Clay
bound water (CBW) is an essential parameter to calculate not
only water saturation but also other petrophysical parameters in shaly
formations. Hence, in order to accurately obtain the information pertaining
the CBW, nuclear magnetic resonance (NMR) is commonly used, which
is sensitive to hydrogen that is adsorbed by clay minerals. Knowing
that temperature can remove CBW, we combined thermal treatment (dehydration
of the samples under a series of temperatures), low field NMR in the
laboratory, and fractal theory to acquire better insights on how NMR
signals can reveal the critical dehydration temperature to determine
the CBW. For this purpose, a shale sample is exposed to a series of
elevated temperatures and then a NMR transverse relaxation signal T
2 was acquired and analyzed with the fractal
theory. The fractal dimensions of the T
2 revealed a sharp decrease as the hydration temperature exceeds a
certain critical value. Furthermore, the T
1/T
2 from the 2D NMR map demonstrated
that at this critical temperature, the signal intensity representing
the hydroxyl group decreases as well, indicating the loss of the absorbed
water. Based on the result, we were able to confirm that fractal dimension
analysis can reveal the critical hydration temperature to ultimately
determine the CBW, most importantly independent of running extra unnecessary
experiments to save costs.