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On Earth, the limit is around 18–19 km (11–12 mi; 59,000–62,000 ft) above sea level, [ 1 ][ 2 ] 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 63,000 feet (19,202 m). The term is named after United States Air ...
Orders of magnitude (pressure) This is a tabulated listing of the orders of magnitude in relation to pressure expressed in pascals. psi values, prefixed with + and -, denote values relative to Earth's sea level standard atmospheric pressure (psig); otherwise, psia is assumed. Magnitude. Pressure. lbf/in 2 or dB.
U.S. customary. ≈ 0.444 44 psi. The metre (or meter) sea water (msw) is a metric unit of pressure used in underwater diving. It is defined as one tenth of a bar. [1][2] The unit used in the US is the foot sea water (fsw), based on standard gravity and a sea-water density of 64 lb/ft 3. According to the US Navy Diving Manual, one fsw equals 0. ...
Pressure as a function of the height above the sea level. The human body can perform best at sea level, [7] where the atmospheric pressure is 101,325 Pa or 1013.25 millibars (or 1 atm, by definition). The concentration of oxygen (O 2) in sea-level air is 20.9%, so the partial pressure of O 2 (pO 2) is 21.136 kilopascals (158.
Some species can also withstand pressures of 6,000 atmospheres, which is nearly six times the pressure of water in the deepest ocean trench, the Mariana Trench. [25] Tardigrades can survive at altitudes of more than 19,600 feet (6,000 meters) and depths of more than 15,000 feet (4,600 m) below the surface. [71]
A well with 5,000 feet of seawater and 15,000 feet of rock could have an overburden pressures at the bottom as high as 17,220 psi (5000 * 0.444 + 15000 * 1.0). That pressure is reduced at the surface by the weight of oil and gas the riser pipe, but this is only a small percentage of the total.
The onboard systems indicated a depth of 37,800 feet (11,521 m; 6,300 fathoms), [24] but this was later revised to 35,814 feet (10,916 m; 5,969 fathoms). [25] The depth was estimated from a conversion of pressure measured and calculations based on the water density from sea surface to seabed. [23]
Pressure as a function of the height above the sea level. There are two equations for computing pressure as a function of height. The first equation is applicable to the atmospheric layers in which the temperature is assumed to vary with altitude at a non null lapse rate of : = [,, ()] ′, The second equation is applicable to the atmospheric layers in which the temperature is assumed not to ...