Abstract
The equations describing a boundary value problem for a vector field u are often equivalent to a variational principle containing an integral ƒf.δud∑ over a part ∑ of the boundary, where f is a prescribed function either of position or, more generally, of the surface values of u and its surface derivatives. In the latter case it is not obvious when such an integral can be written in the useful form δƒ
D
d∑ in terms of a ‘surface potential’ function
D
. This question is here examined in some detail from a general standpoint, with examples.
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