CHAPTER
THREE:
AN OVERVIEW
OF WELL
LOGGING PRACTICE
Table
Of Contents
3.00
Introduction To This Chapter
3.01 What Is Well Logging?
3.02 Creating the Well Log
3.03 Types of Logs
3.04 Present Uses of Logs
3.05 Logging Tools Available
3.06 Resistivity Logs
1. Electrical Survey (ES)
2. Long Electrical Survey (LES)
3. Drill-Stem Sonde (ES) or Slim Hole Electrical
Survey
4. Induction-Electrical Survey (IES)
5. Slim Hole Induction Electrical Survey (IES)
6. Dual Induction - LL8 and Dual Induction - SFL
(DIL)
7. Induction-Spherically Focused Log (ISF)
8. Laterolog 3 (LL3)
9. Laterolog 7 (LL7)
10. Dual Laterolog Sequential Type (DLL)
11. Dual Laterolog Simultaneous Type (DLL)
12. Phasor Induction Log (DIT-E)
13. Array Induction Log (AIT)
14. Azimuthal Resistivity Log (ARI)
15. High Resolution Array Laterolog (HRL)
16. Multicomponent Induction Log
3.07 Microresistivity Logs
1. Microlog (MLC)
2. Microlaterolog (MLLC)
3. Proximity Log (PLC)
4. Microspherically Focused Log (MSFL)
5. Dipmeter Log (HDT)
6. Gyro Dipmeter (HDT)
7. Stratigraphic High Resolution Dipmeter (SHDT)
8. Formation Microscanner (FMS)
9. Formation Micro Imager (FMI)
10. Electromagnetic Propagation Log (EPT)
11. Thin Bed Resistivity Tool (TBRt)
3.08 Porosity Lithology Logs
1. Sonic Log Uncompensated Type (SL)
2. Borehole Compensated Sonic Log (BHCS)
3. Formation Density Log Uncompensated Type (DL)
4. Formation Density Log Compensated Type (FDC)
5. Litho-Density Log (LDT)
6. Gamma Ray Neutron (GRN)
7. Sidewall Neutron Porosity Log (SNP)
8. Compensated Dual-Spacing Neutron Log (CNL)
9. Slim-Hole Compensated Neutron (CNL)
10. Gamma Ray Log (GR)
11. Spectral Gamma Ray Log (NGT)
12. Nuclear Magnetic Resonance Log (NML, CMR, MRIL)
13. Borehole Gravity Meter (BGM)
14. Thermal Neutron Decay Time Log (TDT)
15. Slim Hole Thermal Neutron Decay Time (TDT)
16. Dual Spacing Thermal Neutron Decay Time Tool
(TDT)
17. Carbon Oxygen Log (also called Induced Gamma
Ray Spectrolog) (GST)
18. Array Sonic Log (xxx)
19. Dipole Shear Imaging Log (DSI)
20. Ultrasonic Borehole Imaging Log (UBI)
21. Integrated Porosity Lithology Tool (IPL)
3.09 Logging Scales and Grids
3.10 Typical Log Presentations
3.11 Logging Tool Resolution
3.12 Which Logs Should be Run?
3.13 In Conclusion
3.14 Exercises For Chapter Three
3.15 Bibliography For Chapter Three
Click
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Publication
History: This Chapter formed Chapter Three of the Log Analysis
Handbook, Pennwell 1986. Extensive updates have been added to
this eText edition. Sections 3.06 through 3.08, 3.11, and 3.12
were added, and the balance was edited and revised February 2001.
CHAPTER
THREE: AN
OVERVIEW OF
WELL LOGGING
PRACTICE
3.00
Introduction To This Chapter
This Chapter describes what well logs are, what logs are available,
and why logs are used. Very little theory of logging tool operation
is presented as this subject matter fills a textbook by itself,
and is adequately covered in other publications. In short, this
chapter provides a handy compact reference for teaching purposes
and for review prior to learning the details of quantitative analysis.
3.01
What Is Well Logging?
Well logging is the process of recording various physical, chemical,
electrical, or other properties of the rock/fluid mixtures penetrated
by drilling a well into the earth's mantle. A log is a record
of a voyage, similar to a ship's log. In this case, the ship is
a measuring instrument of some kind, and the trip is taken into
and out of the wellbore.
In
its most usual form, an oil well log is a record displayed on
a graph with the measured physical property of the rock on one
axis and depth (distance from the surface) on the other axis.
More than one property may be displayed on the same graph.
None
of the logs actually measure the physical properties that are
of most interest to us, such as how much oil or gas is in the
ground, or how much is being produced. Such important knowledge
can only be derived, from the measured properties listed above
(and others), using a number of assumptions which, if true, will
give reasonable estimates of hydrocarbon reserves.
Thus,
analysis of log data is required. The art and science of log analysis
is mainly directed at reducing a large volume of data to more
manageable results, and reducing the possible error in the assumptions
and in the results based on them. When log analysis is combined
with other physical measurements on the rocks, such as core analysis
or petrographic data, the work is called petrophysics or petrophysical
analysis. The results of the analysis are called petrophysical
properties or mappable reservoir properties. The petrophysical
analysis is said to be “calibrated” when the porosity,
fluid saturation, and permeability results compare favourably
with core analysis data. Further confirmation of petrophysical
properties is obtained by production tests of the reservoir intervals.
The
use of well logs for evaluating mineral deposits other than oil
and gas, such as coal, potash, uranium, and hard rock sequences
has been practiced since the early 1930’s and is widespread
today. Although the vast majority of logs are run to evaluate
oil and gas wells, an increased number are being run yearly for
other purposes, including evaluation of geothermal energy and
ground water. A large portion of this handbook is aimed at oil
and gas, but the other topics are not ignored. Most Chapters apply
to both hydrocarbon and mineral exploration.
When
logs are used for purposes other than evaluation of oil and gas,
they are often called geophysical logs instead of well logs. The
science is called borehole geophysics instead of petrophysics.
This difference is merely a matter of semantics and training.
The theory doesn't change - just the nomenclature, and sometimes
the emphasis.
3.02
Creating the Well Log
To perform a logging operation, the measuring instrument, often
called a probe or sonde, is lowered into the borehole on the end
of an insulated electrical cable. The cable provides power to
the downhole equipment. Additional wires in the cable carry the
recorded measurement back to the surface. The cable itself is
used as the depth measuring device, so that properties measured
by the tools can be related to particular depths in the borehole.

FIGURE 3.01: The Well Logging Operation
A
logging tool is made up of a sonde and a cartridge. The sonde
is the portion of the tool which gives off energy, receives energy,
or both. The cartridge contains the electrical circuitry or computer
components needed to control the downhole equipment, and to transmit
data to and from the surface.
Combination
logging tools consist of more than one sonde and cartridge, so
that more than one log can be recorded on a single trip into the
wellbore.
Surface
equipment is mounted in a logging truck, van, or skid unit from
which all logging operations are controlled. The logging unit
contains hoisting equipment for lowering and raising the tools
in the hole, and electronic or computer equipment for controlling
and recording the downhole measurements.

FIGURE 3.02: Recording the Well Log
Measurements
are recorded in two forms, analog and digital. The analog data
may be recorded on photographic film, electronic plotter, or chart
recorder. The same data are captured in digital form on magnetic
tape or disc for later use in computer aided analysis. Many instrument
control and calibration functions are now handled by the same
computer used to record the digital data, with some human control.
The result is a log, as seen below.

FIGURE 3.03: Example of a Well Log showing standard 3 track
presentaion of log curves (left)
and image log presentation (right)
All
logging tools and surface equipment must be properly calibrated.
Service companies have calibration procedures for most tools,
some of which are based on standards established by the American
Petroleum Institute (API). Each tool must be calibrated at the
surface before placing it in the hole to make measurements, and
must pass certain calibrations after the measurements are complete
to verify that measurement accuracy has not drifted. Some tools
also have downhole calibration checks.
After
reaching total depth, or some other location of interest in the
borehole, measurements are made while pulling the tool upward
over several hundred feet of the borehole. This is called the
repeat run, and is used to determine the repeatability of the
measurements when compared to the main logging pass. After the
repeat run is complete, the tool is lowered to the bottom of the
hole, and the main logging pass is commenced. During the early
portion of these measurements, the responses are compared to those
of the repeat run to determine that no instrument drift has occurred.
Results of all field calibrations and repeats are attached to
the bottom of the well log record.
In
addition to the actual measurements, the well log itself contains
information about the logging process which supports use and interpretation
of the data. The well name, location, date, surface measurements
on the mud system, drill bit size, casing information, and logging
equipment data are found on the log heading, Any pertinent information
or comments regarding the logging job may be recorded in the remarks
section.
The
logging equipment is carried to the wellsite on a truck (for land
based operations near roads), or transported by helicopter on
skids (for remote land operations) or are permanently mounted
on offshore rigs. Some typical logging units are shown below.
|
|
FIGURE
3.04 Logging Trucks and Skid Units |
Computerized
surface equipment is now the rule rather than the exception. Such
units, on a truck and with logging tools on board, can cost over
$1,000,000.

FIGURE 3.05: Inside a Modern Logging Unit
3.03 Types of Logs
Logs run in a hole which has just been drilled, and before it
is cased, are called open-hole logs. Logs run after the well is
cased are call cased-hole logs. Open hole logs are mainly used
to determine the petrophysical properties of the rocks. Some cased
hole logs are used for the same purpose. Others are used to assess
the integrity of the well completion; others are used to assess
fluid flow into the well.
Other
types of logs require no cable, such as a mud log which may record
up to 5 or 10 properties of the drilling fluid, or a drilling
log which records the rate of penetration and other functions
of the drilling process.
The
geology log, often called the stratigraphic log, strat log, or
sample description log, is a record of the rock samples retrieved
from the drilling mud, and is one of the primary sources of rock
and fluid descriptions for the well. It consists of a verbal description
of the rock type as well as qualitative or interpretive data concerning
evidence of the fluid content of the rock. These are all useful
logs and are used in any analysis of a well, if they are available.
Most
logs can now be recorded while drilling is going on or while
tripping the drill pipe. This is called
measurements while drilling (MWD) or logging while drilling (LWD).
Open-hole logs require that the drill string be removed from the
well bore before the logging tools can be lowered into the hole.
MWD does not have this need, so measurements are available continuously
as drilling proceeds.
A
composite log is made up of measurements and interpretations from
many sources of data. It is usually made up in the office in a
standard format (for the company or agency who owns the well).
Since it compresses a great deal of data onto one log, it is often
one of the most used items in the well file.
More
details on specific open-hole logging tools are found later in
this Chapter.
Most
open and cased-hole logs are recorded continuously as the tools
are pulled out of the hole. A few logs, however, may only be recorded
when the tool is stationary in the hole, such as the gravity meter
survey. Such logs are called station-by-station logs as opposed
to continuous logs. Some early station-by-station logs, by virtue
of significant improvements in measuring and recording techniques,
have become continuous logs. The first electrical log run in 1927
was station-by-station, but soon after, electrical logs were run
as continuous logs.
Most open hole logs are run in a conductive mud system. Muds
with relatively high resistivity are called fresh muds, and
those with low resistivity are called salt muds. Salt muds may
be salted on purpose to reduce erosion in shales or solution of
salt beds while drilling through them.
Oil-base muds are non-conductive and cause a few
problems, but not many are serious. You cannot run SP, microlog,
microlaterolog, or laterlog because they need conductive mud.
Dipmeter and Formation Micro Scanners need scratcher pads but
otherwise operate normally. Sonic, density, neutron, gamma ray,
NMR, caliper, induction logs all work normally.
3.04 Present Uses of Logs
Logs are used for a variety of purposes depending on the nature
of the data gathered. Correlation from well to well is the oldest
and probably the most common use of logs. It allows the subsurface
geologist to map formation depths and thicknesses and then to
identify conditions that could trap hydrocarbons.
Correlation
is usually based on the shapes of the recorded curves versus depth.
Correlation in complex geologic areas may be difficult or impossible,
and in any event requires corroboration from actual rock samples
for the initial correlations in an area. After the curve shape
patterns are recognized, they can often be used in subsequent
wells without relying too heavily on rock sample data.
Identification
of the lithology of the rock sequence is another important use
of logs. A log shows many variations from top to bottom. Each
wiggle has significance, but it can be related to the rocks being
logged only by comparing the log with actual rock samples or a
core from the well. After acquiring experience in an area it is
possible for a log analyst to make an educated guess as to lithology
by looking at the log. Modern analytical methods permit more accurate
lithology identification, but this requires charts or mathematical
solutions in addition to the curve shapes.
One
of the important uses of logs today is the determination of rock
porosity. This measurement is significant because it tells how
much storage space a rock has for fluids. No log actually measures
porosity directly, but many analytical methods are available to
help estimate this important property.
Another
of the routine uses of logs is the determination of the water,
oil, or gas saturation in the rock pores. When the porosity, oil
or gas saturation, the thickness and extent of the reservoir are
known, then it is possible to tell how much hydrocarbon is in
place in the reservoir. Again, no log actually measures the fluid
saturation directly, so analysis of indirect measurements is required.
The logs most often run for the above purposes are resistivity,
sonic travel time, density, neutron, gamma ray and spontaneous
potential logs.
One
of the older, but very useful, surveys is the caliper log. In
open hole logging, it is used to determine hole volume and aids
the engineer in designing a cementing program. It also indicates
mud cake build-up and hole wash-out. Both of these indications
are of interest to the log analyst when he considers the other
logs. In cased hole work the caliper is often used to find casing
damage and separated casing.
A
more recent development in logging is fracture-finding. It is
important because fractures will often produce large quantities
of fluid even though the rock the fractures are in would not otherwise
produce commercially. Many open-hole logs have some artifacts
caused by fractures, but the formation micro-scanner and borehole
televiewer are the most useful.
When
it is time to perforate the casing to allow fluid to flow into
the well, there may be some doubt about how well the perforator
depths match the log depths. To overcome this uncertainty, a casing
collar gamma ray log is often run. This log is correlated to the
open-hole log. Even though the actual depths may not agree, the
zone of interest on the open hole logs is related to the collar
log depth. Then the perforating gun is positioned in relation
to the collars in the casing and perforating accuracy is assured.
The
measurement of fluid flow in and near the wellbore is often of
vital importance. Such measurements can indicate channels behind
casing, casing leaks, packer leaks, tubing leaks, water influx
problems, cross flow from one reservoir to another, and other
production problems.
Another
common use for this type of measurement is the determination of
water input profiles in water injection wells. A thief zone may
take most of the water and leave the rest of the reservoir unflooded.
Surveys of this type point out the type of remedial action that
is necessary to establish a more desirable water input distribution.
Generally
it is not advisable to complete a well in a zone that has poor
bond between cement and casing without first squeezing in more
cement to seal the casing to the rock formation. A cement bond
or cement evaluation log is used to identify this problem.
The
temperature log is commonly used to indicate the top of cement
behind a newly cemented string of casing. The setting cement liberates
heat and warms up the well bore, which is thus recognizable on
a temperature log of the well.
Another
use for the temperature log is the location of points of fluid
entry in a well bore or of fluid flow behind casing. As the fluid
enters the well it expands and cools creating abnormally low temperature
in the well at the point of entry. Acoustic noise logs also find
flow entry and flow behind pipe by the noise caused by the flowing
fluid.
The
most significant change in the use of logs, in recent years, is
production monitoring. The thermal decay time log (often called
a pulsed neutron log) allows for the interpretation of porosity
and fluid saturation behind casing. The fluid saturation will
change over time as a reservoir is depleted by production, and
the changes may be monitored by logging at regular intervals,
say once a year. If the production pattern is not as predicted,
remedial action may be possible. The log is also used to provide
porosity and fluid saturation data in wells which are not, or
could not, be logged in the more conventional open-hole manner.
A
large suite of logging instruments is available to evaluate fluid
type, fluid flow, and mechanical conditions in producing or injecting
wells, in addition to those already mentioned. These are generically
called production logs and are usually run in cased holes, but
some are also effective in open hole or "bare-foot"
completions. Production log analysis is not described in this
book as excellent treatments are available elsewhere.
The
same logs that are used to evaluate porosity and water saturation
in oil and gas wells are also used to evaluate other resources
such as ground water, coal, potash, salt, uranium, oil shale,
gypsum, sulfur, geothermal energy, tar sands, and hard rock minerals.
Logs are also used to explore the earth's surface in general,
such as in the Deep Sea Drilling Program which has helped to document
the theory of plate tectonics, sea floor spreading, and continental
drift.
The
wealth of logging tool types, analysis methods and applications
of log data is so great that no-one (and no book) can cover all
topics adequately. This dilemma provides a unique opportunity
for ambitious and talented geologists, engineers, and scientists
to overcome the data deluge and become practical analysts in spite
of the often confusing and conflicting information.
3.05
Logging Tools Available To The Analyst
The following sections outline the most common open hole logs
available. Some are obsolete and could not be run today, but will
be found in existing well files. Many subtle variations and combinations
of these basic tools will also be found. There is often some hyperbole
in the descriptions of
newer tools, so use some editorial judgment - you might try for
a demonstration run in your well before you recommend the service
to management.
The
tool names and abbreviations shown are those used by Schlumberger.
Other service companies use other names and abbreviations. The
curve name abbreviations used in this handbook are shown following
each curve name along with the usual units of measurements. Many
other slim hole tools used in the mineral industry are not listed
here. Consult your local service companies for up-to-date information.
Curves
marked with an asterisk are optional and may not be present on
a particular log.
The
fact that many of the tools listed are obsolete should not discourage
you from knowing what they measured, because you will find all
these logs in existing well files and you will have to know what
the curves are and how to use them.
3.06
Resistivity Logs
Resistivity is measured in units of ohm-meters squared per meter.
This reduces to ohm-meters and is abbreviated ohm-m. The reciprocal
of resistivity is conductivity. It is measured in milli-mhos per
meter or milli-Seimens per meter (abbreviated mS/M).
Resistivity
logs can be classified into three distinct categories.
1.
Electrical logs use electrodes to impress a current through the
mud system into the formation. Other electrodes are used to measure
the voltage set up by the current over a specified distance, namely
the electrode spacing. The current, voltage and geometry of the
tool define the resistivity of the formation. Depending on the
relative arrangement of the current and voltage electrodes, the
log may be termed a lateral or a normal curve. The borehole must
contain a conductive fluid so that the current can get to the
formation.
2.
Because the current flow in the borehole influences the resulting
resistivity value, especially in very conductive muds, the laterolog
was developed. It uses two matched sets of electrodes, similar
to electrical survey electrodes, one of which is arranged upside
down compared to the other. This provides some focusing for the
current flow so that it cannot as easily flow up and down the
borehole. As a result, some service companies refer to these logs
as focused or guard logs. These logs also require a conductive
mud, preferably very conductive. Some tools measure conductivity;
others measure resistivity. All present resistivity on the log.
3.
Induction logs impress a current into the formation by electromagnetic
radiation from one or more coils. The current rings the borehole,
and in turn creates its own electromagnetic field. This field
induces a current in one or more receiving coils, the value of
which is proportional to the conductivity of the formation. Fortunately,
the received signal is out of phase from the transmitted signal,
so the two can be segregated by the receiver circuits. This log
does not require conductive mud in the borehole, but is often
used in fresh mud. Although conductivity is measured, the usual
presentation of the log converts conductivity to resistivity so
that the logs are visually compatible with ES and laterologs.

FIGURE 3.06 Some Resistivity Log Presentations

FIGURE 3.07 More Resistivity Log Presentations
 |
Figure
3.07A: Modern Resistivity Log Presentations - Array Induction
and Azimuthal Laterolog |
1.
Electrical Survey (ES)
| Curves |
Units |
Abbreviations |
| 16"
normal |
ohm-m |
R16
or RESS |
| 64"
normal |
ohm-m |
R64
or RESD |
| 18'
8" lateral |
ohm-m |
R18
|
| spontaneous
potential |
mv |
SP |
| |
| Restrictions:
Hole fluid should not be extremely resistive or extremely
conductive. Fresh muds, little invasion, hole size constant
are best. |
| |
|
|
Special
Features: No longer commonly available in most locations.
See Chapter Thirty-Seven
for more details on variations of this tool |
|
2.
Long Electrical Survey (LES)
| Curves |
Units |
Abbreviations |
| 20'
normal |
ohm-m |
R20
or RESD |
| spontaneous
potential |
mv |
SP |
| |
| Restrictions:
Used for definition of perma-frost, or high resistivity
behind deep invasion. |
| |
|
|
| Special
Features: No longer commonly available in most locations. |
|
3.
Drill-Stem Sonde (ES) or Slim Hole Electrical Survey
| Curves |
Units |
Abbreviations |
| 16"
normal |
ohm-m |
R16
or RESS |
| 64"
normal |
ohm-m |
R64
or RESD |
| 18'
8" lateral |
ohm-m |
R18
|
| spontaneous
potential |
mv |
SP |
| |
| Restrictions:
Hole fluid should not be extremely resistive or extremely
conductive. Fresh muds, little invasion, hole size constant
are best. Maximum hole size 6" for accurate logging. |
| |
|
|
| Special
Features: Tool is 1 1/2 " OD and flexible. Can
be run through drill pipe to open hole below pipe with
or without pump down. Minimum open-hole size 1 3/4".
No longer available in most areas. |
|
4.
Induction-Electrical Survey (IES)
| Curves |
Units |
Abbreviations |
| 16"
normal |
ohm-m |
R16
or RESS |
| induction
conductivity |
mS/m |
COND |
| induction
resistivity |
ohm-m |
RIL
or RESD |
| spontaneous
potential |
mv |
SP |
| *
gamma ray |
API |
GR |
| |
| Restrictions:
Mud must be conductive for SP and 16" normal. Resolution
poor above 100 ohm-m. Usually requires standoffs for
best accuracy. |
| |
|
|
| Special
Features: Induction curve can be run in oil or air-filled
holes, with gamma ray for correlation and shale indication.
Tool is superceded by newer models. |
|
5.
Slim Hole Induction Electrical Survey (IES)
| Curves |
Units |
Abbreviations |
| 16"
normal |
ohm-m |
R16
or RESS |
| induction
conductivity |
mS/m |
COND |
| induction
resistivity |
ohm-m |
RIL
or RESD |
| spontaneous
potential |
mv |
SP |
| |
| Restrictions:
Mud must be conductive for SP and 16" normal. Resolution
poor above 100 ohm-m. Usually requires standoffs for
best accuracy. |
| |
|
|
| Special
Features: 2 3/16" OD. Can be run through drill
pipe to open hole below pipe, with or without pump down.
Minimum open-hole size 4". |
|
6.
Dual Induction - LL8 and Dual Induction - SFL (DIL)
| Curves |
Units |
Abbreviations |
| deep
induction resistivity |
ohm-m |
ILD
or RESD |
| medium
induction resistivity |
ohm-m |
ILM
or RESM |
| shallow
resistivity |
ohm-m |
RLL8
or RSFL or RESS |
| spontaneous
potential |
mv |
SP |
| *
gamma ray |
API |
GR
|
| *
quick look ratio |
frac |
Rxo/Rt |
| *
apparent water resistivity |
ohm-m |
Rwa |
| *
formation factor ratio |
frac |
Fr/Fs |
| |
| Note:
Conductivity curves CILD, CILM, CLL8 are recorded on
disc but may not be displayed. Both averaged SFLA and
unaveraged SFLU are recorded. |
| |
| Restrictions:
Mud must be conductive for SP, SFL and LL8. Resolution
poor above 100 ohm-m. Usually requires standoffs for
best accuracy. |
| |
|
|
| Special
Features: When invaded zone resistivity is greater than
true formation resistivity this is the very best resistivity
log. Provides capacity for Rxo/Rt quick look interpretation
curve. Combinable with sonic log, making possible recording
of apparent water resistivity (Rwa) or formation factor
from the sonic (FS). Resistivity can be on logarithmic
or linear scale. May still be available in some areas
from some smaller service companies. Superceded by Phasor
Induction, later by Array Induction. |
|
7.
Induction-Spherically Focused Log (ISF)
| Curves |
Units |
Abbreviations |
| shallow
resistivity |
ohm-m |
RSFL
or RESS |
| deep
induction resistivity |
ohm-m |
ILD
or RESD |
| deep
induction conductivity |
mS/m |
COND |
| spontaneous
potential |
mv |
SP |
| sonic
travel time |
usec/ft
|
DT
or DELT |
| *
gamma ray |
API |
GR |
| *
quick look ratio |
frac |
Rxo/Rt |
| *
apparent water restivity |
ohm-m |
Rwa |
| *
formation factor ratio |
frac |
Fr/Fs |
| |
| Restrictions:
RSFL and ILD are presented on 2 cycle logarithmic grid
when run with sonic log. This restricts available resistivity
range. |
| |
|
|
| Special
Features: When invaded zone resistivity is greater than
true formation resistivity it is the best resistivity
log. Superceded by Phasor Induction, later by Array
Induction. |
|
8.
Laterolog 3 (LL3)
| Curves |
Units |
Abbreviations |
| deep
laterolog resistivity |
ohm-m |
RLL
or RESD |
| gamma
ray |
API |
GR |
| spontaneous
potential |
mv |
SP |
| |
Restrictions:
Needs conductive mud, preferably very salty. The mud
resistivity should be less than formation resistivity. |
| |
|
|
| Special
Features: Good in salty mud systems. Superceded by DLL. |
|
9.
Laterolog 7 (LL7)
| Curves |
Units |
Abbreviations |
| deep
laterolog resistivity |
ohm-m |
RLL
or RESD |
| gamma
ray |
API |
GR |
| spontaneous
potential |
mv |
SP |
| |
Restrictions:
Needs conductive mud, preferably very salty, The mud
resistivity should be less than formation resistivity.
SP is recorded 28 feet off depth; it may or may not
be spliced on depth. If it is, 10 foot and 50 foot
grid lines will not line up with rest of log. Superceded
by DLL and later by ARI. |
| |
|
|
| Special
Features: Good in salty mud systems. |
|
10.
Dual Laterolog Sequential Type (DLL)
| Curves |
Units |
Abbreviations |
| deep
laterolog resistivity |
ohm-m |
LLD
or RESD |
| shallow
laterolog resistivity |
ohm-m |
LLS or RESM |
| spontaneous
potential |
mv |
SP |
| gamma
ray |
api
|
GR |
| |
Restrictions:
Needs conductive mud, preferably very salty. The mud
resistivity should be less than formation resistivity.
Log is recorded on two passes. Dual log requires hand
tracing of one resistivity curve onto the other. |
| |
|
|
| Special
Features: Interpretation in invaded zone is much improved.
Extends the useful resistivity range of laterologs.
Makes possible improved calculations of true resistivity.
Superceded by simultaneous version. |
|
11.
Dual Laterolog Simultaneous Type (DLL)
| Curves |
Units |
Abbreviations |
| deep
laterolog resistivity |
ohm-m |
LLD
or RESD |
| shallow
laterolog resistivity |
ohm-m |
LLS or RESM |
| spontaneous
potential |
mv |
SP |
| gamma
ray |
api
|
GR |
| |
Restrictions:
Needs conductive mud, preferably very salty. The mud
resistivity should be less than formation resistivity.
Log is recorded on one pass. |
| |
|
|
| Special
Features: Interpretation in invaded zone is much improved.
Extends the useful resistivity range of laterologs.
Makes possible improved calculations of true resistivity,
plus the timesaving of simultaneous recording and the
advantages of having a caliper curve and a micro-resistivity
curve, when combined with microspherically focused log
(MSFL) and caliper. The preferred log in salty mud or
in fresh mud when formation resistivity exceeds 200
ohm-m. Superceded by Azimuthal Resistivity Log. |
|
12.
Phasor Induction Log (DIT-E)
| Curves |
Units |
Abbreviations |
| *
deep induction resistivity |
ohm-m |
ILD
or RESD |
| *
medium induction restivity |
ohm-m |
ILM or RESM |
| deep
phasor resistivity |
ohm-m |
IDPH
or RESD |
| medium
phasor restivity |
ohm-m |
IMPH
or RESM |
| *
deep enhanced phasor resistivity |
ohm-m
|
IDER
or RESD |
| *
medium enhanced phasor restivity |
ohm-m |
IMER
or RESM |
| *
deep very enhanced phasor |
ohm-m |
IDER
or RESD |
| *
medium very enhanced phasor |
ohm-m |
IMER
or RESM |
| shallow
resistivity |
ohm-m |
RSFL
or RESS |
| spontaneous
potential |
mv |
SP |
| *
gamma ray |
API |
GR |
| *
quick look ratio |
frac |
Rxo/Rt |
| *
apparent water resistivity |
ohm-m |
Rwa |
| *
formation factor ratio |
frac |
Fr/Fs |
| |
Note:
Conductivity curves are recorded on disc for all resistivity
curves except SFL but may not be displayed. Both averaged
SFLA and unaveraged SFLU are recorded. Bed resolution
on phasor curves is about 4 feet, enhanced is about
2 feet and very advanced is 1 foot, the latter may
be noisy. |
| |
|
|
| Restrictions:
Mud must be conductive for SP, SFL and LL8. Resolution
poor above 500 ohm-m. Usually requires standoffs for
best accuracy. |
| |
| Special
Features: Better bed resolution than standard ILD. Superceded
by Array Induction. |
|
13.
Array Induction Log (AIT)
| Curves |
Units |
Abbreviations |
| four
foot resistivity 10 inch depth |
ohm-m |
AF10,
AHF10, ASF10 (RESS) |
| four
foot resistivity 20 inch depth |
ohm-m |
AF20, AHF20, ASF20 |
| four
foot resistivity 30 inch depth |
ohm-m |
AF30,
AHF30, ASF30 (RESM) |
| four
foot resistivity 60 inch depth |
ohm-m |
AF60,
AHF60, ASF60 |
four
foot resistivity 90 inch depth
(see Special Features listed below) |
ohm-m
|
AF90,
AHF90, ASF90 (RESD) |
| *
resistivity |
Rwa,
or Sw |
image,
colour |
| *
spontaneous potential |
mv |
SP |
| *
mud resistivity |
ohm-m |
AHMF |
| *
gamma ray |
API |
GR |
| |
Note
1: Baker Atlas tool has 120 inch depth as well as
the 5 others, all with different mneumonics than Schlumberger. |
| |
|
|
| Note
2: One foot and two foot curves may also be recorded
and displayed separately (ADxxx and ATxxx) as well as
environmentally corrected four foot resistivity (AExxx).
Some conductivity curves are also recorded but seldom
displayed. Extrapolated values for Rxo and Rt are also
generated for each of the 3 bed thickness resolutions. |
| |
| Restrictions:
Mud must be conductive for SP. |
| |
| Special
Features: A colour image presentation showing resistivity,
or Rwa, or water saturation vs depth of investigation
can be displayed. |
|
14.
Azimuthal Resistivity Log (ARI)
| Curves |
Units |
Abbreviations |
| deep
laterolog resistivity |
ohm-m |
RLLD
or RESD |
| shallow
laterolog resistivity |
ohm-m |
RLLS or RESM |
| high
resolution laterolog resistivity |
ohm-m |
LLHR
or RESD |
| *
resistivity image, colour |
|
|
| *
12 individual azimuthal resistivity curves |
|
|
| *
directional survey data |
|
|
| *
spontaneous potential |
mv |
SP |
| *
gamma ray |
API |
GR |
| |
Restrictions:
Needs conductive mud. |
| |
|
|
| Special
features: Azimuthal resistivity is very useful in horizontal
wells. Curves looking up might see cap rock or shale,
those looking down might see water zone, shale, or tight
zone, those looking sideways should see reservoir properties.
A colour image of resistivity around the wellbore is
usually displayed. LLHR has deep depth of investigation
and 8 inch bed resolution. Tool is used as a low resolution,
low-cost dipmeter and fracture finder. |
|
15.
High Resolution Array Laterolog (HRL)
| Curves |
Units |
Abbreviations |
| two
foot resistivity 10 inch depth |
ohm-m
|
HRLA1
(RESS) |
| two
foot resistivity 20 inch depth |
ohm-m |
HRLA2 |
| two
foot resistivity 30 inch depth |
ohm-m |
HRLA3
(RESM) |
| two
foot resistivity 60 inch depth |
ohm-m |
HRLA4
|
| two
foot resistivity 90 inch depth |
ohm-m |
HRLA5
(RESD) |
| *
resistivity image, colour |
|
|
| *
spontaneous potential |
mv |
SP |
| *
gamma ray |
API |
GR |
| |
Restrictions:
Needs conductive mud. |
| |
|
|
| Special
features: Used in saltier mud or very high resistivity
formations as replacement for array induction log. |
|
16.
Multicomponent Induction Log
| Curves |
Units |
Abbreviations |
| horizontal
resistivity |
ohm-m |
Rh |
| vertical
resistivity |
ohm-m |
Rv |
| resistivity
ratio |
fraction |
Rv/Rh |
| *
spontaneous potential |
mv |
SP
|
| *
gamma ray |
API |
GR |
| |
Note
1: Rv is normally equal to or higher than Rh. |
| |
|
|
| Restrictions:
Mud must be conductive for SP. |
| |
| |