|
|
||||||||
1Department of Anesthesiology and 3Department of Physiology, Academic Medical Centre, University of Amsterdam, Amsterdam, The Netherlands; and 2Nepal International Clinic, Kathmandu, Nepal
Submitted 16 December 2006 ; accepted in final form 24 April 2007
| ABSTRACT |
|---|
|
|
|---|
cerebral circulation; hypoxia
60 ml blood·100 g brain tissue–1·min–1 is delivered. Loss of cerebral autoregulation (CA) is thought to be rare, and most often reported in severe brain pathology, such as in ischemic stroke (31), traumatic brain injury (6), after cardiac arrest (36), and in malignant hypertension (16). In these patients, cerebral blood flow (CBF) fluctuates parallel with arterial blood pressure, implicating that a decrease in blood pressure can jeopardize cerebral perfusion, whereas an increase in blood pressure may cause cerebral edema.
Impaired CA has also been reported in healthy lowland subjects when they are exposed to high altitudes. Measurements in mountain climbers entering 5,500 m (22) or 4,243 m (17) revealed that middle cerebral artery (MCA) blood flow velocity (
mca) changes along with blood pressure. In addition, in newcomers at 3,900 m, CA is reduced during sleep but not during wakefulness (2). Also in Sherpas in Nepal who reside permanently above 4,000 m and who are known for their superior exercise capacity under extreme hypoxia, CA is impaired (17).
The observation that in newcomers to high altitude and in permanent high-altitude residents CA is lost may suggest that CA is a reversible response of the cerebral vessel tone regulation to the hypoxia of high altitude. In support, animal studies demonstrate that, during acute hypoxia, CA is impaired when the arterial PO2 is below 25 Torr, values that are not compatible with sustained life at altitude (13, 20).
We hypothesize that CA is intact in high-altitude residents when they live at lower altitudes, but the altitude where autoregulation is lost remains unknown. We further tested the hypothesis that the administration of oxygen restores a totally impaired autoregulation. It is important to understand CBF regulation under conditions of high-altitude hypoxia, since high-altitude hypoxia affects workers and tourists and at least some 140 million persons who reside at altitudes above 2,500 m worldwide. In this study, we investigated CA at various altitude levels and we also studied whether the impaired autoregulation at the highest altitude may be corrected with the administration of oxygen.
| METHODS |
|---|
|
|
|---|
Measurements. A blood pressure cuff (Light Monitor, Datex, Finland) was applied on the upper arm to measure MAP. This monitor was also used to measure percent oxygen saturation of arterial hemoglobin (SaO2) with fingerpulse oximetry and to measure end-tidal PCO2 (PETCO2) from a mouthpiece using side-stream sampling (200 ml/min).
mca was measured with a 2-MHz pulsed-wave transcranial Doppler system with online spectrum analysis (T2–64; EME). With a hand-held probe, Doppler signals from the left MCA were identified through the temporal window and obtained at a depth of 45–60 mm, corresponding to the proximal segment of the MCA. The MCA mean velocity (
mca) is automatically calculated by the standard algorithm of the instrument for each 4-s sweep and is displayed on the apparatus. Each
mca value, as used in the study, is then the average of four successive readings over 1–1.5 min. We analyzed the reproducibility of the velocities both at sea level and at altitude by calculating the coefficient of variation (CV) of each of four readings. The CV value was calculated from the equation CV = SD of four
mca readings/mean value of the four readings x 100%, where SD is standard deviation. Twenty (4.4%) of a total of 474 CVs were higher than 6%, and only 7 (1.4%) were between 7.5% and 12%. Thus CV values of each of the four readings are within the CV of 6–11% as determined for intraobserver variation for measurements of
mca (25). The reproducibility of the four readings is thus acceptable for our measurement method of
mca.
Blood from a forearm vein was sampled to measure hematocrit (Ht) (Depex). Given Ht values (%) are expressed as the average of two measurements.
Protocol.
The subjects, who were lying comfortably in a supine position, rested at least 15 min before the start of the measurements. An intravenous needle was introduced in a forearm vein. Baseline values for MAP,
mca, SaO2, and PETCO2 were obtained during stable hemodynamic and ventilatory conditions. Thereafter, a slow increase of MAP of
30–35 mmHg was induced over a 20- to 30-min interval period by intravenous infusion of phenylephrine (0.02%), administered through a pump (Perfusor Secura, Braun, Germany). During this period, 5–12 paired values of MAP and
mca were obtained in each subject (35, 38). At the end of the protocol, SaO2 and PETCO2 were measured to verify that ventilatory conditions had not changed.
To study whether the acute administration of oxygen had an effect on the CA, we repeated the study in the Sherpas in the highest village at 4,243 m (Pheriche-O2 group). Thus they were allowed to breath, with a nose clip, through a mouthpiece with the addition of oxygen (5 l/min) to the inspired air. After an adjustment period of
15 min, the study protocol was repeated.
Autoregulation index.
Because the relation between the systemic blood pressure and CBF within the autoregulatory range is considered linear, regression analysis on the acquired blood pressure values and their corresponding
mca values were performed to yield a regression line. When MAP1 and MAP2 are, respectively, the lowest and the highest blood pressure values as measured in each subject, then
mca1 and
mca2 are considered the corresponding
mca values on the regression line.
To compare the autoregulation between groups and subjects, the autoregulatory capacity was quantified using the autoregulation index (AI) (35). AI is the percent change in estimated cerebral vascular resistance (CVRe, which is calculated as MAP/
mca) per percent change in MAP:
![]() | (1) |
![]() | (2) |
Full autoregulatory capacity is present when the percent change in CVRe is equal to the percent change in MAP. No change in
mca in response to an increase of MAP would result in an AI of 1.0 and implies that
mca is totally independent of MAP. A totally absent autoregulation would result in an AI of 0, and
mca changes proportionally with alterations of MAP (35, 38).
Statistical analysis. Data are presented as means ± SD. Possible association between AI and the baseline characteristics (age, weight) in the four Sherpa groups was explored with Pearson correlation coefficient. ANOVA and Bonferroni correction for post hoc analysis and paired t-test were used where appropriate. A level of P < 0.05 was considered statistically significant.
| RESULTS |
|---|
|
|
|---|
mca between the four Sherpa groups (Table 1). The Sherpas at 4,243 m had significantly higher Ht than the group at 1,330 m. SaO2 at 4,243 m was significantly lower than at the lower altitudes, and SaO2 at 3,440 m was lower than at 2,650 and 1,330 m. During the study protocol, mean PETCO2 values of each group remained within 0.08 kPa, and mean SaO2 values remained within 0.3% from the resting control values. During the highest phenylephrine infusion rate, MAP increases in the various groups were 31–35 mmHg (Table 2), and corresponding
mca changes showed increases in
mca that were higher in the group at 4,243 m than in all other groups (P < 0.01).
|
|
mca data of each subject at the five altitude levels, are shown in Fig. 1. The mean AI of Sherpas at 4,243 m was lower than the mean AI of Sherpas who resided at the lower altitudes (P < 0.0005). The Caucasian group at sea level had an AI of 0.81.
|
mca decreased from 59 to 56 cm/s (paired t-test; P = 0.039). AI increased from 0.22 to 0.49 (paired t-test; P = 0.0082; Fig. 2).
|
| DISCUSSION |
|---|
|
|
|---|
4,000 m, critical changes occur in CA of high-altitude dwellers, which are reversible with the administration of oxygen.
The effect of acute hypoxia on the cerebral circulation shows invariably vasodilatation and an increase in CBF (19). With more prolonged exposure to hypoxia at altitude, the effect diminishes after 3–5 days and CBF returns to the prehypoxic CBF levels (28, 29, 32). However, Tibetan and Andean highlanders have a normal or below normal CBF (15, 26, 27, 33). This normal, sea-level CBF, despite a low arterial PO2, is probably caused by an increased blood viscosity due to the higher Ht in high-altitude residents as a result of erythropoietin upregulation (5, 27). Milledge and Sørensen (27) found that breathing 100% oxygen in natives in Cerro de Pasco decreased CBF by 18%, demonstrating no blunting of the vasodilatation reflex under lifelong hypoxia, and showed that vasodilatation by hypoxia persists after a lifetime of exposure to high altitude. Krasney et al (21), in a review, provided evidence that the primary CBF response to acute hypoxia does not adapt during lifelong hypoxia. There is thus no resetting of the CBF in the face of a continuing hypoxic stimulus for vasodilatation. Thus highlanders are left with some cerebral vasodilatation due to a low Po2 and an average sea-level CBF due to an increase in packed cell volume. The identical
mca values in our subjects at 4,243 and at 1,330 m are thus fully explained by the 25% lower Ht in the latter group.
Loss of autoregulation.
Although the nature of the autoregulatory dysfunction is unknown, our results are consistent with the idea that vasodilatation of the cerebral vessels occurring during high-altitude hypoxia at 4,243 m might be responsible for the loss of autoregulation. Mechanisms that, at sea level, produce cerebral vasodilatation have an inherent capability to impair CA. Such mechanisms include hypercapnia (13), drugs that "directly" dilate cerebral vessels such as volatile anesthetics, and severe hypoxia in animals (13, 20). Cerebral vessel dilatation probably also occurs during high-altitude hypoxia at 4,243 m. Support for cerebral vessel dilatation at high altitude is provided by a study that showed that, during acute exposure to increasing hypoxic levels,
mca increases when SaO2 drops below 90% (11). This corresponds to an arterial PO2 of 58 Torr, which is higher than conventionally reported arterial PO2 levels of 50–53 Torr, which were obtained in anesthetized dogs (24). We measured SaO2 of 88% in the Sherpas at 4,243 m, and, because Sherpas have a normal hemoglobin-oxygen dissociation curve (30), the SaO2 of 88% corresponds with an arterial PO2 of 55 Torr, which is even lower when we consider that chronic mountain dwellers have a slightly alkalotic pH, yielding a lower arterial PO2 at a given oxygen saturation through a leftward shift of the hemoglobin-oxygen dissociation curve. This effect of vasodilatation below the SaO2 level of 90% may play a role in explaining the almost total loss of CA at 4,243 m.
Hyperoxic breathing.
The underlying idea that vasodilatation of the cerebral vessels at 4,243 m as a response to the high-altitude hypoxia may account for the critically impaired autoregulation is supported by our finding of the improvement of the autoregulation during the administration of oxygen. Paulson et al. (29) found that, just as cerebral vasodilatation impairs autoregulation, cerebral vasoconstriction, as caused by oxygen replenishment, reestablishes an impaired autoregulation. During hyperoxic breathing, at least two mechanisms contribute to produce cerebral vasoconstriction. First, hyperoxia has a direct cerebral vasoconstrictive effect and produces a marked decrease in CBF at altitude, as shown in Andean high-altitude natives (26, 27, 33), as well as at sea level (9, 40). Second, hyperoxia causes an increase in minute ventilation and a decrease of PETCO2 (4). This last process is possibly initiated by increased production of reactive oxygen species during hyperoxia, which stimulate central carbon dioxide chemoreceptors to increase ventilation and is known as hyperoxic hyperventilation (7). During oxygen administration in our study,
mca decreased from 59 to 56 cm/s and PETCO2 decreased from 4.0 to 3.8 kPa. Thus it is likely that cerebral vasoconstriction occurs during hyperoxic breathing at altitude, which might improve the impaired autoregulation. We did not measure the effect of hyperoxic breathing on the autoregulation in the lower altitude regions. However, if we consider the AI values of 0.63, 0.57, and 0.57 at 1,330, 2,650, and 3,440 m, respectively, as slightly impaired compared with AI values of 0.80–0.90 in our Caucasian group at sea level and in healthy awake subjects (12, 37), hyperoxic breathing should similarly improve CA at the lower altitudes.
Physiological mechanism. Although impairment of the CA at altitude can be, at least partially, explained by physiological mechanisms that produce cerebral vasodilatation, on the molecular level there exists a lack of contractility of the vessels that regulate CA in the brain. There should be either a surplus of vasodilator activity, such as nitric oxide (NO), or a lack of vasoconstrictors, such as endothelin-1 (1).
NO acts locally on the arteriolar smooth muscle. However, NO regulation of vessel diameter, which resides within the endothelium, is separate from the NO regulation of vessel diameter, which is dependent on the oxygen content of blood, more specifically on the red blood cells. Red blood cells are able to release NO in the presence of hypoxia far from their location of formation, and this function, mediated by S-nitrosohemoglobin, accounts for hypoxia-induced vasodilatation (34). In this respect, exhalation of NO by Tibetans living at 4,200 m is increased compared with that shown in sea-level subjects (3). Recently, it was shown that, in rat brains during permanent exposure to hypobaric hypoxia, there is a decrease of endothelin-1 production within the brain, which may help protect neurons by preventing or limiting the constriction of cerebral microvessels during hypoxia (18). Thus a surplus of NO and/or a decrease of endothelin-1 production might account for the impaired CA in the high-altitude residents.
Critique of the study.
Hypoxia can impair the autoregulation in one of two ways: it can affect either the position of the upper and/or lower limits of autoregulation (width of the autoregulatory plateau) or the gradient of the autoregulatory plateau or both. Because the maximally attained MAP did not exceed 160 mmHg in any subject, the MAP values remained within the normal autoregulatory range of
60–160 mmHg, and we assessed the gradient of the autoregulatory plateau. However, it is possible that under the hypoxic conditions at 4,243 m the gradient of the autoregulatory plateau had been affected or that the right upper limit of the autoregulatory plateau had been shifted. On the one hand, hypoxia and vasodilatation might shift the upper limit leftward, which would cause increases in MAP beyond this limit to produce pressure passive increases in CBF. On the other hand, an increased sympathetic activity, as has been demonstrated at least in newcomers at altitude (14), might shift the upper limit rightward and thus prevent cerebral hyperperfusion. Because the raw autoregulatory curves at 4,243 m in Fig. 1A all show upward inclinations and fit a straight line, it might indicate that we assessed the gradient of the autoregulatory plateau and that the upper limit was not shifted leftward.
Employing transcranial Doppler sonography to test for "static" CA requires, under the hypoxic circumstances of high altitude, the diameter of the MCA to not change during the infusion of phenylephrine. The intravenous infusion of phenylephrine, an exogenous amine with
1-agonist properties, besides its effect of increasing MAP, may have produced vasoconstriction of the MCA. However, studies performed at sea level show a lack of vasoconstriction of cerebral blood vessels from
-adrenergic agonists (8, 10). Furthermore, in response to chronic high-altitude hypoxia, the cerebral arteries of adult sheep show decreased density of
1-adrenergic receptors (39) and decreased contractile responses to norepinephrine and other
-agonists (23, 24). Thus it is not likely that the administration of phenylephrine, as in this study, has important effects on the diameter of the MCA, which might interfere with autoregulation measurements.
In summary, the results of these investigations demonstrate that, with increasing altitudes, CA becomes increasingly impaired in Himalayan high-altitude dwellers. Furthermore, the altitude region between
3,500 and 4,200 m is a region above which CA becomes critically impaired, and we demonstrated that increasing the SaO2 with the administration of oxygen partially improves this critically impaired autoregulation.
| 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. Section 1734 solely to indicate this fact.
| REFERENCES |
|---|
|
|
|---|
1-adrenergic receptors, IP3 responses, and NE-induced contraction in cerebral arteries. Am J Physiol Heart Circ Physiol 271: H2313–H2319, 1996.
1-adrenergic receptors and Ins(1,4,5)P3 responses in cerebral arteries. Am J Physiol Regul Integr Comp Physiol 272: R669–R674, 1997.This article has been cited by other articles:
![]() |
P. N. Ainslie, S. Ogoh, K. Burgess, L. Celi, K. McGrattan, K. Peebles, C. Murrell, P. Subedi, and K. R. Burgess Differential effects of acute hypoxia and high altitude on cerebral blood flow velocity and dynamic cerebral autoregulation: alterations with hyperoxia J Appl Physiol, February 1, 2008; 104(2): 490 - 498. [Abstract] [Full Text] [PDF] |
||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| Visit Other APS Journals Online |