The Trap of the Constant
When we first learn about heat transfer, the formula Q=mCΔT is drilled into our heads. It's elegant, simple, and works perfectly—as long as the specific heat capacity C is a constant. But nature isn't always so accommodating. In this problem, we are introduced to a substance where the specific heat capacity is temperature-dependent, given by C=kT.
This means that as the substance gets hotter, it becomes increasingly "stubborn" and requires more heat to raise its temperature by the same amount. If you try to plug this into the standard formula, you'll immediately hit a wall. Which temperature do you use? The initial? The final? The average? None of them will give you the exact answer. We need a more powerful tool.
The Calculus of Heat
Enter calculus. When a quantity is continuously changing, we can't look at the macroscopic picture all at once. We have to zoom in. Imagine adding a microscopic amount of heat, dQ, which causes a microscopic rise in temperature, dT. Over this tiny interval, the temperature is essentially constant, so our trusty formula works in its differential form: dQ=mCdT.
To find the total heat Q, we must sum up all these microscopic heat contributions from our starting temperature to our ending temperature. This continuous summation is exactly what an integral does. Geometrically, if we plot C against T, the total heat required is the area under the curve between our initial and final states.
The Absolute Temperature Catch
Before we rush into integrating, there is a classic trap waiting for us: units. The problem gives us temperatures in Celsius (−73∘C and 27∘C), but the formula C=kT explicitly states that T is the absolute temperature.
Absolute temperature is measured in Kelvin. If we integrate using Celsius, our limits will be negative and positive, and the math will completely break down, giving us a physically meaningless result. We must convert our bounds:
Ti=−73+273=200 K
Tf=27+273=300 K
Executing the Math
Now we are ready to set up our integral. We know the mass m=1 kg and C=kT.
Substituting our values:
Since k is a constant, we can pull it out of the integral:
The integral of T with respect to T is simply 2T2. Now we evaluate this from 200 to 300:
Let's do the arithmetic. 3002 is 90,000, and 2002 is 40,000.
The problem states that the total heat required is nk. By comparing our result to this expression, it is crystal clear that n=25000.
This problem is a beautiful reminder that physics is not just about memorizing formulas; it's about understanding the underlying principles. When the rules of the game change—like a variable specific heat—calculus provides the framework to adapt and conquer.