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Consider two fluids, one with a large coefficient of volume expansion and the other with a small one. In what fluid will a hot surface initiate stronger natural convection currents? Why? Assume the viscosity of the fluids to be the same.

Short Answer

Expert verified
Answer: A fluid with a large coefficient of volume expansion will have stronger natural convection currents when a hot surface is introduced, as it will experience a greater change in density leading to stronger buoyancy forces and, consequently, stronger convection currents.

Step by step solution

01

Understand the concept of natural convection currents

Natural convection currents are the circulation of fluid caused by the differences in fluid density due to temperature changes. When a fluid is heated, it expands, and its density reduces. As a result, the heated fluid becomes lighter and rises, while the cooler, denser fluid sinks. This creates a continuous circulation of the fluid, forming convection currents.
02

Relate the coefficient of volume expansion to density change

The coefficient of volume expansion (denoted as \(\beta\)) is a measure of how much a fluid expands when its temperature increases. It is defined as the fractional change in volume per unit change in temperature at constant pressure: $$\beta = \frac{1}{V} \frac{dV}{dT}$$ A larger coefficient of volume expansion means that, for a given temperature change, the fluid will experience a larger volumetric expansion. This results in a larger change in fluid density (\(\Delta \rho\)) due to the temperature change. Since natural convection is driven by differences in fluid densities, this will directly affect the strength of convection currents.
03

Compare the convection currents in the two fluids

Now that we have established the relationship between the coefficient of volume expansion, density change, and natural convection currents, we can compare the two fluids. Fluid 1: Large coefficient of volume expansion (\(\beta_1\)) Fluid 2: Small coefficient of volume expansion (\(\beta_2\)) Assuming the same temperature change: As the coefficient of volume expansion of Fluid 1 is larger than Fluid 2, the change in density (\(\Delta \rho_1\)) for Fluid 1 will be larger than that of Fluid 2 (\(\Delta \rho_2\)). The larger change in density will result in stronger buoyancy forces acting on the fluid, causing it to rise more quickly. This will, in turn, create stronger natural convection currents in Fluid 1 as compared to Fluid 2.
04

Conclusion

Based on the analysis above, we can conclude that a hot surface will initiate stronger natural convection currents in the fluid with a large coefficient of volume expansion compared to the fluid with a small coefficient of volume expansion, assuming the viscosity of the fluids to be the same. This is because the larger coefficient of volume expansion results in a more significant change in fluid density, leading to stronger buoyancy forces and, consequently, stronger natural convection currents.

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Key Concepts

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

Coefficient of Volume Expansion
The coefficient of volume expansion is a key factor when dealing with fluid dynamics and heat transfer. It reflects how much a fluid's volume changes when its temperature changes and is denoted by the symbol \( \beta \). Essentially, it measures the fraction of volume change per degree of temperature increase, given by the formula:

\[ \beta = \frac{1}{V} \frac{dV}{dT} \]

Where \( V \) is the original volume and \( dT \) is the change in temperature.

A higher coefficient of volume expansion means that even a small rise in temperature will cause the fluid to expand significantly. This is because the fluid molecules move faster and require more space, thus reducing the fluid’s density. This change in density is crucial for natural convection, as it drives the buoyant forces causing the fluid to move.
Buoyancy Forces
Buoyancy forces come into play when there are variations in fluid density, primarily caused by heating. When a fluid is heated, it becomes lighter due to decreased density, causing it to rise. This upward movement is driven by buoyancy forces, which act against gravity and encourage the fluid motion known as convection currents.

The relationship between buoyancy forces and fluid density is direct; greater changes in density, resulting from higher coefficients of volume expansion, lead to stronger buoyancy forces. These forces are critical in creating natural convection currents, where the lighter fluid rises above the cooler, denser fluid. This sets off a cycle where the fluid continuously circulates, forming noticeable convection patterns.
Fluid Density
Fluid density refers to the mass of fluid per unit volume. It is affected significantly by temperature changes in the fluid themselves. As a fluid heats up, its density decreases because its volume increases. Conversely, cooling increases fluid density as the volume reduces. This varying density within the fluid is a vital component of natural convection.

In practical terms, fluids with a larger coefficient of volume expansion will experience more pronounced changes in density when heated. This means they will create stronger currents compared to fluids with a smaller coefficient, given equal heating. The rapid rise of lighter, hot fluid creates significant circulation that reinforces convection currents, which is central to effective heat transfer.
Heat Transfer Basics
Heat transfer is essential to understanding how energy moves between different parts of a fluid. In the context of natural convection, heat transfer relies on the movement of fluid itself to carry energy from one place to another. This is different from conduction, where heat transfers through a solid directly without movement. Natural convection occurs spontaneously within fluids due to density differences induced by temperature changes. As hot parts of the fluid rise and cooler parts sink, they set up a flow pattern that moves heat throughout the fluid. The rate of heat transfer depends heavily on the strength of convection currents—stronger currents facilitate more efficient heat movement, which is why a fluid with a high coefficient of volume expansion, providing larger density changes and stronger buoyancy forces, typically undergoes more dynamic heat transfer.

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Most popular questions from this chapter

The overall \(U\)-factor of a fixed wood-framed window with double glazing is given by the manufacturer to be \(U=\) \(2.76 \mathrm{~W} / \mathrm{m}^{2} \cdot \mathrm{K}\) under the conditions of still air inside and winds of \(12 \mathrm{~km} / \mathrm{h}\) outside. What will the \(U\)-factor be when the wind velocity outside is doubled? Answer: \(2.88 \mathrm{~W} / \mathrm{m}^{2} \cdot \mathrm{K}\)

Will a hot horizontal plate whose back side is insulated cool faster or slower when its hot surface is facing down instead of up?

Skylights or "roof windows" are commonly used in homes and manufacturing facilities since they let natural light in during day time and thus reduce the lighting costs. However, they offer little resistance to heat transfer, and large amounts of energy are lost through them in winter unless they are equipped with a motorized insulating cover that can be used in cold weather and at nights to reduce heat losses. Consider a 1 -m-wide and \(2.5\)-m-long horizontal skylight on the roof of a house that is kept at \(20^{\circ} \mathrm{C}\). The glazing of the skylight is made of a single layer of \(0.5\)-cm-thick glass \((k=0.78 \mathrm{~W} / \mathrm{m} \cdot \mathrm{K}\) and \(\varepsilon=0.9)\). Determine the rate of heat loss through the skylight when the air temperature outside is \(-10^{\circ} \mathrm{C}\) and the effective sky temperature is \(-30^{\circ} \mathrm{C}\). Compare your result with the rate of heat loss through an equivalent surface area of the roof that has a common \(R-5.34\) construction in SI units (i.e., a thickness-to-effective-thermal- conductivity ratio of \(\left.5.34 \mathrm{~m}^{2} \cdot \mathrm{K} / \mathrm{W}\right)\). Evaluate air properties at a film temperature of \(-7^{\circ} \mathrm{C}\) and \(1 \mathrm{~atm}\) pressure. Is this a good assumption?

What is buoyancy force? Compare the relative magnitudes of the buoyancy force acting on a body immersed in these mediums: \((a)\) air, \((b)\) water, \((c)\) mercury, and \((d)\) an evacuated chamber.

Consider a 1.2-m-high and 2-m-wide glass window with a thickness of \(6 \mathrm{~mm}\), thermal conductivity \(k=0.78 \mathrm{~W} / \mathrm{m} \cdot \mathrm{K}\), and emissivity \(\varepsilon=0.9\). The room and the walls that face the window are maintained at \(25^{\circ} \mathrm{C}\), and the average temperature of the inner surface of the window is measured to be \(5^{\circ} \mathrm{C}\). If the temperature of the outdoors is \(-5^{\circ} \mathrm{C}\), determine \((a)\) the convection heat transfer coefficient on the inner surface of the window, \((b)\) the rate of total heat transfer through the window, and \((c)\) the combined natural convection and radiation heat transfer coefficient on the outer surface of the window. Is it reasonable to neglect the thermal resistance of the glass in this case?

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