NMR Logging to Estimate Hydraulic Conductivity in Unconsolidated Aquifers |
| |
| Authors: | Rosemary Knight David O Walsh James J Butler Jr Elliot Grunewald Gaisheng Liu Andrew D Parsekian Edward C Reboulet Steve Knobbe Mercer Barrows |
| |
| Affiliation: | 1. Vista Clara Inc., 12201 Cyrus Way, Suite 104, Mukilteo, WA 98275;2. 425‐493‐8122;3. Kansas Geological SurveyUniversity of Kansas, Lawrence, KS 66047;4. (785) 864–2116;5. Vista Clara Inc., 12201 Cyrus Way, Suite 104, Mukilteo, WA, 98275;6. (785) 864–2115;7. 1000 E. University Ave., Dept. 3006University of Wyoming, Laramie, WY 82071;8. (307) 766–3603;9. (785) 864–2173;10. Kansas Geological SurveyUniversity of Kansas Lawrence, KS 66047;11. (785) 864–2111;12. 6010 Canyonside Rd., La Crescenta, CA 91214;13. (818) 415–1913 |
| |
| Abstract: | Nuclear magnetic resonance (NMR) logging provides a new means of estimating the hydraulic conductivity (K) of unconsolidated aquifers. The estimation of K from the measured NMR parameters can be performed using the Schlumberger‐Doll Research (SDR) equation, which is based on the Kozeny–Carman equation and initially developed for obtaining permeability from NMR logging in petroleum reservoirs. The SDR equation includes empirically determined constants. Decades of research for petroleum applications have resulted in standard values for these constants that can provide accurate estimates of permeability in consolidated formations. The question we asked: Can standard values for the constants be defined for hydrogeologic applications that would yield accurate estimates of K in unconsolidated aquifers? Working at 10 locations at three field sites in Kansas and Washington, USA, we acquired NMR and K data using direct‐push methods over a 10‐ to 20‐m depth interval in the shallow subsurface. Analysis of pairs of NMR and K data revealed that we could dramatically improve K estimates by replacing the standard petroleum constants with new constants, optimal for estimating K in the unconsolidated materials at the field sites. Most significant was the finding that there was little change in the SDR constants between sites. This suggests that we can define a new set of constants that can be used to obtain high resolution, cost‐effective estimates of K from NMR logging in unconsolidated aquifers. This significant result has the potential to change dramatically the approach to determining K for hydrogeologic applications. |
| |
| Keywords: | |
|
|
