This chapter is not relevant to any specific Section from the 2017 CICM Primary Syllabus, because there is no specific entry for "describe the physiology of being sucked out of an airlock". However, Question 10 from the second paper of 2009 specifically asked for "the respiratory physiological responses to altitude". The examiners also wanted a discussion of "the changes in inspired and alveolar oxygen partial pressure with increasing altitude", which allows for some fascinating digressions. So that the reader can avoid these, a brief exam-focused summary follows:
- With altitude:
- Barometric pressure decreases and is ~ 200 mmHg at 10,000m altitude
- Saturated vapour pressure remains stable at 37 ºC (47 mmHg)
- Alveolar PO2 decreases, and is ~ 30 mmHg at 8,000m altitude
- PaCO2 decreases due to hypoxic drive, and is ~ 10mmHg at 8,000m
- The physiological responses to altitude are:
- Minute volume increases due to hypoxic reaspiratory drive, mediated by peripheral chemoreceptors
- Tachycardia and increased cardiac output due to increased sympathetic drive
- There is also a mild blood pressure increase
- Decreased cognitive function
- With profound hypoxia, delirium can develop
- Renal and electrolyte:
- Decreased serum bicarbonate (due to hypcapnia)
- Minute volume remains the same
- Tidal volume may gradually increase due to thoracic remodelling
- Heart rate and stroke volume return to normal values as the haematocrit adapts
- Haematocrit increases over days/weeks, largely due to haemopoiesis and haemoconcentration
Though the term "altitude" of course implies "great height", barometric pressure is a continuum which spans in both directions from the impossibly narrow range of physiologically normal values. In this chapter, some effort will be spent to cover both the highs and the lows, as they are equally interesting. Some discussion of the more practical aspects of this is also discussed in a chapter concerning critical illness due to high altitude. A good single reference for adaptation to low barometric pressure is Martin & Windsor (2009), which would be enough for anybody preparing for CICM exams.
Atmospheric pressure drops with increasing altitude, such that at around 8000m altitude we encounter what is lovingly known as the "death zone" in mountaineering circles, where survival without supplemental oxygen is impossible. If one were to plug a progression of altitude values into a simple formula, a graph like this could be generated, which appears to agree with empirically measured values.
What puts the "death" into "death zone" is, of course, the fall in the concentration of oxygen which occurs with decreasing barometric pressure. To borrow some data from Ortiz-Prado et al (2019), a handy chart can be generated to represent the thin 10km sliver of lowermost troposphere:
The gas mixture at this lowish altitude remains relatively stable in its proportion of partial pressures. In other words, at an altitude of 10,000m where the atmospheric pressure is 200mmHg, oxygen still makes up 21% of the gas mixture, which gives it a partial pressure of 42 mmHg. For this reason, "high altitude" for purposes of medical discussion is defined at about 2,700m above sea level, where the partial pressure of oxygen is 60 mmHg, enough to bring about all those interesting physiological phenomena so beloved by CICM examiners.
Beyond the relatively thin layer of troposphere, the composition of which is recognisable as a human-breathable gas mixture, there is a huge diffuse layer which has a very different composition. Here is a graphic borrowed from mrreid.org which is based on the NASA MSIS-90 atmosphere model:
As one can see, by the time we reach an altitude of 800-900 km, the dominant gases in the mixture are now helium and hydrogen. The physiological implications of breathing this sort of gas mixture will not be discussed here any further, as the barometric pressure at 100km is already 0.0008 mmHg, and therefore resembles interplanetary vacuum for the intents and purposes of respiratory physiology.
With altitude, the temperature of the gas mixture also changes, plateauing at around -57 ºC from around 40,000m onwards. Fortunately, the human upper respiratory tract has excellent efficiency as a heater and humidifier, which means that even at such temperatures the gas mixture reaching the lungs would be heated to body temperature and maximally humidified. Thus, the saturated vapour pressure of water remains a constant 47 mmHg, at least until you hit the Armstrong limit.
This is a problem, as the constant partial pressure of water vapour reduces the potential space for oxygen in the gas mixture. The other gas in the alveolar mixture is CO2, which fortunately does not stay at sea level values, mainly because hypoxia produces vigorous hyperventilation. Healthy young anaesthetists at the summit of Everest had PaCO2 values of around 10-15 mmHg as the result of this.
So, what are the implications of this for alveolar oxygen? If one were to plot the results of the alveolar gas equation, estimating a relatively linear progression of CO2 decrease (down to a minimum of 10 mmHg) it would look like this:
In summary, without supplemental oxygen, the alveolar oxygen content would be zero by about 15,000m altitude (at a total atmospheric pressure of around 86 mmHg). At the summit of Everest, the aforementioned splendid examples of courage were able to survive with a PaO2 of around 30 mmHg on average (an arterial pO2 of ~ 25 mmHg, giving peripheral sats in a range of 34-69%), mainly because they were fit, healthy, and preceded their ascent with a period of acclimatisation.
At risk of trespassing out of respiratory territory and into cardiovascular, the following acute changes occur with a sudden exposure to hypobaric pressure:
|Altitude||TUC (normal ascent)||TUC (rapid decompression)|
|5,500 m||20 to 30 minutes||10 to 15 minutes|
|6,700 m||10 minutes||5 minutes|
|7,600 m||3 to 5 minutes||1.5 to 3.5 minutes|
|8,550 m||2.5 to 3 minutes||1.25 to 1.5 minutes|
|9,150 m||1 to 2 minutes||30 to 60 seconds|
|10,650 m||30 secs to 1 minute||15 to 30 seconds|
|12,200 m||15 to 20 seconds||7 to 10 seconds|
|13,100 m||9 to 12 seconds||5 seconds|
|15,250 m||9 to 12 seconds||5 seconds|
Fluid balance and haematological changes:
Unfortunately, in some circumstances, there may be no time to undergo physiological adaptation in any meaningful sense, as hypobaric conditions may arrive suddenly. If this happens and you happen to have a ready supply of 100% oxygen, ongoing (unhappy) survival can be assured at minimum barometric pressures of around 190 mmHg, which corresponds to an altitude of about 10,000m.
To go higher than that for any extended period of time would require the use of a pressurised suit. Harry Armstrong, after whom the Armstrong Limit is named, described the upper limits of even short-term survival as being around the territory of 18,000-19,000m above sea level, where the boiling point of water at that pressure (47 mmHg) falls below the temperature of the human body fluids. The partial pressure of atmospheric oxygen at this altitude is so low that total anoxia should be assumed, and the conditions are assumed to be rapidly lethal.
At this stage, and beyond, survival is unlikely unless urgent repressurisation takes place. As if anoxia were not enough, as pressure drops even more disturbing phenomena take place. For instance, as blood in arteries and veins is relatively pressurised in comparison to the external environment, it is not expected to boil at the Armstrong limit, but in complete vacuum that is exactly what might happen. In the soft tissues, the extracellular fluid evaporates, creating painful pockets of vapour ("ebullism"); in the intravascular volume the evolution of bubbles produces "vapour lock" of the cardiac chambers, producing a cessation of circulation within 10-15 seconds. As the intrathoracic air content expands, the pressure on mediastinal structures also produces a profound vagal bradycardia."Some degree of consciousness will probably be retained for 9 to 11 seconds", the Bioastronautics Data Book helpfully remarks. Presumably, it would be acceptable to perform compression-only CPR in this scenario. In short, the immediate consequences of explosive decompression are:
Most of these data are derived from cruel animal experiments performed by well-meaning villains such as Bancroft & Dunn (1965). "A generalized muscle spasticity, a few gasps, momentary convulsive seizures, apnea, and gross swelling of the body and extremities" were reported; in spite of these phenomena all dogs exposed for less than 120 seconds survived, albeit usually with some neurological sequelae (eg. blindness).
Human experience of sudden vacuum exposure seems to be thankfully limited; or at least, most of the time the subject is in no position to be rescued and studied. One often-quoted case is described by Emanuel Roth (1968). A vacuum chamber technician was the victim. At an equivalent altitude of around 40,000m, "the subject decompressed his pressure suit in a vacuum chamber by disrupting a connection on his chamber umbilical hose", the narrative went.
"The subject lost consciousness in 12 to 15 seconds after decompression. Clonic and tonic movements of the feet were noted. After only 20 seconds in a vacuum, the suit was recompressed to 3.7 psia. Within a period of 27 seconds the chamber was at 6 psia. He regained consciousness at this time. There was no recollection of chest or abdominal pain in the accident report."
Extraterrestrial cases of accidental suit failure are poorly reported. An event often quoted as "Landis, G.A. Personal communication, 1999" records the recollection of the astronaut Gregory Bennett, which was apparently reported via a post he had made on the sci.space Usenet group:
"Incidentally, we have had one experience with a suit puncture on the Shuttle flights. On STS-37, during one of my flight experiments, the palm restraint in one of the astronaut’s gloves came loose and migrated until it punched a hole in the pressure bladder between his thumb and forefinger. It was not an explosive decompression, just a little 1/8 inch hole, but it was exciting down here in the swamp because it was the first injury we’ve ever had from a suit incident. Amazingly, the astronaut in question didn’t even know the puncture had occurred; he was so hopped on adrenaline it wasn’t until after he got back in that he even noticed there was a painful red mark on his hand. He figured his glove was chafing and didn’t worry about it…. What happened: when the metal bar punctured the glove, the skin of the astronaut’s hand partially sealed the opening. He bled into space, and at the same time his coagulating blood sealed the opening enough that the bar was retained inside the hole."
Any list of poorly reported space accidents must also mention the Soyuz 11 catastrophe, where the return capsule depressurised on reentry, killing the three crew members inside. Georgy Dobrovolskiy, Vladislav Volkov and Viktor Patsaev died as the consequence of what appears to be a valve leak. Communication was lost shortly after the capsule undocked from the space station, and communication was lost with the crew, who were found lifeless upon their descent. It appeared that at an altitude of approximately 168 km, the cabin depressurised to a barometric pressure of 0 mmHg over approximately 100 seconds. An inspection of the ship's interior revealed that the shoulder straps of all the cosmonauts were unfastened, and the commander was tangled in his straps. Telemetery recording of these final moments observed that the respiratory rate of the crew increased to 40-50 in the four seconds following seal failure; death occurred after 48-49 seconds. Onboard voice tapes reveal that the crew were able to identify the source of the leak within a few seconds, but the remaining TUC was too short.
The discussion of atmospheric and alveolar gas in free-range humans are far less informed, because there are more heights on earth than depths, and the depths are less thoroughly plumbed. Tan et al (2008), on trying to create some sort of overview for this topic, found themselves without anything to overview:
"the authors emphasise that detailed pressure and density measurements within deep mines could not be found in the literature despite an intensive search, and probably do not exist".
However, the change in temperature with depth is known - on average, for every kilometre of crust, the mineshaft heats up by 10-25 ºC. The deepest mine (currently, the Mponeng gold mine) has a rockface temperature of 66 ºC, and management ends up having to pump thousands of litres of ice slurry down there purely as a means of keeping the miners alive. Unfortunately, nobody seems to care about those miners' alveolar gas content (or their lives in general), and sexy British anaesthetists have never descended into that shaft with an ABG machine, so we have no direct data to inform our discussion. Using the same formulae as above, it is possible to construct some intelligent speculations regarding atmospheric pressure, at least:
Thus, theoretically at least, at the bottom of a mine shaft which penetrates 10km into the Earth's crust, you would be enjoying an atmospheric pressure of 2200 mmHg (2.8 atm), with an atmospheric PO2 of 466mmHg on room air. So; would you be ...healthier... down there? Unlikely, given that the temperature would be around 150 ºC. But, let's consider a more plausible scenario, where hyperbaric conditions are experienced occupationally or therapeutically, i.e. with conditions made as pleasant and survivable as possible.
The most commonly encountered hyperbaric situation in CICM past papers is hyperbaric oxygen and this is discussed in some detail elsewhere. The effects and complications of high oxygen concentrations are described best in the chapter on the pharmacology of oxygen. To summarise here:
If the inspired fraction of oxygen remains unchanged, raised barometric pressure still has undesirable effects, except now the nitrogen becomes harmful. A classic example of this is nitrogen narcosis, which manifests as "certain changes in personality and performance in men subjected to increased pressures of air" It is mainly seen in deep divers breathing compressed nitrogen/oxygen mixtures. Though most authors report "proper" party-level narcotic effects at 10-15 atmospheres of pressure (Pastena et al, 2005, and Thomas et al, 1976), there is clearly some psychomotor slowing even at 3 atmospheres of air pressure (Kiessling & Maag, 1962). Hyperbaric nitrogen toxicity manifests as:
So, with seizures on oxygen and delirium on nitrogen, a trend seems to emerge which might suggest that hyperbaric gases cause neurological complications. D'Agostino et al (2009) evolved this concept further in a discussion of hyperbaric gas effects on nervous system function, which can be summarised effectively by borrowing one of their concluding statements:
"The neurological consequences of breathing hyperbaric gases are directly related to the gas' partial pressure, lipid solubility, and capacity to alter the physicochemical properties of adjoining membrane nanostructures through oxidation and mechanical perturbation"
Following from this, one might surmise that gases which have low lipid solubility would be well tolerated under high pressures. This is probably true; helium has the lowest solubility in lipid membranes compared with other gases, and truly insane pressures of helium can be tolerated with apparently little physiological effect.
Enough of the effects of gases, what about the pressure itself? Dean & D'Agostino also have an excellent chapter on this topic in Neuman & Thom's Physiology and Medicine of Hyperbaric Oxygen Therapy which is somehow available online. In short, the effects of pressure itself are as far-reaching as one might expect from something which governs the very properties of matter and the rate of chemical reactions which maintain life. At any given constant temperature, the equilibrium constant of all chemical relationships is affected by the pressure variable, causing reactions to go faster or slower. Indeed, deep-sea organisms which live at extreme pressures (eg. 1100 atmospheres, at the bottom of the Challenger Deep) have had to make major molecular modifications to their enzymes and lipid bilayers in order to function (Macdonald, 1997). For example, the tidepool snailfish Liparis florae has a version of lactate dehydrogenase which functions optimally at a pressure of around 60 MPa, where the LDH of surface-dwellers suffers from a greatly decreased activity (Gerringer et al, 2017).
So, what is the uppermost limit of pressure for the sustained survival of complex organisms? Pradillon & Gaill have an excellent article outlining the challenges of survival at great depth. Under high pressure, delicate protein structures tend to unfold and denature. Deep sea fish have met the need to keep proteins stable under pressure by producing copious amounts of trimethylamine oxide (TMAO), but this is something limited by hyperosomolarity: it is an "idiogenic osmole", and beyond a certain intracellular concentration of this substance, intracellular osmolarity would increase to the point where much ATP would be used to pump water out of the cells. Given the extreme scarcity of metabolic substrate down in the oceanic trenches, this is unlikely to be viewed as a satisfactory solution by the locals. As the result of this, there may be a real biochemical constraint to the survival of vertebrates under extreme pressure, which Yancy et al (2014) put at 8400m, or approximately 840 atmospheres of pressure. That's fragile vertebrates, mind you. Supergiant amphipods look quite healthy as they scurry around in the Mariana Trench, and we have no clear idea as to how much deeper they could get.
What about life in general? There are solid chemical limits to what can be expected from unmodified carbon-based molecules under great pressure. Elo et al (2000) determined that the tertiary strurure of proteins begins to self-dismantle at a pressure of around 5000 atmospheres. At around the same pressure, the DNA strand loses its helical properties. Ultimately, at 15,000 atmospheres, the primary structure of proteins unravels, and they disintegrate into individual amino acids. In case anybody is interested, that's probably the pressure range one encounters under the lowermost cloud layer of Jupiter.
One might at this stage point out that human beings are in fact adapted to life at sea level, and the discussion of Hadal crustaceans and gas giants is probably pointless to anyone who might be mainly interested in human physiology. What, then, is the limit of human survival at high pressure? The exact number is unknown, as to test it would require the nonsurvival of some of the subjects. We do know however that trained professionals can tolerate extreme pressure for short periods safely. The current record is held by Theo Mavrostomos, who spent about 7 hours at a pressure of 70 atmospheres, equivalent to a depth of 701 metres. He was pressurised over about 18 days, and depressurised over 24 days (Gardette et al, 1992). The gas mixture he was breathing consisted of 99.5% helium and hydrogen in approximately 2:1 fractions. There was only 0.5% oxygen, to maintain a PAO2 of less than 200 mmHg. No complex biochemical monitoring was undertaken, but the following signs and symptoms were observed, attributed mainly to the pressure effects themselves rather than to helium:
Physiological effects of such massively increased barometric pressure include:
So, 70 atmospheres is the record, and humans have gone no deeper. However, at even higher pressures, on the basis of animal studies, it is theorised that even helium will have a neurotoxic effect. It is not the fault of helium, which is inert as inert can be, but rather the effect of the pressure itself, exerted by aforementioned mechanisms of changing lipid membrane properties and chemical reaction rates. This was elegantly demonstrated by Brauer et al (1982). Rats exposed to helium at pressures in excess of 200 atmospheres were observed to develop incoordination followed by seizures; rats breathing a perfluorocarbon liquid mixture at a similar pressure developed exactly the same clinical features, suggesting that hydrostatic pressure itself was to blame. This probably represents some sort of maximum for multicellular organisms adapted to Earth surface pressures.
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