Acoustic logs or Sonic logs measure the slowness of elastic waves of the formation.
In sonic log, the capacity of formation to transmit sound waves is measured.
The capacity varies with porosity, lithology, and rock texture.
Travel time of a wave is the distance that the wave travels times the slowness of the medium, Thus,
Slowness = 1/Velocity
Types of sonic logging tools are explained briefly with help of animation and what are the application of these tools in determining the formation properties.
Acoustic logs or Sonic logs measure the slowness of elastic waves of the formation.
In sonic log, the capacity of formation to transmit sound waves is measured.
The capacity varies with porosity, lithology, and rock texture.
Travel time of a wave is the distance that the wave travels times the slowness of the medium, Thus,
Slowness = 1/Velocity
Types of sonic logging tools are explained briefly with help of animation and what are the application of these tools in determining the formation properties.
WELL LOG : Types of Logs, The Bore Hole Image, Interpreting Geophysical Well Logs, applications, Production logs, Well Log Classification and Cataloging
WELL LOG : Types of Logs, The Bore Hole Image, Interpreting Geophysical Well Logs, applications, Production logs, Well Log Classification and Cataloging
It is the type of a caliper log. A device for measuring the internal diameter of a casing , tubing or open borehole using high frequency acoustic signals
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4. Types of porosity
Primary porosity
The porosity of the rock that formed at the
time of its deposition.
Secondary porosity
Develops after deposition of the rock. For
example: Fracture spaces formed in fractured
reservoirs
5. Primary porosity
Effective Porosity
the pores are connected,
Effective Porosity liquid can easily flow
through (sponge)
Ineffective Porosity
the pores are not connected.
Liquid cannot find a path through; it just gets
stuck in the holes. (cork)
Total Porosity (ΦT) = Effective Porosity (Φe) + Ineffective Porosity (Φi)
The ratio of the entire pore space in a rock to its bulk volume
6. Note !
Effective Porosity
the pores are connected
Permeability
Is the ability of the rock to transmit fluid
9. P-WAVES
is the fastest kind of seismic wave, and, the first to 'arrive' at a seismic station. The P wave can
move through solid rock and fluids
P wave, particles move in the same direction that the the wave is moving in, which is the
direction that the energy is traveling in
10. S-WAVES
The second type of body wave is the S wave or secondary wave, which is the second wave you
feel in an earthquake. An S wave is slower than a P wave and can only move through solid rock,
not through any liquid medium
S waves move rock particles up and down, or side-to-side--perpendicular to the direction that
the wave is traveling in
11. Stoneley wave
When generated at low frequency, Stoneley waves travel as a
tube wave
They loose amplitude at the contact of permeable intervals, and
are reflected by fractures.
The loss of amplitude can be related to formation permeability
16. sonic tools
The sonic tools create an acoustic
signal and measure how long it
takes to pass through a rock.
Delay time / slowness
17. sonic tools types
Early sonic tools
Dual receiver sonic tools
Borehole Compensated Sonic
Long spacing sonic tools
Array sonic tools
18. Early sonic tools
• Early tools had one Tx and one Rx.
• The body of the tool was made from rubber (low velocity
and high attenuation material) to stop waves travelling
preferentially down the tool to the Rx.
19. Early sonic tool problems
The measured travel time was always too long because the time
taken for the elastic waves to pass through the mud was
included in the measurement.
he measured time was A+B+C rather than just B. (ii) The length
of the formation through which the elastic wave traveled (B) was
not constant because changes to the velocity of the wave
depending upon the formation altered the critical refraction
angle
20. Dual receiver sonic tools
These tools were designed to overcome the problems in the early
tools.
They use two receivers a few feet apart, and measure the difference
in times of arrival of elastic waves at each Rx from a given pulse from
the Tx
This time is called the sonic interval transit time (Dt) and is the time
taken for the elastic wave to travel through the interval D (i.e., the
distance between the receivers).
21. Dual receiver sonic tools
The time taken for elastic wave to reach Rx1: TRx1= A+B+C
The time taken for elastic wave to reach Rx2: TRx2 = A+B+D+E ·
The sonic interval transit time: DT = (TRx2 - TRx1) = A+B+D+E – (A+B+C)
= D+E-C. ·
If tool is axial in borehole: C = E, so DT = (TRx2 - TRx1) = D
The problem with this arrangement is that if the tool is tilted in the hole, or
the hole size changes
22. Dual receiver sonic tool problem
The problem with this arrangement is that if the tool is tilted in
the hole, or the hole size changes
23. Borehole Compensated Sonic (BHC)
It has two transmitters and four receivers,
arranged in two dual receiver sets, but with one set inverted
(i.e., in the opposite direction).
Each of the transmitters is pulsed alternately, and Dt values are
measured from alternate pairs of These two values of Dt are
then averaged to compensate for tool misalignment, at to some
extent for changes in the borehole size.
24. Long Spacing Sonic (LSS) Tool
It was recognized that in some logging conditions a longer Tx-Rx
distance could help. Hence Schlumberger developed the long
spacing sonic (LSS), which has two Tx two feet apart, and two Tx
also two feet apart but separated from the Tx by 8 feet. This tool
gives two readings; a near reading with a 8-10 ft. spacing, and a
far reading with a 10-12 ft. spacing
25. Array sonic tools
Multi-spacing digital tool.
First to use STC processing.
Able to measure shear waves and Stoneley waves in hard formations.
Used for: Porosity. Lithology. Seismic tie in / time-to-depth conversion. Mechanical properties
(from shear and compressional).
racture identification (from shear and Stoneley).
Permeability (from Stoneley)
26. Tool Calibration
The tool is calibrated inside the borehole opposite beds of pure and known lithology, such as
anhydrite (50.0 ms/ft.), salt (66.7 ms/ft.), or inside the casing (57.1 ms/ft.).
27. Time record
the sonic log record the time T that required for a sound wave
to travel in giving distance on formation
time record in sonic tool depend on lithology and pore fluid
porosity decrease velocity increase
29. Factor affecting in sonic log
Lithology !
gas
Mud type
Pore hole rugosity
Secondary porosity
Compaction
Overpressure
30. Secondary and Fracture Porosity
The sonic log is sensitive only to the primary intergranular porosity
The sonic pulse will follow the fastest path to the receiver and this will avoid fractures
Comparing sonic porosity to a global porosity (density log, neutron log)should indicate zone of
fracture.
31. Compaction
As a sediment becomes compacted, the velocity of elastic waves
through it increases
If one plots the interval transit time on a logarithmic scale against
depth on a linear scale, a straight line relationship emerges
Compaction trends are constructed for single lithologies, comparing
the same stratigraphic interval at different depths
Compaction is generally accompanied by diagenetic changes which
do not alter after uplift
Amount of erosion at unconformities or the amount of uplift from
these trends can be estimated
32. Overpressure
An increase in pore pressures is shown on the sonic log by a
drop in sonic velocity or an increase in sonic travel time
35. Stratigraphic Correlation
The sonic log is sensitive to small changes in grain size, texture, mineralogy, carbonate content,
quartz content as well as porosity
This makes it a very useful log for using for correlation and facies analysis
36. Well to seismic tie
Synthetic Seismograms
Represents the seismic trace that should be observed
with the seismic method at the well location
Improve the picking of seismic horizons
Improve the accuracy and resolution of formations of
intere