The Setup
A Battle of Temperatures
Imagine a classic thermal showdown. On one side, we have 50 g of water sitting comfortably at 40∘C. On the other side, we drop in an unknown mass of ice, let's call it x g, chilling at −20∘C.
When these two meet, a rapid exchange of heat begins. The water wants to cool down, and the ice wants to warm up and melt.
The problem gives us a crucial piece of intel: the final temperature of the mixture settles exactly at 0∘C, and there is still 20 g of ice left unmelted. This detail is the key to unlocking the entire puzzle.
The Master Equation
Principle of Calorimetry
In any isolated thermal system, energy is conserved. The heat lost by the hotter object must be exactly equal to the heat gained by the colder object.
Here, the water is the hot body losing heat, and the ice is the cold body gaining heat. Let's break down each side of this equation.
Calculating the Heat Lost
The water starts at 40∘C and cools down to 0∘C. The formula for heat transfer during a temperature change is:
Plugging in the values for water:
So, the water releases 8400 J of heat energy into the system.
Calculating the Heat Gained
The Tricky Part
Now, let's look at the ice. This is where many students make a silly mistake. The ice doesn't just melt instantly.
First, the entire mass of ice (x g) must warm up from −20∘C to 0∘C.
Qwarming=x×2.1×(0−(−20))=42x
Once all the ice is at 0∘C, it starts to melt. But wait! The problem states that 20 g of ice remains unmelted. This means only (x−20) g of ice actually underwent the phase change into water.
The total heat gained by the ice is the sum of these two processes:
The Final Showdown
Equating and Solving
Now we bring it all together. We equate the heat lost by the water to the total heat gained by the ice.
Let's isolate x:
The calculated mass is approximately 40.10 g. Looking at our options, the closest value is 40 g.
This problem beautifully illustrates how heat transfer happens in stages. Always remember to account for warming up before phase changes!