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Biomedical subjects

J T Florio

Publications and source records attributed to J T Florio.

8 recordsLinked to original sources

U.K. deep diving trials.

Using a breathing medium of 40 kPa oxygen, remainder helium, 18 volunteer subjects participated in a series of 15 exposures to pressures equivalent to depths of 180-540 m s.w. The time of exposure at these pressures was mostly 2 days, except for the 540 m s.w. exposure, when 6 days were spent at full pressure. Compression procedures, based upon placing 'stages' at 60 m s.w. intervals, evolved with experience and proved to be a highly successful way of achieving acceptable pressure-time courses. Decompression combined slow linear release of pressure with overnight halts for sleep. On one occasion a depth of 660 m s.w. was reached by breathing 40 kPa oxygen, 10% nitrogen, remainder helium. Throughout all exposures, teams of investigators followed the changes in cardiovascular, respiratory, haematological, neurophysiological and metabolic status, and mental performance of the volunteers. Some major findings were that the neurophysiological and behavioural changes could be assigned to the motor, or vestibular, or cerebral, or autonomic systems, and were mainly first observed during compression. The subjects suffered, apparently from severe nitrogen narcosis, when breathing 10% (by volume) nitrogen in oxygen-helium at 420 m s.w. Lung ventilation was remarkably adaptable to the oxygen requirements of exercise at all depths, but cardiac output was adversely affected at 540 m s.w., particularly for heavier workloads. Ventilatory responses to carbon dioxide were significantly elevated after diving. Thermal balance was seen to be precarious, but nevertheless it was achieved by the normal subjective assessments of comfort. Water loss was affected by diminished evaporation from the skin. Skin temperature sensitivity was changed and took many days after the dives to return to normal. Energy requirements increased for work purposes, but basal metabolic rate was undisturbed. Body chemistry altered at pressures in excess of 300 m s.w., for example thyroid hormone and nitrogen balances were affected. No decompression sickness was encountered until the pressures were low, but marked haematological changes could occur during decompression. Every change that occurred during these dives reverted to normal, mostly before the end of the decompression. It is concluded that diving with oxygen-helium breathing mixtures to depths as great as 540 m s.w. can be effective and safe. An attempt is made to assess the physiological significance of the principal findings.

Adult↗

Respiratory heat transfer in cold water and during rewarming.

Respiratory heat loss was measured during cold water (5-6 degrees C) excursions to depths of 300 m. Losses were computed with and without respiratory gas heating when wearing a diving helmet in current commercial and Service use. A magnitude of heat loss, sufficient to cause undue stress to the respiratory tract, was observed even with gas heating provided, particularly at maximum depth. If the hyperbaric gas is both heated and humidified to a maximum comfort level then respiratory gains in the order of 40 W are possible at 250 m. This technique of utilizing warm wet gas introduced into the respiratory tract was tested as a rewarming technique following immersion in cold water (4-5 degrees C) to the limit of peripheral endurance.

Body Temperature Regulation↗

Effects of CO2 insensitivity and respiratory pattern on respiration in divers.

In a study of respiratory function under hyperbaric conditions one diver (TM) was found to have an extremely low ventilatory response to exercise with a postinspiratory pause typical of certain "carbon dioxide retaining divers." The respiratory function of diver TM is compared with that of four other divers having a normal ventilatory response. In exercise at 4 ATA hypoventilation and hypercapnia were potentiated to a greater extent in TM than in the other divers. Diver TM maintained a ventilation 25%-50% lower than that of the other divers and whereas their end-tidal Pco2 remained within reasonable limits (Pco2 less than or equal to 55 mmHg), that of TM rose to levels considered hazardous (Pco2 less than or equal to 76 mmHg). Results suggest that when a diver exhibits a postinspiratory pause in the breathing cycle, mixing of alveolar and dead space gas takes place. As a result, physiological dead space calculated according to the Bohr formula is unusually small. As alveolar Pco2 will rise during postinspiratory pause, mean arterial Pco2 may be lower than end-tidal Pco2. Such a respiratory pattern has a greater ventilatory efficiency than normal and may afford the diver some protection, albeit incomplete, from hypercapnia.

Atmospheric Pressure↗

Breathing pattern and ventilatory response to carbon dioxide in divers.

The breathing pattern and ventilatory response to carbon dioxide of 10 experienced divers was compared with that of 10 nondivers of similar age and build. Breathing pattern was described by the equation VE = M (VT - K) and the response to carbon dioxide by VE = S(PCO2 - B). The divers exhibited a value form 27% lower than the nondivers; S was 33% lower. The difference was significant (P less than 0.05) in both cases. B was significantly higher (P less than 0.05) in the divers than nondivers. These differences are not attributable to age, build, or vital capacity. S was well correlated with M when all subjects were considered a single group. Within the diving group no correlation of S and M with diving experience was found.

Adaptation, Physiological↗

Observations after loss of consciousness under water.

Two diving incidents were investigated in which 1) an experienced professional diver (A) lost consciousness during an air dive to 69 meters, and 2) an amateur sports diver (D) lost consciousness during a 40-meter air dive. In subsequent tests both divers' ventilatory responses to inspired carbon dioxide were found to be extremely low. Under simulated diving conditions, Divers A and D exhibited marked carbon dioxide retention during exercise at 30 meters (end-tidal PCO2 = 65 and 57 mmHg, respectively) and at 70 meters, Diver A stopped work in less than 3 min because of severe dizziness. Reduced sensitivity to carbon dioxide, perhaps caused by the interaction of hypercapnia and nitrogen narcosis, is thought to have been partly responsible for these incidents.

Carbon Dioxide↗

Effects of increased O2-N2 pressure and breathing apparatus on respiratory function.

The ventilatory response of four subjects was measured at rest and various intensities of exercise. Experiments were conducted in a dry pressure chamber (1) at 1 ATA and 4 ATA with the subjects breathing from a low-resistance mouthpiece, and (2) at ATA with the subjects breathing from open-circuit breathing apparatus (Royal Naval Swimmers' Air Breathing Apparatus). At 4 ATA there was significant hypoventilation and hypercapnia, together with an increased tidal volume and lower respiratory frequency. The use of the breathing apparatus tended to amplify these changes in ventilatory response. In addition, the extent of hypercapnia at 4 ATA was related to the exercise intensity. When subjects breathed from a low-resistance mouthpiece, oxygen uptake was significantly greater at 4 ATA than at the surface for the same ergometric work load, but when they breathed from the breathing apparatus, the increase in oxygen uptake was not significant in comparison to surface values. At 4 ATA bradycardia was evident at all levels of exercise but was not affected significantly by the presence of the breathing apparatus.

Atmosphere Exposure Chambers↗