TY - GEN
T1 - Correlation between the average and forecasted curvatures caused by hard coal exploitation conducted at the great depth in several coal seams
AU - Mielimąka, Ryszard
AU - Orwat, Justyna
N1 - Publisher Copyright:
© SGEM 2018.
PY - 2018
Y1 - 2018
N2 - In this article was designated a relation of average values of measured curvatures of mining terrain with their forecasted values. These values were calculated by the use of the Bialek’s formula with the values of its parameters determined from the geodesic measurements results. The average graphs of measured curvatures were obtained on the base of average values of terrain subsidence caused by multi-seams exploitation of hard coal at the great depth. An exploitation was conducted by the use of longwall system, in the 338/2, 341 and 358/1 coal beds. The subsidence of terrain surface were observed within 10 years, at the measuring points of 8th observational line which was stabilized parallel to the run of the B – 2 longwall in the 338/2 coal bed. The average graphs of measured subsidence were determined using the least squares method. The smoothed splines were applied as an approximating function. Thanks to average courses of observed curvatures, it’s possible a making of the model verification which was used to the calculation of curvatures forecasted graphs.
AB - In this article was designated a relation of average values of measured curvatures of mining terrain with their forecasted values. These values were calculated by the use of the Bialek’s formula with the values of its parameters determined from the geodesic measurements results. The average graphs of measured curvatures were obtained on the base of average values of terrain subsidence caused by multi-seams exploitation of hard coal at the great depth. An exploitation was conducted by the use of longwall system, in the 338/2, 341 and 358/1 coal beds. The subsidence of terrain surface were observed within 10 years, at the measuring points of 8th observational line which was stabilized parallel to the run of the B – 2 longwall in the 338/2 coal bed. The average graphs of measured subsidence were determined using the least squares method. The smoothed splines were applied as an approximating function. Thanks to average courses of observed curvatures, it’s possible a making of the model verification which was used to the calculation of curvatures forecasted graphs.
KW - Average and forecasted curvatures
KW - Mining exploitation impacts
KW - Smoothed spline
KW - The Bialek’s formula
UR - https://www.scopus.com/pages/publications/85058903756
U2 - 10.5593/sgem2018/2.2/S09.084
DO - 10.5593/sgem2018/2.2/S09.084
M3 - Conference contribution
AN - SCOPUS:85058903756
SN - 9786197408355
T3 - International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM
SP - 669
EP - 676
BT - Micro and Nano Technologies, Space Technologies and Planetary Science
PB - International Multidisciplinary Scientific Geoconference
T2 - 18th International Multidisciplinary Scientific Geoconference, SGEM 2018
Y2 - 2 July 2018 through 8 July 2018
ER -