Buoyancy (DP IB Physics: SL): Revision Note

Ashika

Written by: Ashika

Reviewed by: Caroline Carroll

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Buoyancy

  • Buoyancy is experienced by a body which is partially or totally immersed in a fluid

    • The buoyancy force is exerted on a body due to the displacement of the fluid it is immersed in

  • Buoyancy keeps boats afloat and allows balloons to rise through the air

  • When a body travels through a fluid, it also experiences a buoyancy force (upthrust) due to the displacement of the fluid

  • Buoyancy is calculated using:

Fb = ρVg

  • Where:

    • Fb = buoyancy force (N)

    • ρ = density of the fluid (kg m–3)

    • V = volume of the fluid displaced (m3)

    • g = acceleration of free fall (m s–2)

  • If you were to take a hollow ball and submerge it into a bucket of water, you would feel some resistance

  • Some water will flow out of the bucket as it is displaced by the ball

  • The buoyancy force, Fb of the water will push upward on the ball

  • When you let go of the ball, the buoyancy force of the water on the ball will cause the ball to accelerate to the surface

  • The ball will remain stationary floating on the surface of the water

  • A this point, the weight of the ball acting downward, Fg, is equal to the buoyancy force acting upwards, Fb

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The ball floats when the buoyancy force and its weight are balanced

  • Notice that

Fg = ρVg = mVVg = mg

  • Where:

    • m = mass of the ball (kg)

    • ρ = density of the ball (kg m–3)

    • V = volume of the ball (m3)

  • The buoyancy force and the weight force are equal

Drag Force at Terminal Speed

  • Terminal velocity, or terminal speed, is useful when working with Stoke’s Law

  • This is because, at terminal velocity, the forces in each direction are balanced

Ws = Fd +Fb (Equation 1)

  • Where:

    • Ws = weight of the sphere (N)

    • Fd = the drag force (N)

    • Fb = the buoyancy force / upthrust (N)

1-2-10-viscous-drag-force-ib-2025-physics

At terminal velocity, the forces on the sphere are balanced

  • The weight of the sphere is found using volume, density and gravitational field strength

Ws = ρsVsg 

Ws = 43πr3ρsg (Equation 2)

  • Where

    • Vs = volume of the sphere (m3)

    • ρs = density of the sphere (kg m–3)

    • r = radius of the sphere (m)

    • g =  acceleration of free fall (m s−2)

  • Recall Stoke’s Law

Fd = 6πηrv (Equation 3)

  • Where

    • Fd = viscous drag force (N)

    • η = fluid viscosity (N s m−2 or Pa s)

    • r = radius of the sphere (m)

    • v = velocity of the sphere through the fluid (ms−1)

      • In this case, v is the terminal velocity

  • The buoyancy force equals the weight of the displaced fluid

    • The sphere is fully submerged in the fluid, so the volume of displaced fluid is the same as the volume of the sphere

    • The weight of the fluid is found using volume, density and acceleration of free fall

Fb = 43πr3ρfg (Equation 4)

  • Where

    • ρf = density of the fluid (kg m–3)

  • Substitute equations 2, 3 and 4 into equation 1

43πr3ρsg = 6πηrv + 43πr3ρfg 

  • Rearrange to make terminal velocity the subject of the equation

v = 43πr3g(ρs   ρf)6πηr = 4πr3g(ρs   ρf)18πηr 

  • Finally, cancel out r from the top and bottom to find an expression for terminal velocity in terms of the radius of the sphere and the coefficient of viscosity

v =2πr2g(ρs   ρf)9πη 

 

  • This final equation shows that terminal velocity is:

    • directly proportional to the square of the radius of the sphere

    • inversely proportional to the viscosity of the fluid

Worked Example

Icebergs typically float with a large volume of ice beneath the water. Ice has a density of 917 kg m-3 and a volume of Vi.

The density of seawater is 1020 kg m-3.

What fraction of the iceberg is above the water?

A. 0.10 Vi          

B. 0.90 Vi          

C. 0.97 Vi          

D. 0.20 Vi

Worked example - Archimedes' principle iceberg (2), downloadable AS & A Level Physics revision notes

Examiner Tips and Tricks

Remember that ρ in the buoyancy force equation is the density of the fluid and not the object itself!

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Ashika

Author: Ashika

Expertise: Physics Content Creator

Ashika graduated with a first-class Physics degree from Manchester University and, having worked as a software engineer, focused on Physics education, creating engaging content to help students across all levels. Now an experienced GCSE and A Level Physics and Maths tutor, Ashika helps to grow and improve our Physics resources.

Caroline Carroll

Reviewer: Caroline Carroll

Expertise: Head of Content Delivery

Caroline graduated from the University of Nottingham with a degree in Chemistry and Molecular Physics. She spent several years working as an Industrial Chemist in the automotive industry before retraining to teach. Caroline has over 12 years of experience teaching GCSE and A-level chemistry and physics. She is passionate about delivering high-quality resources to help students achieve their full potential.