Armstrong line

The Armstrong limit or Armstrong's line is a measure of altitude above which atmospheric pressure is sufficiently low that water boils at the normal temperature of the human body. Exposure to pressure below this limit results in a rapid loss of consciousness, followed by a series of changes to cardiovascular and neurological functions, and eventually death, unless pressure is restored within 60–90 seconds. On Earth, the limit is around above sea level, above which atmospheric air pressure drops below 0.0618 atm (6.3 kPa, 47 mmHg, or about 1 psi). The U.S. Standard Atmospheric model sets the Armstrong limit at an altitude of .

The term is named after United States Air Force General Harry George Armstrong, who was the first to recognize this phenomenon.

Effect on body fluids

At or above the Armstrong limit, exposed body fluids such as saliva, tears, urine, and the liquids wetting the alveoli within the lungs—but not vascular blood (blood within the circulatory system)—will boil away if the subject does not wear a full-body pressure suit. A test subject at the NASA Johnson Space Center accidentally exposed to near vacuum in 1965 "reported that ... his last conscious memory was of the saliva on his tongue beginning to boil."

At the nominal body temperature of , water has a vapour pressure of ; which is to say, at an ambient pressure of , the boiling point of water is . A pressure of 6.3 kPa—the Armstrong limit—is about 1/16 of the standard sea-level atmospheric pressure of . At higher altitudes water vapour from ebullism will add to the decompression bubbles of nitrogen gas and cause the body tissues to swell up, though the tissues and the skin are strong enough not to burst under the internal pressure of vapourised water. Formulas for calculating the standard pressure at a given altitude vary—as do the precise pressures one will actually measure at a given altitude on a given day—but a common formula shows that 6.3 kPa is typically found at an altitude of .

Hypoxia below the Armstrong limit

Well below the Armstrong limit, humans typically require supplemental oxygen in order to avoid hypoxia. For most people, this is typically needed at altitudes above 4,500 m (15,000 ft). Commercial jetliners are required to maintain cabin pressurization at an equivalent effective cabin altitude of not greater than . U.S. regulations on general aviation aircraft (non-airline, non-government flights) require that the minimum required flight crew, but not the passengers, be on supplemental oxygen if the plane spends more than half an hour at an equivalent effective cabin altitude above . The minimum required flight crew must be on supplemental oxygen if the plane spends ''any'' time above an equivalent effective cabin altitude of , and even the passengers must be provided with supplemental oxygen above an equivalent effective cabin altitude of . Skydivers, who are at altitude only briefly before jumping, do not normally exceed .

Historical significance

The Armstrong limit describes the altitude associated with an objective, precisely defined natural phenomenon: the vapor pressure of body-temperature water. In the late 1940s, it represented a new fundamental, hard limit to altitude that went beyond the somewhat subjective observations of human physiology and the timedependent effects of hypoxia experienced at lower altitudes. Pressure suits had long been worn at altitudes well below the Armstrong limit to avoid hypoxia. In 1936, Francis Swain of the Royal Air Force reached flying a Bristol Type 138 while wearing a pressure suit. Two years later Italian military officer Mario Pezzi set an altitude record of , wearing a pressure suit in his Caproni Ca.161bis biplane even though he was well below the altitude at which body-temperature water boils.

A pressure suit is normally required at around for a well conditioned and experienced pilot to safely operate an aircraft in unpressurized cabins. In an unpressurized cockpit at altitudes greater than above sea level, the physiological reaction, even when breathing pure oxygen, is hypoxia—inadequate oxygen level causing confusion and eventual loss of consciousness. Air contains 20.95% oxygen. At , breathing pure oxygen through an unsealed face mask, one is breathing the same partial pressure of oxygen as one would experience with regular air at around above sea level. At higher altitudes, oxygen must be delivered through a sealed mask with increased pressure, to maintain a physiologically adequate partial pressure of oxygen. If the user does not wear a pressure suit or a counter-pressure garment that restricts the movement of their chest, the high-pressure air can cause damage to the lungs.

For modern military aircraft such as the United States' F22 and F35, both of which have operational altitudes of or more, the pilot wears a "counter-pressure garment", which is a gsuit with high-altitude capabilities. In the event the cockpit loses pressure, the oxygen system switches to a positive-pressure mode to deliver above-ambient-pressure oxygen to a specially sealing mask as well as to proportionally inflate the counter-pressure garment. The garment counters the outward expansion of the pilot's chest to prevent pulmonary barotrauma until the pilot can descend to a safe altitude.

See also

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* Effects of high altitude on humans
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References

External links

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* {{cite web, work=The Engineering ToolBox, archive-url=https://web.archive.org/web/20161109044753/http://www.engineeringtoolbox.com/air-altitude-pressure-d_462.html, url=http://www.engineeringtoolbox.com/air-altitude-pressure-d_462.html , title=Air Pressure and Altitude above Sea Level, archive-date=2016-11-09

Atmosphere
Aviation medicine
Altitudes in aviation
Human spaceflight
Human physiology