SFT 3033
MECHANICS
WEEK 13 : EQUILIBRIUM, ELASTICITY & FLUID
MECHANICS
Dr Anis Diyana Bt Halim
Copyright © 2012 Pearson Education Inc.
Introduction
• Many bodies, such as
bridges, aqueducts, and
ladders, are designed so they
do not accelerate.
• Real materials are not truly
rigid. They are elastic and do
deform to some extent.
• We shall introduce concepts
such as stress and strain to
understand the deformation
of real bodies.
Copyright © 2012 Pearson Education Inc.
Conditions for equilibrium (For extended body)
• First condition: The sum of all
the forces is equal to zero:
Fx = 0 Fy = 0 Fz = 0
• Second condition: The sum of
all torques about any given point
is equal to zero.
Copyright © 2012 Pearson Education Inc.
Center of Mass
• For a collection of particles with masses m1, m2, …..and coordinates (x1, y1, z1),
(x2,y2,z2) the coordinates xcm, ycm and zcm is given by :
Copyright © 2012 Pearson Education Inc.
Center of gravity
• We can treat a body’s
weight as though it all
acts at a single point
—
the center of gravity.
• If we can ignore the
variation of gravity
with altitude, the
center of gravity is the
same as the center of
mass.
Copyright © 2012 Pearson Education Inc.
Calculation : Walking the plank
Copyright © 2012 Pearson Education Inc.
Copyright © 2012 Pearson Education Inc.
Strain, stress, and elastic moduli
• Stretching, squeezing, and twisting a real body causes it to deform,
as shown in Figure below. We shall study the relationship between
forces and the deformations they cause.
• Stress is the force per unit area and strain is the fractional
deformation due to the stress. Elastic modulus is stress divided by
strain.
• The proportionality of stress and strain is called Hooke’s law.
Copyright © 2012 Pearson Education Inc.
Strain, stress, and elastic moduli
• The proportionality of stress and strain is called Hooke’s law.
Copyright © 2012 Pearson Education Inc.
Tensile and compressive stress and strain
• Tensile stress = F /A and tensile strain = l/l0. Compressive
stress and compressive strain are defined in a similar way. (See
Figures 11.13 and 11.14 below.)
• Young’s modulus is tensile stress divided by tensile strain, and is
given by Y = (F/A)(l0/l).
Copyright © 2012 Pearson Education Inc.
Some values of elastic moduli
Copyright © 2012 Pearson Education Inc.
Tensile stress and strain
• In many cases, a body can experience both tensile and
compressive stress at the same time, as shown in figure
below
Copyright © 2012 Pearson Education Inc.
Tensile stress and strain
Copyright © 2012 Pearson Education Inc.
Tensile stress and strain
Copyright © 2012 Pearson Education Inc.
Bulk stress and strain
• Pressure in a fluid is force
per unit area: p = F/A.
• Bulk stress is pressure
change p and bulk strain
is fractional volume change
V/V0. (See Figure
11.16.)
• Bulk modulus is bulk stress
divided by bulk strain and is
given by B =
–p/(V/V0).
Copyright © 2012 Pearson Education Inc.
Sheer stress and strain
• Sheer stress is F||/A and
sheer strain is x/h, as
shown in Figure 11.17.
• Sheer modulus is sheer
stress divided by sheer
strain, and is given by
S = (F||/A)(h/x).
Copyright © 2012 Pearson Education Inc.
Sheer stress and strain
Copyright © 2012 Pearson Education Inc.
Sheer stress and strain
FLUID MECHANICS
INTRODUCTION
• Why must the shark keep moving to
stay afloat while the small fish can
remain at the same level with little
effort?
• We begin with fluids at rest and then
move on to the more complex field of
fluid dynamics.
DENSITY
• The density of a material is its mass per
unit volume:  = m/V.
• The specific gravity of a material is its
density compared to that of water at 4°C.
DENSITY
DENSITY
DENSITY
PRESSURE IN A FLUID
• The pressure in a fluid is the normal force per
unit area: p = dF/dA.
PRESSURE IN A FLUID
PRESSURE AT DEPTH IN A FLUID
• The pressure at a depth h in a fluid of uniform
density is given by P = P0 + gh. As Figure
12.6 at the right illustrates, the shape of the
container does not matter.
• The gauge pressure is the pressure above
atmospheric pressure. The absolute pressure is
the total pressure.
PASCAL’S LAW
• Pascal’s law: Pressure applied to an enclosed
fluid is transmitted undiminished to every
portion of the fluid and the walls of the
containing vessel.
• The hydraulic life shown an application of
Pascal’s law.
TWO TYPES OF PRESSURE GAUGE
• Figure 12.8 below shows two types of gauges for measuring
pressure.
ARCHIMEDES PRINCIPLE
• Archimedes’ Principle: When a body is completely or partially
immersed in a fluid, the fluid exerts an upward force (the “buoyant
force”) on the body equal to the weight of the fluid displaced by the
body. (See Figure 12.11 below.)
SURFACE TENSION
• The surface of a liquid
behaves like a membrane
under tension, so it resists
being stretched. This force is
the surface tension. (See
Figure 12.15 at the right.)
• The surface tension allows the
insect shown at the right to
walk on water.
FLUID FLOW
• The flow lines in the bottom figure
are laminar because adjacent layers
slide smoothly past each other.
• In the figure at the right, the upward
flow is laminar at first but then
becomes turbulent flow.
Copyright © 2012 Pearson Education Inc.
The continuity equation
• The figure at the right shows a flow
tube with changing cross-sectional area.
• The continuity equation for an
incompressible fluid is A1v1 = A2v2.
• The volume flow rate is dV/dt = Av.
Copyright © 2012 Pearson Education Inc.
Bernoulli’s equation
• Bernoulli’s equation is
p1 + gy1 + 1/2 v1
2
=
p2 + gy2 + 1/2 v2
2
• Refer to Figure 12.22 at the right.
Copyright © 2012 Pearson Education Inc.
Water pressure in the home
Copyright © 2012 Pearson Education Inc.
Water pressure in the home
Copyright © 2012 Pearson Education Inc.
The Venturi meter
Copyright © 2012 Pearson Education Inc.
Viscosity and turbulence
• Viscosity is internal friction
in a fluid. (See Figures 12.27
and 12.28 at the right.)
• Turbulence is irregular
chaotic flow that is no longer
laminar. (See Figure 12.29
below.)
Copyright © 2012 Pearson Education Inc.
A curve ball (Bernoulli’s equation applied to sports)
• Does a curve ball really curve? Follow Conceptual Example
12.11 and Figure 12.30 below to find out.
Copyright © 2012 Pearson Education Inc.
THANK YOU

M13_Equilibrium, Elasticity and Fluid Mechanics.pptx

  • 1.
    SFT 3033 MECHANICS WEEK 13: EQUILIBRIUM, ELASTICITY & FLUID MECHANICS Dr Anis Diyana Bt Halim
  • 3.
    Copyright © 2012Pearson Education Inc. Introduction • Many bodies, such as bridges, aqueducts, and ladders, are designed so they do not accelerate. • Real materials are not truly rigid. They are elastic and do deform to some extent. • We shall introduce concepts such as stress and strain to understand the deformation of real bodies.
  • 4.
    Copyright © 2012Pearson Education Inc. Conditions for equilibrium (For extended body) • First condition: The sum of all the forces is equal to zero: Fx = 0 Fy = 0 Fz = 0 • Second condition: The sum of all torques about any given point is equal to zero.
  • 5.
    Copyright © 2012Pearson Education Inc. Center of Mass • For a collection of particles with masses m1, m2, …..and coordinates (x1, y1, z1), (x2,y2,z2) the coordinates xcm, ycm and zcm is given by :
  • 6.
    Copyright © 2012Pearson Education Inc. Center of gravity • We can treat a body’s weight as though it all acts at a single point — the center of gravity. • If we can ignore the variation of gravity with altitude, the center of gravity is the same as the center of mass.
  • 7.
    Copyright © 2012Pearson Education Inc. Calculation : Walking the plank
  • 8.
    Copyright © 2012Pearson Education Inc.
  • 9.
    Copyright © 2012Pearson Education Inc. Strain, stress, and elastic moduli • Stretching, squeezing, and twisting a real body causes it to deform, as shown in Figure below. We shall study the relationship between forces and the deformations they cause. • Stress is the force per unit area and strain is the fractional deformation due to the stress. Elastic modulus is stress divided by strain. • The proportionality of stress and strain is called Hooke’s law.
  • 10.
    Copyright © 2012Pearson Education Inc. Strain, stress, and elastic moduli • The proportionality of stress and strain is called Hooke’s law.
  • 11.
    Copyright © 2012Pearson Education Inc. Tensile and compressive stress and strain • Tensile stress = F /A and tensile strain = l/l0. Compressive stress and compressive strain are defined in a similar way. (See Figures 11.13 and 11.14 below.) • Young’s modulus is tensile stress divided by tensile strain, and is given by Y = (F/A)(l0/l).
  • 12.
    Copyright © 2012Pearson Education Inc. Some values of elastic moduli
  • 13.
    Copyright © 2012Pearson Education Inc. Tensile stress and strain • In many cases, a body can experience both tensile and compressive stress at the same time, as shown in figure below
  • 14.
    Copyright © 2012Pearson Education Inc. Tensile stress and strain
  • 15.
    Copyright © 2012Pearson Education Inc. Tensile stress and strain
  • 16.
    Copyright © 2012Pearson Education Inc. Bulk stress and strain • Pressure in a fluid is force per unit area: p = F/A. • Bulk stress is pressure change p and bulk strain is fractional volume change V/V0. (See Figure 11.16.) • Bulk modulus is bulk stress divided by bulk strain and is given by B = –p/(V/V0).
  • 17.
    Copyright © 2012Pearson Education Inc. Sheer stress and strain • Sheer stress is F||/A and sheer strain is x/h, as shown in Figure 11.17. • Sheer modulus is sheer stress divided by sheer strain, and is given by S = (F||/A)(h/x).
  • 18.
    Copyright © 2012Pearson Education Inc. Sheer stress and strain
  • 19.
    Copyright © 2012Pearson Education Inc. Sheer stress and strain
  • 20.
  • 21.
    INTRODUCTION • Why mustthe shark keep moving to stay afloat while the small fish can remain at the same level with little effort? • We begin with fluids at rest and then move on to the more complex field of fluid dynamics.
  • 22.
    DENSITY • The densityof a material is its mass per unit volume:  = m/V. • The specific gravity of a material is its density compared to that of water at 4°C.
  • 23.
  • 24.
  • 25.
  • 26.
    PRESSURE IN AFLUID • The pressure in a fluid is the normal force per unit area: p = dF/dA.
  • 27.
  • 28.
    PRESSURE AT DEPTHIN A FLUID • The pressure at a depth h in a fluid of uniform density is given by P = P0 + gh. As Figure 12.6 at the right illustrates, the shape of the container does not matter. • The gauge pressure is the pressure above atmospheric pressure. The absolute pressure is the total pressure.
  • 29.
    PASCAL’S LAW • Pascal’slaw: Pressure applied to an enclosed fluid is transmitted undiminished to every portion of the fluid and the walls of the containing vessel. • The hydraulic life shown an application of Pascal’s law.
  • 30.
    TWO TYPES OFPRESSURE GAUGE • Figure 12.8 below shows two types of gauges for measuring pressure.
  • 31.
    ARCHIMEDES PRINCIPLE • Archimedes’Principle: When a body is completely or partially immersed in a fluid, the fluid exerts an upward force (the “buoyant force”) on the body equal to the weight of the fluid displaced by the body. (See Figure 12.11 below.)
  • 32.
    SURFACE TENSION • Thesurface of a liquid behaves like a membrane under tension, so it resists being stretched. This force is the surface tension. (See Figure 12.15 at the right.) • The surface tension allows the insect shown at the right to walk on water.
  • 33.
    FLUID FLOW • Theflow lines in the bottom figure are laminar because adjacent layers slide smoothly past each other. • In the figure at the right, the upward flow is laminar at first but then becomes turbulent flow.
  • 34.
    Copyright © 2012Pearson Education Inc. The continuity equation • The figure at the right shows a flow tube with changing cross-sectional area. • The continuity equation for an incompressible fluid is A1v1 = A2v2. • The volume flow rate is dV/dt = Av.
  • 35.
    Copyright © 2012Pearson Education Inc. Bernoulli’s equation • Bernoulli’s equation is p1 + gy1 + 1/2 v1 2 = p2 + gy2 + 1/2 v2 2 • Refer to Figure 12.22 at the right.
  • 36.
    Copyright © 2012Pearson Education Inc. Water pressure in the home
  • 37.
    Copyright © 2012Pearson Education Inc. Water pressure in the home
  • 38.
    Copyright © 2012Pearson Education Inc. The Venturi meter
  • 39.
    Copyright © 2012Pearson Education Inc. Viscosity and turbulence • Viscosity is internal friction in a fluid. (See Figures 12.27 and 12.28 at the right.) • Turbulence is irregular chaotic flow that is no longer laminar. (See Figure 12.29 below.)
  • 40.
    Copyright © 2012Pearson Education Inc. A curve ball (Bernoulli’s equation applied to sports) • Does a curve ball really curve? Follow Conceptual Example 12.11 and Figure 12.30 below to find out.
  • 41.
    Copyright © 2012Pearson Education Inc. THANK YOU