Let us consider a
parallel-faced slab whose cross-sectional area is A and length L. Let its faces
be maintained at steady temperatures θ1 and θ2. Heat will flow through the slab
from the face at higher temperature θ1 to that at the lower temperature θ2. Let
us assume that no heat escapes out from the sides of the slab by convection or
radiation. Thus, the lines of flow will be at all points normal to the faces of
the slab. In these circumstances, under steady state, the quantity of heat Q
entering one face in a given time is same as the heat leaving the other face in
the same time. Experiment shows that the heat Q is
- Directly proportional to
the cross-sectional area A of each face, that isQ α A,
- Directly proportional to
the temperature-difference (θ1 – θ2) between the two
faces, that is,Q α (θ1 – θ2),
- Directly proportional to
the time t for which the heat flows, that is,Q α t
- Inversely proportional
to the length 1 of the slab (distance between hot and cold faces), that is,Q α 1/t
Q α A (θ1 – θ2) t
/ l
Q = KA (θ1 – θ2) t
/ l
Where K is a constant
depending on the material of the slab. It is called the "coefficient of
thermal conductivity" of the material of the slab. The coefficient of
thermal conductivity K of a material is defined as the amount of heat that
flows in unit time through unit area of the material perpendicular to the flow
under unit temperature-gradient, when the steady state has been reached.
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