Influence of simulated altitude on the performance of five blood glucose meters

OBJECTIVE: To determine the reliability of five blood glucose meters (BGMs) at various simulated altitudes using a hypobaric chamber. RESEARCH DESIGN AND METHODS: Blood glucose levels (ranged from 1.5 to 26.3 mmol/l, according to the reference method) were measured in 18 venous blood samples by each BGM at 200, 1,000, and every 500 m up to 4,000 m in a hypobaric chamber, where temperature and humidity were held constant. RESULTS: Four BGMs underestimated and one overestimated blood glucose concentration while barometric pressure decreased. The average percent error varied in relation to simulated altitude from 0.26 +/- 4.8% (SD) at 200 m to -28.9 +/- 4.5% at 4,000 m (Glucometer 3; P < 0.05), from 28.4 +/- 5.7 to 49.3 +/- 5.9% (Accu-Chek Easy; P < 0.05), from -10.5 +/- 2.6 to 19.8 +/- 4.3% (Tracer, P < 0.05), from -5.5 +/- 2.6 to -11.2 +/- 3.0% (Reflolux; NS), and from 17.8 +/- 4.3 to 14.8 +/- 3.6% (One Touch; NS). The most accurate seemed to be the Reflolux, except for high blood glucose levels at simulated high altitudes. The One Touch II showed a good agreement, whatever the barometric pressure and the range of blood glucose concentrations. The highest underestimation was seen with the Glucometer 3. CONCLUSIONS: Except for the Accu-Chek Easy, low barometric pressure underestimated the BGM results in comparison with measurements taken at simulated low altitudes. The lack of accuracy and consistency of performance > 2,000 m should be known by diabetic patients practicing sports activities, such as trekking or skiing at high altitudes.     

Dermatophagoides sp. and IgE anti-D. pteronyssinus and D. farinae detection in a Venezuelan community at more than 2000 m above the sea level

BACKGROUND: It has been reported that the concentration of Dermatophagoides sp. population, the main trigger of asthma in sensitized atopic subjects, is inversely related with altitude and probably directly with humidity and that this population are scarcely found over 1750 m above sea level. OBJECTIVE: We studied the presence of Dermatophagoides sp. in a Venezuelan community between 2040 and 2600 m above sea level, and also the IgE response to D. pteronnyssinus and D. farinae in atopic subjects living on that region. METHODS: The presence of Dermatophagoides sp. was determined by microscopic identification of mites in dust, obtained by brushing the mattresses surface in 93 randomly selected houses between 2040 and 2600 m above sea level. The indoor relative humidity was also measured. The specific IgE serum levels were studied in 65 subjects classified as asthmatics, allergic non-asthmatics and non-allergic. RESULTS: A mean concentration of 188 mites/g of room dust was determined in 82.4% of houses with an indoor relative humidity ranging from 89% and 92% independently of altitude. The density of Dermatophagoides sp. was sufficiently high to sensitize the atopic subjects, IgE levels were 6.8 PRU mean value for asthmatic, against 0.38 PRU in non-atopic. CONCLUSIONS: We conclude that: (a) Dermatophagoides sp. can be found up to 2600 m above sea level in a Venezuelan neotropical region where a high indoor relative humidity is characteristic of most dwellings; (b) sensitization by D. pteronyssinus and D. farinae were demonstrated in atopic subjects resident at that region.     

Quantitative EEG in acute mountain sickness

OBJECTIVES: To investigate if the EEG response at moderate altitude may predict a person's tolerance to acute mountain sickness (AMS). MATERIALS AND METHODS: Frequency analysis (QEEG) of tape-recorded ambulatory EEG was performed in 6 climbers during a mountaineering expedition to 7546 m above sea level. The QEEG response in climbers, measured at sea level, at 4500 m, and at 1800 m 1-4 days after maximal altitude exposure, was compared to the change observed during consecutive sea level recordings in 10 control subjects. RESULTS: Three climbers experienced slight (grade 1) AMS symptoms both at 4500 m and at maximal altitude exposure (Group 1). Three other climbers (Group 2) had no symptoms at 4500 m, but they developed AMS (grades 1, 2, or 3) at maximal altitude. Alpha amplitudes were higher at 4500 m in group 1 climbers, while it was lower in group 2 climbers compared to the sea level recording. Significant time x group interactions in ANOVA were found for delta (P = 0.005), theta (P = 0.001) and alpha (P = 0.001) amplitude, indicating that QEEG amplitudes decreased significantly at high altitude in group 2 climbers. CONCLUSION: The QEEG response to moderate hypobaric hypoxia is not uniform, but the direction of QEEG amplitude change, particularly in the alpha band, may possibly predict the risk of developing AMS.     

Performance incentives and means: how regulatory focus influences goal attainment

A study was performed to evaluate the effect of prolonged environmental hypobaric hypoxia on the ultrastructure of rat cornea. 60-day-old female Wistar rats were exposed to a simulated altitude of 5,500 m (350 mmHg) and pO2 of 76 mmHg for 30 days. Control rats were exposed to atmospheric sea level pressure (760 mmHg) and pO2 of 150 mmHg, for the same period. Ultrastructural analysis of the corneal epithelium did not reveal any relevant difference between control and treated rats. In contrast, the corneal stroma of rats subjected to hypoxia showed vascularization with advanced vessel differentiation and signs of active proliferation. The endothelium of hypoxic cornea showed swollen mitochondria and large empty cytoplasmic areas. The endothelial intercellular junctions could hardly be identified in the hypoxic condition. Nevertheless, the most evident change in hypoxic cornea was in Descemet's membrane, which was considerably thickened, to approximately twice that of the control specimen. These results suggest that environmental hypobaric hypoxia induces marked alterations in the corneal stroma and endothelium morphology, probably related to reduced oxygen tension in the aqueous humor, consequent to hypoxemia.     

Bronchoarterial ratio on thin section CT: comparison between high altitude and sea level

PURPOSE: Our goal was to measure normal bronchial to accompanying pulmonary arterial diameter ratios and normal bronchial wall thickness on thin section CT at high altitude and at sea level. METHOD: Seventeen normal, healthy, nonsmoking subjects living at 1,600 m altitude and 16 living at sea level underwent thin section CT (1.5 to 2.0 mm collimation). All images were photographed at window levels of -450 and -700 HU and window width of 1,500-1,600 HU. Internal diameters of the segmental and subsegmental bronchi were measured and compared with the diameter of the adjacent pulmonary artery. Bronchial wall thickness of each bronchus was measured. Only bronchi and arteries seen in cross section and within 1 mm from each other were included in the analysis. RESULTS: Four hundred sixty-seven bronchi (215 at high altitude, 252 at sea level) were assessed. At window level of -450 HU, the bronchoarterial ratio was 0.76 +/- 0.14 (mean +/- SD) at altitude and 0.62 +/- 0.13 at sea level (p < 0.001). Bronchial wall thickness measured 0.92 +/- 0.09 mm (mean +/- SD) at altitude and 1.12 +/- 0.19 mm at sea level (p < 0.001). At window level of -700 HU, there was an artifactual decrease in the bronchoarterial diameter ratios and an increase in bronchial wall thickness. CONCLUSION: Bronchoarterial ratio increases and bronchial wall thickness decreases with altitude. These findings are presumably related to hypoxic bronchodilatation and vasoconstriction.     

Determining Fault Permeability from Subsurface Barometric Pressure

Measured barometric pressure fluctuations in a borehole drilled 600 m into the unsaturated zone at a site on the eastern slope of Yucca Mountain, Nevada, are used to compute pneumatic diffusivities and air permeabilities of layered tuffaceous rocks. Of particular interest is the occurrence of increasing pressure amplitude and decreasing phase lags observed at several deep stations. The pressure amplitude increases by 13% and the pressure peak arrives 65 to 72 h earlier as the depth of the unsaturated zone increases from 407 to 436 m. This observation is inconsistent with a conventional 1D downward pressure decay model, but can be explained by hypothesizing the existence of a lateral pneumatic flow path from a nearby fault. A 2D numerical model has been constructed to test this lateral flow hypothesis. The modeling results indicate that a leaky-fault hypothesis can reconcile the measured barometric data with other geologic mapping and permeability measurements at the site. The inferred fault permeability ranges from 0.6 × 10?12 to 0.12 × 10?9 m2, and that of the surrounding tuff layers ranges from 0.4 × 10?13 to 0.8 × 10?12 m2. Our analysis also demonstrates that although the larger-amplitude, longer-period synoptic signals lack coherence and periodicity, determination of air permeability in deep unsaturated zones must rely on these longer-period oscillations of barometric pressure whose periods are on the order of weeks to months because the shorter-period diurnal and semidiurnal barometric oscillations generally are not detectable at deep depths.     

Endothelial selectins in acute mountain sickness and high-altitude pulmonary edema

STUDY OBJECTIVES: Mechanical or inflammatory injury to pulmonary endothelial cells may cause impaired pulmonary gas exchange in acute mountain sickness (AMS) and noncardiogenic pulmonary edema in high-altitude pulmonary edema (HAPE). This study was designed to determine whether markers of endothelial cell activation or injury, plasma E- and P-selectin, were increased after ascent to high altitude, in AMS or in HAPE. DESIGN: We collected clinical data and plasma specimens in control subjects at sea level and after ascent to 4,200 m, and in climbers with AMS or HAPE at 4,200 m. Data analysis was performed using standard nonparametric statistical methods, and results reported as mean+/-SD. SETTING: National Park Service medical camp at 4,200 m on Mt. McKinley (Denali), Alaska. PATIENTS: Blood samples and clinical data were collected from 17 healthy climbers at sea level and again after ascent to 4,200 m, and from a different group of 13 climbers with AMS and 8 climbers with HAPE at 4,200 m. Climbers with AMS were divided into normoxic (n=7) and hypoxemic (n=6) groups. MEASUREMENTS AND RESULTS: Using an enzyme immunoassay technique, plasma E-selectin concentrations were found to be increased in the 17 control subjects after ascent to 4,200 m (17.2+/-8.2 ng/mL) as compared to sea level (12.9+/-8.2 ng/mL) (p=0.001). Plasma E-selectin concentrations were also increased in subjects with hypoxemic AMS (30.6+/-13.4 ng/mL) and HAPE (23.3+/-9.1 ng/mL) compared to control subjects at sea level (p=0.009). Increased plasma E-selectin concentration significantly correlated with hypoxemia (p=0.006). Plasma P-selectin concentrations were unchanged after ascent to 4,200 m and in subjects with AMS and HAPE. CONCLUSION: Because E-selectin is produced only by endothelial cells, increased plasma E-selectin after ascent to high altitude and in hypoxemic climbers with AMS and HAPE provides evidence that endothelial cell activation or injury is a component of hypoxic altitude illness.     

Ambulatory blood pressure monitoring in the aged. The EPICARDIAN study. The EPICARDIAN Work Group

OBJECTIVE: To determine reference values for ambulatory blood pressure in a random sample of Spanish elderly population, and their correlations with office blood pressure measurements. METHODS: A representative random sample was obtained, stratified by sex and age, of 1,227 elderly subjects aged > 65 years, residents in an urban district, Barrio de Salamanca, or Madrid, Spain. In a random subsample (n = 420), two different blood pressure measurement approaches were performed: Office blood pressure and twenty-four hour ambulatory blood pressure (spacelabs 90207) were recorded, and two periods were defined: awake and sleeping, on the basis of the daily activities. Hypertension was defined if the average of casual blood pressure was > or = 140/90 mmHg or if there was current use of antihypertensive drugs. RESULTS: Among the 420 participants, 333 ambulatory blood pressure monitorings were performed, 301 with valid registers, of whom 105 were receiving antihypertensive drug treatment. Office, 24 hour, awake and sleeping pressures averaged 147/84 mmHg, 128/72 mmHg, 132/77 mmHg and 122/66 mmHg respectively. Differences between whole sample and no treated group were not significant (p = 0.2), nor between the whole sample and the treated group (p = 0.7). Office blood pressure was markedly higher than 24 hour and awake averages (20 and 15 mmHg for systolic and 12 and 7 mmHg for diastolic, respectively). The differences between clinic and awake average blood pressures were significantly higher in females (p = 0.001) and increased, in both genders, as age (p = 0.001) and clinic blood pressure values (p < 0.000) increased. Correlation coefficients between office and the average awake period of the ambulatory blood pressures were of 0.60 and 0.48 for systolic and diastolic respectively. The ambulatory blood pressure value equivalent to 140/90 mmHg when obtained by causal measurement, was 15 mmHg lower when considering the 24 h average, or 10 mmHg lower when the awake averages. CONCLUSION: Ambulatory systolic and diastolic blood pressure values in the elderly are markedly lower than office values, specially in the case of systolic blood pressure. Differences in results between the two methods increase with age and with clinic blood pressure values, and are bigger in females. The cut-off point for ambulatory blood pressure monitoring equivalent to 140/90 mmHg in the casual measurement is of 125/75 mmHg for the 24 hour average and of 130/80 mmHg for awake average.     

"Living high-training low": effect of moderate-altitude acclimatization with low-altitude training on performance

The principal objective of this study was to test the hypothesis that acclimatization to moderate altitude (2,500 m) plus training at low altitude (1,250 m), "living high-training low," improves sea-level performance in well-trained runners more than an equivalent sea-level or altitude control. Thirty-nine competitive runners (27 men, 12 women) completed 1) a 2-wk lead-in phase, followed by 2) 4 wk of supervised training at sea level; and 3) 4 wk of field training camp randomized to three groups: "high-low" (n = 13), living at moderate altitude (2,500 m) and training at low altitude (1,250 m); "high-high" (n = 13), living and training at moderate altitude (2,500 m); or "low-low" (n = 13), living and training in a mountain environment at sea level (150 m). A 5,000-m time trial was the primary measure of performance; laboratory outcomes included maximal O2 uptake (VO2 max), anaerobic capacity (accumulated O2 deficit), maximal steady state (MSS; ventilatory threshold), running economy, velocity at VO2 max, and blood compartment volumes. Both altitude groups significantly increased VO2 max (5%) in direct proportion to an increase in red cell mass volume (9%; r = 0.37, P < 0.05), neither of which changed in the control. Five-kilometer time was improved by the field training camp only in the high-low group (13.4 +/- 10 s), in direct proportion to the increase in VO2 max (r = 0.65, P < 0.01). Velocity at VO2 max and MSS also improved only in the high-low group. Four weeks of living high-training low improves sea-level running performance in trained runners due to altitude acclimatization (increase in red cell mass volume and VO2 max) and maintenance of sea-level training velocities, most likely accounting for the increase in velocity at VO2 max and MSS.     

A patient with Wegener''s granulomatosis presenting with a subarachnoid hemorrhage: case report and review of CNS disease associated with Wegener''s granulomatosis

1. Travellers to high altitude often complain of paroxysmal cough, which has not been previously investigated. We recorded overnight cough frequency and cough-receptor sensitivity to inhaled citric acid in a group of climbers travelling to 5300 m or higher. 2. Cough frequency, monitored in ten subjects, increased from a median of 0 coughs at sea level (range 0-1) to 5 coughs at 5000 m (range 0-13) and to over 60 coughs in subjects ascending to 7000 m. Citric acid cough threshold, measured in 42 subjects, was unchanged on arrival at 5300 m compared with sea level (geometric mean difference 1.26, 95% confidence intervals 0.84-1.89, P = 0.25), but was significantly reduced after 6 days, or more, at altitude compared with sea level (geometric mean difference 2.2, 95% confidence intervals 1.54-3.15, P = 0.0002). Cough threshold was not related to symptoms of acute mountain sickness, oxygen saturation, carbon dioxide tension or lung function. 3. These results indicate an increase in cough and cough-receptor sensitivity after some days at altitude. This may be due to respiratory tract damage from breathing cold dry air at increased ventilatory rates. Other explanations, such as sub-clinical pulmonary oedema or an effect on the cough centre of acclimatization to altitude, cannot be excluded.     

A Preliminary Analysis of the Relationship between Precipitation Variation Trends and Altitude in China

Characteristics of the relationship between precipitation variation trends (PVT) and altitude were analyzed using monthly mean precipitation data from 526 observation stations in China from 1961 to 2008. With respect to elevation, China was divided into three subregions, below 200 m, 200-1500 m, and above 1500 m. The results showed that the correlations between annual PVT and altitude are different among the three regions. In the region below 200 m in elevation, the best relationship has a correlation coefficient of-0.19 (0.49), passing the 90%(99.9%) significance level south (north) of 35°N. However, the correlation coefficient is close to zero, and the latitude strongly governs the spatial distribution of the amplitude of annual PVT in the 200-1500-m elevation region. In most of the Tibetan Plateau, where the elevation is greater than 1500 m, there is a weak negative correlation. The Mann-Kendall method was used to test the trend of regional mean annual precipitation, which indicated that the annual mean precipitation had no obvious trend of change in China due to the reverse significant variation trends in different areas of the country.     

Evidence for cell-mediated immunity to collagen in progressive systemic sclerosis

The activities of glucose-6-phosphate dehydrogenase (D-glucose-6-phosphate: NADP oxidoreductase, G6PD), 6-phosphogluconate dehydrogenase (6-phospho-d-gluconate: NADP oxidoreductase, 6PGD), hexokinase (ATP:D-hexose 6-phosphotransferase, HK), lactic dehydrogeanse (L-lactate: NAD oxidoreductase, LDH) and aspirate aminotransferase (L-aspartate: 2-oxoglutarate aminotransferase, Asp.T) were determined in red blood cells of 11 healthy individuals. The determinations were carried out on samples drawn every 4 h over a 24 h period. The activities of G6PD, 6PGD, LDH and Asp.T exhibited a semi-circadian rhythm, namely, two peaks of activity during 24 h while HK activity demonstrated a true circadian rhythm. In addition a polymorphism of the G6PD and LDH activity patterns was observed. The implications of a biological clock in enucleated cells are discussed.     

Validating curriculum-based measurement in reading from a behavioral perspective.

Examined the effects of setting and method accuracy in curriculum-based measurement (CBM). The effects of who administers the assessment (teacher vs school psychologist), the physical location of the assessment (reading group vs teacher's desk vs office outside the classroom), and whether the performance is timed or untimed was examined for oral reading rates of 100 3rd- and 4th-grade students in regular education. 35 students were reading below their average grade level, 31 at average grade level, and 34 above average grade level. Effects of these conditions on the number of words read correctly per minute were examined in 3 separate analyses for each participant group (low, average, and high level readers). Results show significant effects for the reading level, tester, settings, and task demand variables. (PsycINFO Database Record (c) 2010 APA, all rights reserved)     

Changes of cerebral blood flow during short-term exposure to normobaric hypoxia

Decreased arterial partial oxygen pressure (PaO2) below a certain level presents a strong stimulus for increasing cerebral blood flow. Although several field studies examined the time course of global cerebral blood flow (gCBF) changes during hypoxia at high altitude, little was known about the regional differences in the flow pattern. Positron emission tomography (PET) with [(15)O]H2O was used on eight healthy volunteers to assess regional cerebral blood flow (rCBF) during short-term exposure to hypoxia corresponding to simulated altitudes of 3,000 and 4,500 m. Scans at the simulated altitudes were preceded and followed by baseline scans at the altitude of Zurich (450 m, baseline-1 and baseline-2). Each altitude stage lasted 20 minutes. From baseline to 4,500 m, gCBF increased from 34.4 +/- 5.9 to 41.6 +/- 9.0 mL x minute(-1) x 100 g(-1) (mean +/- SD), whereas no significant change was noted at 3,000 m. During baseline-2 the flow values returned to those of baseline-1. Statistical parametric mapping identified the hypothalamus as the only region with excessively increased blood flow at 4,500 m (+32.8% +/- 21.9% relative to baseline-1). The corresponding value for the thalamus, the structure with the second largest increase, was 19.2% +/- 16.3%. Compared with the rest of the brain, an excessive increase of blood flow during acute exposure to hypoxia is found in the hypothalamus. The functional implications are at present unclear. Further studies of this finding should elucidate its meaning and especially focus on a potential association with the symptoms of acute mountain sickness.     

Glucose and maltodextrin in enteral diets have different effects on jejunal absorption of nutrients, sodium and water and on flow rate in mini pigs

BACKGROUND: The effect of altitude on subjects between 8 to 22 and 23 to 51 years, that resided at sea level, or in the highlands, and developed altitude lung edema, is presented in series of 21 prospective registered patients at 4,800 to 5,000 m altitude in the Andes mountains of Ecuador. PATIENTS MATERIAL AND METHODS: The 21 sick patients were evaluated at 2 h and at 8 hr after exposition to the high altitude. They were immediately evacuated from the high altitudes. Clinical and radiological methods were used. The statistical analysis was performed with chi(2) test with Yates correction and relative risk. RESULTS: The younger patients tended to develop illness with a higher frequency (p < 0.01). The place of residence influenced the development of the illness only for the group of persons between the ages of 23 to 51 years (p < 0.03); and also in comparing all of the subjects from the coast with those from the highlands. CONCLUSIONS: A inverse relationship was found between the age and the possibility of the development of altitude pulmonary edema, possibly due t a basic incrementation of the pressure of the pulmonary artery, or because of a relative immaturity of the adaptative mechanisms. The place of residence was significantly associated with a higher frequency of pulmonary edema in persons between the ages of 23 to 51 years.     

Paternal directional mating in two Amerindian subpopulations located at different altitudes in northwestern Argentina

We used mitochondrial DNA (mtDNA) and Y-chromosome DNA polymorphisms to analyze the ethnic origin of maternal and paternal lineages in two Amerindian subpopulations from northwestern Argentina. One of the subpopulations was from San Salvador de Jujuy, located 1200 m above sea level. The second subpopulation inhabits the Quebrada de Humahuaca area at altitudes ranging from 2500 to 3500 m. Both subpopulations have the same ethnic background. All mtDNA haplotypes were identified as Amerindian with a frequency of 64.6% of the B form (9-bp deletion in mtDNA region V). Because all Central Andean Amerindian populations studied so far exhibit high frequencies of the B haplotype, we propose that they probably are derived from a common ancestral population that inhabited the Central Andes 6000-8000 years B.P. The presence of paternal directional mating (asymmetric contribution of one parental lineage to interethnic gene mixtures) was demonstrated by the finding of an average introgression of 40.5% Spanish Y chromosomes into our Amerindian sample. This introgression was more evident at low altitude than at high altitude, with frequencies of 64.3% in San Salvador de Jujuy (low altitude) and 27.6% in Quebrada de Humahuaca (high altitude) (p < 0.05). The San Salvador de Jujuy subpopulation also showed a significantly higher Y-chromosome gene variability than the Quebrada de Humahuaca subpopulation. These findings are in good agreement with historical reports indicating that the colonization of South America was undertaken by men who usually practiced polygamous unions with Amerindian women and that San Salvador de Jujuy was the main northwestern Argentinian region of European to Amerindian gene admixture. We found 16.7% of cases with Spanish Y chromosomes and Amerindian family names, and the same percentage with Amerindian Y chromosomes and Hispanic names. The former group probably is the result of unions between Hispanic men, who transmitted the Y chromosome, and Amerindian women, who transmitted the family name to the progeny. The latter group likely illustrates the practice of changing names from Amerindian to Hispanic during the baptism of native Americans in colonial times.     

Early experience of retrograde cerebral perfusion

Continuous records of arterial blood pressure can be obtained non-invasively with Finapres, even for periods of 24 hours. Increasingly, storage of such records is done digitally, requiring large disc capacities. It is therefore necessary to find methods to store blood pressure waveforms in compressed form. The method of selection of significant points known from ECG data compression is adapted. Points are selected as significant wherever the first derivative of the pressure wave changes sign. As a second stage recursive partitioning is used to select additional points such that the difference between the selected points, linearly interpolated, and the original curve remains below a maximum. This method is tested on finger arterial pressure waveform epochs of 60 s duration taken from 32 patients with a wide range of blood pressures and heart rates. An average compression factor of 4.6 (SD 1.0) is obtained when accepting a maximum difference of 3 mmHg. The root mean squared error is 1 mmHg averaged over the group of patient waveforms. Clinically relevant parameters such as systolic, diastolic and mean pressure are reproduced with an offset error of less than 0.5 (0.3) mmHg and scatter less than 0.6 (0.1) mmHg. It is concluded that a substantial compression factor can be achieved with a simple and computationally fast algorithm and little deterioration in waveform quality and pressure level accuracy.     

Increased 2,3-diphosphoglycerate during normocapnic hypobaric hypoxia

The effect of 96 h of exposure to hypobaric hypoxia with and without 3.8% CO2 supplementation was studied in two groups of subjects. Five subjects (CO2) were exposed to 440-465 mm Hg barometric pressure (4000-4400 m), and 4 subjects (no-CO2) were exposed to 455-492 mm Hg (3500-1400 m) in order to produce similar levels of resting end-tidal PO2. After 24 h, 2,3-DPG levels of both groups significantly increased and remained elevated. The CO2 group had higher levels than the non-CO2 group after 48 and 72 h. Concurrent measurements of P50 showed similar changes over the same time course. Mean corpuscular hemoglobin concentrations remained normal for 48 h and then decreased in both groups, the CO2 group showing the larger decrease. We conclude that altitude exposure may produce an increase in 2,3-DPG without the presence of respiratory alkalosis previously thought necessary.     

The mystery of angiography and the "unawarded" Nobel Prize: Egas Moniz and Hans Christian Jacobaeus

STUDY OBJECTIVES: To compare arterial blood gas (ABG) and pulmonary gas exchange variables (alveolar-arterial oxygen pressure difference [P(A-a)O2] and physiologic dead space to tidal volume ratio [VD/VT]) measured during incremental exercise test (IET) and constant work (CW) exercise at a matched oxygen uptake (VO2). DESIGN: A comparison of IET and CW variables was accomplished using patient data from clinical referrals for cardiopulmonary exercise testing and control data not reported from a previous study. SETTINGS: El Paso, Tex, located at an altitude of 1,270 m (barometric pressure, 656 mm Hg). PARTICIPANTS: Sixteen patients with dyspnea on exertion/exercise intolerance and nine normal subjects were evaluated above the anaerobic threshold (AT); seven patients were also studied below the AT. INTERVENTIONS: Participants had a maximal IET followed in 1 h by a 5-min CW test. Arterial blood samples were obtained from a radial catheter every other minute during IET and during minute 5 of CW. Cardiopulmonary measurements were obtained using an automated system in a breath-by-breath fashion (60-s averaging). RESULTS: Above the AT, no differences were observed in normal subjects between IET and CW at a matched VO2 in the following: PaO2 (79 vs 79 mm Hg); arterial oxygen saturation (SaO2) (94% vs 94%); P(A-a)O2 (16 vs 16 mm Hg); and VD/VT (0.09 vs 0.09) (mean values). Similarly, no differences were observed in patients above the AT in PaO2 (69 vs 68), SaO2 (90 vs 90), and VD/VT (0.24 vs 0.23). PaCO2 was 2 mm Hg higher (36 vs 34) in normal subjects and in patients (34 vs 32) during IET. A significant (p<0.05), albeit clinically unimportant, difference was also observed in P(A-a)O2 (28 vs 29) in patients. No statistically significant differences were observed below the AT between IET and CW for any of the variables measured. CONCLUSIONS: These data demonstrate the reliability of ABG and pulmonary gas exchange variables measured during 1-min IET for clinical use in patients and normal subjects. However, PaCO2 tends to be slightly higher during IET vs CW.     

Iron metabolism during pregnancy at high altitudes

A comparative study of iron metabolism was conducted in pregnant women for three Peruvian localities of different elevations: Lima (sea level), La Oroya (3.700 m) and Puno (3.900 m). As predicted, the survey showed hematocrits and hemoglobin concentration values 20 to 30% higher in the Andean women, but the serum iron concentration was unexpectedly lower in Lima than at the higher localities (49 vs. 85 to 90 ug/dl). These results may be explained by the larger iron content found in the water consumed as well as in the cooking pottery utilized at high altitude.