Rapid non-contacting resistivity logging of core

Author:

Jackson P. D.1,Lovell M. A.2,Roberts J. A.3,Schultheiss P. J.3,Gunn D.1,Flint R. C.14,Wood A.5,Holmes R.6,Frederichs T.7

Affiliation:

1. British Geological Survey Nottingham NG12 5GG, UK pdj@bgs.ac.uk

2. Department of Geology University of Leicester LE1 7RH, UK

3. Geotek Limited, 3 Faraday Close Daventry, Northampton NN11 5RD, UK

4. Department of Aeronautical & Automotive Engineering Loughborough University LE11 3TU, UK

5. Adrian Wood Associates Danehill, Brookhill Road, Copthorne, Crawley RH10 3PS, UK

6. British Geological Survey Edinburgh EH9 3LA, UK

7. Department of Geosciences, University of Bremen P.O. Box 330 440, D-28334 Bremen, Germany

Abstract

AbstractWe demonstrate a non-contact approach to whole-core and split-core resistivity measurements, imaging a 15 mm-thick, dipping, conductive layer, producing a continuous log of the whole core and enabling the development of a framework to allow representative plugs to be taken, for example. Applications include mapping subtle changes in grain fabric (e.g. grain shape) caused by variable sedimentation rates, for example, as well as the well-known dependencies on porosity and water saturation.The method operates at relatively low frequencies (i.e. low induction numbers), needing highly sensitive coil pairs to provide resistivity measurements at the desired resolution. A four-coil arrangement of two pairs of transmitter and receiver coils is used to stabilize the measurement. One ‘coil pair’ acts as a control, enabling the effects of local environmental variations, which can be considerable, to be removed from the measurement at source.Comparing our non-contact approach and independent traditional ‘galvanic’ resistivity measurements indicates that the non-contact measurements are directly proportional to the reciprocal of the sample resistivity (i.e. conductivity). The depth of investigation is discussed in terms of both theory and practical measurements, and the response of the technique to a variety of synthetic ‘structures’ is presented.We demonstrate the potential of the technique for rapid electrical imaging of core and present a whole-core image of a dipping layer with azimuthal discrimination at a resolution of the order of 10 mm. Consequently, the technique could be used to investigate different depths within the core, in agreement with theoretical predictions.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference7 articles.

1. Carmichael R.S. (1982) Handbook of Physical Properties of Rocks (CRC Press, Boca Raton, FL).

2. (1991) Study of Research and Development Requirements in Core Analysis, Geoscience Report to the Department of Energy (OSO), October 1991 (HMSO, London). DEPARTMENT OF ENERGY.

3. Introduction to induction logging and application to logging of wells drilled with oil base mud;Doll;Transactions of the American Institute of Mining and Metallurgical Engineers,1949

4. Electrical core imaging I: A new technology for high resolution investigation of petrophysical properties;Jackson;Scientific Drilling,1995

5. Electrical core imaging II: investigation of fabric and fluid flow characteristics;Lovell;Scientific Drilling,1995

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