Division of Respiratory and Critical Care Physiology and Medicine,
Harbor-University of California Los Angeles Medical Center,
Torrance, California 90509 - 2910
lactic acidosis threshold; maximum oxygen consumption; carbon
dioxide transport; arteriovenous carbon dioxide difference; cardiac
output
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INTRODUCTION |
OUR LABORATORY
RECENTLY demonstrated that direct Fick principle calculated
cardiac output using CO2 (COCO2)
agrees well with cardiac output using O2
(COO2) in normal subjects at rest and during
exercise (51), as predicted by Fick (16).
Other investigators, to avoid blood sampling, have calculated
COCO2 indirectly (7, 12, 15, 29,
36). This approach, although superficially attractive,
pays insufficient attention to the effect of pH and change in buffer
base on the accuracy and precision of the estimation of CO2
concentration (CCO2) from
PCO2, particularly during work rates at which
lactate is increased. Blood CCO2 is influenced by pH, PCO2, Hb concentration, and
oxyhemoglobin saturation (SO2). During
exercise, the CO2 pressure-concentration relationship
(PCO2-CCO2 relationship) may be more complex than the near-linear relationship depicted in textbooks and the original reports (8, 38,
56), because it is assumed that there is no change in buffer
base as PCO2 increases. A frequently referenced
report, which presents formulas for refining the influences of
PCO2, Hb, and SO2 on
CCO2 at rest and during exercise, concludes
that "the relationship (PCO2-CCO2) is only
slightly influenced by changes in pH" (34). Although
some investigators recommend correction for acid-base changes
(18, 27), most investigators have calculated the
arteriovenous CCO2 difference [mixed venous
CCO2
(C
CO2)-arterial
CCO2 (CaCO2)] for
estimating cardiac output by the indirect Fick method from mixed venous
PCO2 (P
CO2) and
arterial PCO2 (PaCO2),
correcting only for changes in Hb and SO2, but
ignoring pH changes (6, 9-11, 26, 31-33, 35, 37,
42).
It is well known that acidemia due to lactic acidosis occurs with
symptom-limiting exercise, both in normal subjects and patients (3, 4, 21, 50-55), resulting in an almost
stoichiometric decrease in bicarbonate concentration
([HCO
]) as lactate increases (46, 48,
55). This intimate relationship challenges the concept that
changes in pH only slightly influence CCO2
during exercise. We measured pH, PCO2, Hb, and
SO2 in both arterial and mixed venous blood
during progressively increasing work rate exercise to maximum (Max) in
normal subjects to determine the relative importance of the changes in
pH, Hb, and SO2 on the PCO2-CCO2 relationship
and on each component in CO2 transport. We hypothesized
that, by ignoring changes in acid-base balance during exercise, major
errors result in estimates of CCO2 from PCO2 at work rates above the lactic acidosis
threshold (LAT). This could translate into major errors when these
values are used to calculate cardiac output by the Fick principle.
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METHODS |
Subjects, Protocol, and Measures
Subjects.
The research protocol was approved by the Human Subjects Committee at
Harbor-UCLA Medical Center. Informed consent was obtained from five
healthy nonsmoking male subjects that participated in the study.
Catheter placement.
A flow-directed pulmonary artery catheter (Arrow International,
Reading, PA) was introduced via a femoral vein sheath (Cordis, Miami,
FL), which had been inserted percutaneously into the right femoral vein
and positioned in the main pulmonary artery under direct fluoroscopic
guidance. An arterial catheter was placed percutaneously into the left
brachial artery. Each catheter was attached to an infusion apparatus
(Continu-Flo, Baxter Health Care, Deerfield, IL), which provided a
slow, continuous flow (15 ml/h) of heparinized normal saline (1,000 U
heparin/l) and allowed periodic bolus flushings.
Exercise protocols.
An increasing work rate exercise test was performed on an
electromagnetically braked cycle ergometer (type 18070, Gould-Godart, Bilthoven, the Netherlands). The rate of work rate increase (range 25-40 W/min) depended on a preliminary, noninvasive increasing work rate exercise test designed to achieve exhaust in ~10 min. Gas-exchange and heart rate measurements were averaged for each 30-s
period during 3 min of rest and 3 min of unloaded pedaling and during
the progressively increasing work rate test to maximum tolerance. Pedal
frequency was maintained at 60 rpm.
Respired-gas analysis.
The subjects respired through a mouthpiece during the test. Expired air
was directed to a Fleisch type 3 pneumotachograph via a breathing valve
(100-ml dead space). The PO2,
PCO2, and partial pressure of N2 at
the mouthpiece were continuously measured by mass spectrometry
(MGA-1100, Perkin Elmer, Pomona, CA). Minute ventilation
(BTPS) and O2 uptake
(
O2) and CO2 production
(
CO2) (both STPD) were
calculated as whole breath averages for each 30-s exercise period, as
previously reported (49). The LAT and maximal
O2, defined as the
O2 averaged over the last 30 s of
exercise, were determined (4). Later, for tabular and
graphic representations of the group response, the
O2 was normalized to LAT with
O2 at LAT set as 1.00 for each subject
and all other values on either side of LAT set as a ratio of LAT.
Values were calculated at each minute of exercise.
Blood samples.
Blood was sampled simultaneously from the pulmonary artery and brachial
artery during rest and unloaded cycling and at each minute of
increasing work rate exercise. Blood-gas samples were drawn over a 15- to 20-s period. The samples were collected in glass syringes that
contained a small amount (mean 0.14 ml) of liquid heparin (1,000 U/ml).
The blood samples were agitated to prevent clotting and were
immediately placed in an ice slurry.
Blood analyses.
Blood-gas analyses were performed by using an Instrumentation
Laboratory 1306 blood-gas analyzer (Lexington, MA) for pH,
PCO2, and PO2 and an
Instrumentation Laboratory 482 CO-oximeter for Hb and
SO2. The blood-gas analyzer was recalibrated
every 20-30 min. Tonometered blood samples were used to verify
accuracy. The measured values were corrected for heparin dilution and
the known consistent underestimation of blood
PCO2 values >45 Torr (23, 51).
Calculation of CCO2,
C
CO2-CaCO2,
COCO2, and Plasma [HCO
]
Values of CCO2,
C
CO2-CaCO2,
COCO2, and plasma [HCO
].
The plasma CCO2
(CCO2 pl) (mM) and plasma
[HCO
] (mM) were calculated from the standard formula derived from the Henderson-Hasselbalch equation (13, 21,
34, 38)
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(1)
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(2)
|
where s is the plasma solubility coefficient (in
mM/Torr) of CO2 and pK' is the apparent
dissociation constant of the CO2-HCO
system. The variable s is 0.0307 in plasma at 37°C and pH
7.4 in normal human subjects (1). The variable
pK' was calculated from Kelman's equation (13,
28), assuming the temperature was stable at 37°C during
short-period exercise (51)
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(3)
|
Total blood CCO2 (mM) was calculated
from the equation of Douglas et al. (13), modified from
Visser's equation (34) after taking into account the
effects of changing pH during exercise on pK'
|
(4)
|
where [Hb] is Hb concentration.
Substituting CCO2 pl of Eq. 1 into Eq. 4, we obtained Eq. 5
|
(5)
|
After CaCO2 and
C
CO2 were calculated
(Eq. 5), the
C
CO2-CaCO2 and
concurrent COCO2 were calculated, the latter by the Fick principle (16).
Default values of CCO2,
C
CO2-CaCO2, and
COCO2.
To compare the magnitude of error caused by the failure to acknowledge
changes in pH, Hb, and SO2 from rest to
exercise on the
PCO2-CCO2 relationship,
default (Def) values of CCO2 were calculated by
using the resting values of pH, Hb, and/or SO2
for each individual. Def values are so named because they do not
acknowledge the changes in one or more of the independent variables
during exercise. For example, if the changing
PCO2, Hb, and SO2
values were used to calculate CCO2 during each
minute of exercise but the pH remained at its resting (or Def) value,
the CCO2 would be identified as Def-pH
CCO2. In the same way, we calculated Def-Hb, Def-SO2, and the combined Def-pH, Hb and
SO2, the latter when changes in all three
values were not taken in to account. The percent errors of the Def
values from the actual values of CaCO2, C
CO2,
C
CO2-CaCO2, and
COCO2 for each stage of exercise were calculated using the following formula: %error = 100 × (default
actual)
actual.
Relative importance of multiple factors on the
PCO2-CCO2 relationship
during exercise.
Besides physically dissolved CO2 ([CO2]),
which depends only on PCO2 under isothermic
conditions, the two major factors influencing the
PCO2-CCO2 relationship
in the Douglas equation are the HCO
factor
(Fbic, i.e., the effect of pH on the quantity of
[HCO
] in both plasma and red blood cell) and the
Hb factor (FHb, i.e., the effect of Hb binding to
CO2). The FHb consists of three subfactors, the
Hb concentration (FHbHb), the
SO2
(FHbSO2),
and the pH (FHbpH), on Hb binding of
CO2. The formulas for the two major factors and the
three subfactors are given in APPENDIX A. After calculation
of actual values of each factor and subfactor using these equations,
the relative importance of the changes in each factor and subfactor at
each stage of exercise was calculated. Thus the influence of a specific
factor or subfactor at any stage of exercise depends on how far its
ratio differs from 1.00.
Estimation of Each Component of Blood CO2 During
Exercise
The CO2 is transported as six components in human
blood, [CO2], [HCO
], and carbamino
concentration ([NH-CO2]) in both the plasma and the red
blood cell. To compare the relative importance and change of each
component of CO2 during exercise, we calculated each of
these six components using the equations in APPENDIX B.
Data Analysis and Statistics
Unless otherwise specified, all data are expressed as means ± SD, with range values in parentheses. Data were analyzed
predominantly by ANOVA; paired t-tests were used only when
specified. The values of CCO2 calculated from
Douglas' equation and APPENDIX B were compared by using
linear regression and Pearson product-moment correlation coefficients.
A P < 0.05 was considered significant.
 |
RESULTS |
The subject's physical characteristics and aerobic parameters
were as follows: age, 25 ± 5 (20-34) yr;
height, 179 ± 3 (173) cm; body weight,
73 ± 5 (68-80) kg; work rate at LAT, 126 ± 25 (98-154) W; maximum work rate, 302 ± 47 (225-360) W;
O2 at LAT, 2.00 ± 0.31 (1.50-2.35) l/min; and maximal
O2, 3.91 ± 0.61 (2.74-4.31) l/min. From rest to Max,
O2 increased
over 10-fold, from 0.37 ± 0.04 to 3.91 ± 0.61 l/min;
CO2 increased over 16-fold, from 0.29 ± 0.04 to 4.84 ± 0.71 l/min; heart rate increased
nearly threefold, from 63 ± 6 to 178 ± 12 beats/min;
whereas cardiac output increased over threefold, from 7.06 ± 2.37 to 25.38 ± 3.90 l/min. The rate of increase in
O2 as related to work rate increase was
10.03 ± 0.34 (9.50-10.68)
ml · min
1 · W
1, similar to
that previously reported (24, 25, 52).
Actual Changes in Blood CO2 Content
Both mixed venous and arterial Hb increased slightly but
significantly above the LAT as Max was approached (P < 0.05 to P < 0.01) (Table 1).
Mixed venous values for Hb are not shown because they differed
minimally from arterial values (0.2 ± 0.3 g/dl). The mixed venous
SO2 progressively decreased from rest to Max (P < 0.05 to P < 0.001), whereas arterial
SO2 decreased slightly near Max
(P < 0.05) (Table 1). Both mixed venous pH
(pH
) (P < 0.05 to P < 0.001) and arterial pH (pHa) (P < 0.05)
progressively decreased from rest to Max, with pH
decreasing more than the pHa (P < 0.05 to
P < 0.01 by paired t-test) (Fig.
1 and Table 1).
P
CO2 increases were marked, with progressively increasing values from rest to Max, particularly above the LAT (P < 0.05 to P < 0.001) (Fig. 1 and Table
1). PaCO2 increased slightly from rest
(P < 0.05) to LAT, then stabilized, and then decreased
moderately near Max (P < 0.01 vs. LAT;
P < 0.05 vs. rest value) (Fig. 1). Thus mixed
venous-arterial differences of O2 concentration,
C
CO2-CaCO2 (Fig.
1), SO2, pH, and PCO2
all progressively increased from rest to Max (P < 0.05 to P < 0.001) (Table 1).
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Table 1.
Values of Hb, SO2, pH, and
PCO2 in mixed venous and arterial blood and
their differences at rest and during exercise
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Fig. 1.
PCO2 (A), CO2
concentration (B), pH (C), and O2
concentration (D) in both mixed venous (solid symbols) and
arterial (open symbols) blood as related to O2 uptake
( O2) normalized to the lactic
acidosis threshold (@LAT) for 5 normal subjects. The first symbol on
the left of each plot identifies the resting value, whereas the second
symbol of each plot identifies the value at unloaded pedaling.
Subsequent symbols from left to right are at
approximately minute intervals during incre mental work to maximum
(Max). The x-axis is normalized so that
O2@LAT = 1.0. The actual
average O2 at LAT is 2.0 with a range of
1.50-2.35 l/min. Note the widening differences between mixed
venous and arterial values for all variables as work intensity
increases. The differences become more marked above the LAT. The
concentration of O2 was calculated from the following
equation: concentration of O2 (mM) = (1.34 × Hb × SO2 + 0.00326 × PO2) 2.226, where
SO2 is oxyhemoglobin saturation
(51). The decrease in C CO2
during heavy exercise, despite the concurrent rise in
P CO2, is noteworthy. Values are means ± SE.
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It is impressive how little change took place in
C
CO2 from rest (23 mM) to Max (24 mM),
despite large changes in P
CO2 (47-78 Torr)
(see Figs. 1 and 2 and Table
2). Initially, as exercise became more
intense, C
CO2 increased more than
CaCO2. C
CO2 then
stabilized, whereas CaCO2 began to decrease
(P < 0.05 or P < 0.01) (Fig. 1). As
exercise increased to maximum, the C
CO2 decreased from its peak level (Table 2, at 5 min of incremental exercise) to slightly above its rest value in the case of
C
CO2 (P < 0.01) and
below the rest value in the case of mixed venous [HCO
] (Fig. 2B). In contrast,
CaCO2 decreased to a much greater degree with
little change in PaCO2. Thus the progressive increase
in C
CO2-CaCO2
below LAT was due to an increasing C
CO2,
whereas above LAT it was primarily due to a decreasing
CaCO2 (Fig. 2).

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Fig. 2.
CO2 (CCO2;
A) and plasma bicarbonate concentrations
([HCO ]; B) as related to
PCO2 at minute intervals in both mixed venous
(solid symbols) and arterial (open symbols) blood in response to
increasing work rate to Max. Arrows connect the corresponding arterial
and mixed venous values at rest, LAT, and Max. Dotted lines, iso-pH
values, assuming a Hb of 15 g/dl and a SO2 of
100%. A: from rest to LAT,
C CO2 increased as
P CO2 increased. Above LAT,
C CO2 temporarily stabilized and then
decreased, despite the increasing P CO2.
CaCO2 increased slightly as
PaCO2 and H+ increased below the LAT.
Above the LAT, CaCO2 sharply decreased because
of a decrease in [HCO ], pH, and
PaCO2. Mixed venous-arterial differences
[C CO2-CaCO2]
progressively widened as exercise intensity increased (Table 2). Below
the LAT, increases in
C CO2-CaCO2 were
mainly due to the increases in C CO2;
above LAT increases in
C CO2-CaCO2 were
primarily due to decreases in CaCO2.
B: the similarity of the patterns in the changes in plasma
[HCO ] indicates the dominance of
HCO as the primary form of CO2 in the
PCO2-CCO2 relationship
during exercise.
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Influence of pH on the
PCO2-CCO2 and
PCO2-[HCO
] relationships
during exercise.
As shown in Fig. 2A and Table 2, the
PCO2-CCO2 relationship
was markedly influenced by pH changes during exercise. From rest to
LAT, C
CO2 increased relatively less than
P
CO2 because of a moderate decline in
pH
(P < 0.001). Transiently, above
LAT, C
CO2 stabilized, despite further increases in P
CO2 due to the start of a fall in
[HCO
] reflected by the decrease in
pH
. Eventually, despite the continuously increasing
P
CO2 (P < 0.001), C
CO2 decreased at Max (P < 0.05, Max vs. LAT) due to the marked decrease in
pH
(P < 0.001, Max vs. LAT).
Simultaneously, on the arterial blood side,
CaCO2 increased insignificantly at work rates
below LAT (P > 0.05), whereas PaCO2
increased (P < 0.05) and pHa decreased
slightly (P < 0.05). Above LAT,
CaCO2 and [HCO
] decreased
when lactic acid production increased, causing a significant decrease
in pHa (P < 0.001) with only slight
decreases in PaCO2 (Fig. 2).
As shown in Fig. 2B, the pattern of changes in plasma
[HCO
] was quite similar to the changes in CCO2 as a function of
PCO2. This similarity reflects the dominant role of changes in pH and buffer base on the
PCO2-CCO2 relationship. It is clear from Figs. 1 and 2 that an increase in
PCO2 in venous blood does not necessarily
predict an increase in HCO
and therefore
CCO2. Thus there is no single
PCO2-CCO2 relationship that can be used to predict CCO2 from
PCO2 during exercise.
Errors in Def CCO2 and
COCO2 During Exercise
Table 2 shows the absolute values and percent errors of Def-pH
CCO2 from actual CCO2
values. Errors in C
CO2,
CaCO2, and C
CO2-CaCO2
increased consistently from actual values as exercise intensity
increased, because changes in pH were not accounted for during exercise
(P < 0.05 below LAT; P < 0.01 above
LAT). Although errors in C
CO2 and
CaCO2 were directionally the same, the absolute
and percent errors of Def-pH C
CO2 were
always larger than those of Def-pH CaCO2
(P < 0.001 by paired t-test), resulting in
consistent overestimation of Def-pH
C
CO2-CaCO2.
Although absolute errors of Def-pH
C
CO2-CaCO2 were
always smaller than either those of Def-pH
C
CO2 or Def-pH
CaCO2 (Table 2), the percent difference of
Def-pH
C
CO2-CaCO2 was
always larger than those of Def-pH C
CO2
or Def-pH CaCO2 (Table 2; P < 0.001 by paired t-test). The overestimation of
CaCO2, C
CO2, and
C
CO2-CaCO2 that
results from failure to use pH in the calculation of
CCO2 ranged from
0.2 to 27, 2 to 60, and 18 to 120%, respectively, even when correct, directly measured arterial
and mixed venous PCO2, Hb, and
SO2 are used in the calculation.
Figure 3 shows the percent errors of
specific Def values of
C
CO2-CaCO2,
despite the use of correct measurements of
PCO2, when no change during exercise is assumed
in Hb, SO2, and/or pH. Defaulting changes in Hb
during exercise results in trivial error (only
0.2 to 0.6%).
Defaulting the change in SO2 results in slight underestimation in
C
CO2-CaCO2 over
the entire exercise period (
6 to
3%; P < 0.05).
In contrast, defaulting changes in either pH alone or pH, Hb, and
SO2 together cause large errors, i.e., a
progressive overestimation in
C
CO2-CaCO2 as
exercise intensity increases, reaching ~50% at LAT and 100% at Max.

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Fig. 3.
Errors in
C CO2-CaCO2
during exercise caused by ignoring changes in pH, Hb, and/or
SO2 from resting values. Horizontal dotted
line, actual value at each point calculated from measured mixed venous
and arterial PCO2, pH, Hb, and
SO2 at rest and during exercise, normalized to
0. Values are means ± SE. Each symbol indicates percent errors of
C CO2-CaCO2 from
the actual values caused by ignoring exercise-induced changes from rest
in pH, Hb, and/or SO2 in mixed venous and
arterial blood, despite correct values for P CO2
and PaCO2. Ignoring changes in pH or all 3 variables
from rest causes overestimation of
C CO2-CaCO2
exceeding 100% at Max. Ignoring changes in SO2
from rest causes underestimation of
C CO2-CaCO2 by
3-6%. Ignoring changes in values of Hb causes trivial
underestimation of
C CO2-CaCO2.
O2/ O2@LAT,
ratio of O2 to
O2@LAT.
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As seen in Fig. 4, the percent errors in
COCO2 that result from defaulting the influence
of Hb, SO2, and/or pH on the
PCO2-CCO2 relationship
are always opposite to those on
C
CO2-CaCO2. As with its effect on
C
CO2-CaCO2, the
change in Hb causes a trivial effect on COCO2
(only
0.6 to 0.2%), whereas the changes in
SO2 cause the estimate of
COCO2 to be 3-6% higher than actual
(P < 0.05). In contrast, defaulting on either pH alone
or pH, Hb, and SO2 together causes errors in
COCO2 by >30% at LAT and >50% at Max.

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Fig. 4.
Errors in cardiac output using CO2
(COCO2) during exercise caused by ignoring
changes in pH, Hb, and/or SO2 from resting
values. Horizontal dotted line, actual value calculated from measured
mixed venous and arterial PCO2, pH, Hb, and
SO2 at rest and during exercise and
CO2 production, normalized to 0. Values are means ± SE. Each symbol indicates percent errors of
COCO2 from the actual values caused by ignoring
exercise-induced changes in pH, Hb, and/or SO2
in mixed venous and arterial blood, despite correct values for
P CO2 and PaCO2. Ignoring
changes in all 3 variables or pH alone from rest causes underestimation
of COCO2 exceeding 50% at Max. Ignoring
changes in SO2 from rest causes overestimation
of COCO2 by 3-6%. Ignoring changes in Hb
from rest causes trivial overestimation of
COCO2.
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Relative importance of multiple factors on the
PCO2-CCO2 relationship
during exercise.
The influence of each of several factors on the
PCO2-CCO2 relationship
is shown in Table 3, with factor
influence increasing as its value deviates from 1.0. Thus the
deviations during exercise of Fbic (which are due to pH
changes) far exceed those of FHb, both in mixed venous and
arterial blood, during exercise (Table 3). Considering the subfactors
of FHb, the deviations during exercise of
FHbpH (due to the
effect of pH changes on [NH-CO2]) exceed those of
FHbSO2
and FHbHb, both in mixed venous and arterial
blood. Thus the changes and influence of pH (Fbic and
FHbpH) are quantitatively much more important
in blood CO2 transport during exercise, both in mixed
venous and arterial blood, than are the changes and influences of
change in Hb and SO2. These findings contrast
importantly with the conclusions of McHardy (34).
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Table 3.
Factors describing the magnitude by which Hb,
SO2, or pH changes affect the
PCO2-CCO2 relationship
during exercise
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Changes in Blood Components of
CCO2 During Exercise
The total CCO2 and each of its fractional
components in mixed venous and arterial blood and the mixed
venoarterial differences at rest and during exercise are shown in Fig.
5 and Table
4. These data were
calculated from the equations described in APPENDIX B. Both C
CO2 and
CaCO2 correlated well with the same variables
calculated from the Douglas equation (r = 0.9998, P < 0.0001), with only very small deviations
(
0.06 ± 0.14 mM) at rest and during exercise.

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Fig. 5.
Changes in CCO2 at 5 levels of
exercise (rest, mild, moderate, heavy, and very heavy). In each group
of 3 bars, left bar shows the total mixed venous ( )
CCO2, middle bar is arterial (a)
CCO2, and right bar is mixed
venous-arterial ( -a) CCO2 difference.
Each bar is divided into the [HCO ], carbamino
concentration ([NH-CO2]), and physically dissolved
CO2 concentration ([CO2]) components for
whole blood. During exercise, changes in [CO2]
(PCO2 dependent) and [NH-CO2]
(PCO2, pH, Hb, and SO2
dependent) fractions are dwarfed by the changes in
[HCO ] (both PCO2 and pH
dependent). Ex-2 and Ex-7, 2 and 7 min of incremental exercise,
respectively.
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In Fig. 5, both mixed venous [CO2] and
[NH-CO2] increased progressively from rest to Max
(P < 0.05). Smaller percent but larger absolute
changes in [HCO
] dwarfed the impact of the larger
percent but smaller absolute changes in mixed venous
[CO2] and [NH-CO2]. Below LAT, trends in
change in C
CO2 were similar to those in
[CO2] or [NH-CO2], but they differed
markedly above LAT. The arterial [CO2] and
[NH-CO2] increased only slightly from rest at LAT
(P < 0.05) and then returned to near resting values at
the highest work rate. In contrast to the relatively stable arterial
[CO2] and [NH-CO2], large declines in
arterial [HCO
] above the LAT caused marked
decreases in CaCO2. Thus changes in
C
CO2 and CaCO2
conformed mainly to changes in [HCO
] with
changes in [CO2] and [NH-CO2] having a
relatively small effect.
Referring to Table 4 (selected exercise intensities), ratios of
CCO2 to [CO2]
(CCO2/[CO2]) were calculated by
dividing the CCO2 by the sum of plasma and red
blood cell components of [CO2]. Note that the
CCO2/[CO2] for mixed
venous blood progressively decreased as the exercise intensity
increased (P < 0.05), especially above LAT
(P < 0.01). The
CCO2/[CO2] in arterial blood,
which did not change significantly below LAT (P > 0.05), progressively decreased at and above LAT (P < 0.05), because of the reduction in [HCO
]. Thus
CCO2/[CO2] is not constant but
depends on the source of blood and the intensity of exercise.
It is also evident from Table 4 and Fig. 5 that plasma and red
blood cell [HCO
] together comprise ~85% (mixed
venous) and 90% (arterial) of the CCO2 at rest
and during exercise. Even though the absolute values of mixed venous [HCO
] are always greater than those of the
arterial [HCO
], the mixed venous [HCO
]/CCO2 are always
lower than the arterial
[HCO
]/CCO2
(P < 0.001) because of the greater amount of
[CO2].
Relative contributions of the three forms of
CO2-to-CO2 exchange are shown for each level of
exercise in Table 5. From rest to Max,
[HCO
] exchange remained large and quite constant
at ~76-77% of total CO2 excreted, i.e.,
C
CO2-CaCO2. In
contrast, [CO2] and [NH-CO2] accounted
for ~9 and 14%, respectively, of total CO2 excreted at
rest. Above LAT, the relative contribution to CO2 output of
[CO2] progressively increased to 13% (P < 0.05) and that of [NH-CO2] decreased to ~10%
(P < 0.01).
Finally, to support the validity of our calculated values for
CaCO2, C
CO2, and
C
CO2-CaCO2 at
all levels of exercise, we compared the COCO2
measured by the Fick principle with COO2 at rest and each level of exercise for the five subjects in this study
(Table 6). At each level but Max, the
mean values are in good agreement. As noted in Table 6, in other quite
similar exercise studies (51), the
COCO2 was insignificantly different from
COO2 at peak and all other levels of exercise.
 |
DISCUSSION |
Major Findings
This study discloses several important findings. 1)
During exercise, CCO2 and
[HCO
] do not consistently increase in proportion
to PCO2. 2) Because of the acidemia
caused by increased lactate production,
C
CO2 and mixed venous
[HCO
] decrease to near resting values as maximal
O2 is approached, despite increasing
P
CO2. 3) Above LAT, while
P
CO2 increases to high levels,
PaCO2 decreases because of ventilatory compensation for the exercise lactic acidosis; consequently,
CaCO2 decreases to a greater degree than does
C
CO2. 4) The increase in
C
CO2-CaCO2 during exercise is mainly due to the increase in
C
CO2 below LAT and the decrease in
CaCO2 above LAT. 5) Changes in
SO2 and Hb have minor influences on the
PCO2-CCO2 relationship
during exercise, whereas changes in pH due to changes in buffer base have a major influence. 6) Because pH
decreases more than pHa, there are large errors in
calculated C
CO2-CaCO2 when
the pH change is ignored. 7) At rest and during all levels
of exercise, over threefourths of the total CO2
exchange from the blood to lung gas (i.e.,
C
CO2-CaCO2) is
due to dissociation of [HCO
], whereas less than
one-fourth is due to the combination of venoarterial differences in
[CO2] and [NH-CO2] at rest to Max.
The Dominant Role of pH in the
PCO2-CCO2 Relationship
During Exercise
As evidenced by
CO2 measurements
during exercise, the lung progressively increases the excretion of
CO2 as work rate increases. Because cardiac output
increases much less than
CO2, the
difference between C
CO2 and
CaCO2 necessarily widens. Figures 1 and 2
depict the progressive increase in the differences among
C
CO2, CaCO2, [HCO
], PCO2, and pH as
work rate increases. The metabolic acidosis found in our
subjects during high-intensity exercise causes plasma and red blood
cell CCO2 and [HCO
] to
decrease in both mixed venous and arterial blood, but especially in
arterial blood.
As commonly graphed, the
PCO2-CCO2 relationship
is depicted as nearly linear between PCO2
values of ~30-80 Torr and CCO2 values of
~12-28 mM but without reference to or depiction of the effect of
a pH change (8, 38, 56). Changes in
CCO2 are sometimes fractionated into plasma and
red blood cell components, and the differences between mixed venous and
arterial blood due to Hb and SO2 are also
considered, again with exclusion of the effect of pH (8, 38,
56). However, as seen in Figs. 1 and 2A and Tables 1
and 2, widely divergent P
CO2 values (47-78
Torr) may occur with reasonably similar
C
CO2 values (22.8-23.9 mM). This is
due to relatively large decreases in the buffer base reflected in the
change in pH
(7.362-7.130) (Table 1 and Fig.
1). Furthermore, reasonably similar PaCO2 values (41-38 Torr) may pair with widely different
CaCO2 values (20.9-15.2 mM) because of
relatively large differences in pH. Thus when the C
CO2 is calculated from
P
CO2, the change in blood pH
during exercise must not be ignored. During heavy exercise,
CCO2 is not linearly related to the
PCO2 in either arterial or mixed venous blood
(see Fig. 2A). In fact, PCO2 and
CCO2 change in opposite directions in mixed
venous blood as metabolic acid is added to the blood by the muscles. In
contrast to original reports and textbooks (8, 38, 56),
Fig. 2 shows that C
CO2 does not increase
as a function of P
CO2 during exercise above the LAT.
We suggest that the addition of pH (or [H+])
isopleths to diagrams depicting the plasma
[HCO
]-PCO2 and
CCO2-PCO2
relationships, such as shown in Fig. 2, conveys necessary and important
information that is lacking in the present standard depictions of these
relationships (8, 38, 56). Such isopleths clarify and
reinforce the importance of the acid-base changes that can occur during exercise.
Total blood [HCO
] comprises ~85% (mixed venous)
or 90% (arterial) of the CCO2 (Table 4).
Although the percent changes in mixed venous [CO2] and
[NH-CO2] are appreciable (Tables 4 and 5 and Fig. 5),
their impact is dwarfed by the magnitude of the large absolute changes
in [HCO
]. Additionally, Tables 2 and 3 and Fig. 3,
which give Def values and factor ratios, analyze the relative
importance of the components of CCO2 in the
Douglas equation and confirm the dominance of pH factors. In Table 3
and Fig. 3, it is shown that the pH change factor (Fbic
from 1.00 at rest to 0.59 at Max) dominates over other factors. Within
the red blood cell, the pH factor even dominates over the change in Hb
concentration and SO2 factors (Table 3). Thus
making adjustments for the influences of Hb and
SO2 while ignoring pH to calculate
C
CO2 or CaCO2
during exercise, as was done earlier (34), results in
major errors.
Relevance of the
CCO2-PCO2
Relationship to the Accuracy and Precision of Estimation of
C
CO2-CaCO2 and
COCO2
Our calculations of CCO2 come from direct
measurements of mixed venous and arterial PCO2,
pH, Hb, and SO2. As previously shown, the
relationship between PCO2 and
CCO2 is positively correlated between rest and
LAT but then becomes negatively correlated as increasing metabolic
acidosis develops. Thus a given PCO2 value can
be associated with widely divergent CCO2 values.
It would be convenient if errors in measurement of
C
CO2 and CaCO2
were to be offset in the calculation of
C
CO2-CaCO2, but
this is not the case. It is evident from Table 2 that omitting the
change in pH in calculating
C
CO2-CaCO2
causes a much larger error than when
C
CO2 and CaCO2
are calculated individually. Figure 4 shows that, when these erroneous
measurements are applied to calculate cardiac output, errors of large
magnitude result. In contrast, ignoring the changes in [Hb] and
SO2 during exercise results in relatively
unimportant errors compared with ignoring changes in pH.
Possible Measurement and Calculation Errors in Our Data
The gas exchange, rate of increase in
O2 as related to work rate increase, and
mixed venous and arterial blood values are unlikely to be significantly
inaccurate or imprecise in this study, considering the similarity of
these values to those of other studies in normal men and the quality
control procedures used in our laboratory (3, 4, 21, 24, 25,
46-55). A limitation of this study is the absence of direct
measurements of CaCO2 and
C
CO2. Because all methods for such
measurements require a minimum of 30 min for each blood sample, it was
unrealistic to obtain the many measurements needed on so many samples
(~24-28) for each study. However, the similar values obtained
for COO2 and COCO2 at
rest and all levels of exercise (Table 6) give credence to the
reliability of the concurrent measurements of pH and
PCO2 and calculated mixed venous and arterial
concentrations of CO2 and O2 at all levels of exercise.
We did not measure blood or body temperatures during exercise. From
other studies using a similar exercise protocol, we estimated that the
temperature increase from rest to peak exercise would be
0.2-0.8°C (51). We calculated that a temperature
rise of 0.5°C during exercise would affect the values of
CaCO2, C
CO2, and
C
CO2-CaCO2 by
<1% at peak exercise (51). Therefore, this small
temperature change would not significantly alter our findings.
Considering the diversity of sources and complexity of equations in
APPENDIX B that were used to calculate the six components
of CCO2, the sum values for each blood sample
from the six sources agree remarkably well with those calculated from the simpler Douglas equation. The CCO2 values
calculated from the Douglas equation have excellent linear correlation
with the total sum values at all levels of CCO2
for both arterial and mixed venous blood (r = 0.9998, Table 4).
Possible Errors Due to a Disequilibria of pH and CO2
There is no evidence that an alveolar-arterial CO2
disequilibrium occurs, except under conditions of high levels of
carbonic anhydrase inhibition. The latter is a model of CO2
disequilibrium. In contrast, there are good arguments using
physiological data against disequilibrium for CO2 at high
work rates as follows.
1) End-tidal PCO2
(PETCO2) exceeds PaCO2
during exercise with a maintained negative
PaCO2-PETCO2 differnce of
~4 Torr, despite the increase in
CO2
to very high levels (54). If there were a disequilibrium,
PaCO2-PETCO2 difference
and PaCO2 should increase relative to
PETCO2 as
CO2 increases. However, the change in PETCO2 parallels the change in
PaCO2 as
CO2 increases
to maximum and remains above it (54).
2) If there were a disequilibrium, calculated dead space
volume/tidal volume should increase as work rate increases, because PaCO2 would be increased relative to
PETCO2. This happens when a right-to-left
shunt opens during exercise but does not happen normally. Dead space
volume/tidal volume decreases with exercise and remains decreased to
similar levels or decreases further as work rate increases to the
maximum in normal subjects.
3) If there were a disequilibrium,
CO2 would not increase appropriately as
high-metabolic rates are achieved and PaCO2 would increase. Increasing
CO2 keeps pace with
increasing
O2 even for very fit men and
exceeds
O2 once lactic acidos