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FORMATION FACTOR BOUNDS

To obtain some useful bounds, I again consider the form of (1)  
 \begin{displaymath}
G(g_1,g_2) = \frac{g_1}{F_1} + \frac{g_2}{F_2} +
\int_0^\infty \frac{dx {\cal G}(x)}{\frac{1}{g_1} + \frac{x}{g_2}}.
 \end{displaymath} (4)
For reasons that will become apparent I want to compare the values of G(g1+2g0,g2+2g0) and G(g1,g2)+2g0, where g0 can take any positive value, but g0 is limited in the negative range by the limitations that both g1+2g0 and g2+2g0 must always be nonnegative. A straightforward, but somewhat tedious calculation shows that  
 \begin{displaymath}
\begin{array}
{l}
G(g_1+2g_0,g_2+2g_0) - G(g_1,g_2) - 2g_0 =...
 ...cal
G}(x)}{(1+x)(g_2+xg_1)[g_2+xg_1+2(1+x)g_0]}\, .\end{array} \end{displaymath} (5)
The right hand side of this equation is always positive whenever g0 >0 and $g_1 \ne g_2$. It vanishes when g0 = 0 or g1 = g2. If g1 < g2, then for negative values of the parameter g0, allowed values of g0 lie in the range $0 \gt 2g_0 \ge -g_1$. For such values of g0, the right hand side of (5) is strictly negative.

The limiting case obtained by taking $2g_0 \to -g_1$ is most useful because, in this limit, $G(g_1+2g_0,g_2+2g_0) \to (g_2-g_1)/F_2$-- thus eliminating the unknown functional ${\cal G}(x)$ from this part of the expression. Then, (5) shows that  
 \begin{displaymath}
G(g_1,g_2) \ge g_1 + \frac{g_2-g_1}{F_2} \equiv S_2(g_1,g_2),
 \end{displaymath} (6)
which is a general lower bound on G(g1,g2) without any further restrictions on the measurable quantities $g_1 \le g_2$, and F2.

A second bound can be obtained (again in the limit 2g0 = -g1) by noting that  
 \begin{displaymath}
\int_0^\infty \frac{dx x{\cal G}(x)}{(1+x)(g_2+xg_1)} \le
\int_0^\infty \frac{dx {\cal G}(x)}{g_2+xg_1},
 \end{displaymath} (7)
and then recalling that  
 \begin{displaymath}
\int_0^\infty \frac{dx {\cal G}(x)}{g_2+xg_1} =
\frac{1}{g_1g_2}\left[G(g_1,g_2) - \frac{g_1}{F_1} -
\frac{g_2}{F_2}\right].
 \end{displaymath} (8)
Substituting (7) into (5) produces an upper bound on G(g1,g2). By subsequently substituting (8) and then rearranging the result, the final bound is  
 \begin{displaymath}
G(g_1,g_2) \le g_2 + \frac{g_1-g_2}{F_1} \equiv S_1(g_1,g_2).
 \end{displaymath} (9)

Comparing (6) and (9), I see consistency requires that  
 \begin{displaymath}
g_1 + \frac{g_2-g_1}{F_2} \le g_2 + \frac{g_1-g_2}{F_1}
 \end{displaymath} (10)
must be true. Rearranging this expression gives the condition  
 \begin{displaymath}
0 \le (g_2-g_1)\left(1 - \frac{1}{F_1} - \frac{1}{F_2}\right),
 \end{displaymath} (11)
the validity of which I need to check. In the limit g1 = g2 = 1, a sum rule follows from (4), and from this I have:  
 \begin{displaymath}
1 - \frac{1}{F_1} - \frac{1}{F_2} = \int_0^\infty\frac{dx {\cal G}(x)}{1+x} \ge 0.
 \end{displaymath} (12)
This shows explicitly that (11) is always satisfied as long as $g_2 \ge g_1$. If this inequality $g_2 \ge g_1$does not hold, then the sense of the bounding inequalities is changed, so the expressions for the upper and lower bounds trade places.

When $g_2 = \hbox{const}$ and g1 varies (as would be expected in a series of thermal conductivity experiments with different fluids in the same porous medium), then (6) and (9) are both straight lines that cross at g1 = g2. The general bounds are therefore  
 \begin{displaymath}
\min(S_1,S_2) \le G(g_1,g_2) \le \max(S_1,S_2),
 \end{displaymath} (13)
where S1 and S2 were defined in (6) and (9).


next up previous print clean
Next: SECOND DERIVATION Up: Berryman: Bounds on transport Previous: THE ANALTYICAL FORMULATION
Stanford Exploration Project
10/23/2004