2016
DOI: 10.1007/s00024-015-1234-3
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Monitoring Velocity Changes Caused By Underground Coal Mining Using Seismic Noise

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Cited by 19 publications
(12 citation statements)
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“…This parameter determines the rate of growth of the cracked area [10] and if it is near the critical value then its increase may be noticeable in the measurement data, both seismological and seismic [5]. Ouchi in [11], shows that an increase in seismic events dn (t) depends on the size of the population n(t) and the coefficients of growth and also depends on a h(t) representing local conditions: …”
Section: Geomechanical Aspects Of the Hydrofracturing Processmentioning
confidence: 99%
“…This parameter determines the rate of growth of the cracked area [10] and if it is near the critical value then its increase may be noticeable in the measurement data, both seismological and seismic [5]. Ouchi in [11], shows that an increase in seismic events dn (t) depends on the size of the population n(t) and the coefficients of growth and also depends on a h(t) representing local conditions: …”
Section: Geomechanical Aspects Of the Hydrofracturing Processmentioning
confidence: 99%
“…Equally dangerous is the situation in which there is an increase in rock damage, which is manifested by a velocity decrease, often to values smaller than those recorded before. On this basis, attempts have been made to use seismic tomography to predict changes in the rock mass, especially to identify seismic risks or rock bursts and to locate the seismic events more accurately (Dubinski and Mutke 2005;Mutke 2007;Banka 2009). In the case of an underground mine, where data are obtained from seismological networks, there are much less unknown parameters.…”
Section: Introductionmentioning
confidence: 99%
“…Mining operation in the conditions of rockburst hazard require effective prevention measures, including long-term and short-term control strategies developed in the mining practice [1]. Broadly-understood rockburst control and forecasting of the rockburst threat levels rely mostly on geophysical methods: seismic and seismoacoustic observations, seismic measurements involving seismic profiling in coal seams and seismic tomography [2][3][4][5][6][7][8][9]. In recent years analytical and numerical methods were also developed and effectively used to determine the range and extent of stress concentration zones, de-stressed regions in the proximity of longwall/shortwall faces and near the development entries [10][11].…”
Section: Introductionmentioning
confidence: 99%