2016
DOI: 10.3390/en9090702
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The Development of Dewatering Predictions of the Velenje Coalmine

Abstract: Abstract:The complex hydro-geological situation, particularly in terms of groundwater, has been a constant threat to the mining carried out at the Velenje colliery since its inception. Of particular interest to the authors are the difficulties presented to the colliery by the adjacent sand aquifers, as the water pressure within these sands directly impacts mining safety, and the aquifers themselves are most directly affected by dewatering. In order to monitor water levels and estimate dewatering at the Velenje… Show more

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Cited by 11 publications
(13 citation statements)
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“…Additionally, the most significant changes of hydraulic properties occur during the period of maximum subsidence. Increases of one or two orders of magnitude in permeability and a moderate increase in storativity from before and after subsidence are often reported, along with typical increases of an order of magnitude in the inner subsidence and two in the marginal tensional zone [5,6,46].…”
Section: Interactions Between Subsidence and Water Bodiesmentioning
confidence: 99%
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“…Additionally, the most significant changes of hydraulic properties occur during the period of maximum subsidence. Increases of one or two orders of magnitude in permeability and a moderate increase in storativity from before and after subsidence are often reported, along with typical increases of an order of magnitude in the inner subsidence and two in the marginal tensional zone [5,6,46].…”
Section: Interactions Between Subsidence and Water Bodiesmentioning
confidence: 99%
“…As the shields (hydraulic supports) move, the mine roof behind them continues to cantilever and caves into the mine void, which experiences the process of elastic deformation, plastic deformation, and failure [16,20], producing two types of tensile fractures at the surface over the panel: static tensile fracture above the side of a panel and dynamic tensile fractures that follow behind the advancing face [16,17]. The dynamic tensile fractures close as a result of compressional stress after the advance of the face, and static tensile fractures remain open for several months after mining [17], Currently, a variety of methods, ranging from analytical methods and field experiments to numerical and physical simulation, have been used that mainly focus on the mining-induced effects on the movement of overburden strata, the generation of fractures, and subsidence [2,13,29,30,[45][46][47]. However, very few detailed studies of the caving mechanism of overburden strata have been reported.…”
Section: Fractures Changes Due To Longwall Miningmentioning
confidence: 99%
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“…We are interested in how long the water will retain the constant temperature without any impact of the cold return water inflow (random data) [4][5][6][7]: Volume-specific heat capacity of the deposit is derived as follows:…”
Section: Resultsmentioning
confidence: 99%
“…Wang et al [23] applied a three-dimensional finite-difference forward analysis approach to verify the feasibility of a dewatering scheme for a large deep foundation pit. In further studies, researchers used different techniques for dewatering of foundation pits in various regions of the world [24][25][26][27][28][29][30][31].…”
Section: Introductionmentioning
confidence: 99%