One important feature concerning connections betweens the points in
the two planes (,
) and
(
,
) is the fact that
(with only a few exceptions that will be noted)
straight lines in one plane transform into straight lines in the
other. For example, points satisfying
= A + B
in the (,
)-plane (where A and B are constant
intercept and slope, respectively), then satisfy
= A^-1 - A^-1B
in the (,
)-plane. So long as
in (AB1), the straight line in (AB1) transforms into the
straight line in (AB2). This observation is very important because
the straight line in (patchy) corresponds to a straight line
in the saturation-proxy plot in the (
,
)-plane.
But this line transforms into a straight line in data-sorting
plot in the (
,
)-plane. In fact the
apparent straight line along which the data align themselves
in these plots is just this transformed patchy saturation line.
When A = 0 in (AB1) [which seems to happen rarely if ever in the real
data examples, but needs to be considered in general], the resulting
transformed line will just be one of constant ,which is a vertical line on the (
,
)-plane.
The more interesting special case is when B=0, in which situation
or
. But this case includes
that of Gassmann-Domenico for homogeneous mixing of the fluids at
low to moderate saturation values. For B = 0, on both planes we
have horizontal straight lines, but their lengths can differ
significantly on the two displays.