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Fractured-bedrock aquifer studies based on a descriptive statistics of well-logging data: A case study from the Dajia River basin, Taiwan

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
A simple descriptive-statistical approach is proposed for evaluating the transmissivity of fractured-bedrock under field conditions. Based on standard well logging and identification of structural discontinuities from borehole televiewer, the approach consists of four steps: (1) determination of discontinuity properties, namely the frequency of discontinuities and the ratio of open fractures along the borehole; (2) ranking the three well logs and the discontinuity properties into tertiles (high-to-low); (3) performing statistical analysis (F-test) for the three well logs to assess the significance of open fractures on the water-transmitting potential and then assigned a weighting factor; and (4) a semi-quantitative indicator, RGVFO, is obtained by multiplying all predictive indexes and weighting factors. It is a multi-criteria evaluation procedure that elucidates the quantitative and qualitative importance of all selected geophysical indexes. A high cross-correlation between transmissivity to RGVFO value is found, which indicates that by a combined consideration of well logging and structural discontinuities, an appropriate estimate of bedrock water-transmitting potential can be derived.
Czasopismo
Rocznik
Strony
564--584
Opis fizyczny
Bibliogr. 22 poz.
Twórcy
autor
  • Geotechnical Engineering Research Center, Sinotech Engineering Consultants, Inc., Taipei, Taiwan
autor
  • Geotechnical Engineering Research Center, Sinotech Engineering Consultants, Inc., Taipei, Taiwan
autor
  • Geotechnical Engineering Research Center, Sinotech Engineering Consultants, Inc., Taipei, Taiwan
autor
  • Geotechnical Engineering Research Center, Sinotech Engineering Consultants, Inc., Taipei, Taiwan
autor
  • Geotechnical Engineering Research Center, Sinotech Engineering Consultants, Inc., Taipei, Taiwan
Bibliografia
  • Atekwana, E.A., W.A. Sauck, and D.D. Werkema Jr. (2000), Investigations of geoelectrical signatures at a hydrocarbon contaminated site, J. Appl. Geophys. 44, 2-3, 167-180, DOI: 10.1016/S0926-9851(98)00033-0.
  • Barker, J.A. (1988), A generalized radial flow model for hydraulic tests in fractured rock, Water Resour. Res. 24, 10, 1796-1804, DOI: 10.1029/WR024i010p01796.
  • Binley, A., G. Cassiani, R. Middleton, and P. Winship (2002), Vadose zone flow model parameterisation using cross-borehole radar and resistivity imaging, J. Hydrol. 267, 3-4, 147-159, DOI: 10.1016/S0022-1694(02)00146-4.
  • Budhu, M. (2011), Earth fissure formation from the mechanics of groundwater pumping, Int. J. Geomech. 11, 1, 1-11, DOI: 10.1061/(ASCE)GM.1943-5622.0000060.
  • Chambers, J.E.,O. Kuras., P.I. Meldrum, R.D. Ogilvy, and J. Hollands (2006), Electrical resistivity tomography applied to geologic, hydrogeologic, and engineering investigations at a former waste-disposal site, Geophysics 71, 6, B231-B239, DOI: 10.1190/1.2360184.
  • Chang, Y.C., H.D. Yeh, K.F. Liang, and M.C.T. Kuo (2011), Scale dependency of fractional flow dimension in a fractured formation, Hydrol. Earth Syst. Sci. 15, 7, 2165-2178, DOI: 10.5194/hess-15-2165-2011.
  • Chou, P.Y., H.C. Lo, S.M. Hsu, Y.T. Lin, and C.C. Huang (2012), Prediction of hydraulically transmissive fractures using geological and geophysical attrib utes: a case history from the mid Jhuoshuei River basin, Taiwan, Hydrogeol. J. 20, 6, 1101-1116, DOI: 10.1007/s10040-012-0861-3.
  • Cook, P.G. (2003), A Guide to Regional Groundwater Flow in Fractured Rock Aquifers, Seaview Press, Henley Beach, South Australia.
  • Lato, M.J., M.S. Diederichs, and D.J. Hutchinson (2010), Bias correction for viewlimited Lidar scanning of rock outcrops for structural characterization, Rock Mech. Rock Eng. 43, 5, 615-628. DOI: 10.1007/s00603-010-0086-5.
  • Le Borgne, T., O. Bour, J.R. de Dreuzy, P. Davy, and F. Touchard (2004), Equivalent mean flow models for fractured aquifers: Insights from a pumping tests scaling interpretation, Water Resour. Res. 40, 3, W03512, DOI: 10.1029/2003WR002436.
  • Le Borgne, T., F. Paillet, O. Bour, and J.P. Caudal (2006), Cross-borehole flowmeter tests for transient heads in heterogeneous aquifers, Groundwater 44, 3, 444-452, DOI: 10.1111/j.1745-6584.2005.00150.x.
  • Legchenko, A., J.M. Baltassat, A. Beauce, and J. Bernard (2002), Nuclear magnetic resonance as a geophysical tool for hydrogeologists, J. Appl. Geophys. 50, 1-2, 21-46, DOI: 10.1016/S0926-9851(02)00128-3.
  • Muldoon, M., and K.R. Bradbury (2005), Site characterization in densely fractured dolomite: comparison of methods, Groundwater 43, 6, 863-876, DOI: 10.1111/j.1745-6584.2005.00091.x.
  • Paillet, F.L., J.H. Williams, J. Urik, J. Lukes, M. Kobr, and S. Mares (2011), Crossborehole flow analysis to characterize fracture connections in the Melechov Granite, Bohemian-Moravian Highland, Czech Republic, Hydrogeol. J. 20, 1, 143-154, DOI: 10.1007/s10040-011-0787-1.
  • Sandberg, S.K., L.D. Slater, and R. Versteeg (2002), An integrated geophysical investigation of the hydrogeology of an anisotropic unconfined aquifer, J. Hydrol. 267, 3-4, 227-243, DOI: 10.1016/S0022-1694(02)00153-1.
  • Schultz, R.A., and H. Fossen (2008), Terminology for structural discontinuities, AAPG Bull. 92, 7, 853-867, DOI: 10.1306/02200807065.
  • Sharma, S.P., and V.C. Baranwal (2005), Delineation of groundwater-bearing fracture zones in a hard rock area integrating very low frequency electromagnetic and resistivity data, J. Appl. Geophys. 57, 2, 155-166, DOI: 10.1016/j.jappgeo.2004.10.003.
  • Slater, L., A.M. Binley, W. Daily, and R. Johnson (2000), Cross-hole electrical imaging of a controlled saline tracer injection, J. Appl. Geophys. 44, 2-3, 85-102, DOI: 10.1016/S0926-9851(00)00002-1.
  • Verbovšek, T. (2009), Influences of aquifer properties on flow dimensions in Dolomites, Groundwater 47, 5, 660-668, DOI: 10.1111/j.1745-6584.2009.00577.x.
  • Viviroli, D., H.H. Dürr, B. Messerli, M. Meybeck, and R. Weingartner (2007), Mountains of the world, water towers for humanity: Typology, mapping, and global significance, Water Resour. Res. 43, 7, W07447, DOI: 10.1029/2006WR005653.
  • Williams, J.H., and F.L. Paillet (2002), Using flowmeter pulse tests to define hydraulic connections in the subsurface: a fractured shale example, J. Hydrol. 265, 1-4, 100-117, DOI: 10.1016/S0022-1694(02)00092-6.
  • Zhou, C., L. Liu, and J.W. Lane Jr. (2001), Nonlinear inversion of borehole-radar tomography data to reconstruct velocity and attenuation distribution in earth materials, J. Appl. Geophys. 47, 3-4, 271-284, DOI: 10.1016/S0926-9851(01)00071-4.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-e2d485da-de9c-4639-959d-24b466fe9ec3
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