Chapter 7 Gamma Ray (GR) log
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Transcript of Chapter 7 Gamma Ray (GR) log
Chapter 7
Gamma Ray (GR) log
Lecture notes for PET 370
Spring 2012
Prepared by: Thomas W. Engler,
Ph.D., P.E.
GR Log Uses
• Estimate bed boundaries, stratigraphic correlations
• Estimate shale content
• Perforating depth control
• Identify mineral deposits of potash, uranium, and coal
• Monitor movement of injected radioactive material
GR Log Background
• The Gamma Ray log is a continuous measurement of
the natural radioactivity emanating from the formations.
• Principal isotopes emitting radiation are Potassium-40,
Uranium, and Thorium (K40, U, Th)
• Isotopes concentrated in clays; thus higher radioactivity
in shales than other formations.
• Sensitive detectors count the number of gamma rays per
unit of time
• Recorded in “API Units” which is 1/200th of the
calibrated, standard response.
GR Log General GR Response
GR Log Factors affecting tool response
(1). Radiation intensity of the formation
(2). Counter’s efficiency
(3). Time constant (rc)
(4). Logging speed
(5). Borehole environment
GR Log
Gamma Ray Logs never repeat
exactly! The minor variations are
statistical fluctuations due to the
random nature of the radioactive
pulses reaching the detector.
Typical ranges are 5 - 10 API Units in
shales, and 2 - 4 units in clean
formations
Reduce statistical fluctuations by
optimizing the time constant and
logging speed.
Time constant/logging speed
GR Log
Effect of Time Constant
and Logging Speed
on bed resolution
Time constant/logging speed
GR Log The faster the logging speed, the less time the tool can sufficiently react and
properly count the radiation intensity.
Two effects:
1. The tool response is shifted in the direction the tool is moving. This
lag or critical thickness (hc) is given by hc = n tc; where n is logging
speed (ft/sec) and tc is the time constant (sec).
2. The log cannot properly respond when h < hc
Time constant/logging speed
GR Log
The time constant and logging speed are regulated so that the GR log
is representative of the formation radioactivity.
1. By experience, hc = 1 ft., avoids excessive distortion of the GR
curve.
2. Common combinations are:
n (ft/hr) tc (seconds)
3,600 1
1,800 2
1,200 3
900 4
Time constant/logging speed
GR Log Borehole effects
Correction typically ignored except for quantitative analysis such
as shale volume calculations.
Function of tool type, borehole size, mud weight, eccentricity
GR Log
Examples:
(1). A GR-CNL-LDT combination is run eccentered. What is the
corrected response if the log response is 40 API units in a 9” hole
with 8.3 ppg mud? ...16” hole ...?
(2). A GR - BHC combination is run centered. What is the corrected
response if the log response is 40 API units in a 9” hole with 16 ppg
mud? ....16” hole....?
Borehole effects
GR Log Vsh estimation
• Vsh is the bulk volume of shale (precisely the volume of silt, dry
clay, and bound water) to bulk volume.
• Calculate shale index, IRA , by
where
RAmin is clean zone reading
RAsh is shale zone (max) reading
RA is reading in zone of interest
• GR correlations based on:
– shale distribution type
– age of shale (tertiary or older)
– local area
• Disadvantage: Contamination from non-shale radioactive sources.
minRA
shRA
minRARA
RAI
GR Log
Shale Distribution
GR Log Vsh estimation
0.0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1.0
0.0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1.0
Radioactivity Index, IRA
Sh
ale
Vo
lum
e, V
sh
laminated
Clavier, et al
Larionov (older rocks)
Stieber
Larionov (tertiary rocks)
GR Log SP/GR Comparison
GR Log References
Bassiouni, Z: Theory, Measurement, and Interpretation of Well Logs, SPE
Textbook Series, Vol. 4, (1994)
Chapter 2, Sec 2.1 – 2.5
Chapter 7, Sec all
Schlumberger, Log Interpretation Charts, Houston, TX (1995)
Western Atlas, Log Interpretation Charts, Houston, TX (1992)