To solve this problem, we need to understand the energy exchanges that occur when water freezes and evaporates in a thermally isolated system. In this scenario, we have 100 g of water at 0°C, and when the air is pumped out, some of this water will freeze into ice, while some will evaporate. The key is to balance the energy lost during freezing with the energy gained during evaporation.
Understanding the Energy Changes
First, let's convert the mass of water into kilograms since the latent heat values are given in J/kg. We have:
- Mass of water, m = 100 g = 0.1 kg
Next, we need to define the latent heats involved:
- Latent heat of vaporization of water, Lv = 2.10 × 106 J/kg
- Latent heat of fusion of ice, Lf = 3.36 × 106 J/kg
Energy Balance Equation
When some water freezes, it releases energy equal to the latent heat of fusion. Conversely, when some water evaporates, it absorbs energy equal to the latent heat of vaporization. If we let x be the mass of water that freezes into ice, then the mass of water that evaporates will be (0.1 - x) kg. The energy released by freezing must equal the energy absorbed by evaporation:
Energy released by freezing = Energy absorbed by evaporation
Mathematically, this can be expressed as:
x × Lf = (0.1 - x) × Lv
Substituting Values
Now, substituting the known values into the equation:
x × (3.36 × 106) = (0.1 - x) × (2.10 × 106)
Expanding this gives:
3.36 × 106 x = 2.10 × 106 (0.1 - x)
Distributing the right side:
3.36 × 106 x = 2.10 × 106 × 0.1 - 2.10 × 106 x
Which simplifies to:
3.36 × 106 x + 2.10 × 106 x = 2.10 × 105
Combining like terms:
(3.36 + 2.10) × 106 x = 2.10 × 105
5.46 × 106 x = 2.10 × 105
Calculating the Mass of Ice Formed
Now, we can solve for x:
x = (2.10 × 105) / (5.46 × 106)
Calculating this gives:
x ≈ 0.0385 kg
To express this in grams:
x ≈ 38.5 g
Final Result
Thus, the mass of ice formed when the air is pumped out of the vessel is approximately 38.5 grams. This result shows how energy conservation principles apply in phase changes, demonstrating the balance between freezing and evaporation in a closed system.