| Themes > Science > Physics > Geophysics > Systems Methods and Applications > Borehole Geophysics | |
The Method Borehole geophysics provide a means of evaluating a great variety of physical properties of subsurface rocks, sediments, and fluids. Borehole logging offers an economical alternative to continuous sampling or coring, furnishing continuous, objective data sets in a graphical form that can be rapidly interpreted in the field. Additionally, geophysical logging provides information about the subsurface that cannot be obtained through standard drilling and sampling techniques. Some of the more commonly used techniques for downhole geophysical methods are listed below: Natural Gamma Resistivity Electromagnetic
Induction (EM) Spontaneous
Potential (SP) Fluid Temperature &
Resistivity Borehole VideoEmployed to visually inspect boreholes, well casings and screens. Depth encoded images from the borehole camera are recorded for later review, and provide a permanent record of open borehole conditions, fractures, well screen placement, cracks in casing, etc. Field Procedures Downhole probes are lowered
on an armored cable into the borehole. Measurements for most probes
are recorded on the way up the borehole. Data are digitally recorded
allowing for computer processing at a later time. A number of
combination probes (i.e., fluid temperature / resistivity, spontaneous
potential / single point-resistance / natural gamma) are available,
performing several measurements in a single pass through the borehole.
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