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Differential Momentum Balance

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Estimation of net rate of momentum out of element ... Stress= force per unit area (=F/A) ... Example1: Drag (Couette) flow between. two parallel plates ... – PowerPoint PPT presentation

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Title: Differential Momentum Balance


1
Differential Momentum Balance
Rate of accumulation of momentum
Sum of forces acting on system
Rate of momentum out
Rate of momentum in
-

(15.6)
  • Estimation of net rate of momentum out of element

z
x
y
  • Estimation of forces acting on the element

2
Reminder Definition of stress
  • Stress force per unit area (F/A)
  • Normal stress acts perpendicular to the surface
    (Fnormal force).

F
F
F
F
A
A
Tensile causes elongation
Compressive causes shrinkage
  • Shear stress acts tangentially to the surface
    (Ftangential force).

F
A
F
3
Forces acting on a differential element (3-D)
P
szz
z
tzx
tzy
txz
x
y
tyz
P
sxx
P
txy
tyx
syy
  • The first subscript indicates the direction of
    the normal to the plane on which the stress acts.
  • The second subscript indicates the direction of
    the stress.

4
Differential Momentum Balance
  • Estimation of forces acting on the element

z
x
y
5
Equations of Motion
  • x-component of momentum equation

(15.7a)
  • y-component of momentum equation

(15.7b)
  • z-component of momentum equation

(15.7c)
6
Stress Deformation relationship
Reminder Newtons law in one direction
  • In general the stresses are linearly related to
    the rates of deformation
  • (shear stress) (viscosity)x(rate of shear
    strain)
  • In Cartesian coordinates, for the 3-D case

(15.8)
7
Navier-Stokes Equations
  • Taking into account the stress-deformation
    relationships (Eq. 15.8) and making the following
    assumptions
  • The fluid has constant density
  • The flow is laminar throughout
  • The fluid is Newtonian
  • we obtain the Navier-Stokes Equations

8
Navier-Stokes Equations
(15.9a)
  • x-component
  • y-component

(15.9b)
  • z-component

(15.9c)
9
Navier-Stokes Equations
In cylindrical (polar) coordinates
(15.10a)
  • r-component

(15.10b)
  • ?-component

10
Navier-Stokes Equations
(15.10c)
  • z-component

11
Solution Procedure
  • Make reasonable simplifying assumptions (i.e.
    steady state, incompressible flow, coordinate
    direction of flow)
  • Write down continuity and momentum (or
    Navier-Stokes) equations and simplify them
    according to the assumptions of Step 1.
  • Integrate the simplified equations.
  • Invoke boundary conditions in order to evaluate
    integration constants obtained in Step 3.
  • No-slip condition
  • Continuity of velocity
  • Continuity of shear stress
  • Solve for pressure and velocity. Derive shear
    stress distributions if desired. Apply numerical
    values.

12
Example1 Drag (Couette) flow between two
parallel plates
  • Consider two flat parallel plates separated by a
    distance b as shown in the figure. The top plate
    moves in the x-direction at a constant speed V,
    while the bottom plate remains stationary. The
    fluid between the plates is assumed
    incompressible. As the top plate moves the fluid
    is dragged along. This type of flow is often
    referred as Couette flow. It has important
    applications in lubrication applications (such as
    rotating journal bearings) and instruments for
    measurement of viscosity.
  • Prove that the velocity profile for this type of
    flow is linear. What is the volumetric flow rate?

13
Sample Worksheet
  • Step 1 State assumptions
  • - Steady-state (all derivatives with respect to
    time 0), incompressible flow (r const.).
  • - Decide on coordinate system, determine
    direction of flow, identify non-zero velocity
    components.
  •  - Inspect for any other reasonable assumptions.
  •  
  • Step 2 Write down continuity (chose from
    15.1-15.5) and Navier-Stokes equations (chose
    from 15.9 or 15.10) for the appropriate
    coordinate system and direction of flow.
  • Then simplify them, according to assumptions of
    Step 1.
  • Step 3 Integrate the simplified Navier-Stokes
    equation.

14
Sample Worksheet
  • Step 4 Identify appropriate boundary conditions.
    Use them to determine the integration constants
    obtained above.
  • Step 5 Obtain velocity profile.
  • Step 6 (If needed) Obtain volumetric flow rate
    by integrating
  • For flow in channels (Wwidth)
  •  
  • - For flow through circular cross-sections
  • Step 7 (If needed) Obtain shear stress
    distributions, chosing the appropriate
    stress-deformation relationship, from eq (15.8)
    and simplifying it.

15
Example 2 Pressure driven (Poiseuille) flow
between parallel plates
  • The figure below shows a fluid of viscosity m
    that flows in the x direction between two
    rectangular plates, whose width is very large in
    the z direction when compared to their separation
    in the y direction. Such a situation could occur
    in a die when a polymer is being extruded at the
    exit into a sheet, which is subsequently cooled
    and solidified. We will determine the
    relationship between the flow rate and the
    pressure drop between the inlet and exit,
    together with several other quantities of
    interest.

16
Example 2 Pressure driven flow between parallel
plates
  • Now solve the following problem
  • A highly viscous fluid having a viscosity of 950
    Pa.s and density of 780 kg/m3 is flowing through
    a rectangular (flat) die having length of 25 cm,
    width of 1.75 m and gap of 1.8 mm. The pressure
    drop for this flow is 55.6 MPa. What is the mass
    flow rate? How much is the shear stress at the
    wall?

17
Summary of some useful results
  • Steady pressure driven, laminar flow between
    fixed parallel plates

W
L
Velocity Profile
where
Volumetric flow rate
18
Summary of some useful results
  • Steady, laminar, Drag (Couette) flow between
    parallel plates

Velocity profile
Volumetric flow rate
19
Summary of some useful results
  • Steady, pressure driven, laminar flow in circular
    tubes

Velocity Profile
where
Volumetric flow rate
20
Summary of some useful results
  • Steady, Pressure driven, Axial, Laminar flow in
    an Annulus

r
Vz
z
Vz
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