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Wyszukujesz frazę "seismic wave velocity" wg kryterium: Temat


Wyświetlanie 1-2 z 2
Tytuł:
Impact of voids and backfill on seismic wave velocity-preliminary results
Autorzy:
Mukhamedyarova, Zarina
Suorineni, Fidelis
Aldubay, Temirlan
Sapinov, Gylym
Powiązania:
https://bibliotekanauki.pl/articles/2201421.pdf
Data publikacji:
2022
Wydawca:
Główny Instytut Górnictwa
Tematy:
seismic event source location accuracy
constantly changing mine conditions
real-time seismic wave velocity
void and cemented sand backfill effect with time
dokładność lokalizacji źródła zdarzeń sejsmicznych
stale zmieniające się warunki kopalniane
prędkość fali sejsmicznej w czasie rzeczywistym
Opis:
In this study, laboratory experiments were conducted on discrete physical models that mimic mining effects to better understand the impact of continuous changes in mining environments on seismic wave velocities. The discrete physical models are represented by concrete and granite cubic samples of different sizes with holes of different diameters filled and unfilled with cemented sand backfill of different cement-sand content ratios. The hole diameters range from 0 to 150 mm in block sizes ranging from 150 mm to 450 mm in increments of 75 mm. The increasing hole size mimics increasing extraction in the mine with time. Cemented sand fills at cement contents ranging from 0 to 20% are used to fill the voids after testing them empty and retesting the same at different backfill cured ages. The SAEU3H AE eight-channel system is used in the study. Preliminarily results show that the impact of continuous changes in mining environments significantly affects the seismic wave velocities. The impact of voids and their contents on the seismic wave velocity depends on the sensor location relative to source and void, and it backfills cement content with time.
Źródło:
Journal of Sustainable Mining; 2022, 21, 4; 319--333
2300-1364
2300-3960
Pojawia się w:
Journal of Sustainable Mining
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The application of seismic interferometry for estimating a 1D S-wave velocity model with the use of mining induced seismicity
Autorzy:
Czarny, R.
Pilecki, Z.
Drzewińska, D.
Powiązania:
https://bibliotekanauki.pl/articles/92182.pdf
Data publikacji:
2018
Wydawca:
Główny Instytut Górnictwa
Tematy:
seismic interferometry
induced seismicity
Rayleigh surface wave
S-wave velocity
mining terrain
interferometria sejsmiczna
sejsmiczność indukowana
fala powierzchniowa Rayleigha
prędkość fali S
teren górniczy
Opis:
The main objective of this paper is to present the usefulness of the seismic interferometry method to determine the S-wave velocity model of the rock mass affected by exploitation in the KGHM Rudna copper ore mine. The research aim was achieved on the basis of seismic data, acquired from seismograms, of 10 strong seismic events of magnitude greater than 2.6. They were recorded by a pair of seismometers deployed on mining terrain. In the first stage, the Rayleigh wave between seismometers was estimated. Then, the group velocity dispersion curves of fundamental and first higher modes were identified. Finally, inversion of the dispersion curves to a 1D S-wave velocity model up to 500m in depth was obtained. The velocity model was determined for the part of the rock mass partially affected by mining. The results confirm similar rock mass structure and velocities of the subsurface layers as those obtained by the archival 3D model. In both models, a high degree of correlation in the boundary location between the overburden of the Cenozoic formations and the bedrock of the Triassic formations was observed. The applied methodology can be used to estimate the S-wave velocity model in other mining regions characterized by strong seismicity.
Źródło:
Journal of Sustainable Mining; 2018, 17, 4; 209-214
2300-1364
2300-3960
Pojawia się w:
Journal of Sustainable Mining
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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