All Issue

2014 Vol.19, Issue 3 Preview Page
30 June 2014. pp. 39 ~ 46
Abstract
Hydraulic conductivity is an important parameter, representing permeable property of the groundwater in aquifers, in the issues of groundwater development, groundwater contamination, and groundwater flow, etc. We estimated a relationship between hydraulic conductivity and electrical properties (formation factor, chargeability, and time constant) of silty sand in the laboratory. For this study, we conducted grain size analysis, constant head permeameter test, and measured electrical resistivity and spectral induced polarization of silty sand samples collected from the riverside alluvium of the Nakdong River in Nogok-ri area, Dasan-myeon, Goryeong-gun in Gyeongbook Province, Korea. In the laboratory test, we used soil samples of approximately uniform porosity with 0.5% error range, and kept the electrical resistivity of pore water with 100 ohm-m. As a result, the relationship between effective particle size and hydraulic conductivity agrees fairly well with the existing empirical formulas. Hydraulic conductivity was correlated with formation factor, chargeability, and time constant: hydraulic conductivity increased with increasing formation factor and time constant as well as with decreasing chargeability.

References
  1. Allessandrello, E. and Lemoine, Y., 1983, Determination de la permeabilite des alluvions a partir de la prospection electrique, Bull. Int. Assoc. Eng. Geol., 26(27), 357-360.
  2. Archie, G.E., 1942, The electrical resistivity log as an aid in determining some reservoir characteristics. Trans. AIME, 146, 54-62.10.2118/942054-G
  3. Binley, A., Slater, L., Fukes, M., and Cassiani, G., 2005, Relationship between spectral induced polarization and hydraulic properties of saturated and unsaturated sandstone, Water Resour. Res., 41(12), W12417
  4. Borner, F.D., Schopper, J.R., and Weller, A., 1996, Evaluation of transport and storage properties in the soil and groundwater zone from induced polarization measurements, Geophysical Prospecting, 44, 583-602.10.1111/j.1365-2478.1996.tb00167.x
  5. Cole, K.S. and Cole, R.H., 1941, Dispersion and absorption in dielectrics. I. Alternating current characteristics, J. Chem. Phys., 9, 341-352.10.1063/1.1750906
  6. Dias, C.A., 1972, Analytical model for a polarizable medium at radio and lower frequencies, J. Geophys. Res., 77(26), 4945-4956.10.1029/JB077i026p04945
  7. Dias, C.A., 2000, Developments in a model to describe low-frequency electrical polarization of rocks, Geophysics, 65(2), 437-451.10.1190/1.1444738
  8. Fetter, C.W., 2001, Applied Hydrogeology, 4th edition, Prentice Hall, 598 p.
  9. Frohlich, R.K., Fisher, J.J., and Summerly, E., 1996, Electrichydraulic conductivity correlation in fractured crystalline bedrock: Central Landfill, Rhode Island, USA, J. Appl. Geophys., 35(4), 249-259.10.1016/0926-9851(96)00028-6
  10. Heigold, P.C., Gilkeson, R.H., Cartwright, K., and Reed, P.C., 1979, Aquifer transmissivity from surficial electrical methods, Ground Water, 17(4), 338-345.10.1111/j.1745-6584.1979.tb03326.x
  11. Jougnot, D., Ghorbani, A., Revil, A., Leroy, P, and Cosenza, P., 2010, Spectral induced polarization of partially saturated clayrocks: a mechanistic approach, Geophys. J. Int., 180, 210-224.10.1111/j.1365-246X.2009.04426.x
  12. Kelly, W.E., 1977, Geoelectric sounding for estimating aquifer hydraulic conductivity. Ground Water, 15(6), 420-425.10.1111/j.1745-6584.1977.tb03189.x
  13. Kemna, A., Binley, A., and Slater, L., 2004, Cross-borehole IP imaging for engineering and environmental applications, Geophysics, 69, 97-107.10.1190/1.1649379
  14. Kim, S., Park, S., and Hamm, S.-Y., 2013, Relationship between hydraulic conductivity and electrical resistivity of standard sand and glass bead, Econ. Environ. Geol., 46(3), 215-220.10.9719/EEG.2013.46.3.215
  15. Koch, K., Kemna, A., Irving, J., and Holliger, K., 2011, Impact of changes in grain size and pore space on the hydraulic conduc tivity and spectral induced polarization response of sand, Hydrol. Earth Syst. Sci., 15, 1785-1794.10.5194/hess-15-1785-2011
  16. Kosinski, W.K. and Kelly, W.E., 1981, Geoelectrical soundings for perdicting aquifer properties, Ground Water, 19(2), 163-171.10.1111/j.1745-6584.1981.tb03455.x
  17. Park, S.G., 2004, Physical property factors controlling the electrical resistivity of subsurface, Jigu-Mulli-wa-Mulli-Tamsa., 7(2), 130-135.
  18. Ponzini, G., Ostroman, A., and Molinari, M., 1983, Empirical relation between electrical transverse resistance and hydraulic transmissivity, Geoexploration, 22(1), 1-15.
  19. Revil, A. and Florsch, N., 2010, Determination of permeability from spectral induced polarization in granular media, Geophys. J. Int., 181, 1480-1498.
  20. Reynolds, J.M., 2011, An Introduction to Applied and Environmental Geophysics, 2nd edition, WILEY, 709 p.
  21. Slater, L. and Lesmes, D.P., 2002, Electrical-hydraulic relationships observed for unconsolidated sediments, Water Resour. Res., 38(10), 31-1 - 31-13.
  22. Slater, L., 2007, Near surface electrical characterization of hydraulic conductivity: From petrophysical properties to aquifer geometries-A review, Surv. Geophys., 28, 169-197.10.1007/s10712-007-9022-y
  23. Todd, D.K. and Mays, L.W., 2005, Groundwater hydrology, 3rd edition, John Wiley & Sons Inc., 636 p.
  24. Tong, M., Wang, W., Li, L., Jiang, Y., Shi, D., 2004, Estimation of permeability of shaly sand reservoir from induced polarization relaxation time spectra, J. Petrol. Sci. Eng., 45, 1-10.10.1016/j.petrol.2004.05.007
  25. Urish, D.W., 1981, Electrical resistivity-hydraulic conductivity relationships in glacial outwash aquifers, Water Resour. Res., 17(5), 1401-1408.10.1029/WR017i005p01401
Information
  • Publisher :The Korean Society of Soil and Groundwater Environment
  • Publisher(Ko) :한국지하수토양환경학회
  • Journal Title :Journal of Soil and Groundwater Environment
  • Journal Title(Ko) :지하수토양환경
  • Volume : 19
  • No :3
  • Pages :39 ~ 46