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Thread: Static Pressure and Pressure Head in Fluids

  1. #1

    Static Pressure and Pressure Head in Fluids

    The pressure indicates the normal force per unit area at a given point acting on a given plane. Since there is no shearing stresses present in a fluid at rest - the pressure in a fluid is independent of direction.
    For fluids - liquids or gases - at rest the pressure gradient in the vertical direction depends only on the specific weight of the fluid.
    How pressure changes with elevation can be expressed as
    dp = - γ dz (1)
    where
    dp = change in pressure
    dz = change in height
    γ = specific weight
    The pressure gradient in vertical direction is negative - the pressure decrease upwards.
    [h=Specific Weight]3[/h] Specific Weight can be expressed as:

    γ = ρ g (2)
    where
    γ = specific weight
    g = acceleration of gravity
    In general the specific weight - γ - is constant for fluids. For gases the specific weight - γ - varies with the elevation.

    [h=Static Pressure in a Fluid]3[/h] For a incompressible fluid - as a liquid - the pressure difference between two elevations can be expressed as:
    p2 - p1 = - γ (z2 - z1) (3)
    where
    p2 = pressure at level 2
    p1 = pressure at level 1
    z2 = level 2
    z1 = level 1
    (3) can be transformed to:
    p1 - p2 = γ (z2 - z1) (4)
    or
    p1 - p2 = γ h (5)
    where
    h = z2 - z1 difference in elevation - the dept down from location z2.
    or
    p1 = γ h + p2 (6)
    [h=Example - Pressure in a Fluid]4[/h] The absoute pressure at water depth of 10 m can be calulated as:

    p1 = γ h + p2
    = (1000 kg/m3) (9.81 m/s2) (10 m) + (101.3 kPa)
    = (98100 kg/ms2 or Pa) + (101300 Pa)
    = 199.4 kPa

    where
    ρ = 1000 kg/m3
    g = 9.81 m/s2
    p2 = pressure at surface level = atmospheric pressure = 101.3 kPa
    The gauge pressure can be calulated setting p2 = 0

    p1 = γ h + p2
    = (1000 kg/m3) (9.81 m/s2) (10 m)

    = 98.1 kPa
    [h=The Pressure Head]3[/h] (6) can be transformed to:
    h = (p2 - p1) / γ (6)
    h express the pressure head - the height of a column of fluid of specific weight - γ - required to give a pressure difference of (p2 - p1).
    [h=Example - Pressure Head]4[/h] A pressure difference of 5 psi (lbf/in2) is equivalent to

    (5 lbf/in2) (12 in/ft) (12 in/ft) / (62.4 lb/ft3)
    = 11.6 ft of water
    (5 lbf/in2) (12 in/ft) (12 in/ft) / (847 lb/ft3)
    = 0.85 ft of mercury
    when specific weight of water is 62.4 (lb/ft3) and specific weight of mercury is 847 (lb/ft3).

    Heads at different velocities are indicated in the table below:

    Velocity
    (ft/sec)
    Head Water
    (ft)
    0.5 0.004
    1.0 0.016
    1.5 0035
    2.0 0.062
    2.5 0.097
    3.0 0.140
    3.5 0.190
    4.0 0.248
    4.5 0.314
    5.0 0.389
    5.5 0.470
    6.0 0.560
    6.5 0.657
    7.0 0.762
    7.5 0.875
    8.0 0.995
    8.5 1.123
    9.0 1.259
    9.5 1.403
    10.0 1.555
    11.0 1.881
    12.0 2.239
    13.0 2.627
    14.0 3.047
    15.0 3.498
    16.0 3.980
    17.0 4.493
    18.0 5.037
    19.0 5.613
    20.0 6.219
    21.0 6.856
    22.0 7.525

    • 1 ft (foot) = 0.3048 m = 12 in = 0.3333 yd

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  3. #2
    [h=Recommended water flow velocity on suction side of pump]2[/h]
    Capacity problem, cavitation and high power consumption in a pump, is often the result of the conditions on the suction side. In general - a rule of thumb - is to keep the suction fluid flow speed below the following values:
    Pipe bore Water
    inches mm m/s ft/s
    1 25 0.5 1.5
    2 50 0.5 1.6
    3 75 0.5 1.7
    4 100 0.55 1.8
    6 150 0.6 2
    8 200 0.75 2.5
    10 250 0.9 3
    12 300 1.4 4.5

    More about NPSH suction problems can be read here:

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  5. #3
    [h=Pump suction head as affected by altitude]2[/h]
    Suction head affected by altitude as:
    Elevation above Sea Level Pressure Practical Suction Lift
    (ft) (m) (psig) (ft H2O) (bar) (ft H2O) (m H2O)
    0* 0* 14.71 33.95 1 22 6.7
    1320 402 14.02 32.38 0.97 21 6.4
    2640 805 13.33 30.79 0.92 20 6.1
    3960 1207 12.66 29.24 0.87 18 5.5
    5280 1609 12.02 27.76 0.83 17 5.2
    6600 2012 11.42 26.38 0.79 16 4.9
    7920 2414 10.88 24.13 0.75 15 4.6
    10560 3219 9.88 22.82 0.68 14 4.3

    * Sea Level

  6. #4
    Thanks for these several posts. Are they fro single source like:

    [link Point to another website Only the registered members can access] or can you pl direct all users to the source sites. That will be more helpful because interests of others can be more than what has been put up by you.
    However thanks again


  7. #5
    Quote Originally Posted by aseptman View Post
    Thanks for these several posts. Are they fro single source like:

    [link Point to another website Only the registered members can access] or can you pl direct all users to the source sites. That will be more helpful because interests of others can be more than what has been put up by you.
    However thanks again

    very thanks aseptman , yes most of this articles from engineeringtoolbox web site but i select the best on it also i will share any interested articles i found while i search internet ans i will referee to it's source site if any one can want to read more

    i think that will be good idea to all of us , to share any interested articles or web site we found while we search for any information on the internet

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