Fluid Mechanics
Lecture 4: Buoyancy
ME12076
Dr Lee Nissim
ln480@bath.ac.uk
Fluid statics
These three lectures are focussed on ‘fluid statics’ (fluids that are not
moving) as opposed to ‘fluid dynamics’, which together make up
‘fluid mechanics’.
Last lecture, we looked at pressure
This lecture we will look at buoyancy
Next lecture we will look at forces on submerged bodies
Archimedes principle
The upthrust on a body is equal to the weight of
the fluid displaced by the body
weight of the body, ρb h3
g
upthrust (weight of
displaced fluid, ρf h3
g)
The body will sink
The body will float
Archimedes principle
Visualiser!
Example: Conical buoy
A conical buoy with a base radius of 0.5 m and height of 2.5 m has a mass of 180 kg and is
moored in salt water to a long length of steel cable with a mass per unit length of
12.2 kg/m. The height of the buoy protruding from the water is 0.63 m. , is 1026 kg/m3
.
Neglecting the buoyancy force on the cable, find the water depth, H.
Example: Conical buoy
Visualiser!
Compressible fluids
e.g. air: density is a function of temperature (ideal gas)
Hydrostatic pressure:
Temperature, pressure and density are all related.
z
sea level
International Standard Atmosphere
International Standard Atmosphere
Visualiser!
International Standard Atmosphere
Example: Weather balloon
A spherical balloon of 8 m diameter and mass 60 kg is filled with Helium and released
from its mooring at sea level. Find the height to which the balloon will rise, assuming
that the balloon does not stretch, and that the air obeys the international standard
atmosphere:
where , and = 288 K
And , where =1.225 kg/m3
Take the density of helium, , to be 0.17 kg/m3
.
Example: Weather balloon
Visualiser!
Example: Ice cube
The density of ice is approximately 900 kg/m3
, so an ice cube will float with 10% of its
volume above the water.
As the ice melts, its density increases to that of water (1000 kg/m3
), what happens to
the water level?
d
Example: Ice cube
Visualiser!
Summary
Archimedes’ principle tells us that the upthrust on a body is equal to the
weight of fluid displaced by the body
In air, changes in hydrostatic pressure drive changes in density, which in
turn drive changes in buoyancy force with altitude.
You can now attempt Q1 – Q3 on Tutorial Sheet 2!
Fluid Mechanics
Lecture 4: Buoyancy
ME12076
Dr Lee Nissim
ln480@bath.ac.uk

Fluid Mechanics - - - - - Buoyancy.pptx