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Seismic Measurement-Systems
Land Marine
Seismic System
Source Receiver
ComputerSeismic waves
Seismic sources
Important properties:• Energy• Waveform• Repeatability• Cost and use in the field
Seismic/Acoustic spectrum
Seismic sources and receivers
MultipulseGeochirp
VibroseisVibrator plateRayleigh wave generator
Vibrator
Hydrophones (streamers)Geophone, accelerometerReceivers:
Airgun PingerGas gun Boomer Sleeve gun SparkerWater gun Steam gun
DynamiteDetonating cordAirgunShotgunBorehole sparker
Impulsive
Sledge hammerDrop-weightAccelerated weight
Sources:Impact
On waterOn land
Hammer
Shear wave hammer
Dynamite (explosive impulsive source):
• 40% of the seismic measurements• Not really repeatable• Exact time of detonation is difficult to obtain• Detonators are sometimes used for shallow applications• High energy• For each application the amount of dynamite can be adjusted
dynamite
Trigger cable
Betsy gun
Shot fired into a protected chamber
Vibrator:Vibroseis truck
Reynolds, 1997
Earliest known seismoscope
Used to indicate the occurrence of an earthquake in the year 138(Reynolds)
Principle of a geophone
Characteristic of a geophone
Damping factor: hCritical damping (h=1) is minimumamount required which will stop anyoscillation of the system from occurring.
Most geophones are slightly underdamped, typically around h=0.6-0.66.
Damping can be changed by changing the shunt resistor
(Reynolds)
Array of geophones:“destructive and constructive interference”
α
Apparent velocity:sinα
vvapp =
fvapp
app =λApparent wavelength:
∞=appv∞=appλ
v=appv
fv
=appλ
( )β sin)(nβsin
=RResponse function:
where:
app
xλπβ ∆
=
And n is the number of geophones in a group
x∆ x∆ x∆ x∆
Array response function
apparent
Geophone array
Clustered geophones(no filter effect)
Geophone arrays
Marine seismicMarine seismicdata acquisitiondata acquisition
PGS J.W. Schoolmeesters
Airgun
Principle of an Airgun
(Bolt-Systems)
Inside of an airgun
(Bolt-Systems)
Response from an airgun
Air gun array
One air gun Array of air guns
Sonobuoy
Chirp:MarineVibrator5-100 HzSweep of 6 seconds
Boomer
(Huntec-systems)
Hydrophone
Principle of piezoelectric effect
Voltage proportional to the variation of the pressure
Acquisition Techniques
Ocean Bottom Cable
Streamer
Vertical Cable Dragged Array Anchored Cable
PGS J.W. Schoolmeesters
Marine streamer
PGS J.W. Schoolmeesters
Tail Buoy
Processing room
Multi-channel seismic recording system
(Kearey and Brooks, 1991)
Registration of the measured data at certain time intervals
Sampling interval τsampling rate (sampling frequency) 1/ τSampling will preserve all frequencies up to the Nyquist frequency:fN=1/(2 τ), TN= 2 τ : two samples per period is the minimum!
sampling
12 samples per period
Aliasing
(Kearey and Brooks, 1991)
Nyquist Frequency:
fNy12---τ⋅=
Typical sampling intervals:0.25, 0.5 ms:
High resolution seismic1 ms, 2 ms
Oil exploration4 ms or larger
Crust seismic
τ
8 samples per period
6 samples per 5 periods
two samples per period are needed to
avoid aliasing
Range which can be measured using different number of bits:
8-bit : 1 mV - 256 mV
24-bit: 1 µV - 16 V
Dynamic range
⎟⎠⎞
⎜⎝⎛
min
maxlog20AA
Dynamic range is expressed in dB:
dB481mV
256mVlog20 =⎟⎠⎞
⎜⎝⎛
dB144V1
16Vlog20 =⎟⎟⎠
⎞⎜⎜⎝
⎛µ
Examples:
mV
124816
32
64
128
Analog Signal 53
Working of an AD-converter
1 0 1 0 1 1 0 0
= 1+..+4+..+16+32+..+..
Saving requirements depend on:
• Number of channels• Number of values per channel(Sampling rate,Time window of sampling)
• Number of bytes per sampled value
Example
Channels: 96Sampling rate: 2 msTime window: 0.8 sFormat: 4 Bytes per value
⇒ (800 / 2) Values x 96 channels x 4 Bytes = 0.146 MBytes
Saving requirements
Question
Sampling at 4ms intervals• What is the Nyquist frequency• In absence of anti-alias filtering, at what
frequency would noise at 200 Hz be aliased back into the Nyquistinterval?fN=1/(2τ)=125 Hz
125-(200-125)=50Hz