Assessment of the impact of an overlying coal seam edge using seismic profiling of refracted Pwave velocity

This paper presents the results of seismic profiling along the sidewalls of two headings of a longwall in a coal-seam at a depth of about 850 and 870 metres in a coal mine in the Upper Silesian Coal Basin, Poland. The seismic profiles were located in a zone of impact of the same overlying edge of th...

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Main Authors: Szreder Zbigniew, Barnaś Maciej
Format: Article
Language:English
Published: EDP Sciences 2017-01-01
Series:E3S Web of Conferences
Online Access:https://doi.org/10.1051/e3sconf/20172401007
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spelling doaj-ccd8d7e4f51941dabe1eff4e408946902021-04-02T10:42:59ZengEDP SciencesE3S Web of Conferences2267-12422017-01-01240100710.1051/e3sconf/20172401007e3sconf_ag2017_01007Assessment of the impact of an overlying coal seam edge using seismic profiling of refracted Pwave velocitySzreder ZbigniewBarnaś MaciejThis paper presents the results of seismic profiling along the sidewalls of two headings of a longwall in a coal-seam at a depth of about 850 and 870 metres in a coal mine in the Upper Silesian Coal Basin, Poland. The seismic profiles were located in a zone of impact of the same overlying edge of the coal-seam located about 40 m above. This study was interesting from that point of view since there were no other geological and mining factors present which could disturb the impact of the coal seam edge. The profiling of refracted P-wave velocity changes was carried out according to the Dubinski method. This method is used for the assessment of relative stress in a coal seam in the side wall of the excavation. The results obtained on both seismic profiles are very similar, which demonstrates the small impact of the overlying edge of the coal seam in both headings of a longwall. It should be emphasised that at greater exploitation depths, the calculated reference velocity is less reliable than the measured reference velocity. Presumably, the method of calculating seismic anomaly requires updating under such conditions, but additional evidence should be collected.https://doi.org/10.1051/e3sconf/20172401007
collection DOAJ
language English
format Article
sources DOAJ
author Szreder Zbigniew
Barnaś Maciej
spellingShingle Szreder Zbigniew
Barnaś Maciej
Assessment of the impact of an overlying coal seam edge using seismic profiling of refracted Pwave velocity
E3S Web of Conferences
author_facet Szreder Zbigniew
Barnaś Maciej
author_sort Szreder Zbigniew
title Assessment of the impact of an overlying coal seam edge using seismic profiling of refracted Pwave velocity
title_short Assessment of the impact of an overlying coal seam edge using seismic profiling of refracted Pwave velocity
title_full Assessment of the impact of an overlying coal seam edge using seismic profiling of refracted Pwave velocity
title_fullStr Assessment of the impact of an overlying coal seam edge using seismic profiling of refracted Pwave velocity
title_full_unstemmed Assessment of the impact of an overlying coal seam edge using seismic profiling of refracted Pwave velocity
title_sort assessment of the impact of an overlying coal seam edge using seismic profiling of refracted pwave velocity
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2017-01-01
description This paper presents the results of seismic profiling along the sidewalls of two headings of a longwall in a coal-seam at a depth of about 850 and 870 metres in a coal mine in the Upper Silesian Coal Basin, Poland. The seismic profiles were located in a zone of impact of the same overlying edge of the coal-seam located about 40 m above. This study was interesting from that point of view since there were no other geological and mining factors present which could disturb the impact of the coal seam edge. The profiling of refracted P-wave velocity changes was carried out according to the Dubinski method. This method is used for the assessment of relative stress in a coal seam in the side wall of the excavation. The results obtained on both seismic profiles are very similar, which demonstrates the small impact of the overlying edge of the coal seam in both headings of a longwall. It should be emphasised that at greater exploitation depths, the calculated reference velocity is less reliable than the measured reference velocity. Presumably, the method of calculating seismic anomaly requires updating under such conditions, but additional evidence should be collected.
url https://doi.org/10.1051/e3sconf/20172401007
work_keys_str_mv AT szrederzbigniew assessmentoftheimpactofanoverlyingcoalseamedgeusingseismicprofilingofrefractedpwavevelocity
AT barnasmaciej assessmentoftheimpactofanoverlyingcoalseamedgeusingseismicprofilingofrefractedpwavevelocity
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