Geophysics Department TU Clausthal
|
Applied Geophysics : Seismics
|
Huygens' Principle
Applet
( in separate window,
ca. 390 x 275 Pixel )
The applet simulates a simplified demonstration of
Huygens' Principle :
- A separate frame displays
- the vertical cross-section of a 2-dimensional
subsurface model,
- a spread of 24 equally spaced receivers along the
free surface
- and
- the corresponding traces,
- resulting from
- a single shot of ( almost ) arbitrary position above the
interface ( SHOT RECORD )
- or from
- shot / receiver
pairs at identical surface positions ( ZERO OFFSET ).
Table of Content
- Comments
- HOWTO
- Examples
- Download
Comments
The interface is represented by max. 281 discrete points
( = parallel lines in the 2-d model ), emitting elementary
waves when hit by the direct wave.
Each trace is calculated as the superposition of all elemetary waves
arriving at the corresponding receiver location.
Trace samples are calculated in constant time steps
( sampling interval Δt ), determined by the min.
point distance along the interface
( ALL PNTS = 281 ) and the velocity selected.
A subset ( 71 PNTS ... 1 POINT )
of interface points and corresponding elementary waves can be selected to
observe the formation of the final result for ALL PNTS in a series of
SHOT RECORDS / ZERO OFFSET sections using an increasing number of interface
points.
- For compressional waves
- the vertical component ( VER (P-WAVE) )
- or
- the horizontal inline component
( HOR (P-WAVE) )
- of the ground displacement can be calculated,
- for horizontally polarized shear waves
- the transverse component ( S-H (S-WAVE) ).
- ( ! Direct wave and elemenary waves are assumed to be
of identical type, i.e. no conversion at the
interface ! )
- The amplitudes of the direct wave are scaled to be of the magnitude of the
reflexion amplitudes :
- max amp ( DIR ) of all traces = max
amp ( RFL ) of all traces.
- ! The simulation is restricted to primary waves,
- i.e. direct waves only can excite elementary waves !
- ! No velocity contrast at the interface,
- i.e. impedance contrast due to density change only =>
no refraction !
- ! Boundary conditions at the free surface and at the interface are
neglected,
- i.e. "reflexioncoefficient" +1 at the interface.
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Table of Content
HOWTO
Examples
HOWTO
Dialogue Window
( Screenshot )
- SHOW / HIDE
- SHOW starts the applet and displays the model + trace frame,
- HIDE hides the frame and frees its resources.
- INFO
- displays informations to the actual cursor postion :
- X [m] / Z [m] ( model window ) and
X [m] / T [ms] ( trace window ).
- HELP
- displays possible mouse interactions :
- in model window
- horizontal zoom,
- adjustment of position and geometry of the interface
and the receiver spread,
- shot position
- and
- of the "wave length" of the source signal.
- in trace window
- vertical ( =TWT ) zoom,
- adjustment of the AGC window.
The dialogue field INTERFACE refers to the model geometry and scaling :
- 1 - COS / TRIANGLE / PARABOLA / RAMP
- selects the general shape of the interface,
to be modified by dragging characteristic points with the mouse.
- ALL PNTS / 71 PNTS ... 1 POINT
- selects representaion of the interface by all ( 281 ) or a
reduced number of discrete points to clarify the superposition of
elementary waves.
- SCAL x 0.1 ... SCAL x 10.
- applies a scaling factor to the subsurface model and
the receiver spread
- ( and to the wave length of the source signal ),
- to vary the horizontal extent from approx. 60 [m] to approx.
6 [km].
VELOCITY n.nn [km/s] :
- DEC, INC and BY 1.00 .. BY 0.01
- increments / decrements the velocity used for calculation
- in steps of 1.00 ... 0.01 [km/s].
SIGNAL :
- KUEPPERS_2 / KUEPPERS_4 / ZERO PHASE
- selects the wave form of the source signal
- ( Kueppers wavelet of order 2 / 4 or autocorrelation of a
sweep ).
- SHOW SOURCE SIGNAL
- displays the source wavelet in the model window,
- scaled identically to the vertical scale of the model
- ( its wavelength can be adjusted using the mouse ).
TRACES :
- VER (P-WAVE) / HOR (P-WAVE) /
S-H (S-WAVE)
- selects the component to be displayed in the trace window.
- NO GEOM. SPREAD. / CYL. SPREADING /
SPHER. SPREADING
- includes NO,
1 / SQRT(R)
or 1 / R scaling in trace calculation.
SECTION :
- SHOT RECORD / ZERO OFFSET
- selects the type of seimic section to be displayed in the
trace window.
- DISP WAVE FRONTS
- displays direct and elementary wave fronts during trace
calulation,
- if SHOT RECORD is selected and
- the aspect ratio of the model display SCALE VER :
HOR = 1.0 : 1
- ( evtl. adjust the aspect ratio of model + trace window ).
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Table of Content
HOWTO
Examples
The dialogue field TRACE DISPLAY refers to the display parameters of the
seimic section :
- AMPLITUDE SCALING
- TRUE AMPLITUDE :
- const. scaling of all traces, determined by the max.
amplitude of all traces,
- AMAX PER WIND. :
- as above, but max. amplitude taken in actual TWT ( zoom )
window,
- AUTOM. GAIN :
- AGC scaling of traces,
- length of source signal ( blue ) and of AGC window ( red )
shown in the upper left corner of the trace display
- ( always active during recording cycle, length of AGC window : mouse
adjustable ).
- DEFLECTION
- D-TRC × 0.5
... D-TRC × 5.0 :
- the clip limit for each trace in units of trace distance.
- MAX AMPL.
- DEFL × 0.1 ... DEFL × 10. :
- a const. factor, applied before plotting
( and clipping ) a sample.
- SHOW DIRECT WAVE
- shows / hides the direct wave in the trace display.
- RUN
- continuous calculation and display of wave fronts and
traces.
- STEP
- calculation and display of wave fronts and traces in
single time step mode.
- RESET
- resets the trace calculation,
- displays the message
! CLICK TO CALC ... ! and
- alows adjustment of the AGC window for the next recording
cycle.
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Table of Content
HOWTO
Examples
- HOR ZOOM ( model window ) :
- The left mouse button sets the horizontal display
range of the model ( + traces ),
- marked as hor. rectangle ( cyan, starting inside the actual window,
may end outside ),
- the right button resets the horizontal extend to a value
covering the receiver spread ( incl. shot position in SHOT RECORD
mode ).
- The vertical range of the model window is set
automatically ( surface, Z=0 [m], to max. depth of the
interface / length of source signal, if shown )
- TWT ZOOM ( trce window ) :
- The left mouse button sets the time range of the
trace display
- ( min. start = 0 [ms], max. end =
2 × max. TWT ),
- the right button ( or the start of a new recording
cycle ) resets the time range to
0 [ms] ... max. TWT.
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Table of Content
HOWTO
Examples
Examples
Parameters common to all frames :
- Model :
- syncline ( 1 - COS ),
- hor. -100 [m] ... +100 [m],
ver. 50 [m] ... 130 [m],
- total hor. extent -280 [m] ... +280 [m]
( SCAL × ;1.0 )
- => point distance approx. 2 [m] for ALL PNTS,
approx. 28 [m] for 21 PNTS.
- Velocity :
- 2.00 [km/s] => Delta-T = 1 [ms]
- Source Signal :
- Kueppers, Order 2, L-Sig = 20 [ms] = 40 [m],
SHOW SOURCE SIG
- Traces :
- Vertical component, CYL. SPREADING
- Trace Display :
- Wiggle + Area, D-TRC × 1.0, DEFL × 1.0,
SHOW DIRECT WAVE
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HOWTO
ZERO OFFSET section and SHOT RECORD,
showing the typical 'tie' reflexion pattern.
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HOWTO
Examples
Snapshots of recording cycle at TWT = 60 [ms] and
TWT = 80 [ms]
( model represented by 21 points, to reduce number of elementary
wave fronts ).
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HOWTO
Examples
ZERO OFFSET section and SHOT RECORD,
covering the total horizontal extend of the model,
represented by 3 points and showing the resulting
diffraction hyperbola.
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HOWTO
Examples
SHOT RECORD ( parmeters identical to the first example ).
AGC scaling applied to the trace display reveals effects of
final horizontal extent of the model ( ±280 [m] ).
Below 180 [ms] :
small amplitude diffraction signals from both ends,
though a cosine taper is applied to the impdance contrast of
approx. 20 points at both ends of the interface
( ! ALL PNTS mode only ! ).
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Table of Content
HOWTO
Examples
Download
Class and html files for a local installation of the applet are available as
a
zip file and as
a
tar.gz file.
More applets :
the author's
Homepage
Rev. 27-jul-2006
Comments to Fritz Keller
( ned gschempfd isch globd gnueg )
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Examples
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Applet Index ( Geophysics Dept.,
TU Clausthal )