A Brief History of Planetary Science
Download
Report
Transcript A Brief History of Planetary Science
Archimedes’ Principle
Physics 202
Professor Lee Carkner
Lecture 2
“Got to write a book, see,
to prove you’re a
philosopher. Then you
get your … free official
philosopher’s loofah.”
--Terry Pratchett, Small
Gods
PAL #1 Fluids
Column of water to produce 1 atm of
pressure
r = 1000 kg/m3
h = P/rg = 10.3 m
Double diameter, pressure does not change
On Mars pressure would decrease
Archimedes’ Principle
The fluid exerts a force on the object
If you measure the buoyant force and the
weight of the displaced fluid, you find:
An object in a fluid is supported by a buoyant
force equal to the weight of fluid it displaces
Applies to objects both floating and
submerged
Buoyancy
Will it Float?
What determines if a object will sink or float?
A floating object displaces fluid equal to its
weight
A sinking object displaces fluid equal to its
volume
Floating
How will an object float?
The denser the object, the lower it will float, or:
Example: ice floating in water,
W=rVg
Vi/Vw=rw/ri
rw = 1024 kg/m3 and ri = 917 kg/m3
Iceberg
Ideal Fluids
Steady -Incompressible -Nonviscous -Irrotational --
Real fluids are much more complicated
The ideal fluid approximation is usually not very
good
Moving Fluids
Consider a pipe of cross sectional area A with
a fluid moving through it with velocity v
Mass must be conserved so,
If the density is constant then,
Av= constant = R = volume flow rate
Because the amount of fluid going in must
equal the amount of fluid going out
Continuity
R=Av=constant is called the equation
of continuity
You can use it to determine the flow
rates of a system of pipes
Can’t lose or gain any material
Continuity
The Prancing Fluids
How can we keep track of it all?
The laws of physics must be obeyed
Neither energy nor matter can be
created or destroyed
Bernoulli’s Equation
Consider a pipe that bends up and gets wider at
the far end with fluid being forced through it
The work of the system due to lifting the fluid is,
The work of the system due to pressure is,
Wp=Fd=pAd=DpDV=-(p2-p1)DV
The change in kinetic energy is,
Equating work and DKE yields,
p1+(1/2)rv12+rgy1=p2+(1/2)rv22+rgy2
Fluid Flow
Consequences of Bernoulli’s
Equation
Fast moving fluids exert less pressure than
slow moving fluids
This is known as Bernoulli’s principle
Based on conservation of energy
Note that Bernoulli only holds for moving fluids
Constricted Flow
Bernoulli in Action
Blowing between two pieces of paper
Convertible top bulging out
Shower curtains getting sucked into the
shower
Shower Physics
Lift
Consider a thin surface with air flowing
above and below it
This force is called lift
If you can somehow get air to flow over an
object to produce lift, what happens?
December 17, 1903
Deriving Lift
Consider a wing of area A, in air of density r
Use Bernoulli’s equation:
The difference in pressure is:
pb-pt=1/2rvt2-1/2rvb2
Pressure is F/A so:
L=Fb-Ft and so:
If the lift is greater than the weight of the
plane, you fly
Summary: Fluid Basics
Density =r=m/V
Pressure=p=F/A
On Earth the atmosphere exerts a pressure
and gravity causes columns of fluid to exert
pressure
Pressure of column of fluid:
p=p0+rgh
For fluid of uniform density, pressure only
depends on height
Summary: Pascal and Archimedes
Pascal -- pressure on one part of fluid is
transmitted to every other part
Hydraulic lever -- A small force applied for a
large distance can be transformed into a large
force over a short distance
Fo=Fi(Ao/Ai) and do=di(Ai/Ao)
Archimedes -- An object is buoyed up by a
force equal to the weight of the fluid it
displaces
Must be less dense than fluid to float
Summary: Moving Fluids
Continuity -- the volume flow rate
(R=Av) is a constant
fluid moving into a narrower pipe speeds
up
Bernoulli
p1+1/2rv12+rgy1=p2+1/2rv22+rgy2
Slow moving fluids exert more pressure
than fast moving fluids