2019
DOI: 10.1007/s12517-019-4486-x
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A novel conceptual model of fracture evolution patterns in the overlying strata during horizontal coal seam mining

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Cited by 23 publications
(11 citation statements)
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“…These researches revealed that the floor‐strata strain turns from tensile to compression with mining depths increasing . Second, quick‐setting high‐water materials with constant resistance features and paste materials with high strength and low costs were developed to construct roadside backfill. Compared with traditional wooden stacks, intensive individual props, gangue bags, and concrete blocks, these new materials have greater resistance, faster increasing‐resistance, higher filling efficiency, and better sealing effects .…”
Section: Introductionmentioning
confidence: 99%
“…These researches revealed that the floor‐strata strain turns from tensile to compression with mining depths increasing . Second, quick‐setting high‐water materials with constant resistance features and paste materials with high strength and low costs were developed to construct roadside backfill. Compared with traditional wooden stacks, intensive individual props, gangue bags, and concrete blocks, these new materials have greater resistance, faster increasing‐resistance, higher filling efficiency, and better sealing effects .…”
Section: Introductionmentioning
confidence: 99%
“…According to the theory of the trapezoidal broken model established by Xu et al [11,30,31], the fracture patterns in massive strata controlled by the volume expansion coefficient were obtained, and the consequent fracture parameters were calculated to investigate the fracture formation mechanism in the overburden strata due to caving caused by coal mining. In this model, a series of parallelogram fractures were produced at both ends of the trapezoidal broken model (Figure 1), and each parallelogram was defined by its long side (a), short side (b), height (h), area (S), and dip inclination (α) [11].…”
Section: Sample Geometry and Preparationmentioning
confidence: 99%
“…The groundwater geochemistry of an area is a highly complex and dynamic (Adhikari and Mal, 2019), and the hydrochemical parameters can quantitatively reflect the properties of aquifers. Hydrogeochemical differences occur due to natural environmental processes by means of recharge and discharge, rock-water interaction, flow pattern, and residence times (Liu et al, 2018; Mu et al, 2018; Shi et al, 2019b). After accidental water inrush, it is crucial to quickly identify the water inrush source, find out the cause of the accident, and find mitigation strategies (Shi et al, 2019a; Song et al, 2021).…”
Section: Introductionmentioning
confidence: 99%