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2012-10-16 00:00:00
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Basic theory of compressed air
Basic theory of compressed air
Compression and compression ratio
1 , the compression
Is an adiabatic compression of the gas in the compression process does not produce significant heat of compression process incoming or outgoing . In a cylinder of a fully insulated above process can be a reality . Isothermal compression is a compression process in the gas compression process to keep the temperature constant .
2, the compression ratio : (R)
Compression ratio refers to the compressor discharge and intake of the ratio of the absolute pressure . Example: In the inlet absolute pressure at sea level is 0.1 MPa, the exhaust pressure is absolute pressure 0. 8MPa. The compression ratio:
P2 0.8
R = - = - = 8
P1 0.1
Multi-stage compression advantages:
( 1 ) , save the compression work ;
( 2 ) reduce the exhaust gas temperature ;
( 3 ) , to improve the capacity coefficient ;
( 4 ) , the piston compressors , reduce the gas thrust on the piston .
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Compression media
Why use compressed air to make the media ?
Because air is compressible , clear and transparent, and easy to transport ( non-condensing ) , harmless , safe and inexhaustible .
Inert gas is a function of the inert gas environment , the standard compressor can be the same compressed inert gases. Dry nitrogen and carbon dioxide are inert gases.
Air properties:
Dry air components : nitrogen (N2) oxygen (O2) Carbon dioxide (CO2)
20.93% 0.03% 78.03%
Weight: 28.96
Weighting : In 0 ℃, 760mmHg column when , r0 = 1.2931kg/m3
Specific heat: at 25 ℃, 1 atm , Cp = 0.241 Kcal / kg-℃
At t ℃, pressure of H (mmhg) , the air gravity:
273 H
rt = 1.2931 × - × -kg/m3
273 + t 760
The proportion of wet air should also be considered saturated water vapor partial pressure (0.378ψ, Pb).
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Pressure
1, the pressure
This is a force per unit area , such as the square on the intensity of the pressure by one unit of 1 Newton Pascal :
Namely : 1Pa = 1N/m2
1Kpa = 1,000 Pa = 0.01 kg/cm2
1Mpa = 106Pa = 10 kg / cm2
2 , absolute pressure
Absolute pressure is taken into account with full vacuum or absolute zero compared to our live ambient atmosphere absolute pressure with 0.1Mpa . At sea level , gauge pressure plus atmospheric pressure of 0.1MPa absolute pressure can be drawn . The higher the altitude the lower the atmospheric pressure .
3 , the atmospheric pressure
Barometer is used to measure atmospheric pressure. When coupled with the pressure on the instrument can come to absolute pressure .
Absolute pressure = gauge pressure + atmospheric pressure
Atmospheric pressure mercury MM usually as a unit, but any one can make the same pressure unit good explanation :
A physical atmospheric pressure = 760 mm Hg = 10.33 m water column = 1.033kgf/cm2 ≌ 0.1MPa.
Atmospheric pressure with altitude relation:
H
P = P0 × (1 -) 5.256 mmHg
44300
H - altitude ,
P0 = atmospheric pressure (0 ℃, 760mmHg)
4, the pressure unit conversion :
Unit : MPa, Psi (bf/in2)
1Psi = 0.006895MPa,
1bar = 0.1MPa,
1kgf/cm2 = 98.066KPa = 0.098066MPa ≌ 0.1Mpa