Did you mean to convert | meter of air [0 °C] meter of air [15 °C] |
to | millimeter mercury |
How many meter of air [15 °C] in 1 millimeter mercury? The answer is 11.095961907459. We assume you are converting between meter of air [15 °C] and millimeter mercury [0 °C]. You can view more details on each measurement unit: meter of air [15 °C] or millimeter mercury The SI derived unit for pressure is the pascal. 1 pascal is equal to 0.083226546738322 meter of air [15 °C], or 0.0075006157584566 millimeter mercury. Note that rounding errors may occur, so always check the results. Use this page to learn how to convert between meters of air and millimeters mercury. Type in your own numbers in the form to convert the units!
1 meter of air [15 °C] to millimeter mercury = 0.09012 millimeter mercury
10 meter of air [15 °C] to millimeter mercury = 0.90123 millimeter mercury
20 meter of air [15 °C] to millimeter mercury = 1.80246 millimeter mercury
30 meter of air [15 °C] to millimeter mercury = 2.70369 millimeter mercury
40 meter of air [15 °C] to millimeter mercury = 3.60492 millimeter mercury
50 meter of air [15 °C] to millimeter mercury = 4.50614 millimeter mercury
100 meter of air [15 °C] to millimeter mercury = 9.01229 millimeter mercury
200 meter of air [15 °C] to millimeter mercury = 18.02458 millimeter mercury
You can do the reverse unit conversion from millimeter mercury to meter of air [15 °C], or enter any two units below:
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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