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Pressure

2.2 - Atmospheric Pressure

Origin and Variation

  • Atmospheric pressure is caused by the weight of the layer of air acting on Earth’s surface and objects within the atmosphere.
  • It varies with weather and decreases at higher altitude, where the air is thinner.

Mercury Barometer

  • A mercury barometer uses a glass tube about long, initially filled with mercury and inverted into a mercury-filled bowl.
  • Mercury falls to a stable height, leaving a vacuum above the column. Atmospheric pressure on the mercury in the bowl supports the column.
  • The vertical column height measures atmospheric pressure:
  • For , mercury density and :
  • This reading can also be stated as . Torricelli demonstrated support of the mercury column by atmospheric pressure in 1643.

Fortin and Aneroid Barometers

Fortin barometerAneroid barometer
Uses changes in mercury-column heightUses changes in the volume of a partial-vacuum metal box
Almost one metre high; large and difficult to carrySmall and portable
Takes longer to obtain a readingGives a direct reading quickly
Accuracy up to Accuracy up to
Used at meteorological centresSuitable for homes, ships and aeroplanes
  • In an Aneroid barometer, a mechanical system amplifies the small volume change of the metal box and moves a pointer.

Pressure Units and Conversions

UnitUse or relationship
PaSI unit used in science; convert pressure to Pa before substitution into SI formulae
mm HgMedicine, meteorology, aviation and science; blood-pressure readings such as 120/80 use this unit
m HOWater pressure in seas, reservoirs and dams
millibar (mbar)Meteorology;
  • Bakun Dam: Water pressure is .

  • Convert a liquid-column pressure into Pa using , with in metres. Convert Pa back into column height using .

  • Blood-pressure example: With and :

  • Seaside-wall example: For and :
  • The pressure is therefore . Atmospheric pressure is about ; at Mount Kinabalu’s summit it is about .

High Altitude and Outer Space

  • At high altitude, oxygen absorption in the lungs decreases. Effects include faster breathing, increased metabolic rate, loss of appetite, dehydration and difficulty thinking clearly.
  • Mountain climbers: Prepare and train physically, carry equipment to monitor altitude, blood pressure and body temperature, ascend slowly to adapt to pressure changes, and drink water to prevent dehydration.
  • Aircraft: Pressurise the cabin to approximately sea-level pressure, circulate fresh air with adequate oxygen and maintain water intake during long flights.
  • Atmospheric pressure at Mount Kinabalu’s summit is about 60% of sea-level pressure; at commercial-aircraft cruising altitude it is about one quarter.
  • Outer space: Pressure is almost zero. Spacecraft need cabin pressurisation and an oxygen generator; astronauts outside the cabin need pressure suits to balance body pressure.

Extreme Depth below the Sea Surface

  • Water pressure increases with depth. Each additional adds approximately one atmosphere of water pressure. Actual pressure includes atmospheric pressure as well.
  • A diver at experiences about four times normal atmospheric pressure; a submarine at experiences about 25 times surface pressure.
  • Effects: Body tissues absorb excess nitrogen; nitrogen dissolves in blood; thinking becomes unclear. Rapid pressure reduction can form nitrogen bubbles in tissues or blood vessels.
  • Divers: Train for the high-pressure environment, wear a diving suit to reduce heat loss and ascend slowly to prevent nitrogen bubbles forming.
  • Submarines: Use a steel or titanium body with a circular cross section to withstand surrounding pressure. Maintain cabin pressure near sea-level pressure and supply oxygen using tanks or electrolytic generators.

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