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Biomedical subjects

R C Roach

Publications and source records attributed to R C Roach.

At least 37 records · Page 2Linked to original sources

Body fluid alterations during head-down bed rest in men at moderate altitude.

To determine the effects of hypoxia on fluid balance responses to simulated zero-gravity, measurements were made in six subjects (acclimatized to 5,400 ft; 1,646 m) before and during -5 degrees continuous head-down bed rest (HDBR) over 8 d at 10,678 ft. The same subjects were studied again at this altitude without HDBR as a control (CON) using a cross-over design. During this time, they maintained normal upright day-time activities, sleeping in the horizontal position at night. Fluid balance changes during HDBR in hypoxia were more pronounced than similar measurements previously reported from HDBR studies at sea level. Plasma volume loss (-19% on day 6) was slightly greater and the diuresis and natriuresis were doubled in magnitude as compared to previous studies in normoxia and sustained for 4 d during hypoxia. These changes were associated with an immediate, but transient rise in plasma atrial natriuretic peptide (ANP) to day 4 of 140% in HDBR and 41% in CON (p < 0.005), followed by a decline towards baseline. Differences were less striking between HDBR and CON for plasma antidiuretic hormone and aldosterone, which were transiently reduced by HDBR. Plasma catecholamines showed a similar pattern to ANP (+122%) in both HDBR and CON, suggesting that elevated ANP and catecholamines together accounted for the enhanced fluid shifts with HDBR during hypoxia.

Adult↗

Effects of prolonged head-down bed rest on physiological responses to moderate hypoxia.

To determine the effects of hypoxia on physiological responses to simulated zero-gravity, cardiopulmonary and fluid balance measurements were made in 6 subjects (acclimatized to 5,400 ft) before and during 5 degrees head-down bed rest (HDBR) over 8 d at 10,678 ft and a second time at this altitude as controls (CON). The VO2max increased by 9% after CON, but fell 3% after HDBR (p < 0.05). This reduction in work capacity during HDBR could be accounted for by inactivity. The heart rate response to a head-up tilt was greatly enhanced following HDBR, while mean blood pressure was lower. No significant negative impact of HDBR was noted on the ability to acclimatize to hypoxia in terms of pulmonary mechanics, gas exchange, circulatory or mental function measurements. No evidence of pulmonary interstitial edema or congestion was noted during HDBR at the lower PIO2 and blood rheology properties were not negatively altered. Symptoms of altitude illness were more prevalent, but not marked, during HDBR and arterial blood gases and oxygenation were not seriously effected by simulated microgravity. Declines in base excess with altitude were similar in both conditions. The study demonstrated a minimal effect of HDBR on the ability to adjust to this level of hypoxia.

Acclimatization↗

Acetazolamide in the treatment of acute mountain sickness: clinical efficacy and effect on gas exchange.

OBJECTIVE: To determine the efficacy of acetazolamide in the treatment of patients with acute mountain sickness and the effect of the drug on pulmonary gas exchange in acute mountain sickness. DESIGN: A randomized, double-blind, placebo-controlled trial. SETTING: The Denali Medical Research Project high-altitude research station (4200 m) on Mt. McKinley, Alaska. PARTICIPANTS: Twelve climbers attempting an ascent of Mt. McKinley (summit, 6150 m) who presented to the medical research station with acute mountain sickness. INTERVENTION: Climbers were randomly assigned to receive acetazolamide, 250 mg orally, or placebo at 0 (baseline) and 8 hours after inclusion in the study. MAIN OUTCOME MEASURES: An assessment of acute mountain sickness using a symptom score and pulmonary gas exchange measurements was done at baseline and at 24 hours. MAIN RESULTS: After 24 hours, five of six climbers treated with acetazolamide were healthy, whereas all climbers who received placebo still had acute mountain sickness (P = 0.015). Arterial blood gas specimens were obtained from three of the six acetazolamide recipients and all of the placebo recipients. The alveolar to arterial oxygen pressure difference (PAO2-PaO2 difference) decreased slightly over 24 hours in the acetazolamide group (-0.8 +/- 1.2 mm Hg) but increased in the placebo group (+3.3 +/- 2.3 mm Hg) (P = 0.024). Acetazolamide improved PaO2 over 24 hours (+2.9 +/- 0.8 mm Hg) when compared with placebo (-1.3 +/- 2.8 mm Hg) (P = 0.045). CONCLUSION: In established cases of acute mountain sickness, treatment with acetazolamide relieves symptoms, improves arterial oxygenation, and prevents further impairment of pulmonary gas exchange.

Acetazolamide↗

The effect of vasodilators on pulmonary hemodynamics in high altitude pulmonary edema: a comparison.

High altitude pulmonary edema is characterized hemodynamically by a markedly restricted pulmonary vascular bed. Pulmonary vascular resistance is six to eight times higher than control values at altitude, and mean pulmonary pressure is generally elevated two to four-fold over control values. We wished to compare the effect of various vasodilators on the hemodynamics of HAPE, both to gauge their potential effectiveness in treatment of HAPE, and also to gain clues as to the mechanism of the altered pulmonary circulation. In a series of field experiments using a total of 16 subjects with HAPE and 10 well controls, we measured pulmonary hemodynamics by non-invasive Doppler echocardiography. The per cent reduction in pulmonary vascular resistance and mean pulmonary artery pressure, respectively, were 46 and 33 for oxygen, 30 and 29 for nifedipine, 29 and 25 with hydralazine, 57 and 42 with phentolamine, and 72 and 52 when oxygen and phentolamine were combined. All the vasodilators improved gas exchange, suggesting a link between edema formation and pulmonary vasoconstriction. A number of vasodilators may be useful in the treatment of HAPE; the superiority of an alpha adrenergic blocker may implicate the sympathetic nervous system in the pathophysiology of high altitude pulmonary edema.

Altitude Sickness↗

Effects of acid-base status on acute hypoxic pulmonary vasoconstriction and gas exchange.

To investigate the relationship between hypoxic pulmonary vasoconstriction and respiratory and metabolic acidosis and respiratory alkalosis, the pulmonary gas exchange and pulmonary hemodynamic responses were measured in anesthetized, paralyzed, and mechanically ventilated dogs in two sets of experiments (series A, n = 6; series B, n = 10). The animals were treated with acute hypoxia, CO2 inhalation, hyperventilation, and dinitrophenol in various combinations. Multiple regression analysis indicated that mean pulmonary arterial pressure (Ppa) was significantly correlated with end-tidal PO2, mixed venous PO2, and the mean pulmonary capillary pH (average of arterial and mixed venous pH) as independent variables [series A: r = +0.999, standard error of estimate (SEE) = 0.4 mmHg; series B: r = +0.98, SEE = 1.4 mmHg]. Similar analyses of mean values published by other authors from an acute study on humans with exercise at sea level and simulated altitudes of 10,000 and 15,000 ft also indicated a good relationship (n = 14, r = +0.98, SEE = 2.1 mmHg). The mean data (n = 19) obtained in Operation Everest II at various exercise loads and simulated altitudes gave a correlation of r = +0.87, SEE = 6.1 mmHg. These empirical analyses suggest that variations in the rise of Ppa with hypoxia can be accounted for in vivo by the superimposed acid-base status. Furthermore, ventilation-perfusion inhomogeneity, as estimated in the dogs from end-tidal and arterial O2 and CO2 differences and assuming no true shunt or diffusion impairment, was highly correlated with Ppa and mean pulmonary capillary pH (r = +0.999 in series A, r = +0.77 in series B). The human data from the above studies also showed significant correlations between Ppa and directly measured ventilation-perfusion (standard deviation of perfusion obtained from inert gas measurements). These observations indicate that the beneficial effects of hyperventilation during hypoxia may be related to the marked alkalosis that serves to reduce Ppa and improve pulmonary gas exchange efficiency.

2,4-Dinitrophenol↗

Renal carbonic anhydrase inhibition reduces high altitude sleep periodic breathing.

The efficacy of carbonic anhydrase (CA) inhibitors in amelioration of periodic breathing during sleep at high altitude is not fully understood. Although CA is present in a number of tissues, we hypothesized that selective renal CA inhibition without physiologically important inhibition of other tissue CA, may be sufficient alone by its generation of a mild metabolic acidosis to stimulate ventilation and prevent periodic breathing. We studied benzolamide (3 mg/kg), a selective inhibitor of renal CA, in 4 climbers on ventilation and ventilatory responses at sea level and on arterial O2 saturation (SaO2%) and periodic breathing during sleep at altitude. At sea level, ventilation increased and PaO2 rose accompanied by a mild metabolic acidosis. The isocapnic hypoxic ventilatory response was unchanged but the hyperoxic hypercapnic ventilatory response rose 40%. At high altitude (4400 m), daytime SaO2% improved from 81 to 85 and venous plasma HCO3- fell from 18.9 to 14.8 mM. During sleep, mean SaO2% rose from 76 to 80 and periodic breathing decreased 75%. We conclude that metabolic acidosis occurring with all CA inhibitors is one of the major stimulant actions of these drugs on ventilation while awake and during sleep at high altitude.

Acidosis↗

Operation Everest II: ventilatory adaptation during gradual decompression to extreme altitude.

To assess the ventilatory adaptation during gradual ascent to extreme altitude, we studied seven healthy males as part of the 40 d simulated ascent of Mt. Everest in a hypobaric chamber. We measured resting ventilation (VE, l.min-1), arterial oxygen saturation (SaO2%), the ventilatory response to oxygen breathing, isocapnic hypoxic ventilatory response (HVR), and hypercapnic ventilatory response (HCVR) at sea level prior to the ascent (760 torr), 14,000 feet (428 torr), 24,000 feet (305 torr), and within 24 h of descent (765 torr). VE increased from 9.3 +/- 1.1 l.min-1 at 760 torr to 23.4 +/- 1.3 l.min-1 at 305 torr and remained elevated at 14.7 +/- 0.7 l.min-1 after descent. Oxygen breathing decreased VE by 9.6 +/- 1.3 l.min-1 at 305 torr. Isocapnic HVR (expressed as a positive slope of VE/SaO2, l.min-1.%SaO2(-1) increased from 0.18 +/- 0.07 at 760 torr to 0.34 +/- 0.11 and 0.38 +/- 0.5 at 428 torr and 305 torr (P less than 0.05) respectively. HVR was elevated further upon return to sea level (0.8 +/- 0.09, P less than 0.05). HCVR (S = VE/PETCO2, l.min-1.torr-1) increased from sea level (S = 4.4 +/- 0.09) to 305 torr (S = 18.7 +/- 3.5, P less than 0.01) and remained elevated upon return to sea level (S = 10.7 +/- 4.6, P less than 0.001). This study is the first to investigate the ventilatory response to such extreme altitude and so soon after descent and shows that hypoxic and hypercapnic responses increase during prolonged progressive hypoxic exposure and remain significantly elevated from pre-ascent levels immediately upon descent.

Acclimatization↗

Accuracy of heart-rate monitoring and activity diaries for estimating energy expenditure.

The accuracy of heart-rate monitoring and activity diaries for measuring energy expenditure in free-living individuals was studied in 12 women. Estimates of energy expenditure were calculated from heart-rate monitoring by use of four different prediction equations to describe the relationship between heart rate and energy expenditure. Estimates of energy expenditure from activity diaries were calculated using both individually measured and published values for the energy cost of activities. Energy intake adjusted for changes in body-energy stores was used as a reference. Heart-rate monitoring overestimated group energy expenditure from 2 to 9% and the errors in estimating individual energy expenditure ranged from -53 to 67%. Activity diaries underestimated group energy expenditure by 2-6% and the errors in estimating individual energy expenditure ranged from -39 to 56%. Heart-rate monitoring and activity diaries may prove useful for estimating the energy expenditure of groups but not individuals.

Activities of Daily Living↗

Abnormal control of ventilation in high-altitude pulmonary edema.

We wished to determine the role of hypoxic chemosensitivity in high-altitude pulmonary edema (HAPE) by studying persons when ill and upon recovery. We studied seven males with HAPE and seventeen controls at 4,400 m on Mt. McKinley. We measured ventilatory responses to both O2 breathing and progressive poikilocapnic hypoxia. Hypoxic ventilatory response (HVR) was described by the slope relating minute ventilation to percent arterial O2 saturation (delta VE/delta SaO2%). HAPE subjects were quite hypoxemic (SaO2% 59 +/- 6 vs. 85 +/- 1, P less than 0.01) and showed a high-frequency, low-tidal-volume pattern of breathing. O2 decreased ventilation in controls (-20%, P less than 0.01) but not in HAPE subjects. The HAPE group had low HVR values (0.15 +/- 0.07 vs. 0.54 +/- 0.08, P less than 0.01), although six controls had values in the same range. The three HAPE subjects with the lowest HVR values were the most hypoxemic and had a paradoxical increase in ventilation when breathing O2. We conclude that a low HVR plays a permissive rather than causative role in the pathogenesis of HAPE and that the combination of extreme hypoxemia and low HVR may result in hypoxic depression of ventilation.

Adult↗

The lung at high altitude: bronchoalveolar lavage in acute mountain sickness and pulmonary edema.

High-altitude pulmonary edema (HAPE), a severe form of altitude illness that can occur in young healthy individuals, is a noncardiogenic form of edema that is associated with high concentrations of proteins and cells in bronchoalveolar lavage (BAL) fluid (Schoene et al., J. Am. Med. Assoc. 256: 63-69, 1986). We hypothesized that acute mountain sickness (AMS) in which gas exchange is impaired to a milder degree is a precursor to HAPE. We therefore performed BAL with 0.89% NaCl by fiberoptic bronchoscopy in eight subjects at 4,400 m (barometric pressure = 440 Torr) on Mt. McKinley to evaluate the cellular and biochemical responses of the lung at high altitude. The subjects included one healthy control (arterial O2 saturation = 83%), three climbers with HAPE (mean arterial O2 saturation = 55.0 +/- 5.0%), and four with AMS (arterial O2 saturation = 70.0 +/- 2.4%). Cell counts and differentials were done immediately on the BAL fluid, and the remainder was frozen for protein and biochemical analysis to be performed later. The results of this and of the earlier study mentioned above showed that the total leukocyte count (X10(5)/ml) in BAL fluid was 3.5 +/- 2.0 for HAPE, 0.9 +/- 4.0 for AMS, and 0.7 +/- 0.6 for controls, with predominantly alveolar macrophages in HAPE. The total protein concentration (mg/dl) was 616.0 +/- 3.3 for HAPE, 10.4 +/- 8.3 for AMS, and 12.0 +/- 3.4 for controls, with both large- (immunoglobulin M) and small- (albumin) molecular-weight proteins present in HAPE.(ABSTRACT TRUNCATED AT 250 WORDS)

Adult↗

Dexamethasone for prevention and treatment of acute mountain sickness.

We wished to determine in a field study the effectiveness of dexamethasone for prevention and treatment of acute mountain sickness (AMS). Prevention Trial: We transported 15 subjects from sea level to 4,400 m (PB = 400 mm Hg) on Denali (Mt. McKinley) by means of a 1-h helicopter flight. In a randomized, double-blind fashion we gave eight subjects a placebo and seven subjects 2 mg dexamethasone orally every 6 h, starting 1 h before take-off. The entire placebo group and five of the dexamethasone group developed AMS within 5 h, and became progressively more ill until 12 h when the trial was terminated. We concluded that 2 mg of dexamethasone every 6 h did not prevent AMS in active soldiers rapidly transported to high altitude. Treatment Trial: We treated 11 of those with moderate to severe AMS (symptom score 4.5 +/- 0.7, range 3 to 11) with 4 mg of dexamethasone every 6 h orally or intramuscularly for 24 h. All were markedly improved at 12 h (symptom score 1.0 +/- 0.3, p less than 0.001, range 0 to 3), but symptoms increased after the drug was discontinued at 24 h (symptom score = 2.4 +/- 0.5). We conclude that dexamethasone in a dosage of 4 mg PO or IM every 6 h is an effective treatment for AMS, but that illness may recur with abrupt discontinuation of the drug.

Adult↗

Medical therapy of altitude illness.

Acute mountain sickness (AMS) and high-altitude pulmonary edema (HAPE) continue to cause significant morbidity and occasional deaths among mountain recreationists and residents. Descent to lower altitude is still considered the treatment of choice, but an increased role for medical therapy is emerging. Acetazolamide is currently the drug of choice for prevention of AMS, and probably HAPE as well. Numerous studies have demonstrated the drug's effectiveness when it is started 12 to 24 hours before ascent. Suggestions for indications, dosage, and regimen vary with different authors. Lower dosage offers adequate protection with fewer side effects. Acetazolamide has still not been adequately studied for treatment of altitude illness. Oxygen effectively treats HAPE and mild AMS, but is not as useful for cerebral edema. Dexamethasone recently was found effective for treatment of AMS, including early cerebral edema, but not for advanced cerebral edema. Side effects limit its use for prophylaxis, but dexamethasone offers an alternative to acetazolamide for those with sulfa intolerance.

Acute Disease↗

Respiratory stimulants and sleep periodic breathing at high altitude. Almitrine versus acetazolamide.

We studied the effects of almitrine, acetazolamide, and placebo on the hypoxic ventilatory response (HVR), sleep periodic breathing, and arterial oxygen saturation (SaO2) in 4 healthy climbers. In a laboratory on Denali (Mt. McKinley) at 4,400 m (PB = 440 mm Hg), we used a double-blind, randomized, three-way crossover design. The HVR was measured during the waking state. Periodic breathing and SAO2% were measured during 3-h sleep studies. Almitrine and acetazolamide both increased SaO2% during sleep, although almitrine increased periodic breathing, whereas acetazolamide decreased periodic breathing. The HVR (delta VE/delta SaO2%) was doubled with almitrine (p less than 0.05), but unchanged with acetazolamide. The HVR was positively related to periodic breathing (p less than 0.05). We conclude that periodic breathing during sleep at high altitude is related to the hypoxic ventilatory response, and that acetazolamide is a superior agent to almitrine for ameliorating periodic breathing.

Acetazolamide↗

High-altitude pulmonary edema. Characteristics of lung lavage fluid.

To evaluate the cellular and biochemical composition of bronchoalveolar fluid in high-altitude pulmonary edema (HAPE), we performed bronchoalveolar lavage in three climbers with HAPE in a research facility at 4400 m on Mount McKinley. Three healthy climbers were used as controls. The HAPE fluids contained marked increases in high-molecular-weight proteins, erythrocytes, and leukocytes, most of which were alveolar macrophages. The HAPE fluids also contained detectable amounts of leukotriene B4 and other lipoxygenase products of arachidonic acid metabolism, complement fragments (C5a), inhibitors of neutrophil chemotaxis, and acid proteases but not hydroxyproline, a constituent of collagen. The data from this study indicate that HAPE involves a transient "large pore" leak in the pulmonary circulation. Despite the presence of two potent mediators of inflammation, leukotriene B4 and C5a, HAPE is not characterized by the intense neutrophil accumulation that is typical of other forms of acute lung injury.

Adult↗

High altitude pulmonary edema and exercise at 4,400 meters on Mount McKinley. Effect of expiratory positive airway pressure.

Breathing against positive expiratory pressure has been used to improve gas exchange in many forms of pulmonary edema, and forced expiration against resistance during exercise has been advocated for climbing at high altitude as a method to optimize performance. To evaluate the effect of expiratory positive airway pressure (EPAP) on climbers with high altitude pulmonary edema (HAPE) and on exercise at high altitude, we studied four climbers with HAPE at rest and 13 healthy climbers during exercise on a bicycle ergometer at 4400 m. We measured minute ventilation (VI, L/min), arterial oxygen saturation (SaO2 percent), end-tidal carbon dioxide (PACO2, mm Hg), respiratory rate (RR), and heart rate (HR) during the last minute of a five minute interval at rest in the climbers with HAPE, and at rest, 300, and 600 kpm/minute workloads on a bicycle ergometer in the healthy subjects. The HAPE subjects demonstrated an increased SaO2 percent, no change in HR or VI, and a decrease in RR on EPAP as compared to control. In normal subjects, SaO2 percent, VI, and heart rate were significantly higher on EPAP 10 cm H2O than 0 cm H2O control (p less than 0.01, 0.01, and 0.05, respectively). The RR and PaCO2 were not significantly different. In summary, EPAP improves gas exchange in HAPE subjects at rest. The EPAP in normal subjects at high altitude resulted in a higher SaO2 percent at the expense of a higher VI and higher HR. These results suggest that the work of breathing is higher and the stroke volume lower on EPAP. The positive pressure mask may be an effective temporizing measure for victims of HAPE who cannot immediately go to a lower altitude.

Adult↗

Acute mountain sickness, antacids, and ventilation during rapid, active ascent of Mount Rainier.

A double-blind randomized study of 45 climbers on Mt. Rainier was conducted to test the effectiveness of antacids in preventing acute mountain sickness. All 45 climbed to 3353 m, and 31 continued to the summit. Ten climbers listed acute mountain sickness as the reason for not attaining the summit. Of symptoms monitored throughout the climb, neither headache, nausea, dizziness, pounding heart, nor shortness of breath differed in severity between antacid-treated and placebo-treated groups. In both groups vital capacity decreased significantly with ascent (p less than 0.05), while peak flow (p less than 0.005) and minute ventilation (p less than 0.001) increased significantly. The 7 climbers with the most severe AMS symptom scores above 4000 m had significantly lower peak flow at sea level prior to ascent compared with the other 25 climbers who completed sea level tests (p less than 0.005). The results of this study fail to document efficacy for antacid use for the prevention of acute mountain sickness.

Adult↗