Melting Mechanics

There is an ice cube of side length a a in a cylindrical container of radius r r . Over time, this ice cube will gradually melt and form water around it.

Assuming the ice always remains a cube while melting, what will be its side length (in meters) when it just starts to float in its own water?

Details :

  • a = 1 m a=1\text{ m}
  • r = 1 m r=1 \text{ m}
  • Specific gravity of water is 1.0.
  • Specific gravity of ice is 0.9.


The answer is 0.318.

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2 solutions

Chew-Seong Cheong
Dec 29, 2018

Let the side length of the melting ice cube when it just starts to float be x x . Then its mass is 0.9 x 2 0.9x^2 and this is the weight of the water displaced by the ice. Since water has a specific gravity of 1, the volume displaced is also 0.9 x 3 0.9x^3 . As the ice cube floats with a face horizontal and that it has a uniform cross-sectional area of x 2 x^2 , the side length submerged in water is therefore 0.9 x 0.9x . This is also the depth of the water since the ice cube is just floating. Then we have:

Volume of water + Volume of the submerged part of ice = π r 2 ( 0.9 x ) 0.9 ( 1 x 3 ) + 0.9 x 3 = 0.9 π x 1 = π x x = 1 π 0.318 \begin{aligned} \text{Volume of water}+ \text{Volume of the submerged part of ice} & = \pi r^2 (0.9x) \\ 0.9(1-x^3) + 0.9x^3 & = 0.9 \pi x \\ 1 & = \pi x \\ \implies x & = \frac 1\pi \approx \boxed{0.318} \end{aligned}

Eric Roberts
Jan 22, 2019

The ice will float in the container when the buoyant force from the liquid water is equal to the weight of the ice.

F B = m g F_B = mg

ρ l i q V D g = ρ i c e V i c e g \rho_{liq}V_Dg = \rho_{ice}V_{ice}g ...Eq 1

Where,

ρ \rho is the density of the medium (ice or liquid water).

g g is the acceleration due to gravity.

V i c e = a 3 V_{ice} = a^3 is the volume of ice at this instant.

V D V_{D} is the volume of displaced liquid water.

V D = a 2 h V_{D} = a^2 h ...Eq 2

Where,

a 2 a^2 is the crossectional area of the cube.

h h is the height of the liquid water in the container.

Substitue Eq2 \rightarrow Eq1

Next. the height of the liquid can be written in terms of the net crossectional area of the container and the volume of the liquid:

h = V l i q π r 2 a 2 \displaystyle h= \frac{V_{liq}}{\pi r^2 - a^2} ...Eq 3

Substitue Eq 3 \rightarrow Eq1

Mass is conserved in the phase change, and it follows that the change in mass of the ice is equivalent to the mass of the liquid.

Δ m i c e = ρ l i q V l i q \Delta m_{ice} = \rho_{liq}V_{liq}

ρ i c e ( a o 3 a 3 ) = ρ l i q V l i q \rho_{ice}( {a_o}^3 - a^3 ) = \rho_{liq}V_{liq}

or

V l i q = ρ i c e ( a o 3 a 3 ) ρ l i q \displaystyle V_{liq} = \frac{\rho_{ice} ({a_o}^3 - a^3 )}{\rho_{liq}} ...Eq 4

Substitue Eq 4 \rightarrow Eq1

After the last substitution is made, make the appropriate cancellations and we are left with,

a = a o 3 a 3 π r 2 a 2 \displaystyle a = \frac{{a_o}^3 - a^3}{\pi r^2 - a^2} , which is valid for 0 < a o 2 r 0 < a_o \leq \sqrt{2}r (the cube must have some volume and fit inside the container)

a = a o 3 π r 2 \displaystyle a = \frac{{a_o}^3}{\pi r^2}

Notice the relationship is independent of the material densities between its solid and liquid state. However, the implicit assumption in Eq1 for a body to float is its acceleration must be 0 \geq 0 , so ρ l i q u i d ρ s o l i d \rho_{liquid} \geq \rho_{solid} for this to hold.

Finally, substitute a o = 1 m a_o = \SI{1}{\meter} and r = 1 m r = \SI{1}{\meter}

a = 1 π 0.318 m \displaystyle a = \frac{1}{\pi} \approx \SI{0.318}{\meter}

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