Jump to content

Green's theorem

From Wikiversity

Let be a smooth (differentiable) two-component vector field (or the pair of functions ) on the two dimensional space then the line integral of the field projection onto the unite length vector anti-clockwise field always smoothly tangent to the closed curved over the arbitrary two dimensional closed curve equals the integral of the difference of the partial derivatives , and over the plane region bounded inside the curve or otherwise the outside of the curve values of the field make virtually no contributions to the integral over the region providing that the field is sufficiently smooth that the second derivatives of the field components exists in the region i.e.

where and is the region enclosed by the curve .

Proof

[edit | edit source]

We can approximate the integral on the right side over the region by the finite sum by dividing densely the space around the region into small squares with the sides and the vertices and approximating the bounding curve of the region by the sides of squares which are the closet to the curve as well as the coordinate derivatives of the field by their difference quotients. We will keep the vertices coordinate names for the convenience even if they are equal and keep the square vertices coordinate indices even if they are limited by the region bounded by the curve.

We get

Now the essential in proving the theorem is to focus on the contribution to the finite sum approximating the region integral from the one component of the field itself and notice that because of the cancelation of the sign alternating term the sums reduce to only the end points. For example for and the fixed -line and its length we have

,

Note that while is an infinitesimal (small) linear element of the region boundary curve parallel to the axis and for the unite vector parallel to it and so for the second point with the minus sign the right side is an approximate to the growth of the counter-clockwise line integral i.e.

.

Summing up all the all the contributions over and repeating the considerations for the field component leading to the contributions of the region boundary curve integral we get

and so finally prove .