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Complex Analysis: Explorations with F(Z)
Complimentary software to accompany the text
Complex Analysis: for Mathematics and Engineering
Introduction
In the theory of heat conduction the assumption is made that heat
flows in the direction of decreasing temperature. We also assume that
the time rate at which heat flows across a surface area is
proportional to the component of the temperature gradient in the
direction perpendicular to the surface area. If the temperature
does not
depend on time, then
is given by the vector
where K is the thermal conductivity of the medium and it is
assumed to be constant.
If the domain in which T(x,y) is defined is simply connected, then a
conjugate harmonic function S(x,y) exists, and
is an analytic function. The curves
are called isothermals and are
lines connecting points of the same temperature. The curves
are called the
heat flow lines, and one can visualize the heat flowing along these
curves from points of higher temperature to pints of lower
temperature.
Boundary value problems for steady state temperatures are
realizations of the Dirichelt problem where the value of the harmonic
function T(x,y) is interpreted as the temperature at the point (x,y).
(c) John Mathews, 1998