Analyzing the Initial State
Imagine a serene scene: a cubical block floating peacefully in a pool of water. The problem gives us a crucial piece of information right away—exactly 30% of the block's volume is submerged beneath the surface.
Why does it float? This is the perfect time to invoke Archimedes' Principle, which states that the upward buoyant force exerted on a body immersed in a fluid is equal to the weight of the fluid that the body displaces.
Because the block is in equilibrium, its downward weight must be perfectly balanced by this upward buoyant force. Let's translate this physical reality into mathematics. The weight of the block is given by its volume V, multiplied by its density ρb, and the acceleration due to gravity g.
The buoyant force, on the other hand, depends only on the submerged volume. Since 30% is underwater, the submerged volume is 0.3V. Multiplying this by the density of water ρw and gravity g gives us the buoyant force.
Equating the two, we get:
Notice how beautifully the volume V and gravity g cancel out from both sides! This leaves us with a simple, elegant relationship:
The density of the block is exactly 30% of the density of water. This makes intuitive sense—an object that is 30% as dense as water will float with 30% of its volume submerged.
The Master Equation for the Final State
Now, the problem introduces a challenge. We want to find the maximum weight (or mass m) we can place on top of the block without it sinking completely. "Without fully submerging" means we push the block down until its top surface is exactly flush with the water level. At this point, 100% of its volume is submerged.
Let's set up a new force balance for this final state. The total downward force is now the weight of the block plus the weight of the new mass m.
This total weight is supported by a new, maximum buoyant force. Since the entire block is now underwater, the displaced volume is the full volume V.
Equating the total downward force to the new buoyant force gives us our master equation:
Final Calculation and Conclusion
We can immediately simplify our master equation by dividing every term by gravity g.
Rearranging to solve for our unknown mass m, we factor out the volume V:
Remember our earlier discovery? We found that ρb=0.3ρw. Let's substitute that into our equation:
(Pro-Tip: You could have jumped straight to this step! The added mass m is exactly responsible for pushing the remaining 70% of the block underwater. Therefore, the mass m must equal the mass of the extra 70% of displaced water!)
Now, it's just a matter of plugging in the numbers. The block is a cube with a side length of 0.5 m, so its volume is:
The density of water is given as 103 kg/m3 (or 1000 kg/m3). Substituting these values into our equation for m:
And there we have it! The maximum mass we can place on the block is exactly 87.5 kg. Any more, and the block will sink beneath the waves.