0.022-0.064, for
PANO from
6.7 to
540 · 10
4
mmHg. These values range from 1 to 3% of our
DLNO mean
values; thus the value of
DLNO would
be only marginally affected.
DLNO
depends on chemical reactions not only in terms of rate constants; the
location of NO elimination is also of significance. If NO is already
eliminated within the gaseous phase or on the alveolar surface, the
influence on
DLNO is
maximal, whereas reactions within the red blood cells which
additionally occur to the combining with hemoglobin, would have no
effect, and reactions taking place on capillary endothelium or within
plasma may lead to a slight overestimation of
DLNO.
However, these considerations are of minor importance with regard to
the overall minor contribution of reaction as discussed above.
It has been shown that NO is also endogenously generated and expired
from lungs (9, 26); this could lead to an underestimation of
DLNO.
Assuming that endogenous NO production is independent of inspired NO,
the DLNO
values obtained from single-breath experiments should decrease with
increasing breath-hold duration. From the absence in our data of such a
dependence, we conclude that an endogenous production of NO did not
influence our measurements. This conclusion also becomes evident when
taking into account the exhalation rates of endogenously produced NO in
isolated perfused rabbit lungs (26), amounting to 2 nmol/min compared
with the mean NO uptake rate of our single-breath experiments, which
amounts to 4,000 nmol/min at 8 s of breath holding.
Comparison with data in other studies.
On the basis of Eq. 1,
DmNO can be estimated by using the
DLNO value
of the present study,
NO = 4 ml · ml
1 · mmHg
1 · min
1, as calculated from
Carlsen and Comroe (3) and pulmonary capillary blood volume, 3 ml,
yielding DmNO
2.7 ml · mmHg
1 · min
1.
However, measurements of red blood cell reaction kinetics by rapid-mixing technique, as previously performed (3), may have been
seriously biased by diffusion limitation from unstirred layers (11,
14). Therefore, true
NO may
have been considerably higher (8) and
DmNO would represent an upper
limit rather than the true value. This is confirmed when using the data
of
O2, as has been measured previously (10).
Because both solubility and reaction rate with hemoglobin are greater
for NO than for O2,
O2 is expected to
represent an underestimate of
NO, providing
NO >14
ml · ml
1 · mmHg
1 · min
1.
By using
DLNO = 2.2 ml · mmHg
1 · min
1
and pulmonary capillary blood volume = 3 ml again, such
NO estimate reveals
DmNO
2.3 ml · mmHg
1 · min
1,
hence representing a value that is <5% higher than the overall DLNO.
Altogether,
DLNO should
provide the closest underestimate of Dm that can be obtained from
measurements in vivo.
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ACKNOWLEDGEMENTS |
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The authors gratefully acknowledge the expert technical assistance provided by Bernd Eixmann, Christa Pusch, and Barbara Schreiber.
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FOOTNOTES |
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Address for reprint requests: H. Heller, Dept. of Physiology, Univ. of Bonn, Nussallee 11, D-53115 Bonn, Germany.
Received 24 January 1997; accepted in final form 25 September 1997.
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