2d land seismic data processing training course · · 2016-08-17course i n p a r t n e r s h i p...
TRANSCRIPT
2 D L A N D S E I S M I C DATA
P R O C E S S I N G T R A I N I N G
C O U R S E
I n p a r t n e r s h i p w i t h
Course Overview
The 5 day combined Land and Marine and Transition Zone technical course
is as its name suggest, a fairly heavy technical course. It goes into the
theory of seismic acquisition as it is applied in the cases of Land, Marine
and Transition Zone activities. It is designed for geophysicists or engineers
with some high school grade maths skills, however this is not obligatory as
it makes full use of imagery to explain points. . All the maths is supplied on
a CD ROM in Microsoft Excel format for those who would wish to look
further at these areas.
Who Should Attend
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COMBINED LAND AND
MARINE SEISMIC TECHNICAL COURSE
The 5 Day technical course is an intermediate level course and really
needs a graduate level delegate, probably but not necessarily fairly
junior. The delegates should ideally have a geophysics, maths or
electrical engineering degree. If they are geologists they may struggle
with the technical content.
COMBINED LAND AND MARINE SEISMIC TECHNICAL COURSE
THE FUNDAMENTALS
At this stage we are going to look mainly at
P a es P wave simple mathematics
The No e clatu e of seis ic a es
DESCRIPTION OF P AND S WAVES
How these propagate, relative velocities
THE SEISMIC REFLECTION COEFFICIENT
The usual definition through velocity and
density
HUYGENS PRINCIPLE
The Wave front, applies in seismic just like it
does in optics
“NELL “ LAW A“ IT APPLIE“ TO P AND “ WAVES
Show how S waves obey it too.
SEISMIC SIGNAL GENERATION ON LAND –DRILLED SEISMIC SHOT
A rather good example of an explosive source
shot is shown with reference to the main
signal appearance and basic attributes.
THE DRILLED SEISMIC SHOT
Its signal / noise attributes
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DAY ONE
SEISMIC SURVEY IN WATER
GENERATING THE SIGNAL WITH
AIRGUNS.
THE AIRGUN ARRAY
Starts with a description of basic underwater
sound factors such as the Rayleigh Willis
equation and its effect on the bubble pulse,
airgun array formation and summation,
clustered airguns, gun timing and control
techniques.
AIRGUN ARRAY FAR FIELD SIGNATURE
MEASUREMENT
This section deals with the measurement of
the far field signature of an airgun array and
how it is described.
The use of the Microsoft Excel Analysis
package to carry out a discrete Fourier
transform and plot the logarithmic pressure
output vs frequency of a far-field signature
with an example given to the students to
compute as homework.
COMBINED LAND AND MARINE SEISMIC TECHNICAL COURSE
THE GEOPHONE - HOW IT WORKS
A diagram showing the construction of the
geophone. Natural resonant frequency.
Damping. Their effect on output.
THE HYDROPHONE - HOW IT WORKS
The Acceleration-Cancelling type.
The Deep Water cylindrical type.
MOVEOUT VELOCITY AND THE GROUP
INTERVAL
A big module with an example of how the
calculation is derived and how to make us of
it.
HORIZONTAL WAVELENGTH AND
WAVENUMBER
Description of the phenomenon of horizontal
wavelength and wave number. Examples of
the transformation between spatial and K
wavenumber space. This is a vitally important
topic and plenty of time will be devoted to it.
There will be a presentation on the
mathematics of the relevant computations
from which the displays are derived.
THE GEOPHONE ARRAY PRACTICAL
ARRANGEMENTS
How the result of the array length calculation
will affect survey geometry and the practical
side of the geophone arrays.
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DAY TWO
NYQUISTS THEOREM
Ho Ny uist s theo e applies to seis ic signals both in the time and spatial domains.
Go back to example of a shot record and talk
about how incorrect (too long) array design
can lead to both 'aliased signal' and noise.
LAND & MARINE SURVEYS AND THE CMP
METHOD
Description of how common midpoint,
common offset, common shot and common
receiver gathers are produced in land and
towed marine surveys.
COMMON REFLECTION POINT AND AN
EXAMPLE OF A STUDY
The use of common reflection point studies
if a complex sub-surface exists. The possible
absence of sub-surface illumination in these
areas.
HOMEWORK for evening – DRAW THE
MARINE CMP DIAGRAM FOR THE CASE
WHERE SHOTPOINT INTERVAL = TWICE
STREAMER GROUP LENGTH.
COMBINED LAND AND MARINE SEISMIC TECHNICAL COURSE
SHORT REFRESH ON WAVELENGTH AND
WAVE NUMBER
This is so important. The effect of arrays.
How these affect both source and receiver
array design.
“TACKA‘‘AY
A de factor 2D standard for recording
geometry. The use of abutting receiver
groups. The reduction in noise rejection
when point receivers are used. Why it is still
important to understand this as it applies so
strongly to 2D surveys.
F-K TRANSFORMS OF SYNTHETIC DATA
The f-k t a sfo of a pe fect data set is shown with examples of the f-k transforms
of common perturbations to this perfect
data
EXERCISE
shot and receiver group interval. Spacing
between shallow shot pattern adjacent
shot holes. Group discussion of results.
OTHER PRACTICAL FACTORS
GEOPHONE NATURAL RESONANT
FREQUENCY
The choice of geophone natural frequency.
It is possibly still relevant even with 24 bit
converters and why this is so.
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DAY THREE
LAND SURVEY PRACTICAL FACTORS
Group Discussion of how practical factors affect the
planning and execution of land seismic surveys
SEISMIC SOURCE REQUIREMENTS
Choice of source, Source size, depth and affects on
frequency content and signal strength.
A SEISMIC SOURCE TEST RESULTS PRESENTED
WITH ANALYSIS
The results of a comprehensive seismic source test.
Its results and conclusions are presented. Group
discussion of these, they are so important.
CRITICAL DIFFERENCES BETWEEN LAND AND
MARINE SURVEY FACTORS
A discussion of these factors is presented.
FREE SURFACE GHOSTS FOR PRESSURE AND
VELOCITY SENSORS
The free surface ghosts for both pressure
hydrophone and velocity sensors are discussed.
DUAL SENSOR STREAMERS
The summation of velocity and pressure sensor in
the dual sensor streamer is discussed.
THE TRANSITION ZONE SURVEY.
'Cable-type recording systems with dual sensor.
'Node Type' sensors
Practical issues around Transition Surveys
COMBINED LAND AND MARINE SEISMIC TECHNICAL COURSE
THE VIBROSEIS METHOD, SOURCE AND
SURVEY PLANNING
A description of the seismic vibrator,
vibroseis typical data, the effects of
CMP fold, offset.
VIBROSEIS SWEEP PARAMETERS AND
CORRELATION
A discussion of how Vibroseis
parameters are set-up, the difference
between up and down sweeps.
The theory of Groundforce and its
use in Vibroseis control electronics.
How correlation works.
Harmonic Ghosts.
Examples of correlation outputs.
Number of sweeps per VP vs actual
output.
A set of conclusions.
Brief talk on 'vintage vibroseis data' and how
through the 1980s quality improved due to
the introduction of 'Ground Force Phase
Lock' digital vibrator sweep controllers and
phase out of the 'base plate velocity phase
lock' controllers.
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DAY FOUR
LINEAR AND NON-LINEAR SWEEPS
A display of filter panels from a non-linear and linear
sweep. More on on-linear sweep design and how it
impacts the design of the vibrator and what you need
to watch for.
SEISMIC INSTRUMENTATION
What does it do ?
SEG Recording conventions including
correlated vibroseis data
Brief History of Land & Marine Seismic
Instruments
Telemetry Systems from early
developments up to date
Historic Wireless systems - some of this
material will be in the notes as it is historic
and of interest to those needing to deal
with data recorded by historic systems.
24 bit generalised design
Node seismic systems
HOMEWORK.
What else might affect the choice of geophone
natural frequency for a survey (1 hour)
COMBINED LAND AND MARINE SEISMIC TECHNICAL COURSE
THE SEISMIC STREAMER.
Streamer construction including the
hydrophone design.
A description of basic hydrophone and
streamer design with the reference to
historic improvements. The 'charge
amplifier' hydrophone interface.
Details of how modern methods have
reduced or almost eliminated the 'bulge
wave' phenomenon. Streamer
performance, self noise
FREE SURFACE GHOSTS FOR PRESSURE
AND VELOCITY SENSORS
The free surface ghosts for both pressure
hydrophone and velocity sensors are
discussed.
DUAL SENSOR STREAMERS
The summation of velocity and pressure
sensor in the dual sensor streamer is
discussed.
MARINE SEISMIC SURVEY DESIGN.
A big module
GROUP INTERVAL AND BIN SIZE
Calculation of group interval and bin size
related to seismic velocity, dip and
frequency content.
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DAY FIVE
MIGRATION APERTURE, FRESNEL ZONE AND
DIP
Calculation of migration aperture and Fresnel zone
related to dip and frequency content.
MULTIPLE SOURCE AND STREAMER TOWING
CONFIGURATION
A diagram of a multiple source and streamer
towing configuration is presented followed by an
illustration of an in-water positioning plan.
MODE‘N “T‘EAME‘ CONT‘OL BI‘D
A picture of a modern streamer positioning bird.
THE USE OF AN ACOUSTIC DOPPLER CURRENT
PROFILER ADCP
The use of the ADCP during surveys to calibrate
tidal predictions and plan acquisition etc.
FEATHER ANGLE AND HOW IT AFFECTS
OPERATIONS
A few slides about feather angle and shooting
plans.
CMP COVERAGE FOR MARINE 3D SURVEYS
Description of a possible way of assessing CMP
coverage within offset ranges.
OPERATING THE SURVEY
A few thoughts regarding on-board
representation.
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