Search PubMed⌕ Search

Biomedical subjects

R E McCullough

Publications and source records attributed to R E McCullough.

At least 37 records · Page 2Linked to original sources

Greater maximal O2 uptakes and vital capacities in Tibetan than Han residents of Lhasa.

Maximal O2 uptake provides an index of the integrated functioning of the O2 transport system. Whether lifelong high altitude residents have greater maximal exercise capacities than acclimatized newcomers is of interest for determining whether years to generations of high altitude exposure influence maximal O2 uptake and, if so, what components of O2 transport are involved. We studied 16 Tibetan lifelong residents of Lhasa, Tibet, China (3658 m) and 20 Han ("Chinese") 8 +/- 1 year residents of the same altitude who were matched for age, height, weight and lack of exercise training. At maximal effort, the Tibetans compared to the Hans had greater O2 uptakes (51 +/- 1 vs 46 +/- 1 ml STPD.min-1.(kg bw)-1, P less than 0.05), exercise workloads (177 +/- 5 vs 155 +/- 6 watts, P less than 0.05), minute ventilations (149 +/- 6 vs 126 +/- 4 IBTPS/min, P less than 0.01) and O2 pulse (15.2 +/- 0.4 vs 13.3 +/- 0.5 ml O2 consumption/heart beat, P less than 0.05). Equally high heart rates were present at maximal effort (191 +/- 3 vs 187 +/- 3 beats/min, P = NS), supporting the likelihood that true maxima were achieved in both groups. The greater minute ventilation in the Tibetans resulted from greater tidal volume and the greater maximal tidal volume correlated positively with the resting vital capacity. We concluded that the Tibetans achieved a higher maximal O2 uptake than the Hans, implying an increased capacity for O2 transport to the working muscle.

Acclimatization↗

Combined effects of female hormones and exercise on hypoxic ventilatory response.

Mild elevations in metabolic rate may influence hypoxic ventilatory response (HVR) differently in men and women. The possible involvement of the female hormones in accounting for this gender difference is supported by observations that mild exercise raised HVR in ovariectomized women treated with estrogen and progestin but not in the same women treated with placebo (Regensteiner et al., 1989). We compared the effects of mild exercise on HVR in 12 women in the follicular phase vs the luteal phase of the menstrual cycle and during MPA (medroxyprogesterone acetate, 20 mg tid) vs placebo treatment. End-tidal PCO2 fell in the luteal compared to the follicular phase and in the follicular MPA compared to the follicular placebo condition. Resting HVR was similar in subjects in the follicular versus the luteal phases of the menstrual cycle and in MPA-treated vs placebo-treated subjects at either the existing (eucapnia) or follicular placebo (normocapnia) end-tidal PCO2. Mild exercise increased expired ventilation but not HVR in placebo-treated subjects in the follicular or luteal placebo conditions. In MPA-treated subjects, exercise raised HVR in the luteal phase (P less than 0.05) and tended to increase HVR in the follicular phase (P = 0.08). The increase in HVR with exercise was greater in MPA-treated subjects than in women given placebo (delta rest to exercise = 26% vs 9%, P less than 0.05). We concluded that elevations in progestin levels achieved by administering progestin in the luteal phase of the menstrual cycle potentiated the effect of metabolic rate on HVR.

Adult↗

Decreased ventilation and hypoxic ventilatory responsiveness are not reversed by naloxone in Lhasa residents with chronic mountain sickness.

Persons with chronic mountain sickness (CMS) hypoventilate and are more hypoxemic than normal individuals, but the cause of the hypoventilation is unclear. Studies of 14 patients with CMS and 11 healthy age-matched control subjects residing in Lhasa, Tibet, China (3,658 m) were conducted to test the hypothesis that hypoventilation, blunted hypoxic ventilatory responsiveness (HVR), and hypoxic ventilatory depression of CMS were due to increased endogenous opioid production. Patients with CMS compared with control subjects exhibited hypoventilation (end-tidal carbon dioxide pressure [PETCO2] = 36.6 +/- 1.0 versus 31.5 +/- 0.5 mm Hg, p less than 0.05), lower tidal volume (VT = 0.54 +/- 0.02 versus 0.61 +/- 0.02 ml BTPS, p less than 0.05), blunted HVR (shape parameter A = 17 +/- 8 versus 114 +/- 22 mm Hg/L BTPS/min, p less than 0.05), and a depressant effect of ambient hypoxia on ventilation (delta PETCO2 with acute hyperoxia = -3.5 +/- 0.5 versus -1.0 +/- 0.6 mm Hg, p less than 0.05). Reduced forced expiratory volume in 1 s to vital capacity ratios (FEV1/VC) and a higher proportion of cigarette smokers in the group of patients with CMS compared with control subjects suggested that at least some patients with CMS had mild airway obstructive lung disease. Naloxone infusion (0.14 mg/kg) to six patients with CMS did not change resting VT, PETCO2, HVR, or SaO2.(ABSTRACT TRUNCATED AT 250 WORDS)

Altitude Sickness↗

Increased exercise SaO2 independent of ventilatory acclimatization at 4,300 m.

Arterial O2 saturation (Sao2) decreases in hypoxia in the transition from rest to moderate exercise, but it is unknown whether other several weeks at high altitude SaO2 in submaximal exercise follows the same time course and pattern as that of ventilatory acclimatization in resting subjects. Ventilatory acclimatization is essentially complete after approximately 1 wk at 4,300 m, such that improvement in submaximal exercise SaO2 would then require other mechanisms. On days 2, 8, and 22 on Pikes Peak (4,300 m), 6 male subjects performed prolonged steady-state cycle exercise at 79% maximal O2 uptake (VO2 max). Resting SaO2 rose from day 1 (78.4 +/- 1.6%) to day 8 (87.5 +/- 1.4%) and then did not increase further by day 20 (86.4 +/- 0.6%). During exercise, SaO2 values (mean of 5-, 15-, and 30-min measurements) were 72.7% (day 2), 78.6% (day 8), and 82.3% (day 22), meaning that all of the increase in resting SaO2 occurred from day 1 to day 8, but exercise SaO2 increased from day 2 to day 8 (5.9%) and then increased further from day 8 to day 22 (3.7%). On day 22, the exercise SaO2 was higher than on day 8 despite an unchanged ventilation and O2 consumption. The increased exercise SaO2 was accompanied by decreased CO2 production. The mechanisms responsible for the increased exercise SaO2 require further investigation.

Acclimatization↗

Decreased exercise muscle lactate release after high altitude acclimatization.

Blood lactate concentration during exercise decreases after acclimatization to high altitude, but it is not clear whether there is decreased lactate release from the exercising muscle or if other mechanisms are involved. We measured iliac venous and femoral arterial lactate concentrations and iliac venous blood flow during cycle exercise before and after acclimatization to 4,300 m. During hypoxia, at a given O2 consumption the venous and arterial lactate concentrations, the venous and arterial concentration differences, and the net lactate release were lower after acclimatization than during acute altitude exposure. While breathing O2-enriched air after acclimatization at a given O2 consumption the venous and arterial lactate concentrations and the venous and arterial concentration differences were significantly lower, and the net lactate release tended to be lower than while breathing ambient air at sea level before acclimatization. We conclude that the lower lactate concentration in venous and arterial blood during exercise after altitude acclimatization reflected less net release of lactate by the exercising muscles, and that this likely resulted from the acclimatization process itself rather than the hypoxia per se.

Acclimatization↗

Altitude, low birth weight, and infant mortality in Colorado.

A decrease in birth weight occurs at high altitude, but its relationship to infant mortality is unclear. We examined Colorado vital statistics recorded from 1979 through 1982 to determine whether high altitude increased infant mortality and whether decreased birth weight contributed to the mortality observed. Retardation of intrauterine growth reduced birth weight and doubled the frequency of low-birth-weight infants from the lowest (915 to 1523 m [3000 to 4999 ft]) to the highest (greater than or equal to 2744 m [greater than or equal to 9000 ft]) altitude in the state. Low birth weight increased mortality risk, but the mortality risk of low birth weight was decreased at high compared with low altitudes, resulting in similar infant mortality rates throughout the state. This finding differed from that of 1969 through 1973 when infant mortality doubled at high altitude. A 46% infant mortality reduction had occurred statewide over the ten years due chiefly to decreased mortality risk for preterm low-birth-weight infants. This reduction, particularly pronounced at high altitude, might have been due to better identification and transport of high-risk pregnancies to hospitals with tertiary neonatal treatment centers.

Altitude↗

Usual clinical dose of acetazolamide does not alter cerebral blood flow velocity.

Prior reports indicate that acetazolamide, an inhibitor of carbonic anhydrase, in moderate doses reduces symptoms of acute mountain sickness, and in large doses increases cerebral blood flow. The effect on flow is not known for a moderate dose, but were flow to increase, then increased cerebral oxygen delivery would be one mechanism of benefit from acetazolamide at high altitude. We utilized Doppler ultrasound in 8 volunteers to determine whether a usual acetazolamide dose (250 mg three times daily) would increase flow velocities in internal carotid and vertebral arteries. Acetazolamide during normoxia decreased pHa, PaCO2, and PETCO2, but baseline flow velocity remained unchanged. In 2 subjects without acetazolamide, voluntary hyperventilation decreased both PETCO2 and flow velocity. Both hypoxia and hypercapnia caused increases in arterial velocities. The increases were not altered by acetazolamide administration. In one subject, 1 g acetazolamide by acute i.v. injection induced an increase in flow velocity (40%) concomitant with a 5 mm Hg decrease in PETCO2, confirming prior reports using similar intravenous dose. In doses employed for prevention of acute mountain sickness, acetazolamide induced metabolic acidosis and may have prevented the fall in velocity usually associated with hypocapnia, but it neither increased baseline cerebral blood flow velocity nor velocity responses to hypoxia and hypercapnia. Benefit of acetazolamide at high altitude may relate to mechanisms other than increased cerebral blood flow.

Acetazolamide↗

Oxygen transport to exercising leg in chronic hypoxia.

Residence at high altitude could be accompanied by adaptations that alter the mechanisms of O2 delivery to exercising muscle. Seven sea level resident males, aged 22 +/- 1 yr, performed moderate to near-maximal steady-state cycle exercise at sea level in normoxia [inspired PO2 (PIO2) 150 Torr] and acute hypobaric hypoxia (barometric pressure, 445 Torr; PIO2, 83 Torr), and after 18 days' residence on Pikes Peak (4,300 m) while breathing ambient air (PIO2, 86 Torr) and air similar to that at sea level (35% O2, PIO2, 144 Torr). In both hypoxia and normoxia, after acclimatization the femoral arterial-iliac venous O2 content difference, hemoglobin concentration, and arterial O2 content, were higher than before acclimatization, but the venous PO2 (PVO2) was unchanged. Thermodilution leg blood flow was lower but calculated arterial O2 delivery and leg VO2 similar in hypoxia after vs. before acclimatization. Mean arterial pressure (MAP) and total peripheral resistance in hypoxia were greater after, than before, acclimatization. We concluded that acclimatization did not increase O2 delivery but rather maintained delivery via increased arterial oxygenation and decreased leg blood flow. The maintenance of PVO2 and the higher MAP after acclimatization suggested matching of O2 delivery to tissue O2 demands, with vasoconstriction possibly contributing to the decreased flow.

Acclimatization↗

Pulmonary hypertension and pulmonary vascular reactivity in beagles at high altitude.

It is unclear whether dogs develop pulmonary hypertension (PH) at high altitude. Beagles from sea level were exposed to an altitude of 3,100 m (PB 525 Torr) for 12-19 mo and compared with age-matched controls remaining at low altitude of 130 m (PB 750 Torr). In beagles taken to high altitude as adults, pulmonary arterial pressures (PAP) at 3,100 m were 21.6 +/- 2.6 vs. 13.2 +/- 1.2 Torr in controls. Likewise, in beagles taken to 3,100 m as puppies 2.5 mo old, PAP was 23.2 +/- 2.1 vs. 13.8 +/- 0.4 Torr in controls. This PH reflected a doubling of pulmonary vascular resistance and showed no progression with time at altitude. Pulmonary vascular reactivity to acute hypoxia was also enhanced at 3,100 m. Inhibition of prostaglandin synthesis did not attenuate the PH or the enhanced reactivity. Once established, the PH was only partially reversed by acute relief of chronic hypoxia, but reversal was virtually complete after return to low altitude. Hence, beagles do develop PH at 3,100 m of a severity comparable to that observed in humans at the same or even higher altitudes.

Altitude↗

Possible gender differences in the effect of exercise on hypoxic ventilatory response.

Gender differences in resting ventilation and hypoxic ventilatory response (HVR) have been reported. Ventilation and HVR are closely related to changes in metabolic rate in men. However, it is unclear whether there is a comparable relationship between metabolic rate and ventilation or HVR in women. We studied 13 men and 12 women to determine whether exercise-induced increases in metabolic rate influenced ventilation, HVR, and hypercapnic ventilatory response (HCVR) differently in men and women. Minute ventilation per unit metabolic rate was higher (lower end-tidal PCO2) in women than men during rest and mild exercise. Resting HVR values were similar in men and women. With mild, exercise-induced increases in O2 consumption (24 +/- 4% in men and 27 +/- 2% in women, p = NS), HVR increased in men (p less than 0.05) but not in women. Moderate exercise-induced increases in O2 consumption (313 +/- 13% in men and 330 +/- 13% in women, p = NS), raised hypoxic responses in both sexes. HCVR values were similar in men and women at rest and during mild exercise. Moderate exercise increased HCVR equally in the sexes. Thus the higher resting ventilation and lesser change in HVR during mild exercise suggested that women were less sensitive to mild metabolic rate stimulation than men.

Adult↗

Propranolol blocks metabolic rate increase but not ventilatory acclimatization to 4300 m.

Previously, we found resting metabolic rate increased at high altitude but the mechanism and consequences of this increase were unclear. We sought to test the role of beta-sympathetic activation for increasing metabolic rate and the contribution of an increase in metabolic rate to raising total ventilation at altitude. Following baseline studies at sea level, two groups of six healthy male subjects received either placebo or propranolol (80 mg/8 h) for 3 days prior to ascent to Pikes Peak (4300 m) where treatment was continued for 15 days. O2 consumption increased in placebo-treated subjects with a rise of 20 +/- 5% (X +/- SEM) on day 1 and no change 0 +/- 7% in propranolol-treated subjects (difference between groups, P less than 0.05). The increase in total ventilation upon ascent was 28 +/- 2% in the placebo group vs 9 +/- 7% in the propranolol group (P less than 0.05) and was correlated with metabolic rate in individual subjects. Decreasing end-tidal PCO2, taken as an index of ventilatory acclimatization, was similar in both groups. Thus, beta-sympathetic activation appears to increase metabolic rate upon ascent to high altitude and lead to a proportionate elevation in total ventilation but does not alter ventilatory acclimatization.

Acclimatization↗

Increased HVR in pregnancy: relationship to hormonal and metabolic changes.

In prior studies at high altitude, we have found that pregnancy increases maternal hypoxic ventilatory response (HVR) but the factors responsible are unknown. Changes in metabolic rate and hormones that occur during pregnancy have previously been shown to influence HVR. We therefore sought to determine the contribution of metabolic rate and hormonal changes to the pregnancy-associated rise in HVR. Pregnancy increased HVR in each of 20 normal, low-altitude (1,600 m) residents. As measured by the shape parameter A, HVR at week 36 was 237 +/- 26 (SE) or twofold higher than the 124 +/- 13 value measured 3 mo postpartum (P less than 0.01) despite the presence of the potentially depressant effects of hypocapnia [change in alveolar partial pressure of CO2 (delta PACO2) = -4 +/- 1 mmHg] and alkalosis [change in arterial pH (delta pHa) = 0.02 +/- 0.01 U] during pregnancy. Sixty percent of the increase in HVR values had occurred by week 20 of gestation at which time O2 consumption (VO2) and CO2 production (VCO2) were unchanged relative to values measured postpartum. The remaining 40% rise in HVR paralleled increases in VO2 and VCO2, and further elevation in VO2 and VCO2 with moderate exercise produced an additional increase in HVR. Serum estradiol and progesterone levels increased with pregnancy, but levels did not correlate with HVR. The women reporting the greatest symptoms of dyspnea had higher HVR A values at week 36 than the least dyspneic women (285 +/- 28 vs. 178 +/- 34, respectively, P less than 0.05). We concluded that factors intrinsic to pregnancy in combination with increased metabolic rate raised HVR twofold with pregnancy and may have contributed to the often-reported symptoms of dyspnea in pregnant women.

Adult↗

Internal carotid and vertebral arterial flow velocity in men at high altitude.

Cerebral blood flow increases at high altitude, but the mechanism of the increase and its role in adaptation to high altitude are unclear. We hypothesized that the hypoxemia at high altitude would increase cerebral blood flow, which would in turn defend O2 delivery to the brain. Noninvasive Doppler ultrasound was used to measure the flow velocities in the internal carotid and the vertebral arteries in six healthy male subjects. Within 2-4 h of arrival on Pikes Peak (4,300 m), velocities in both arteries were slightly and not significantly increased above sea-level values. By 18-44 h a peak increase of 20% was observed (combined P less than 0.025). Subsequently (days 4-12) velocities declined to values similar to those at sea level. At altitude the lowest arterial O2 saturation (SaO2) and the highest end-tidal PCO2 was observed on arrival. By day 4 and thereafter, when the flow velocities had returned toward sea-level values, hemoglobin concentration and SaO2 were increased over initial high-altitude values such that calculated O2 transport values were even higher than those at sea level. Although the cause of the failure for cerebral flow velocity to increase on arrival is not understood, the subsequent increase may act to defend brain O2 transport. With further increase in hemoglobin and SaO2 over time at high altitude, flow velocity returned to sea-level values.

Adult↗

Low acute hypoxic ventilatory response and hypoxic depression in acute altitude sickness.

Persons with acute altitude sickness hypoventilate at high altitude compared with persons without symptoms. We hypothesized that their hypoventilation was due to low initial hypoxic ventilatory responsiveness, combined with subsequent blunting of ventilation by hypocapnia and/or prolonged hypoxia. To test this hypothesis, we compared eight subjects with histories of acute altitude sickness with four subjects who had been asymptomatic during prior altitude exposure. At a simulated altitude of 4,800 m, the eight susceptible subjects developed symptoms of altitude sickness and had lower minute ventilations and higher end-tidal PCO2's than the four asymptomatic subjects. In measurements made prior to altitude exposure, ventilatory responsiveness to acute hypoxia was reduced in symptomatic compared to asymptomatic subjects, both when measured under isocapnic and poikolocapnic (no added CO2) conditions. Diminution of the poikilocapnic relative to the isocapnic hypoxic response was similar in the two groups. Ventilation fell, and end-tidal PCO2 rose in both groups during 30 min of steady-state hypoxia relative to values observed acutely. After 4.5 h at 4,800 m, ventilation was lower than values observed acutely at the same arterial O2 saturation. The reduction in ventilation in relation to the hypoxemia present was greater in symptomatic than in asymptomatic persons. Thus the hypoventilation in symptomatic compared to asymptomatic subjects was attributable both to a lower acute hypoxic response and a subsequent greater blunting of ventilation at high altitude.

Adult↗

Propranolol does not impair exercise oxygen uptake in normal men at high altitude.

Decreased maximal O2 uptake (VO2max) and stimulation of the sympathetic nervous system have been previously shown to occur at high altitude. We hypothesized that tachycardia mediated by beta-adrenergic stimulation acted to defend VO2max at high altitude. Propranolol treatment beginning before high-altitude (4,300 m) ascent reduced heart rate during maximal and submaximal exercise in six healthy men treated with propranolol (80 mg three times daily) compared with five healthy subjects receiving placebo (lactose). Compared with sea-level values, the VO2max fell on day 2 at high altitude, but the magnitude of fall was similar in the placebo and propranolol treatment groups (26 +/- 6 vs. 32 +/- 5%, P = NS) and VO2max remained similar at high altitude in both groups once treatment was discontinued. During 30 min of submaximal (80% of VO2max) exercise, propranolol-treated subjects maintained O2 uptake levels that were as large as those in placebo subjects. The maintenance of maximal or submaximal levels of O2 uptake in propranolol-treated subjects at 4,300 m could not be attributed to increased minute ventilation, arterial O2 saturation, or hemoglobin concentration. Rather, it appeared that propranolol-treated subjects maintained O2 uptake by transporting a greater proportion of the O2 uptake with each heartbeat. Thus, contrary to our hypothesis, beta-adrenergic blockade did not impair maximal or submaximal O2 uptake at high altitude due perhaps to compensatory mechanisms acting to maintain stroke volume and cardiac output.

Adult↗

Headache at high altitude is not related to internal carotid arterial blood velocity.

The cause of headache in persons going to high altitude is unknown. Relatively severe hypoxemia in susceptible subjects could induce large increases in cerebral blood flow that then could initiate the headache. Thus we measured noninvasively, by Doppler ultrasound, changes in internal carotid arterial blood velocity (velocity) in 12 subjects in Denver (1,600 m) and repeatedly up to 7 h at a simulated altitude of 4,800 m (barometric pressure = 430 Torr). Six subjects, selected because of prior history of high-altitude headache, developed comparatively severe headache at 4,800 m, and four subjects, without such history, remained well. Two subjects developed moderate headache. Velocity at 4,800 m did not correlate with symptom development, arterial O2 saturation, or end-tidal PCO2. Also, neither velocity nor blood pressure was consistently elevated above the Denver base-line values. During measurements of hypercapnic ventilatory response in Denver, velocity increased linearly with end-tidal PCO2, confirming that our Doppler method could demonstrate an increase. Also, 30 min of isocapnic or poikilocapnic hypoxia caused small increases in velocity (+8 and +6%) during the base-line measurement at low altitude. Although even a small increase in cerebral perfusion could contribute to headache symptoms at high altitude, cerebral blood flow does not appear to play a primary role.

Adult↗

Increased metabolism contributes to increased resting ventilation at high altitude.

Ventilatory acclimation to high altitude results in an increase in total or minute ventilation, and is associated with a fall in alveolar PCO2, i.e. alveolar hyperventilation. However, the extent to which the increase in total ventilation is matched by a greater metabolic rate (VO2, VCO2) vs alveolar hyperventilation is unclear. We sought to determine the contribution of changes in metabolic rate to the increase in minute ventilation observed during exposure to high altitude. In 12 healthy male subjects taken from Denver, Colorado (1600 m) to Pikes Peak, Colorado (4300 m) for 5 days, resting minute ventilation increased from low to high altitude (+ 26% for the 5 days) and arterialized PCO2 fell. Resting metabolic rate increased 16% for the 5 days and could account for more than half of the increase in minute ventilation. Among subjects the increases in ventilation on days 1, 2 and 4 were positively correlated with increased CO2 production; they were not correlated with arterial oxygen saturation on any day. During exercise at high altitude, PCO2 values were not different from those at rest and minute ventilation rose above low altitude values (+ 58% by day 5), but the increase could not be accounted for by an increased CO2 production. Thus at rest but not during exercise a substantial portion of the rise in minute ventilation could be attributed to increased metabolic rate.

Acclimatization↗

Variable inhibition by falling CO2 of hypoxic ventilatory response in humans.

Acute hypoxia stimulates an increase in ventilation but the resulting hypocapnia limits the magnitude of the increase. Thus the hypoxic ventilatory response is usually measured during isocapnia, but this may not reflect events at high altitude. We hypothesized that the degree of inhibition by hypocapnia might depend on individual ventilatory response to CO2 and thus vary between persons. To test this hypothesis we compared the isocapnic hypoxic ventilatory response (end-tidal PCO2 maintained by CO2 addition) with the response in which CO2 was not added and the end-tidal PCO2 fell to a variable extent (poikilocapnic hypoxia). In 14 healthy persons we found that the poikilocapnic hypoxic ventilatory response was determined by two factors: sensitivity to isocapnic hypoxia acting to increase ventilation and sensitivity to CO2 acting to decrease the hypoxic ventilatory response. The ventilatory response to poikilocapnic hypoxia correlated with but was generally less than the isocapnic hypoxic response. The magnitude of the difference between them related to the hypercapnic response. Further, the results suggested that the CO2 response in the high CO2 range related to ventilatory events in the low CO2 range. Thus the magnitude of ventilatory inhibition by hypocapnia may depend on individual ventilatory responsiveness to CO2.

Adult↗