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It is not uncommon for the night sky temperature in desert regions to drop to \(-40^{\circ} \mathrm{C}\). If the ambient air temperature is \(20^{\circ} \mathrm{C}\) and the convection coefficient for still air conditions is approximately \(5 \mathrm{~W} / \mathrm{m}^{2} \cdot \mathrm{K}\). can a shallow pan of water freeze?

Short Answer

Expert verified
Yes, given the conditions, the water can potentially freeze.

Step by step solution

01

Understand the Concept

To determine if the water can freeze, we need to calculate the rate of heat transfer from the water to the night sky by convection. If the heat transfer is sufficient to lower the water temperature to 0°C or below, the water can freeze.
02

Identify Given Data

The problem gives us the following data: ambient air temperature, \( T_{air} = 20^{\circ} C \); night sky temperature, \( T_{sky} = -40^{\circ} C \); and convection coefficient, \( h = 5 \mathrm{~W} / \mathrm{m}^{2} \cdot \mathrm{K} \).
03

Use the Heat Transfer Formula

We use the convective heat transfer equation for the rate of heat transfer per unit area, \( q = h (T_{air} - T_{water}) \). Since we're checking for freezing, we'll use \( T_{water} = 0^{\circ} C \) for our calculation.
04

Calculate the Heat Transfer Rate

Plug in the known values into the formula: \( q = 5 \mathrm{~W} / \mathrm{m}^{2} \cdot \mathrm{K} \times (20^{\circ} C - 0^{\circ} C) \). Therefore, \( q = 5 \times 20 = 100 \mathrm{~W} / \mathrm{m}^{2} \).
05

Assess Freezing Condition

The calculated heat transfer rate of 100 W/m² is the maximum rate at which heat can be removed from the water. If this rate is sufficient to lower the water temperature to 0°C and continue to extract heat, the water can freeze.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Convective Heat Transfer
Convective heat transfer is a process by which heat is transported through the movement of fluids, such as liquids or gases. This process can happen naturally or be forced. In the context of the original problem, the movement of air molecules around the shallow pan of water is an example of natural convection.
Natural convection occurs due to the temperature difference between the water and the surrounding air. This temperature difference causes air molecules to move and transfer heat energy away from the water, effectively cooling it.
Understanding the principles of convective heat transfer is crucial for various applications, including weather predictions, HVAC systems, and even understanding the heat loss properties of buildings and vehicles.
  • Heat is transferred by the mass motion of fluids (such as air).
  • It is influenced by the temperature difference between the object and the surrounding medium.
  • Convective cooling can lower the temperature of an object, such as water in a pan.
Convection Coefficient
The convection coefficient, often denoted as \( h \), is a measure that quantifies the ability of a fluid to conduct heat away from a surface it flows over. In simple terms, it represents the effectiveness of convective heat transfer under specific conditions.
A higher convection coefficient means more efficient heat transfer from the object's surface to the fluid, while a lower coefficient suggests slower heat transfer. In the exercise, the specified convection coefficient is \( 5 \, \mathrm{W/m^2 \cdot K} \). This value is typical for still air, indicating that the air is not moving much and therefore transfers heat at a modest rate.
To apply the convection coefficient in practical scenarios, the equation used is: \[ q = h (T_{surface} - T_{fluid}) \] This equation helps estimate the rate at which heat is leaving or being absorbed by the surface, crucial in determining whether the pan of water will reach a freezing point.
  • Specifies the effectiveness of heat transfer between a surface and a fluid.
  • Depends on factors like fluid type, flow characteristics, and temperature.
  • Used to calculate the rate of heat transfer in engineering applications.
Freezing Point
The freezing point is the temperature at which a liquid turns into a solid. For water, this happens at \( 0^{\circ} C \), known as the freezing point of water. To determine if the water in the pan will freeze, it's necessary for the pan to reach this specific temperature.
In the problem scenario, for water to freeze, the rate at which heat is removed from the water by the surrounding air and night sky must be enough to reduce its temperature to \( 0^{\circ} C \). The calculated heat transfer rate tells us if the cold temperatures and convective processes are capable of meeting or exceeding the heat loss required for freezing.
  • The freezing point is constant for pure substances but can change with impurities or pressure changes.
  • Monitoring the ambient and surface temperature differences helps in predicting freezing.
  • A balance between environmental conditions and heat transfer rates determines the freezing outcome.

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Most popular questions from this chapter

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