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KIRTLAND AIR FORCE BASE ALBUQUERQUE, NEW MEXICO ...

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APPENDIX B<br />

Redox potential or the oxidation/reduction of sulfide mineralization such as pyrite, and<br />

Electromechanical potential or streaming potential from fluid flow directly into or out of the<br />

formation.<br />

The 16-inch Short Normal Resistivity and 64-Inch Long Normal Resistivity logs measure apparent<br />

formation resistivity, utilizing both current and potential electrodes in the borehole and a reference<br />

surface electrode. The formation resistivity, measured in ohm-meters, is affected by grain size, porosity,<br />

and pore fluid. The 16- and 64-inch normal is a quantitative measurement. The radius of investigation of<br />

this tool is related to the spacing between the current and potential electrodes, which in this case is 16 or<br />

64 inches. In highly resistive formations, the radius of investigation is reduced. In hard, low porosity<br />

crystalline formations with very fresh pore water, the apparent resistivity is high. Fracturing in a<br />

crystalline environment has the effect of increasing apparent porosity and thus reducing apparent<br />

resistivity.<br />

The Guard Resistivity measurement is a focused resistivity log. It consists of two guarding electrodes<br />

and a current electrode. In the fluid-filled portion of the borehole, the log is used for very thin bed<br />

resolution and to approximate formation resistivity.<br />

The Induced Polarization (IP) log is a time domain measurement of the residual charge storage (or decay<br />

or secondary voltage) after the formation has been excited with a constant current pulse that is then<br />

turned off. Measurement of the secondary voltage corresponds to the polarizability of the formation.<br />

The secondary voltage is normalized with respect to the primary voltage pulse with IP effect expressed as<br />

the ratio of secondary voltage to primary voltage. Log values are displayed as a ―percentage‖ with 1<br />

percent IP response corresponding to 10 mV/v.<br />

IP logs are generally used qualitatively to semi-qualitatively to detect disseminated sulfide (pyrite) and<br />

sometimes montmorillonite clay.<br />

Caliper Measurement<br />

The caliper log is a mechanical three-arm or a single-arm measurement that physically determines the<br />

average diameter of a borehole. The diameter increases in cavities and, depending on the drilling<br />

techniques used, in weathered zones. An apparent decrease in borehole diameter may result from mud or<br />

drill cutting accumulation along the sides of the borehole and in the bottom of a boring. Data from the<br />

caliper log is used to vertically locate cavities or washouts and to diameter that directly affects the<br />

response of other measurements.<br />

Sonic Measurement A sonic log shows travel times of acoustic waves through rock in microseconds. It<br />

is sometimes accompanied by an amplitude log and a Variable Density Log (VDL) of the full sonic<br />

waveforms. Spacings from 18 to 60 inches or more can be made depending on the specific objectives.<br />

Sonic logs can only be obtained in a fluid filled borehole. Additionally, high-quality sonic logs may not<br />

be acquired where the formation is not fully saturated or poorly consolidated even if the borehole is fluid<br />

filled in this region.<br />

The transmitter on the sonic probe emits an approximate 30 Khz ultrasonic pulse twice a second. This<br />

waveform passes through the borehole fluid in all directions at the fluid velocity (approximately 5000 ft<br />

per second). When it reaches the borehole wall, the waveform travels through the rock mass at higher<br />

velocities and is refracted to 2 different receivers on the logging probe 1 ft apart.<br />

Kirtland AFB<br />

SOPs for Field Investigations B-30 April 2004

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