While studying the subject of heat transfer, one of our objectives is to calculate the rate of heat transfer. From the second law of thermodynamics, we know that there must be a temperature gradient for heat transfer to occur, i.e. heat flows from a location of high temperature to a location of low temperature. Fourier’s law gives the relation between the rate of heat flow and temperature gradient and is therefore considered to be the fundamental law of conduction.
In this chapter, we will first study Fourier’s law and the assumptions behind this law. Then, follow two important consequences of Fourier’s law; the first one being the definition of thermal conductivity—an important transport property of matter, and the second one being the concept of thermal resistance. We will study about the thermal conductivity of solids, liquids and gases and the variation of this property with temperature. Thermal resistance concept simplifies the solution of many practical problems of steady state heat transfer with no internal heat generation, but involving heat transfer through multiple layers or when different modes of heat transfer occur simultaneously.
This is the basic rate equation for heat conduction which gives a relation between the rate of heat transfer and the temperature gradient.
Fourier’s law states that one-dimensional, steady state heat flow rate between two isothermal surfaces is proportional to the temperature gradient causing the heat flow and the area normal to the direction of heat flow.
Referring to Fig. 2.1, we get,
where, |
Q = heat flow rate in X-direction, W |
|
A = area normal to the direction of heat flow (note this carefully), m2 |
dT/dx = temperature gradient, deg./m
k = thermal conductivity, a property of the material, W/(mC) or W/(mK)
This is the differential form of Fourier’s equation written for heat transfer in the X-direction. Negative sign in Eq. 2.2 requires some explanation. We know that heat flows from a location of higher temperature to a location of lower temperature. Referring to Fig. 2.1, if the heat flow rate Q has to occur in the positive X-direction, temperature has to decrease in the positive X-direction, i.e. temperature must decrease as X increases; this means that temperature gradient dT/dx is negative. Since we would like to have the heat flowing in the positive X-direction to be considered as positive, a negative sign is inserted in Eq. 2.2, so that Q becomes positive.
FIGURE 2.1 Fourier’s law
Let us state succinctly the assumptions and other salient points regarding the Fourier’s law:
We can say that
i.e. thermal conductivity of a material is numerically equal to the heat flow rate through an area of one m2 of a slab of thickness 1 m with its two faces maintained at a temperature difference of one degree celcius.
Therefore, the unit of thermal conductivity is obtained from:
Note that W/(mC) and W/(mK) mean the same thing in Eq. 2.3, (T1 – T2) is the temperature difference which is the same whether it is deg.C or deg.K.
We state Fourier’s law again:
Here, k is the thermal conductivity, a property of the material. Its units: W/(mC) or W/(mK). Thermal conductivity, essentially depends upon the material structure (i.e. crystalline or amorphous), density of material, moisture content, pressure and temperature of operation.
Thermal conductivity of materials varies over a wide range, by about 4 to 5 orders of magnitude. For example, thermal conductivity of Freon gas is 0.0083 W/(mC) and that of pure silver is about 429 W/(mC) at normal pressure and temperature.
Fig 2.2 shows the range of variation of thermal conductivity of different classes of materials:
Table 2.1 gives values of thermal conductivities for a few materials at room temperature.
Thermal conductivity of solids is made up of two components,
FIGURE 2.2 Range of thermal conductivities of various materials
First effect is known as electronic conduction and the second effect is known as phonon conduction.
In case of pure metals and alloys,
TABLE 2.1 Thermal conductivity of a few materials at room temperature
Material | k, W/mC |
---|---|
Diamond |
2300 |
Silver |
429 |
Copper |
401 |
Gold |
317 |
Aluminium |
237 |
Iron |
80.2 |
Mercury (l) |
8.54 |
Glass |
0.78 |
Brick |
0.72 |
Water (l) |
0.613 |
Wood (oak) |
0.17 |
Helium (g) |
0.152 |
Refrigerant-12 |
0.072 |
Glass fibre |
0.043 |
Air (g) |
0.026 |
FIGURE 2.3 Variation of thermal conductivity with temperature for a few metals
FIGURE 2.4 Variation of thermal conductivity with temperature for a few alloys
where |
k = thermal conductivity of metal, W/(mK) |
|
σ = electrical conductivity of metal, (ohm.m)–1 |
|
C = Lorentz number, a constant for all metals |
|
= 2.45 × 10–8 W Ohms/K2 |
An important practical application of Weidemann–Franz law is to determine the value of thermal conductivity of a metal at a desired temperature, knowing the value of electrical conductivity at the same temperature. Note that it is easier to measure experimentally the value of electrical conductivity than that of thermal conductivity.
In case of non-metallic solids,
FIGURE 2.5 Variation of thermal conductivity with temperature for insulating materials
Usually, for solids, a linear variation of thermal conductivity with temperature can be assumed without loss of much accuracy.
where, |
k(T) = thermal conductivity at desired temperature T, W/(mC) |
|
k0 = thermal conductivity at reference temperature of 0°C, W/(mC) |
FIGURE 2.6 Variation of thermal conductivity with temperature for a few pure metals
TABLE 2.2 Representative values of k0 and β in Eq. 2.5
Material | k0 (W/mC) | β × 104, (1/C) |
---|---|---|
Metals and alloys |
|
|
Aluminium |
246.985 |
– 2.227 |
Chromium |
97.123 |
– 5.045 |
Copper |
401.5275 |
– 1.681 |
Stainless steel |
14.695 |
+ 10.208 |
Uranium |
26.679 |
+ 8.621 |
Insulators |
|
|
Fireclay brick |
0.76 |
0.895 |
Red brick |
0.56 |
0.66 |
Sovelite |
0.092 |
0.12 |
85% Magnesia |
0.08 |
0.101 |
Slag wool |
0.07 |
0.101 |
Mineral wool |
0.042 |
0.07 |
β = a temperature coefficient, 1/C
T = temperature, °C
Fig. 2.6 shows the variation of k with temperature for a few pure metals. It may be noted that the variation is linear as indicated in Eq. 2.5.
In Eq. 2.5, value of β may be positive or negative. Generally, β is negative for metals (exception being uranium) and positive for insulators and alloys. Table 2.2 gives representative values of k0 and β for a few materials.
Heat propagation in liquids is considered to be due to elastic oscillations. As per this hypothesis, the thermal conductivity of liquids is given by,
where, |
cp = specific heat of liquid at constant pressure |
|
ρ = density of liquid |
|
M = molecular weight of liquid |
|
A = constant depending on the velocity of elastic wave propagation in the liquid; it does not depend on nature of liquid, but on temperature. |
It is noted that the product A.cp is nearly constant. As temperature rises, density of a liquid falls and as per Eq. 2.6 the value of thermal conductivity also drops for liquids with constant molecular weights. (i.e. for non-associated or slightly associated liquids). This is generally true as shown in Fig. 2.7.
Notable exceptions are water and glycerin, which are heavily associated liquids. With rising pressure, thermal conductivity of liquids increases. For liquids, k value ranges from 0.07 to 0.7 W/(mC).
FIGURE 2.7 Thermal conductivity of non-metallic liquids
Liquid metals like sodium, potassium etc. are used in high flux applications as in nuclear power plants where a large amount of heat has to be removed in a small area. Thermal conductivity values of liquid metals are much higher than those for non-metallic liquids. For example, liquid sodium at 644 K has k = 72.3 W/ (mK); liquid potassium at 700 K has k = 39.5 W/(mK); and liquid bismuth at 589 K has k = 16.4 W/(mK).
Thermal conductivity of gases is given by,
where, |
V = mean molecular velocity |
|
l = mean free path |
|
cv = specific heat of gas at constant volume |
|
ρ = density |
where |
G = Universal gas constant = 8314.2 J/kmol K |
|
M = molecular weight of gas |
|
T = absolute temperature of gas, K |
i.e. mean molecular velocity varies directly as the square root of absolute temperature and inversely as the square root of molecular weight of a gas. Specific heat, cv also increases as temperature increases. As a result, thermal conductivity of gases increases as temperature increases.
Fig. 2.8 and Fig. 2.9 show the variation of k with temperature for a few gases.
FIGURE 2.8 Variation of k with temperature for a few gases
FIGURE 2.9 Variation of k with temperature for hydrogen and helium
It is appropriate here to consider insulation systems generally used. In industries where huge amount of thermal energy is dealt with, be it for high temperature or low temperature application, it is necessary to see that the most suitable insulation is adopted. This has become particularly important now, since there is widespread awareness about the energy crunch and the cost of energy.
Insulation is required for high temperature systems as well as low temperature systems. In high temperature systems, any leakage of heat from boilers, furnaces or piping carrying hot fluids represents an energy loss. Similarly, in low temperature/cryogenic systems, any heat leakage into the low temperature region represents an energy loss since from thermodynamics we know that to pump out a given amount of heat from a low temperature region would need a disproportionately large amount of work to be put in at room temperature.
Insulation systems may be classified as,
Since in non-homogeneous insulation materials, a combination of conduction, convection or radiation is involved, they are characterised by an “effective thermal conductivity”. Solid materials have cells of spaces formed inside them by foaming. There may be air or some other gas inside these voids. Type of gas used affects the property of the material. Obviously, density of these systems plays an important role in determining the effective thermal conductivity. Sometimes, the intervening spaces are evacuated to reduce the convection losses. To get extremely low values of thermal conductivity—of the order of a few μW/(mK)—multiple layers of highly reflective materials are introduced in between the insulation layers. These are called superinsulations and are used in cryogenic and space applications.
FIGURE 2.10 Conduction heat flow through a slab—thermal resistance
Table 2.3 gives details about some of the common insulations used in industry.
TABLE 2.3 Common Insulations used in Industry
Consider a slab of thickness L, constant thermal conductivity k, with its left and right faces maintained at temperatures T1 and T2. If T1 is greater than T2, we know that heat will flow from left to right and the heat flow rate is given by Fourier’s law,
Now, consider this: in a pipe carrying a fluid, the flow occurs under a driving potential of a pressure difference and there is resistance to flow due to pipe friction; in an electrical conductor, flow of electricity occurs under the driving potential of a voltage difference and there is a resistance to the flow of electric current. Similarly, considering Eq. 2.9, we can say that flow of heat Q occurs in the slab by conduction under a driving potential of a temperature difference (T1 – T2) and the material offers a thermal resistance to the flow of heat. So, we can write Eq. 2.9 as,
Rth L/(kA) is known as Thermal resistance of the slab for conduction.
It is seen that there is a clear analogy between the flow of heat and flow of electricity, as shown below,
Fig. 2.10 above shows the thermal circuit for the situation of flow of heat through a plane slab by conduction. For the slab, we write,
Note that units of thermal resistance is (C/W) or, K/W.
Consider the case of a fluid flowing with a free stream velocity U and free stream temperature Tf, over a heated surface maintained at a temperature Ts. Let the heat transfer coefficient for convection between the surface and the fluid be h. Then, the heat transfer rate from the surface to the fluid is given by Newton’s rate equation,
This can be written as,
Again, note the analogy between flow of electricity and the flow of heat (see Fig. 2.11).
FIGURE 2.11 Convection heat transfer — thermal resistance
So, for heat transfer by convection, we write,
Note that the units are (C/W) or (K/W).
For the case of heat transfer between two finite surfaces, at temperatures T1 and T2 (Kelvin), net radiation heat transfer between them is given by equation,
where, F1 is known as shape factor or view factor, which includes the effects of orientation, emissivities and the distance between the surfaces. s is the Stefan–Boltzmann constant.
Write the above equation in the following form,
Clearly, the radiation thermal resistance may be written as,
There are two important practical application of the thermal resistance concept:
But in some other cases, the thermal resistances may be in parallel; for example, a heated wall of a furnace may lose heat to ambient by convection as well as radiation, i.e. heat transfer occurs from the wall by these two modes simultaneously in parallel. Then we apply the rule for parallel resistances, i.e. effective resistance is given by,
Thermal resistance concept can be used only when all the following conditions are satisfied.
Note: In this chapter, we have just introduced the concept of thermal resistance. We will study more about this concept and apply it to analyse heat transfer in composite slabs, cylinders and spheres and also to situations where more than one mode of heat transfer exist simultaneously, in Chapter 4. Therein, we shall also solve several numerical problems to illustrate the applications of this concept.
Often, during heat transfer analysis, particularly while dealing with transient conduction problems, we come across a quantity called Thermal diffusivity, defined as,
where, |
k = thermal conductivity of the material, W/(mC) |
|
ρ = density, kg/m3 |
|
cp = specific heat at constant pressure, J/(kg.C) |
Note that unit of α is m2/s.
Let us consider the physical significance of thermal diffusivity, α: Thermal conductivity (k) of a material is a transport property and denotes its ability to conduct heat; higher the value of k, better the ability of material to conduct heat. The product (ρ cp) is known as volumetric heat capacity, has units of J/(m3K), and denotes the ability of the material to store heat. Higher the value of (ρcp), larger the heat storage capacity. Generally, solids and liquids which are good storage media have higher volumetric heat capacity (> 1 MJ/m3 K) as compared to gases (about 1 kJ/m3 K), which are poor heat storage media. Therefore, thermal diffusivity, i.e. the ratio of k to (ρcp) gives the relative ability of the material to conduct heat as compared to its ability to store heat. Larger the value of α, faster the propagation of heat into the material. In other words, α represents the ability of the material to respond to changes in the thermal environment; larger the value of α, quicker the material will come into thermal equilibrium with its surroundings. Values of α for materials vary over a wide range. For example, for copper at room temperature, its value is approx. 113 × 10−6 m2/s, whereas for glass it is about 0.34 × 10−6 m2/s.
Table 2.4 shows typical values of thermal diffusivity for a few materials.
In this chapter, we studied Fourier’s law for one-dimensional conduction. This is a very important topic and student must be clear about the assumptions behind this law; particularly, you should note that the area used in applying this law is the area normal to the direction of heat flow. Fourier’s law opens the door for further learning about conduction; we will use it immediately in the next chapter to derive the general differential equation for conduction heat transfer. In this chapter, we also studied two important consequences of Fourier’s law: firstly, definition of thermal conductivity—an important transport property of material—and, secondly, concept of thermal resistance. We studied in some detail about the thermal conductivity of solids, liquids and gases and the variation of thermal conductivity with temperature. Thermal diffusivity—a significant property while studying transient conduction—was mentioned and its physical significance explained.
TABLE 2.4 Typical values of thermal diffusivity (α) for a few materials at room temperature
Material | α × 106, (m2/s) |
---|---|
Silver |
149 |
Gold |
127 |
Copper |
113 |
Aluminium |
97.5 |
Iron |
22.8 |
Mercury (l) |
4.7 |
Marble |
1.2 |
Ice |
1.2 |
Concrete |
0.75 |
Brick |
0.52 |
Glass |
0.34 |
Glasswool |
0.23 |
Water (l) |
0.14 |
Beef |
0.14 |
Wood (oak) |
0.13 |
In the next chapter, we shall derive the general differential equation for conduction which, when solved, will give the temperature distribution in a material; knowing the temperature distribution, we can easily determine the heat transfer rate by applying the Fourier’s law.
Questions
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