Fluid Mechanics Chapter 3 Fluid Statics - PowerPoint PPT Presentation

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Fluid Mechanics Chapter 3 Fluid Statics

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Title: Fluid Mechanics Chapter 3 Fluid Statics


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Fluid Mechanics EM 208
  • Chapter 3
  • Fluid Statics

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Contents
  • The Basic Equation of Fluid Statics
  • The Standard Atmosphere
  • Pressure Variation in a Static Fluid
  • Hydraulic Systems
  • Hydrostatic Force on Submerged Surfaces
  • Buoyancy and Stability
  • Fluids in Rigid-Body Motion (on the Web)
  • Summary and Useful Equations

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The Basic Equation of Fluid Statics
  • The first objective of this chapter is to obtain
    an equation for computing the pressure field in a
    static fluid.
  • We will deduce what we already know from everyday
    experience, that the pressure increases with
    depth.
  • To do this, we apply Newtons second law to a
    differential fluid element of mass dm with sides
    dx, dy, and dz, as shown

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The Basic Equation of Fluid Statics
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The Basic Equation of Fluid Statics
Body Forces
  • two general types of forces maybe applied to a
    fluid
  • body forces
  • and surface forces.
  • The only body force that must be considered in
    most engineering problems is due to gravity

Surface Forces
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The basic equation of Fluid statics
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The basic equation of Fluid statics
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The basic equation of Fluid statics
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The basic equation of Fluid statics
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The basic equation of Fluid statics
  • pressure values must be stated with respect to a
    reference level.
  • If the reference level is a vacuum, pressures are
    termed absolute
  • Most pressure gages indicate a pressure
    differencethe difference between the measured
    pressure and the ambient level (usually
    atmospheric pressure)
  • Pressure levels measured with respect to
    atmospheric pressure are termed gage pressures

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Absolute and gage pressures, showing reference
levels
  • For example, a tire gage might indicate 30 psi
    the absolute pressure would be about 44.7 psi.
  • Absolute pressures must be used in all
    calculations with the ideal gas equation or other
    equations of state

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The Standard Atmosphere
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Pressure Variation in a Static Fluid
  • Above Equation indicates that the pressure
    difference between two points in a static
    incompressible fluid can be determined by
    measuring the elevation difference between the
    two points.
  • Devices used for this purpose are called
    manometers

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Most important equation in Fluid statics
computations
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Step 1 Assign letters to all points
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Step 1 Assign letters to all points
Step 2 Write governing equation for each of two
point set
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Step 1 Assign letters to all points
Step 3 Obtained as follows
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Step 1 Assign letters to all points
Step 4 Solve it all
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Gases
  • The density of gases generally depends on
    pressure and temperature. The ideal gas equation
    of state,
  • and the pressure variation, in a gas whose
    temperature varies linearly with elevation, is
    given by

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TT0-mz for linear variation of Temp with height
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Review of Centroid
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Introduction
  • The earth exerts a gravitational force on each of
    the particles forming a body. These forces can
    be replace by a single equivalent force equal to
    the weight of the body and applied at the center
    of gravity for the body.
  • The centroid of an area is analogous to the
    center of gravity of a body. The concept of the
    first moment of an area is used to locate the
    centroid.
  • Determination of the area of a surface of
    revolution and the volume of a body of revolution
    are accomplished with the Theorems of
    Pappus-Guldinus.

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Center of Gravity of a 2D Body
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Centroids and First Moments of Areas and Lines
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First Moments of Areas and Lines
  • The first moment of an area with respect to a
    line of symmetry is zero.
  • If an area possesses a line of symmetry, its
    centroid lies on that axis
  • The centroid of the area coincides with the
    center of symmetry.

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Centroids of Common Shapes of Areas
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Hydraulic Force on Submerged surfaces
  • We must know Magnitude of Force, Direction of
    Force and Line of Action of Force

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where pc is the absolute pressure in the liquid
at the location of the centroid of area A.
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Our next task is to determine (x, y), the
location of the resultant force
  • Lets first obtain y by recognizing that the
    moment of the resultant force about the x axis
    must be equal to the moment due to the
    distributed pressure force

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Our next task is to determine (x, y), the
location of the resultant force
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Our next task is to determine (x, y), the
location of the resultant force
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Our next task is to determine (x, y), the
location of the resultant force
  • Equation 3.11a is the integral equation for
    computing the location y of the resultant force
  • Eq. 3.11b is a useful algebraic form for
    computing y when we are interested in the
    resultant force on the submerged side of the
    surface
  • Eq. 3.11c is for computing y when we are
    interested in the net force for the case when the
    same p0 acts at the free surface and on the other
    side of the submerged surface

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Similarly we could get the X of the location of
the resultant force
  • Equation 3.11a is the integral equation for
    computing the location y of the resultant force
  • Eq. 3.11b is a useful algebraic form for
    computing y when we are interested in the
    resultant force on the submerged side of the
    surface
  • Eq. 3.11c is for computing y when we are
    interested in the net force for the case when the
    same p0 acts at the free surface and on the other
    side of the submerged surface

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For resultant Force
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For Location of Force
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Using Algebraic equations
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Using Algebraic equations
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Summary
  • We reviewed basic concepts including
  • Deriving basic equation in vector form
  • Applying this equation to determine pressure
    variation in a static fluid
  • Incompressible fluids pressure increases
    uniformly with depth
  • Gases pressure decreases non uniformly with
    elevation
  • We studied gage and absolute pressures
  • Use of manometers and barometers
  • Analysis of fluid force magnitude and location in
    submerged plane and curved surfaces
  • Principle of Buoyancy

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Useful equations
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Useful equations
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