Welcome to one of the most fascinating topics in thermal physics: Calorimetry! This is the science of measuring heat transfer, and it governs everything from how your morning coffee cools down to how massive industrial steam engines operate.
Imagine you are standing in a laboratory. In front of you is a perfectly insulated container. Inside this container, a dramatic thermal battle is about to take place. On one side, we have M grams of furious, boiling steam at 100∘C. On the other side, we have 200 g of freezing ice at exactly 0∘C.
When these two extremes meet, they exchange energy until they reach a peaceful equilibrium: liquid water at a comfortable 40∘C. Our mission is to find out exactly how much steam (M) was required to achieve this perfect balance.
The Principle of Calorimetry
The fundamental law governing this process is the conservation of energy. Because our container is thermally insulated, no heat can escape into the room, and no heat can enter from the outside.
Therefore, the total heat energy lost by the hot substance (the steam) must be exactly equal to the total heat energy gained by the cold substance (the ice).
Heat Lost=Heat Gained
Let's break down this thermal journey into two distinct paths.
Tracking the Heat Lost (The Steam's Journey)
The steam doesn't just magically become 40∘C water. It has to go through two distinct phases of heat loss.
Phase 1: Condensation
First, the steam at 100∘C must condense into liquid water at 100∘C. This phase change releases a massive amount of energy known as the latent heat of vaporization (Lv).
Q1=M⋅Lv
Phase 2: Cooling
Now that we have boiling water at 100∘C, it must cool down to the final temperature of 40∘C. This temperature change releases sensible heat, governed by the specific heat capacity of water (sw).
Q2=M⋅sw⋅(100−40)
The total heat lost by the steam is the sum of these two quantities:
Qlost=M⋅Lv+M⋅sw⋅60
Tracking the Heat Gained (The Ice's Journey)
Similarly, the ice undergoes its own two-step transformation.
Phase 1: Melting
The solid ice at 0∘C must first melt into liquid water at 0∘C. This absorbs the latent heat of fusion (Lf).
Q3=mice⋅Lf
Phase 2: Warming
This freshly melted, ice-cold water at 0∘C must now warm up to the final temperature of 40∘C. This absorbs sensible heat.
Q4=mice⋅sw⋅(40−0)
The total heat gained by the ice is:
Qgained=mice⋅Lf+mice⋅sw⋅40
The Master Equation
Now, we bring it all together by equating the heat lost to the heat gained:
M⋅Lv+M⋅sw⋅60=mice⋅Lf+mice⋅sw⋅40
We are given the following constants in CGS units:
- Latent heat of vaporization, Lv=540 cal/g
- Latent heat of fusion, Lf=80 cal/g
- Specific heat of water, sw=1 cal/g∘C
- Mass of ice, mice=200 g
Let's substitute these values into our master equation:
M(540)+M(1)(60)=200(80)+200(1)(40)
The Final Calculation
Now, it's just a matter of simple algebra. Let's simplify both sides of the equation.
On the left side, we factor out
M:
540M+60M=600M
On the right side, we calculate the total heat absorbed by the ice:
16000+8000=24000
Equating them gives us a beautifully clean linear equation:
600M=24000
Dividing both sides by 600:
M=60024000=40
And there we have it! Exactly 40 g of steam was required to melt the ice and bring the entire mixture to a perfectly balanced 40∘C.
Calorimetry problems might look intimidating at first glance, but by systematically breaking down the journey of each substance into phase changes and temperature changes, the underlying math reveals itself to be incredibly elegant and logical.