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    Conversion of pressure units

    Name of unit Unit Conversion

    Pascal Pa 1 Pa = 1 N/m2

    Bar bar 1 bar = 0.1 MPa

    Water column metre mH20 1mH20 = 9806.65 PaAtmospheric pressure atm 1 atm = 101325 Pa

    Mercury column metre mHg 1 mHg = 1/0.76atm

    Torr torr 1 torr = 1 mmHg

    The Fundamental Equation of hydrostatics

    We assume the following hypothesis:

    the liquid is incompressible

    the liquid is a gravitational field, thereforeIn general, in a fluid at rest the pressure varies according to the depth. Consider a minute

    column in the fluid as shown in Fig. 3.4. Assume that the sectional area is dA and the pressure

    acting upward on the bottom surface is p and the pressure acting downward on the upper surface(dz above the bottom surface) is p + (dp/dz)dz. Then, from the balance of forces acting on the

    column, the following equation is obtained:

    p dA-(p+ (dp/dz)dA-gdAdz=0

    ordp/ dz = -g=- (1)

    Since is constant for liquid, the following equation ensues:

    p = - dz = -z + c

    When the base point is set at zo below the upper surface of liquid as shown in upper fig.,and p0 is the pressure acting on that surface, then p = po when z = zo, so

    c = po + z (2)Substituting this equation into eqn (2),

    p = p0 + (zo - z) = po + h (3)

    (The fundamental equation of Hydrostatics in a gravitational field)

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    This equation is valid if Oxy water surface.

    The extra pressure po is in most civil engineering cases the atmospheric pressure (pa)

    which in its turn (see last lecture) is totally transmitted to all points of liquid. Therefore, in thesecases, the fundamental equations of Hydrostatics becomes

    zp (also called relative pressure)

    Geometric interpretation of hydrostatic pressure

    Using the form 0pzp one gets

    0p

    zp

    which has a geometric meaning, all the terms having an interpretation of height

    p- absolute height

    zrelative height

    0p

    .supplementary height

    With this, the equation can be geometrically represented as follows:

    Case 1: free water surface and atmospheric pressure

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    Case 2: closed vessels

    (p0>pa) (p0

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    1. Differential manometer.

    In the case of measuring the pressure difference between two pipes in both of which a

    liquid of density flows, a differential manometer as shown:

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    To measure a minute pressure, a glass tube inclined at an appropriate angle as shown in

    Fig. 3.9 is used as an inclined manometer. When the angle of inclination is and the movementof the liquid surface level is L, the differential pressure H is as shown in the following equation:

    H = Lsin

    Accordingly, if is made smaller, the reading of the pressure is magnified.

    1.2. Hydrostatic forces (h.f)

    Hydrostatic forces are the resultant forces of the distribute pressure on a liquid surface. Theydepend on the surface geometry and its orientation in the space.

    1.2.1. H.p. on plane horizontal surface

    By definition we have:

    dAhdApdF

    )( )( )( A A A

    ApAhdAhpdAdFF ,

    which is the traditional meaning of force-pressure relationship.

    The direction ofFis the direction ofp (vertical). To define C(application point ofF), we take

    Varignons theorem:

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    A A

    e dAhydFyFy)(

    '''

    From which:

    and Cis also called centru de carena

    1.2.2. Hydrostatics forces on plane vertical surfaces

    )(''

    AGyAhdAyh

    Gy yAS '' Theorem of static moments

    GG

    c yF

    yAhy '

    ''

    Similarly: GC xx ''

    GC

    AzSGy

    )(

    )(

    A

    GG

    A A

    ApAzzdA

    zdAdFF

    pdAdF

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    Using Varignons theorem:

    1.2.3. H.f. on plane inclined surfaces

    z=zsin for any point

    )( )( )(

    22

    A A A

    C dAzdAzdFzFz

    Iy

    G

    Gy

    y

    y

    y

    y

    CzA

    zAI

    S

    I

    S

    Iz

    2

    0

    G

    G

    yz

    zA

    I 0

    >0

    CGzz

    Cover Calways

    )(

    )( )( )(

    'sin'sin

    sin'

    A

    GG

    A A A

    ApAzdAz

    dAzzdAdFF

    dApdF

    AzS Gy ''

    But: yc

    Iz

    '

    '' (similar to above)

    and then: sin'cc zz