Let
be a smooth (differentiable) scalar field on the three dimensional space and the vector field
is its gradient then the integral of the field gradient projection onto the unite length vector field
always tangent to the curve and pointing continuously along the curve over the arbitrary 3-dimensional curve
with the start point
and the end point
equals only to the difference of the values of the field itself at those points or otherwise the along-line values of the field make virtually no contributions to the integral over the curve providing that the field is sufficiently smooth that its gradient exists along the curve i.e.
where
and the
and
are the consecutive endpoints of
.
We can approximate the integral of the gradient over the curve by the finite sum by dividing densely the space around the curve
into small cubes with the edges
and the corners
and approximating the curve
by the edges of those cubes which are the closet to the curve as well as the coordinate derivatives
of the field
in the gradient by their difference quotients. We will keep the edges coordinate names for the convenience even if they are equal and keep the cube corners coordinate indices
even if they are constrained by the closeness to the curve.
We get
where
is the sign of the contribution depending if the integration over the edge of the cube is in the positive or the negative direction of the perpendicular coordinate.
Note that while
(and so analogically for
and
) is an infinitesimal (small) element of the line parallel to the
axis and for the unite vector
parallel to it
and each term if the sum is an approximate to the growth
of the line integral
i.e.
.
Now the essential in proving the theorem is to focus on the various types of contributions to the finite sum approximating the gradient line integral from the
field and notice that because of the cancelation of the sign alternating terms the sums reduce to only the end points difference. We simply have
,
where
and
,
are the coordinates of the cubic lattice edges near the endpoints
and
of the approximate curve.
To notice that one may consider three cases of the pieces of the approximate curve: 1) When the piece is the long line consisting of many segments with the length
, (or
,
). The sign-alternating terms cancel directly in the sum of difference quotients of the type
to the difference of the endpoint values which later cancel with joining contributions. 2) The piece is the 1-dimensional "stairs" embedded in one 2-dimensional plane of the width
climbing up or down by
(or similarly in two other planes of pairs of directions). In that case the terms differences in one direction cross-cancel to the end points to further cancel with joining contributions between the sum
and
.
3) The 1-dimensional "stairs" are fully 3-dimensional and not in any plane i.e.
,
,
coordinates increments are periodically sequential.
In that case the full sum
cancels to the endpoints because the
shared values of the
at the "stairs" joining points enter the chain sum with the opposite signs.
So summing up all the all the contributions over all of the possible approximate types of the curve pieces approximating fully the curve we get
and so finally prove
.