statics part 1
TRANSCRIPT
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FLUID STATICS
FLUIDS ARE AT REST OR MOVING IN SUCH A MANNER THAT THERE IS NO
RELATIVE MOTION BETWEEN ADJACENT PARTICLES
NO SHEAR STRESSES IN THE FLUID AT REST
PRESSURE IS THE ONLY FORCE DEVELOPED
PRESSURE AT A POINT
Pressure normal force per unit area at a given point acting on a given
plane within the fluid mass of interest
How the pressure at a point varies with the orientation of the plane passing
through the point ?
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sxPs
x
y
z
zxPy
yxPz
x
y
z
2
zyx
g
FORCES ON AN ARBITRARY WEDGE SHAPED ELEMENT OF FLUID
THE PRESSURE AT A POINT IN A FLUID AT REST, OR IN MOTION, IS
INDEPENDENT OF DIRECTION AS LONG AS THERE ARE NO SHEARING
STRESSES PRESENT PASCALS LAW
s
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s
zsin
s
ycosSinsz Cossy
yy amF
yxy a2
zyxSinsxPzxP
yxy ayPP2
zz amF
z
xz
a2
zyx
2zyxgCossxPyxP
ga2
zPP zxz
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Taking the limit x, y, z approch zero while maintaining
zys PPP
IN THE ABSENCE OF SHEARING STRESSES, PRESSURE AT ANY POINT INA FLUID IS INDEPENDENT OF DIRECTION PASCALS LAW
PASCAL BLAISE 1623 1662 39 YEARS
1642 - invented the first mechanical adding machine
Pascal proved by experimentation in 1648 that the level of the mercury column in a
barometer is determined by an increase or decrease in the surrounding atmospheric
pressure rather than by a vacuum, as previously believed.
His methodology reflected his emphasis on empirical experimentation as opposed toanalytical, a priori methods, and he believed that human progress is perpetuated by
the accumulation of scientific discoveries resulting from such experimentation.
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y
z
x
zx2
y
y
PP
zx
2
y
y
PP
yx
2
z
z
PP
yx2
z
z
PP
zy
2
x
x
PP
zy2
x
x
PP
BASIC EQUATION FOR THE PRESSURE FIELD
How does the pressure in a fluid in which there are no shearing
stresses vary from point to point ?
j
i
K
z,y,xP
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T.O.H.......xx
)x(f
2
1x
x
)x(f)x(fxxf
2
2
2
Neglecting all higher order terms
zyx
y
PFy
T.O.H.....2
y
y
P
2
1
2
y
y
P
PP
2
2
2
2yy
2
y
y
PPP
2y
y
zx
2
y
y
PPzx
2
y
y
PPFy
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By Newtons Second Law,
m a = Surface forces (pressure) + Body forces (weight)
a
mF
azyxkzyxzyxP
akP
General equation of motion for a fluid no shearing stress
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PRESSURE VARIATION IN A FLUID AT REST
dz
dp
For liquids or gases at rest the pressure gradient in the vertical
direction at any point in a fluid depends only on the specific weight of
the fluid at that point
akp
PZ
0a;z
p;0
y
p;0
x
p
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INCOMPRESSIBLE FLUID
dz
dp
2
1
2
1
z
z
p
p
dzdp
)zz(pp 1221
This pressure distribution HYDROSTATIC DISTRIBUTION
hghPP 21
Hgofmm76081.910006.13
10325.101
g
PPh
3
21
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PAB
= h + Po
PRESSURE IN A HOMOGENOUS, INCOMPRESSIBLE FLUIDAT REST
depends on the depth of the fluid relative to somereference plane
not influenced by the size of shape of the tank in which
the fluid is held
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F1 = (A1/A2)F2
A1
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COMPRESSIBLE FLUID
dz
dp2z
1z
2p
1p
dzdp Gases are compressible
gTR
pg
dz
dp2z
1z
2p
1pT
dz
R
g
p
dp
2z
1z1
2
T
dz
R
g
p
pln zfT
For isothermal condition
o
12
1
2
TR
)zz(g
p
pln
o
12
1
2
TR
)zz(gexp
p
p
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STANDARD ATMOSPHERE
T = 150 C (288.15 K)
p = 101.33 kPa (abs)
= 1.225 kg/m3
= 12.014 N/m3
= 1.789 10-5 Pa.s
FOR TROPOSPHEREm/K0065.0
zTT a
Airplanes
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2z
1z1
2
T
dz
R
g
p
pln
zfT
m/K0065.0
zTT a
2z
1z
a1
2
zT
dz
R
g
p
pln
zTln1
R
g
p
pln a
1
2
Rg
a1
2 zTlnp
pln
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Graphical Representation of Pressure
ABSOLUTE PRESSURES POSITIVE
GAGE PRESSURES POSITIVE & NEGATIVE
Pabs = Patm Pgage
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BAROMETER
vaporatm php
For mercury at 20o C,
papvapor 158585.0
hpatm
Evangelista Torricelli - 1644
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PIEZOMETER TUBE
Simple and accurate
Suitable only for pressure
greater than atmospheric
pressure
Pressure measured to bereasonably small height will
be large
Capillarity effects are negligible
for large bore tube ie.,diameters greater than 30 mm
atmA phP
0hh
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U-TUBE MANOMETER02211 hhpa
1122a hhp
If A contains gas,
22 hpa
Capillarity effects are
negligible for large bore
tube ie., diameters
greater than 30 mm
DIFFERENTIAL U TUBE MANOMETER
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DIFFERENTIAL U-TUBE MANOMETER
3322b11a hhphp
Capillarity effects cancel
INCLINED TUBE MANOMETER
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INCLINED TUBE MANOMETER
3322b11a hsinlphp
113322 sin hhlpp baIf A and B contain gas
sin22
ba ppl
Amplification issin1
sin
1sin
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Pressure Gage
Pressure gages