Pressure

Pressure (p) = Force (F)  ÷  area (A)       [N/m² = Pas]


SI-Units

  Pas hPas /
mbar
bar Torr /
mm Hg
mWs mmWs atm at psi
1 Pascal = 1 0,01 1,0000·10-5 0,007501 0,0001020 0,1020 9,8692·10-6 1,0197·10-5 0,0001450
1 Hektopascal =
1 Millibar =
100 1 0,001 0,7501 0,0102 10,1972 0,0009869 0,00102 0,0145
1 bar = 100.000 1.000 1 750,06 10,1972 10.197 0,9869 1,0197 14,5038
1 Torr =
1 mm mercury=
133,32 1,3332 0,001333 1 0,01360 13,5951 0,001316 0,001360 0,01934
1 m water column = 9.806,65 98,0665 0,09807 73,5559 1 1.000 0,09678 0,1 1,4223
1 mm water column = 9,8067 0,09807 9,8067·10-5 0,07356 0,001 1 9,6784·10-5 1,0000·10-4 0,001422
1 physical atmosphere = 101.325 1.013,25 1,0133 760 10,3323 10.332 1 1,0332 14,6960
1 technical atmosphere = 98.067 980,67 0,9807 735,56 10 10.000 0,9678 1 14,2233
1 psi =
pounds per sq inch
6.894,76 68,9476 0,06895 51,7149 0,7031 703,07 0,06805 0,07031 1

 

Measures of pressure compare current pressure with reference pressure.
In pressure measurement engineering the following types of pressure are differentiated. They provide a statement about the relationship of measurement pressure to the reference pressure. Absolute pressure always refers to empty space of the universe  (pressure zero).

Absolute pressure:
– Measured pressure above absolute zero
– Reference, ideal vakuum
– Measurement presure is always greater than reference pressure

Overpressure:
– Measured pressure above the barometric air pressure
– Reference ambient pressure
– Measured pressure always greater than reference pressure

Underpressure:
– Measured pressure below the baromatric air pressure
– Reference ambient pressure
– Measured pressure always lower than reference pressure

Differencial pressure:
– Measured pressure belog or above an arbitrary reference pressure
– Measurement pressure greater or lower reference pressure

Atmospherical pressure:
Atmospherical pressure is the most important pressure for life on earth. It arises due to the weight of the atmosphere that surrounds the earth. The atmosphere reaches up until about 500 km. Up until this heigth (absolute pressure pabs = zero) air pressure decreases constantly. Furthermore the atmospherical air pressure is influenced by weather-related variations. At sea level P amb is on average 1013,25hPa. At high pressure or low pressure conditions it could alternate up until ± 5 %.

Source: SI - Systeme