3 edition of Hole-to-surface resistivity measurements at Gibson Dome (drill hole GD-1) Paradox basin, Utah found in the catalog.
Hole-to-surface resistivity measurements at Gibson Dome (drill hole GD-1) Paradox basin, Utah
|Statement||by Jeffrey J. Daniels ; prepared for Department of Energy, Nuclear Waste Program.|
|Series||Open file report -- 82-320., Open-file report (Geological Survey (U.S.)) -- 82-320.|
|Contributions||Geological Survey (U.S.), United States. Dept. of Energy.|
|The Physical Object|
|Number of Pages||27|
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Hole-to-surface resistivity measurements at Gibson Dome (drill hole GD-1) Paradox basin, Utah (U.S. Geological Survey Open file report) [Jeffrey J Daniels] on *FREE* shipping on Author: Jeffrey J Daniels.
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Everyday low prices and free delivery on eligible : Jeffrey J Daniels. 'Hole-to-surface resistivity measurements at Gibson Dome (drill. hole GD-1) Paradox basin, Utah' -- subject(s): Electric. prospecting, Radioactive waste disposal, Radioactive waste disposal.
Publishing History This is a chart to show the publishing history of editions of works about this subject. Along the X axis is time, and on the y axis is the count of editions published. Geophysical well logging techniques with diagrams Geophysical well logging 'Hole-to-surface resistivity measurements at Gibson Dome (drill hole GD-1) Paradox basin, Utah' -- subject(s.
Some considerations on electrical resistivity imaging for characterization of waterbed sediments. while a dipole–dipole array seems to be more sensitive to the accuracy of apparent resistivity measurements and a priori information on water. J.J. DanielsHole-to-surface resistivity by: The type of material filling the borehole and/or the degree of fluid invasion into the formation also may have a significant effect on interpretations of hole–hole and hole–surface potential measurements out to a distance of several borehole diameters away from the current by: Resistivity analysis for plane-layer half-space models with buried current source.
Electrical resistivity measurements using combinations of subsurface and surface electrodes are more. NDOT unnumbered map book County Maps, Nevada,by the Nevada Highway Department (now Nevada Department of Transportation), 49 oversized maps.
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web; books; video; audio; software; images; Toggle navigation. In the figure, the deep measurements (O to 45 feet) include an averaging of the resistivity of the shallow measurements and the resistivity of the to foot depth interval. Figure b shows a horizontal resistivity profile that indicates lateral changes from clay and gravel material in the subsurface.
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Knowledge of the fluid resistivity and the borehole diameter enables the resistivity measurements to be corrected for borehole effects, resulting in resistivity values that are close to the true resistivity of the rocks. A summary of the typical ranges of resistivities of rocks and soils is.
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