Waring, C. L. and Stepanyants, Y. A. and Hankin, S. I. and Airey, P. L. and Peterson, M. A. (2009) Measurement of hydraulic conductivity, porosity and lithology by neutron activation borehole logging at high spatial resolution increments. In: IAH Groundwater in The Sydney Basin Symposium, 4-5 Aug 2009, Sydney, Australia.
Text (Published Version)
A new method of measuring the continuously variable hydraulic conductivity at 20 cm increments surrounding a borehole is described. The method requires injection of a tracer solution and measurement of the variable lateral distance the tracer has moved by prompt gamma neutron activation analysis (PGNAA) geophysical logging. Gamma spectra collected by PGNAA logging from 0.16 to 10 MeV are
analysed to provide a relative abundance of elements H, Si, Al, Fe, Cl and possibly others if sufficiently abundant. The distance a NaCl or KCl tracer solution has migrated into the rock surrounding the borehole is calculated from the greater energy attenuation of a 1.95 MeV low energy Cl gamma emission compared to a 6.1 or 7.4 MeV high energy Cl emission. The differential gamma attenuation is verified by
A simple but sensitive method for measuring relative porosity surrounding a borehole is also presented by measuring the elemental abundances of common rock forming minerals and water, allocating elements to minerals and presenting a water/rock ratio. Relative porosity may be further simplified to H/(H+Si) particularly for sandstones typical from the Sydney Basin. Many boreholes of
hydrological interest are drilled into sedimentary rocks and alluvium dominated by abundant quartz and clay, which can be quantified by relative Si and Al. Similarly, many sedimentary lithologies may be defined by variations in their mineralogy reflected in proportional changes in elemental abundance.
Subtle variations in lithology not apparent by visual inspection such as degree of cementation or clay pore
filling in sandstone may also be detected. Porosity and lithology estimation by PGNAA geophysical logging does not require a tracer solution to be injected and may be measured through borehole casing with screened or unscreened intervals.
Statistics for this ePrint Item
|Item Type:||Conference or Workshop Item (Commonwealth Reporting Category E) (Paper)|
|Publisher:||International Association of Hydrogeologists, New South Wales Branch|
|Item Status:||Live Archive|
|Additional Information (displayed to public):||Presentation is at http://www.dealersgroup.com.au/kb/3-waring-c---hydraulic-conductivity-porosity-and-lithology.pdf|
|Depositing User:||Assoc Prof Yury Stepanyants|
|Faculty / Department / School:||Historic - Faculty of Sciences - Department of Maths and Computing|
|Date Deposited:||04 Mar 2010 10:59|
|Last Modified:||09 Dec 2013 02:47|
|Uncontrolled Keywords:||hydraulic conductivity, geophysics, neutron activation, porosity, borehole logging, PGNAA|
|Fields of Research (FoR):||05 Environmental Sciences > 0503 Soil Sciences > 050305 Soil Physics
05 Environmental Sciences > 0503 Soil Sciences > 050399 Soil Sciences not elsewhere classified
|Socio-Economic Objective (SEO):||E Expanding Knowledge > 97 Expanding Knowledge > 970104 Expanding Knowledge in the Earth Sciences|
Actions (login required)
|Archive Repository Staff Only|