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How many millimeter mercury in 1 atmosphere?
The answer is 759.99996673177.
We assume you are converting between and atmosphere [standard].
You can view more details on each measurement unit:
millimeter mercury or atmosphere
The SI derived unit for pressure is the pascal.
1 pascal is equal to 0.0075006157584566 millimeter mercury, or 9.8692316931427E-6 atmosphere.
Note that rounding errors may occur, so always check the results.
Use this page to learn how to convert between millimeters mercury and atmospheres.
Type in your own numbers in the form to convert the units!
1 millimeter mercury to atmosphere = 0.00132 atmosphere
10 millimeter mercury to atmosphere = 0.01316 atmosphere
50 millimeter mercury to atmosphere = 0.06579 atmosphere
100 millimeter mercury to atmosphere = 0.13158 atmosphere
200 millimeter mercury to atmosphere = 0.26316 atmosphere
500 millimeter mercury to atmosphere = 0.65789 atmosphere
1000 millimeter mercury to atmosphere = 1.31579 atmosphere
You can do the reverse unit conversion from atmosphere to millimeter mercury, or enter any two units below:
millimeter mercury to decibar
millimeter mercury to pieze
millimeter mercury to exapascal
millimeter mercury to ton/square meter
millimeter mercury to foot of air
millimeter mercury to dyne/square centimeter
millimeter mercury to foot of mercury
millimeter mercury to centitorr
millimeter mercury to kip/square foot
millimeter mercury to sthene/square meter
The millimeter of mercury by definition is 133.322387415 Pa (13.5951 g/cm3 × 9.80665 m/s2 × 1 mm), which is approximated with known accuracies of density of mercury and standard gravity.
The torr is defined as 1/760 of one standard atmosphere, while the atmosphere is defined as 101325 pascals. Therefore, 1 Torr is equal to
101325/760 Pa. The decimal form of this fraction is approximately 133.322368421.
The relationship between the torr and the millimeter of mercury is:
1 Torr = 0.999999857533699 mmHg
1 mmHg = 1.000000142466321 Torr
The difference between one millimeter of mercury and one torr, as well as between one atmosphere (101.325 kPa) and 760 mmHg (101.3250144354 kPa), is less than one part in seven million (or less than 0.000015%). This small difference is negligible for most applications outside metrology.
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