Section Summary: 17.7

Surface Integrals

  1. Definitions

    surface integral of f over the surface S:

    displaymath313

    If the surface is the graph of a function z=g(x,y) over a domain D, then

    displaymath314

    If the surface is given parametrically over the domain D, then

    displaymath315

    If it is possible to choose a unit normal vector n at every point on a surface (excluding boundary points) such that n varies continuously over S, then S is called an oriented surface, and the choice of n provides S with an orientation.

    If S is a smooth orientable surface with parameterization tex2html_wrap_inline351 , then

    displaymath316

    For a closed surface (the boundary of a solid region E) the convention is that the positive orientation points outward from E.

    If F is a continuous vector field defined on an oriented surface S with unit normal vector n, then the surface integral of F over S is

    displaymath317

    also known as the flux of F across S.

    For a surface given as the graph of a function, this works out to

    displaymath318

    In the case of a parameterized surface,

    displaymath319

    Electric flux is the integral

    displaymath320

    where tex2html_wrap_inline361 is an electric field. heat flow is an example of a conservative vector field

    displaymath321

    where u(x,y,z) is the temperature function for a region, and K is the conductivity of the substance through which the heat is flowing. Then the rate of heat flow across the surface S in the body is then given by

    displaymath322

  2. Theorems

  3. Properties/Tricks/Hints/Etc.

  4. Summary

    The calculation of surface integrals is yet another example of the standard old trick of integration: the adding up of multitudinous small things weighted by some function to give a larger thing.

    While it is enough to consider the general case of a parameterized surface, the special results are worked out in the case of a surface given as the graph of a function z=g(x,y).




Fri Sep 16 10:56:11 EDT 2005