(thermodynamics) The flow of thermal energy through a substance from a higher-to a lower-temperature region.
| Sci-Tech Dictionary: heat conduction |
(thermodynamics) The flow of thermal energy through a substance from a higher-to a lower-temperature region.
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| Sci-Tech Encyclopedia: Conduction |
The flow of thermal energy through a substance from a higher- to a lower-temperature region. Heat conduction occurs by atomic or molecular interactions. Conduction is one of the three basic methods of heat transfer, the other two being convection and radiation. See also Convection (heat); Heat radiation; Heat transfer.
Steady-state conduction is said to exist when the temperature at all locations in a substance is constant with time, as in the case of heat flow through a uniform wall. Examples of essentially pure transient or periodic heat conduction and simple or complex combinations of the two are encountered in the heat-treating of metals, air conditioning, food processing, and the pouring and curing of large concrete structures. Also, the daily and yearly temperature variations near the surface of the Earth can be predicted reasonably well by assuming a simple sinusoidal temperature variation at the surface and treating the Earth as a semi-infinite solid. The widespread importance of transient heat flow in particular has stimulated the development of a large variety of analytical solutions to many problems. The use of many of these has been facilitated by presentation in graphical form.
For an example of the conduction process, consider a gas such as nitrogen which normally consists of diatomic molecules. The temperature at any location can be interpreted as a quantitative specification of the mean kinetic and potential energy stored in the molecules or atoms at this location. This stored energy will be partly kinetic because of the random translational and rotational velocities of the molecules, partly potential because of internal vibrations, and partly ionic if the temperature (energy) level is high enough to cause dissociation. The flow of energy results from the random travel of high-temperature molecules into low-temperature regions and vice versa. In colliding with molecules in the low-temperature region, the high temperature molecules give up some of their energy. The reverse occurs in the high-temperature region. These processes take place almost instantaneously in infinitesimal distances, the result being a quasi-equilibrium state with energy transfer. The mechanism for energy flow in liquids and solids is similar to that in gases in principle, but different in detail.
| Sports Science and Medicine: heat conduction |
The transfer of heat from the warmer to the cooler of two solid bodies that are in contact. In the human body, the rate of conduction depends on the temperature gradient between the skin and the material with which the skin is in contact, and on the thermal properties of the material. See also clo unit.
| Wikipedia: Conduction (heat) |
In heat transfer, conduction (or heat conduction) is the transfer of thermal energy between neighboring molecules in a substance due to a temperature gradient. It always takes place from a region of higher temperature to a region of lower temperature, and acts to equalize temperature differences. Conduction takes place in all forms of matter, viz. solids, liquids, gases and plasmas, but does not require any bulk motion of matter. In solids, it is due to the combination of vibrations of the molecules in a lattice and the energy transport by free electrons. In gases and liquids, conduction is due to the collisions and diffusion of the molecules during their random motion.
Heat can also be transferred by radiation and/or convection, and often more than one of these processes occur in a given situation.
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The law of Heat Conduction, also known as Fourier's law, states that the time rate of heat transfer through a material is proportional to the negative gradient in the temperature and to the area at right angles, to that gradient, through which the heat is flowing. We can state this law in two equivalent forms: the integral form, in which we look at the amount of energy flowing into or out of a body as a whole, and the differential form, in which we look at the flows or fluxes of energy locally.
The differential form of Fourier's Law of thermal conduction shows that the local heat flux,
, is equal to the product of thermal conductivity, k, and the negative local temperature gradient,
. The heat flux is the amount of energy that flows through a particular surface per unit area per unit time.

where (including the SI units)
is the local heat flux, [W·m−2]
is the material's conductivity, [W·m−1·K−1],
is the temperature gradient, [K·m−1].The thermal conductivity, k, is often treated as a constant, though this is not always true. While the thermal conductivity of a material generally varies with temperature, the variation can be small over a significant range of temperatures for some common materials. In anisotropic materials, the thermal conductivity typically varies with orientation; in this case k is represented by a second-order tensor. In nonuniform materials, k varies with spatial location
For many simple applications, Fourier's law is used in its one-dimensional form. In the x-direction,

By integrating the differential form over the material's total surface S, we arrive at the integral form of Fourier's law:

where (including the SI units)
is the amount of heat transferred per unit time [W] and
is an oriented surface area element [m2]The above differential equation, when integrated for a homogeneous material of 1-D geometry between two endpoints at constant temperature, gives the heat flow rate as:

where
This law forms the basis for the derivation of the heat equation. Ohm's law is the electrical analogue of Fourier's law.
Writing

where U is the conductance, in W/(m2 K).
Fourier's law can also be stated as:

The reciprocal of conductance is resistance, R, given by:

and it is resistance which is additive when several conducting layers lie between the hot and cool regions, because A and Q are the same for all layers. In a multilayer partition, the total conductance is related to the conductance of its layers by:

So, when dealing with a multilayer partition, the following formula is usually used:

When heat is being conducted from one fluid to another through a barrier, it is sometimes important to consider the conductance of the thin film of fluid which remains stationary next to the barrier. This thin film of fluid is difficult to quantify, its characteristics depending upon complex conditions of turbulence and viscosity, but when dealing with thin high-conductance barriers it can sometimes be quite significant.
The previous conductance equations written in terms of extensive properties, can be reformulated in terms of intensive properties.
Ideally, the formulae for conductance should produce a quantity with dimensions independent of distance, like Ohm's Law for electrical resistance:
, and conductance:
.
From the electrical formula:
, where ρ is resistivity, x = length, A cross sectional area, we have
, where G is conductance, k is conductivity, x = length, A = cross sectional area.
For Heat,

where U is the conductance.
Fourier's law can also be stated as:

analogous to Ohm's law:
or 
The reciprocal of conductance is resistance, R, given by:

analogous to Ohm's law: 
The sum of conductances in series is still correct.
Conduction through cylinders can be calculated when variables such as the internal radius r1, the external radius r2, and the length denoted as
.
The temperature difference between the inner and outer wall can be expressed as T2 − T1.
The area of the heat flow: 
When Fourier’s equation is applied:

Rearranged:

Therefore the rate of heat transfer is

The thermal resistance is

And
, where
and it is important to note that this is the log-mean radius.
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