Vol. 87, Issue 2, 862-866, August 1999
SPECIAL COMMUNICATION
Quantitative assessment of changes in blood
CO2 tension mediated by the
Haldane effect
Ivo
Giovannini1,2,
Carlo
Chiarla2,
Giuseppe
Boldrini1,2, and
Renato
Terzi3
1 Department of Surgery
(Geriatric Surgery) and
2 Consiglio Nazionale delle
Ricerche Center for the Study of Pathophysiology of Shock, Catholic
University School of Medicine, I-00168 Rome, Italy; and
3 Intensive Care Unit, Hospital
das Clinicas, University of Campinas School of Medicine, 13100 Campinas, SP, Brazil
 |
ABSTRACT |
Adequate assessment of circulatory and
gas-exchange interactions may involve the quantification of the Haldane
effect (HE) and of the changes in blood
PCO2 mediated by changes in
Hb-O2 saturation and
O2-linked
CO2 binding. This is
commonly prevented by the complexity of the involved calculations. To
simplify the task, a large series of patient measurements has been
processed by regression analysis, thus developing an accurate fit for
this quantification
(n = 247, r2 = 0.99, P
0.001), where
(v-a)PCO2 HE
is the reduction in venous PCO2
(PvCO2, Torr) allowed by the chemical
binding of CO2 in blood due to the
HE (Torr), (a-v)HbO2 is the
arteriovenous difference in Hb-bound
O2 (ml/dl), and Hct is hematocrit
fraction. Values of
(v-a)PCO2 HE
estimated by this expression compared well with the results of
previously published experiments. This formula is useful in assessing
the impact of HE on PvCO2 and
venoarterial PCO2 gradient and the
survival advantage offered by HE in extreme conditions. Use may be
extended to all investigative and clinical settings in which changes in blood O2 saturation and
O2-linked
CO2 binding must be converted into
the corresponding changes in dissolved
CO2 and
PCO2.
carbon dioxide exchange; circulatory failure; respiratory failure; shock; venous hypercapnia; sepsis
 |
INTRODUCTION |
THE HALDANE EFFECT (HE) is a physicochemical phenomenon
involving an increase in blood
CO2-combining capacity, with
opposite changes in dissolved CO2
and PCO2, as a consequence of oxyhemoglobin (HbO2)
desaturation (3). Although HE is an important component of circulatory
and gas-exchange interactions, especially in circulatory and
respiratory failure, its relevance is not commonly emphasized. This is
due to a lack of easily available methods for its quantification, which
involves complex mathematical procedures and models. In particular, an
unsolved problem in physiological studies and in clinical monitoring is
the inability to convert easily changes in blood
O2 saturation and
O2-linked
CO2 binding into the corresponding
changes in dissolved CO2 and
PCO2. This paper describes the
results of a study performed on a large series of patient measurements
to develop a new computational method for this purpose and to quantify
the impact of HE on venous PCO2
(PvCO2, Torr) and venoarterial
PCO2 difference [(v-a)PCO2, Torr].
 |
METHODS |
Measurements (247) performed in 91 patients were processed. Patients
were 53 ± 18 (SD) yr of age, with a body weight of 64.3 ± 12.8 kg, and a body surface area of 1.72 ± 0.19 m2. There were 73 patients with
intra-abdominal sepsis, 11 had retroperitoneal abscesses, 6 had
cholangitis, and 1 had gangrenous fasciitis; 39 patients survived and
52 died of respiratory or multiple organ failure, myocardial depression
or infarction, or pulmonary embolism. Sepsis severity score (5) ranged
from <10 to >20, with a normal Gaussian distribution and a mean ± SD of 15.8 ± 4.0. This patient population provided a
continuous distribution of observations, from relatively compensated to
extremely diseased states with shock, which allowed for a detailed
quantification of the magnitude of HE over a wide spectrum of
cardiorespiratory and metabolic abnormalities (Table 1).
The measurements, all performed for clinical purposes and in accordance
with institutional guidelines, were based on the simultaneous analysis
of arterial and mixed-venous blood gases. From these, arteriovenous
difference in Hb-bound O2
[(a-v)HbO2, ml/dl
blood] was calculated from
O2 saturation difference and Hb
concentration, with Hufner's coefficient of 1.36 ml
O2/g Hb. The venoarterial CO2 concentration difference
[(v-a)CO2, ml
CO2/dl blood] was determined by a model combining the Peters-Van Slyke equation for the buffer line
of plasma from arterial blood with the Henderson-Hasselbalch equation
for venous plasma (9), thus calculating the following quantities on the
CO2 equilibration curve for
arterial blood: 1) the increment in
CO2 concentration
(CCO2)
related to the (v-a)PCO2 increment
at constant O2 saturation by an
iteration related to the Newton-Raphson procedure;
2) the further increase in
CCO2 at
constant PCO2 mediated by
HbO2 desaturation and
O2-linked CO2 binding
[(v-a)CO2 due to HE,
(v-a)CO2 HE, ml
CO2/dl blood] by a complex
fit to the experimental data obtained at 37°C by Klocke (15);
3) the increase in
PvCO2 avoided by the
O2-linked CO2 binding [reduction in
(v-a)PCO2 due to HE,
(v-a)PCO2 HE, Torr] by continuation of the iteration stepwise to find the
increase in PCO2 above
PvCO2 necessary to obtain an increase in CCO2 equal
to
(v-a)CO2 HE.
Data processing was based on regression analysis, with analysis of
residuals, skewness and kurtosis control, and a "simplest best
fit" procedure that allowed selection of the simplest possible regression yielding the best control of variability of the dependent variable, based on Mallows' Cp criteria (22). Reliability
of a nonlinear regression developed to estimate
(v-a)PCO2 HE
was verified by a comparison with experimental values of
(v-a)PCO2 HE [(v-a)PCO2 exp,
Torr] obtainable from previously published studies. These
included the tonometric data reported by Henderson (11) for the
experiments of Christiansen et al. (3), the data of Joffe and Poulton
(13) for the blood of J. J. and W. R., and also the
data of Luft et al. (18) for the HE-mediated change in arterial
PCO2
(PaCO2) from increased
O2 breathing. The
latter effect is equivalent, in terms of HE-induced changes in
PCO2, to that observed by changing
O2 saturation in venous blood (if
linearity of HE at different HbO2
saturations is assumed) (16). Because in tonometric experiments the
CCO2 values
in reduced and oxygenated blood
(CrCO2 and
CoCO2,
respectively, ml/dl) were not the same, an unbiased and verifiable
comparison was carried out as follows. Third-degree polynomials
[y = f (x3,
x2,
x)] were fitted pragmatically
to the data for oxygenated blood (r2 > 0.99 for
each fit). Then, for any point measurement reported for reduced blood,
(v-a)PCO2 exp
was determined as the difference between the
PCO2 yielded by the polynomial at a
CCO2 equal
to CrCO2 and
the PCO2 measured in reduced blood (without extrapolations outside the range of published experiments and
of PCO2 values reported in Table 1).
This corresponded to the determination of the horizontal distance
between the equilibration curves for oxygenated and reduced blood for
any given measured CrCO2. The
obtained
(v-a)PCO2 exp
values were then compared with the values of
(v-a)PCO2 HE estimated by our nonlinear
regression on the basis of the
(a-v)HbO2,
PCO2, and Hct values reported in the
experiments. For the data in Ref. 18, a mean Hct of 0.47 was used for all cases, and case 8 was
dropped because of inexplicably large
O2-linked
PCO2 changes. A total of 34 (v-a)PCO2 exp values, available for comparison from these sources, was pooled together and processed.
 |
RESULTS |
The (v-a)PCO2 gradient was 5.70 ± 2.70 (SD) Torr, (v-a)CO2 was 3.71 ± 1.45 ml/dl, (a-v)HbO2 was
3.93 ± 1.46 ml/dl, (v-a)CO2 HE was 1.06 ± 0.41 ml/dl, and
(v-a)PCO2 HE
was 2.46 ± 0.99 Torr. Linear and nonlinear regression analyses were
performed extensively on blood gas and derived variables to assess the
correlates of
(v-a)PCO2 HE
and to select the best simultaneous correlation by Mallows' Cp
criteria (22). This was provided by the
(PvCO2) following
fit
|
(1)
|
where
r2 = 0.99, P
0.001 for whole regression and
each independent variable; partial
r2 for
(a-v)HbO2 = 0.77 and for
(a-v)HbO2 + PvCO2 = 0.97.
A graphical display of the fit, with source measurements,
is reported in Fig. 1. The analysis
showed further that the very good correlation with
(a-v)HbO2 reflected the relevance
of HbO2 desaturation as a
determinant of HE, and that the simultaneous nonlinear correlation with
PvCO2 and Hct was mediated by the impact of these variables on the slope of the
CO2 equilibration curve. Unexpectedly, there was a lack of simultaneous correlation with pH.
This was because part of the variability of
(v-a)PCO2 HE
related to pH was already accounted for by
PvCO2. Besides, the impact of pH on the
CO2-combining capacity of blood
related to HE was balanced by a simultaneous impact on that unrelated
to HE [because (v-a)PCO2 HE
is the horizontal distance between the equilibration curves for
arterial and venous blood, changes in this distance expected from
pH-mediated changes in magnitude of HE were balanced by pH-mediated
changes in the slope of the curves]. This explanation was
validated by use of our model within the range of distribution of our
measurements; outside this range, in particular at very low pH,
accuracy of the estimated
(v-a)PCO2 HE
is likely to decrease. Reliability of the developed fit was supported
by a high r2 = 0.99 and a SE of estimate = 0.07 Torr, thus implicating comprehension of estimated
(v-a)PCO2 HE
within ±0.14 Torr of the real value in 95% of cases. This was
validated further by showing that actual and estimated values of
(v-a)PCO2 HE
correlated linearly, with slope and intercept not significantly
different from 1.0 and 0.0, respectively
(P > 0.05 for both) and with a
perfectly balanced distribution of residuals over the whole range of
distribution (Fig. 2). It was verified also
that Eq. 1 could be simplified further
by eliminating the exponent of
(a-v)HbO2, as this involved only a
slight overestimation of
(v-a)PCO2 HE,
which never exceeded 0.25%. Comparison with the results of published
experiments showed that the estimated
(v-a)PCO2 HE
was in good agreement with
(v-a)PCO2 exp (7.12 ± 4.16 vs. 7.50 ± 4.65 Torr,
n = 34, P > 0.05). Regression analysis also
showed a good correlation between
(v-a)PCO2 exp and
(v-a)PCO2 HE:
(v-a)PCO2 exp = 1.04[(v-a)PCO2 HE] + 0.16, r2 = 0.87, P < 0.01, with slope and
intercept not significantly different from 1.0 and 0.0, respectively.
This was a satisfactory achievement, given the nature of the comparison
(already involving by itself some uncontrolled variability) and the
magnification of this variability expected from estimating large
(v-a)PCO2 exp values (7.50 ± 4.65 Torr) by a method developed from measurements with smaller
(v-a)PCO2 HE
(2.46 ± 0.99 Torr).

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Fig. 1.
Display of relationship among reduction in venoarterial
PCO2 difference due to Haldane effect
[(v-a)PCO2 HE],
venous PCO2
(PvCO2), arteriovenous difference in
Hb-bound O2
[(a-v)HbO2], and
hematocrit fraction (Hct). Isolines for
(a-v)HbO2 were obtained by
Eq. 1 at different Hct values. Because
(a-v)HbO2 corresponds to
O2 consumption/blood flow,
isolines also quantify impact of any combination of
changes in O2 consumption and
cardiac output on
(v-a)PCO2 HE.
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Fig. 2.
Correlation between actual values of
(v-a)PCO2 HE
and values estimated by Eq. 1, with
identity line.
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|
 |
DISCUSSION |
There are several implications of the assessment of HE performed in our
study. The availability of Eq. 1 is
important in estimating rapidly and accurately the magnitude of
(v-a)PCO2 HE
in physiological and clinical studies without resorting to complex
mathematical procedures or models. This is also useful in assessing and
monitoring cardiocirculatory and gas-exchange interactions. For
instance, increases in (v-a)PCO2 in
critical illness are associated with increasing severity of illness and
poor prognosis, because these reflect decreases in cardiac output and
circulatory failure (with larger
CO2 loading per unit blood flow)
and metabolic acidosis (with reduced blood
CO2 binding and larger increases
in PCO2 for any given
CO2 loading) (1). An additional
and unrecognized cause of increases in
(v-a)PCO2, and thus in
PvCO2 for any given
PaCO2, is the reduction of
(v-a)PCO2 HE.
Indeed,
(v-a)PCO2 HE is the buffering that is exerted constantly by HE on
(v-a)PCO2 for any given
(v-a)CO2. In sepsis with impaired
O2 extraction and reduction of
(a-v)HbO2, loss of this buffering
may become an important determinant of the venous hypercapnia and
acidosis that characterize this stage of the disease (7, 8, 23). In
fact, maximum increases in (v-a)PCO2
and PvCO2 were observed in our septic
patients with circulatory failure when they developed overimposed
metabolic failure with impaired O2 extraction and thus a reduction of
(v-a)PCO2 HE.
With the exception of extreme cases, however, the buffering of pH from
O2-linked H+ binding has a greater general
relevance than the buffering of PCO2
(for instance, small changes in ventilation may affect
PaCO2 and
PvCO2 to a much greater extent than the
HE). Quantifiable evidence of the
O2-linked
H+ binding was provided by us in a
previous study (8). This is obviously related to the
O2-linked
CO2 binding that has been
addressed in this study; however, the two effects are not
quantitatively equivalent, and their relationship has not yet been
adequately assessed (16).
Use of Eq. 1 may be extended
advantageously to many investigative and clinical settings in which
changes in blood O2 saturation and
O2-linked
CO2 binding must be converted into
the corresponding changes of dissolved
CO2 and
PCO2. As mentioned already, (v-a)PCO2 HE
is the horizontal distance between the equilibration curves for
arterial and venous blood. Determination of this quantity may be needed
for several purposes, including, for instance, assessment of the
increase in PaCO2 caused by the HE when
inspired O2 concentration is
increased. Complex procedures are usually required for this purpose,
whereas Eq. 1 may provide this
quantity more simply. In fact, by substituting the increase in arterial
HbO2 due to O2 breathing into
(a-v)HbO2 HE and the basal
PaCO2 into
PvCO2, Eq. 1 will calculate this quantity instead of
(v-a)PCO2 HE.
Similarly, Eq. 1 may be applied to
assess changes in PaCO2 during apneic oxygenation, rebreathing, and breath holding and in the simulation of
blood CO2 exchange under a variety
of conditions. In effect, the reliability of Eq. 1 was also supported by using published results on
Haldane-mediated changes in PaCO2 when
the inspired O2 concentration is
increased (18). Although many other published experiments do not
contain sufficient data for strict and direct comparisons, it may be
easily verified that the impact of HE on blood
PCO2 values, as quantified in those
experiments, is in good agreement with that estimated by
Eq. 1. An example is provided by the
tonometric results in Ref. 14, although some elaboration is needed for
the comparison. This may involve calculation of
CoCO2 and
CrCO2 from the
measured pH, PCO2, and Hct by using
any general expression, including ours in Ref. 9, of the form
CCO2 = a · PCO2 · 10pH
pK'[1
Hct(1
r)]. Then the
data of Peters and Van Slyke (21) for
dCCO2/dpH
may allow estimation of the pH value at which
CoCO2 equals
CrCO2 and of
the corresponding PCO2 in oxygenated blood. The difference with the original
PCO2 in reduced blood may finally be
compared with the
(v-a)PCO2 HE
obtained by Eq. 1, thus showing good
agreement (Fig. 3). Another example is provided by the
experimental results on dilutional anemia in Ref. 4. The comparison is
possible, for instance, by calculating values of arterial
CCO2 and
(v-a)CO2 by the procedure used
previously. Then, the data of Peters et al. (20) may allow conversion
of (v-a)CO2 into the
(v-a)PCO2 and
PvCO2, which should be expected in
the absence of HE. The difference with the actual PvCO2 may finally be compared with the
(v-a)PCO2 HE
obtained by Eq. 1, thus showing again
satisfactory agreement. Easier comparisons may be made with the data in
Refs. 2, 12, 17, and 19, all showing agreement with the
Haldane-mediated changes in PCO2 estimated by Eq. 1 (Fig. 3).

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Fig. 3.
Comparison between
(v-a)PCO2 HE
obtained from studies with incomplete data (see text for elaborations
and assumptions) and values estimated by Eq. 1 from basic data in same studies, with identity line.
Large , extreme data points (PCO2
~28.5 and 57.0 Torr, respectively) for determinations by Kalhoff et
al. (14) in fully oxygenated and reduced adult human blood. , Data
points from mean values of Deem et al. (4) for 8 sets of measurements
on dilutional anemia in rabbits (Hb from 11.6 to 3.9 g/dl). , Data
point from relationship of Hoffmann et al. (12) in extracorporeal
CO2 exchange, for
(a-v)HbO2 = 4.0 ml/dl and
PCO2 = 65 Torr. Small , mean
(v-a)PCO2 HE
for measurements by Brandt et al. (2) in apneic oxygenation. , Mean
(v-a)PCO2 HE
for similar measurements by Merkelbach et al. (19). , Extreme data
points (PCO2 = 20 and 70 Torr,
respectively) from Lenfant nomogram (17) for Hb = 16.0 g/dl and change
in HbO2 saturation = 100%.
Adequacy of fit may vary slightly by varying assumptions and
approximations in the elaborations. It varies more for the point from
Ref. 12 with increasing (a-v)HbO2
or decreasing PCO2, due likely to the
peculiar setting (extracorporeal support in respiratory insufficiency)
and to report of a simplified linear relationship for
(v-a)PCO2 HE
in the study.
|
|
Finally, as an additional implication, it should be mentioned that our
formula for
(v-a)PCO2 HE
is useful in quantifying exactly the survival advantage offered by the
HE in extreme conditions (i.e., circulatory shock, severe hypercapnia,
anemia) by protecting against excessive rises in
(v-a)PCO2 and thus in
PvCO2 and tissue
PCO2. This is an important phenomenon
in organs with high O2 uptake and
CO2 release per unit blood flow,
such as the heart and the brain (10). Maximum
(v-a)PCO2 HE
in our results was close to 7.0 Torr and was 12.0 Torr in an additional case not included in the study. Although our study does not permit reliable extrapolations much above a
PvCO2 of 70 Torr, a more relevant
protection against tissue hypercapnia should be expected above such
level. This is supported by the evidence that HE remains operative at
high PvCO2 (allowing increasingly larger
reductions in PCO2) (3, 13, 24) and
is also consistent with the values of
(v-a)PCO2 HE
predictable by Eq. 1. More work is needed to verify this specific aspect in additional studies to improve
understanding of the mechanisms of survival in extreme conditions.
 |
FOOTNOTES |
The costs of publication of this
article were defrayed in part by the
payment of page charges. The article
must therefore be hereby marked
"advertisement"
in accordance with 18 U.S.C. §1734 solely to indicate this fact.
Address for reprint requests and other correspondence: I. Giovannini,
Via Alessandro VII, 45, I-00167 Rome, Italy.
Received 9 April 1998; accepted in final form 31 March 1999.
 |
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