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A long, uninsulated steam line with a diameter of \(89 \mathrm{~mm}\) and a surface emissivity of \(0.8\) transports steam at \(200^{\circ} \mathrm{C}\) and is exposed to atmospheric air and large surroundings at an equivalent temperature of \(20^{\circ} \mathrm{C}\). (a) Calculate the heat loss per unit length for a calm day. (b) Calculate the heat loss on a breezy day when the wind speed is \(8 \mathrm{~m} / \mathrm{s}\). (c) For the conditions of part (a), calculate the heat loss with a 20 -mm- thick layer of insulation ( \(k=\) \(0.08 \mathrm{~W} / \mathrm{m} \cdot \mathrm{K})\). Would the heat loss change significantly with an appreciable wind speed?

Short Answer

Expert verified
In summary: a) On a calm day, the heat loss per unit length for the uninsulated steam line is approximately 1601.88 W/m. b) On a windy day, the heat loss per unit length for the uninsulated steam line increases to around 4111.57 W/m. c) With a 20 mm-thick layer of insulation, the heat loss per unit length reduces to approximately 22.29 W/m, and the impact of wind speed on heat loss is significantly diminished compared to the uninsulated case.

Step by step solution

01

Analyzing calm day heat transfer mechanism

Since heat transfer across the steam line occurs by both radiation and natural convection on a calm day, we should first determine the heat loss due to both radiation and convection heat transfer mechanisms. For radiation, we can use the Stefan-Boltzmann law, which states that the heat transfer rate by radiation is: \(q_{rad} = \sigma \cdot \epsilon \cdot A(T_{s}^{4} - T_{\infty}^{4})\), where \(q_{rad}\) = heat transfer rate by radiation (W), \(\sigma\) = Stefan-Boltzmann constant (\(5.67 \times 10^{-8} \mathrm{W/m^2K^4}\)), \(\epsilon\) = surface emissivity, \(A\) = surface area (m²), \(T_{s}\) = surface temperature (K), and \(T_{\infty}\) = surroundings temperature (K). For natural convection, we use the equation: \(q_{conv} = h_{c} \cdot A \cdot (T_{s} - T_{\infty})\), where \(q_{conv}\) = heat transfer rate by convection (W), \(h_{c}\) = convection heat transfer coefficient (W/m²K), \(A\) = surface area (m²), \(T_{s}\) = surface temperature (K), and \(T_{\infty}\) = surroundings temperature (K).
02

Calculating heat loss per unit length on a calm day

First, we need to convert the given temperatures from Celsius to Kelvin: \(T_{s} = 200 + 273.15 = 473.15 \mathrm{K}\), \(T_{\infty} = 20 + 273.15 = 293.15 \mathrm{K}\). We know the pipe diameter (\(D = 89 \mathrm{mm} = 0.089 \mathrm{m}\)) and the surface emissivity (\(\epsilon = 0.8\)). To calculate the heat transfer rate per unit length on a calm day, we need the surface area per unit length: \(A = \pi \cdot D = \pi \cdot 0.089 \mathrm{m}\). Now, we can determine the heat loss due to radiation: \(q_{rad} = \sigma \cdot \epsilon \cdot A(T_{s}^{4} - T_{\infty}^{4}) = 5.67 \times 10^{-8} \cdot 0.8 \cdot \pi \cdot 0.089 (473.15^{4} - 293.15^{4}) = 1099.94 \mathrm{W/m}\). Assuming that the natural convection heat transfer coefficient (\(h_{c}\)) is roughly 10 W/m²K, as a general value for natural convection around a cylinder, on average : \(q_{conv} = h_c \cdot A \cdot (T_{s} - T_{\infty}) = 10 \cdot \pi \cdot 0.089 (473.15 - 293.15) = 501.94 \mathrm{W/m}\). Adding both components, the total heat loss per unit length on a calm day is: \(q_{total} = q_{rad} + q_{conv} = 1099.94 + 501.94 = 1601.88 \mathrm{W/m}\). Thus, the heat loss per unit length for a calm day is approximately 1601.88 W/m.
03

Calculating heat loss per unit length on a windy day

On a windy day, forced convection becomes predominant. The forced convection heat transfer coefficient (\(h_{f}\)) can be estimated using empirical correlations as a function of the wind speed. Assuming that \(h_{f}\) for a wind speed of 8 m/s is approximately 60 W/m²K, we can calculate the heat loss due to forced convection: \(q_{wind} = h_{f} \cdot A \cdot (T_{s} - T_{\infty}) = 60 \cdot \pi \cdot 0.089 (473.15 - 293.15) = 3011.63 \mathrm{W/m}\). Therefore, the total heat loss per unit length on a windy day is: \(q_{total(windy)} = q_{rad} + q_{wind} = 1099.94 + 3011.63 = 4111.57 \mathrm{W/m}\). Thus, the heat loss per unit length for a windy day is approximately 4111.57 W/m.
04

Calculating heat loss with insulation and effect of wind

For the conditions given in part (a), we can calculate the heat loss with a 20 mm-thick layer of insulation. Given the thermal conductivity of the insulation material, \(k = 0.08 \mathrm{W/mK}\), the heat transfer resistance for the insulation is given by: \(R_{ins} = \frac{r_{2} - r_{1}}{2 \pi k (r_{1} + r_{2})}\), where \(r_{1} = 44.5 \mathrm{mm}\) (inner pipe radius) and \(r_{2} = 64.5 \mathrm{mm}\) (outer radius with insulation). \(R_{ins} = \frac{0.02}{2 \pi \cdot 0.08 \cdot (0.0445 + 0.0645)} = 25.24 \mathrm{m^2K/W}\). Now, the total heat transfer coefficient with insulation (\(U_{ins}\)) becomes: \(U_{ins} = \frac{1}{R_{ins}} = \frac{1}{25.24} = 0.0396 \mathrm{W/m^2K}\). So, the heat loss per unit length with insulation under calm conditions is: \(q_{ins} = U_{ins} \cdot A \cdot (T_{s} - T_{\infty}) = 0.0396 \cdot \pi \cdot 0.089 \cdot (473.15 - 293.15) = 22.29 \mathrm{W/m}\). The heat loss with insulation is significantly lower than without insulation, as expected. In terms of the effect of wind on heat loss through the insulated steam line, the insulated layer would be relatively more resistant to forced convection, so the change due to the wind would be smaller compared to the uninsulated case. In conclusion: a) The heat loss per unit length on a calm day is approximately 1601.88 W/m. b) The heat loss per unit length on a windy day is approximately 4111.57 W/m. c) The heat loss per unit length with insulation is approximately 22.29 W/m, and it is less affected by wind speed compared to the uninsulated case.

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Key Concepts

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

Stefan-Boltzmann Law
The Stefan-Boltzmann Law is a foundational principle in thermodynamics, describing how objects emit radiation due to their temperature. According to this law, the amount of energy radiated per unit surface area of a black body per unit time is directly proportional to the fourth power of the black body's absolute temperature. Mathematically, it is represented as:

\[q_{rad} = \sigma \cdot \epsilon \cdot A(T_{s}^{4} - T_{\text{{inf}}}^{4})\]

Where \(q_{rad}\) is the heat transfer rate by radiation, \(\sigma\) is the Stefan-Boltzmann constant (\(5.67 \times 10^{-8} \mathrm{{W/m^2K^4}}\)), \(\epsilon\) is the surface emissivity, \(A\) is the surface area, \(T_{s}\) is the surface temperature, and \(T_{\text{{inf}}}\) is the surroundings temperature. In the context of the exercise, this law is used to calculate the heat loss due to radiation from a steam pipe to its surroundings.
Natural Convection
Natural convection is a mode of heat transfer that occurs without any external force and is driven by the buoyancy forces that arise from density differences due to temperature variations in a fluid. In simple terms, as fluid near a hot surface gets heated, it becomes less dense and rises, being replaced by cooler, more dense fluid, and this cycle continues, creating a natural circulation of heat away from the surface. For calculation purposes:

\[q_{conv} = h_{c} \cdot A \cdot (T_{s} - T_{\text{{inf}}})\]

The \(h_{c}\) represents the convection heat transfer coefficient, which can vary depending on the properties of the fluid and the surface involved. For the problem at hand, the natural convection coefficient will depend on specifics like the size of the pipe, its orientation, and the properties of the surrounding air.
Forced Convection
On the other hand, forced convection occurs when a fluid is moved over a surface by external means, such as fans or wind, leading to a higher rate of heat transfer. It is often described using similar mathematical formulas as natural convection, but with a different, usually higher, convection heat transfer coefficient \(h_{f}\) due to the increased fluid motion:

\[q_{wind} = h_{f} \cdot A \cdot (T_{s} - T_{\text{{inf}}})\]

In the provided exercise scenario, when a wind breeze is considered, we see a significant increase in heat loss, demonstrating the more efficient heat transfer capability of forced convection compared to natural convection.
Thermal Insulation
Thermal insulation is the process of reducing heat transfer between objects in thermal contact or in range of radiant influence. A good insulator is one that has a low thermal conductivity, denoted by 'k'. It provides a resistance to heat flow, hence, reducing the rate of heat loss. In the example provided, a layer of insulation is added to the steam pipe, dramatically reducing the heat loss from a calculated 1601.88 W/m down to just 22.29 W/m. This massive decrease underlines the effectiveness of thermal insulation in minimizing energy waste.

The effectiveness of the insulation can be quantified by its resistance value \(R_{ins}\) and taking into account its thickness along with the thermal conductivity.
Heat Transfer Coefficient
The heat transfer coefficient is a pivotal figure in thermodynamics as it quantifies the convective heat transfer between a solid surface and a fluid or between two fluids. It is denoted by 'h' and is measured in W/m²K. This value is highly dependent on the physical properties of the fluid, such as viscosity and thermal conductivity, as well as flow properties, including velocity and flow type (laminar or turbulent). In our exercise, we observe two different scenarios: a natural convection heat transfer coefficient \(h_{c}\) for the calm day and a forced convection coefficient \(h_{f}\) for the windy conditions. The impact of these different 'h' values on the overall heat loss exemplifies their significance in the realm of heat transfer calculations.

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Most popular questions from this chapter

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