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SeismoAcoustic data analysis at I34MN Mongolia Songino

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Erdenet copper mine, which located 300 km north-west produces several ... The distance to Erdenet copper mine is 300 km. and travel time of infrasonic wave is ... – PowerPoint PPT presentation

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Title: SeismoAcoustic data analysis at I34MN Mongolia Songino


1
Seismo-Acoustic data analysis at I34MNMongolia
- Songino
RESEARCH CENTRE OF ASTRONOMY AND GEOPHYSICS OF
MONGOLIAN ACADEMY OF SCIENCES
Ch. Bayarsaikhan, M. Ulziibat, A. Le Pichon, A.
Schlupp
2
TOPICS
  • DESCRIPTION OF MINE EXPLOSIONS AROUND I34MN
  • SEISMO-ACOUSTIC DATA ANALYSIS
  • STATISTICS AND VARIABILITY OF THE PROPAGATION
    PARAMETERS OF MINE EXPLOSIONS
  • EVALUATION OF THE CELERITY
  • SEASONAL VARIATION OF INFRASONIC DETECTION
  • CONCLUSION

3
I34MN INFRASOUND STATION IN SONGINO
Four infrasound sensors arranged as a triangular
array of 3 km aperture.
4
WIND-NOISE REDUCING SYSTEM
6-15 dB _at_ 1-5 Hz
Wind noise
Signals
Gravel filters for wind noise reducing
5
SEISMIC NETWORK
Seismic stations are equipped with 9
vertical component short-period seismometers and
one tree component short and long period seismic
sensors. The 10 seismic stations which form
double circled array with radius 1-3 km.
6
Several large mines in the region routinely
generate explosions that are detected seismically
and with infrasound sensors. Mines are located
40-500 km from the seismic and infrasound array.
Baganuur coal mine, 180 km east of the array,
regularly produces 5-10 seismic detections per
week. Erdenet copper mine, which located 300 km
north-west produces several explosions every
week between 06-07 UTM time. Shariin gol Mine
181.1 km north-east. Borundur 302.2 km
south-east. Bagahangai 97.8 km east-south.
7
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8
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9
IDENTIFYING AND LOCALIZATION OF QUARRY BLAST
USING SEISMIC DATA
  • Real time processing and interpretation of
    seismic data from 15 seismic stations
  • For identifying quarry blast we use waveforms,
    first motion, magnitude ratio of Ms and Ml.
  • JADE and ONYX software are used for determining
    location and origin time of quarry blast.
  • Results are stored in Oracle database.

10
JADE
I arrivals
10 min
11
ONYX
12
SEISMIC LOCATIONS
Quarries identification
Baganuur
Erdenet
Others
Shariingol
13
INFRASONIC DATA PROCESSING
JADE
WinPmcc
12 min

I arrivals
  • Infra and seismic continuous real time data
    observation in JADE
  • Automatic processing of Infrasonic data done by
    PMCC (0.02-4 Hz)
  • Detailed processing of data is done manually
    using WinPmcc

14
WinPmcc analysis different arrivals generated by
one explosion
15
VARIABILITY OF THE PROPAGATION PARAMETERSERDENET
MINE
Average number of detection on 2000-2001 from
April to September no detection
Average azimuth on 2000-2001
Average trace velocity on 2000-2001
Azimuth 309-314
Celerity 0.30 0.34 km/s
Trace velocity 0.35 km/s
16
VARIABILITY OF THE PROPAGATION PARAMETERSBAGANUUR
MINE
Average number of detection on 2000-2001 from
March to July no detection
Average azimuth on 2000-2001
Average trace velocity on 2000-2001
Azimuth 89-92
Celerity 0.25-0.30 km/s
Trace velocity 0.32-0.36 km/s
17
CELERITY ESTIMATION
Celerity calculated using all explosion data C
0.25-0.30 km/s
18
PHASE IDENTIFICATION
19
SEASONAL VARIATION OF INFRASONIC DETECTION
  • Seasonal variation of the detections are
    observed.
  • Baganuur mine explosions are made not on fixed
    time
  • in July and August we got 4 detections.
  • Blue is detections of Infrasound
  • Red is seismic detections
  • For the Erdenet copper mine explosions, we have
    clear
  • seasonal variation.
  • Erdenet mine is making every week one series of
  • explosions.

From November to February, 50 of the
explosions generate also infrasonic arrivals.
20
STATISTICS ON ALL DETECTIONS AUTOMATICALLY
DETECTED BY PMCC
Azimuth distribution of infrasonic detection on
2000-2001
I
II
III
V
VI
IV
Statistics on the number of detections from the
automatic bulletin 0.1-4 Hz 2000-2001
VII
VIII
IX
The source of detection is mainly from mine
explosions, military activity, city noises and
also some time from large teleseismic events
XI
X
XII
21
CONCLUSION
  • Because of surrounding mines, explosions
    are detected by both
  • Infrasound and Seismic stations. The
    seismo-acoustic synergy enables
  • a fine analysis of the source.
  • The detections of Infrasound station
    clearly depend on the
  • season propagation effects and wind-noise
    variability.
  • Future work automatic association of I and
    S arrivals for quarries location.
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