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For the standard botanical author abbreviation Torr., see John Torrey. The torr (symbol: Torr) is a non-SI unit of pressure defined as 1⁄760 of a standard atmosphere, chosen to be roughly equal to the fluid pressure exerted by a millimeter of mercury, i.e. a pressure of 1 Torr is approximately equal to 1 mmHg. Note that the symbol is spelled exactly the same as the unit, but the symbol is capitalized, as is customary in metric units derived from names. It was named after Evangelista Torricelli, an Italian physicist and mathematician who discovered the principle of the barometer in 1644.[1]
[edit] HistoryTorricelli attracted considerable attention when he demonstrated the first mercury barometer to the general public. He is credited with giving the first modern explanation of atmospheric pressure. Scientists at the time were familiar with small fluctuations in height that occurred in barometers. When these fluctuations were explained as a manifestation of changes in atmospheric pressure, the science of meteorology was born. Over time, 760 millimeters of mercury (abbreviated mmHg) came to be regarded as the standard atmospheric pressure. In honor of Torricelli, the torr was defined as a unit of pressure equal to one mmHg. In 1954, the definition of the atmosphere was revised by the 10e Conférence Générale des Poids et Mesures (10th CGPM)[2] to the currently accepted definition: one atmosphere is equal to 101,325 pascals. The torr was then re-defined as 1⁄760 of one atmosphere. This was necessary in place of the definition of a torr as 1 mmHg, because the height of mercury changes at different temperatures and gravities. [edit] SI units of pressureThe SI unit of pressure is the pascal (symbol: Pa), defined as one newton per square meter. Other units of pressure are defined in terms of SI units.[3][4] These include:
These four pressure units are used in different settings. For example, the bar is used in meteorology to report atmospheric pressures.[5] The torr, a more convenient unit for low pressures, is used in high-vacuum physics and engineering.
Example reading: 1 Pa = 1 N/m2 = 10−5 bar = 10.197×10−6 at = 9.8692×10−6 atm, etc. [edit] Manometric units of pressureSee also: Pressure measurement#Liquid column Manometric units are units such as millimeters of mercury or centimeters of water that depend on an assumed density of a fluid and an assumed acceleration of gravity. The use of these units is discouraged.[6] Nevertheless, manometric units are used routinely in medicine and physiology, and they continue to be used in areas as diverse as weather reporting and scuba diving. The millimeter of mercury (symbol: mmHg) is defined as the pressure exerted at the base of a column of fluid exactly 1 mm high, when the density of the fluid is exactly 13.5951 g/cm3, at a place where the acceleration of gravity is exactly 9.80665 m/s2.[7] Under most conditions, 1 mmHg is approximately equal to 1 torr. There are several things to notice about this definition:
In practice, of course, measurements are made using local values, which vary little enough at the Earth's surface. These assumptions limit both the validity and the precision of the mmHg as a unit of pressure. According to the UK’s National Physical Laboratory (NPL):
The performance of modern transducers approaches the precision required to distinguish between the torr and the millimeter of mercury. The NPL concludes
[edit] Manometric units in medicine and physiologyIn medicine, the millimetre of mercury (measured with a sphygmomanometer) is the "gold standard" for blood pressure measurement. In physiology, manometric units are used to measure Starling forces. Other applications include:
Manometric results in medicine are sometimes given in torr. This is usually incorrect, since the torr and the millimetre of mercury are not the same thing. Pressures obtained with a manometer (or its transducer equivalent) should be reported in millimetres of mercury. [edit] Conversion factorsThe mmHg is defined as (13.5951 × 9.80665) Pa = 133.322 Pa, which is approximated with known accuracies of density of mercury and gravitational acceleration. The torr is defined as 1/760 of one atmosphere, while the atmosphere is defined as 101.325 kPa. Therefore, one torr is equal to 101325/760 Pa. The decimal form of this fraction (133.322368421...) is, unfortunately for practical use, an infinitely long, periodically repeating decimal, as is its reciprocal. The relationship between the torr and the mmHg is:
The mmHg and the torr differ from one another by less than 2 × 10−7 torr. The difference between one atmosphere (101.325 Pa) and 760 mmHg (101325.0144354 Pa) less than 0.2 μPa/Pa (less than 0.00002%). This small difference is negligible for most applications outside metrology. [edit] Notes
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