T8 Environmental Issues Related to Oil and Gas Exploration and Production I
Sunday, 16 October 2005
8:00 AM - 12:00 PM
BOREHOLE INDUCTION CONDUCTIVITY AND NATURAL GAMMA LOGGING AT THE OSAGE SKIATOOK RESEARCH SITE, NORTHEASTERN, OKLAHOMA: LESSONS LEARNED
Paper number: T8-4
Program: Technical Sessions
Time: 8:40 AM – 8:55 AM
Authors
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Bruce D. SmithN/A, Denver, CO
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Robert A. ZielinskiU.S. Geological Survey, Denver, CO
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James J. ThordsenMenlo Park, CA
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James K. OttonU.S. Geological Survey, Lakewood, CO
Abstract
The induction conductivity logs show the vertical distribution of soluble salts in the unsaturated zone and of saline ground water in the saturated zone. Induction conductivity logs augment chemical analyses of soil/rock extracts and ground-water samples, and improve estimates of the total volume of rock affected by salts. For example, higher conductivity values found in some shales indicated the extent of penetration of sodium chloride contamination into these low permeability rocks.
Gamma-ray logs were used to identify distinctive radioactive layers and these were used for lithologic correlations. When used in combination with conductivity logs, the gamma-ray logs provided additional lithologic information to supplement, or substitute for, core sample descriptions.
Vertical profiles of estimated electrical conductivity were used in calibration and interpretation of surface electrical conductivity surveys. The borehole logs have provided critical data to assist in other aspects of the study including geologic, geochemical, and hydrologic interpretations.